COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

1020mmto cm

Did you get an itemized estimate? If not, ask for one. Do that when you get a second opinion too. That way you can easily compare the two. Don’t tell the second shop what the other one estimated.

Yeah, tight but not pressed in I had to pry mine out a fraction at a time, going around to keep it from getting jammed. Both GM and an 03 Toyota Camry. The GM had a penta-socket head fastener on one side and a pressed in “rivet” on the other. Still struggling to understand/justify the need for such hardware…

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

John Deere 310SG ; C. Height9 ft 2 in ; Weight13,500 lbs ; Item is Operable: Yes ; Starts and moves under its own power: No ; Item/Stock #:10003230.

Same with a guy I know in my area who passed away back in 2011. He BSed, cobbled together, hacked up, and in general screwed everyone over yet everyone within 25 miles of him praised his name to the mechanical heavens. Go figure…

202452 — What Other Symptoms Indicate Bad Wheel Bearings? · Unusual noises coming from the wheels · Poor handling · Pulling to one side while driving or ...

Bg3--76 to 97 cm (30 to 38 inches); grayish brown (2.5Y 5/2) loam; weak medium subangular blocky structure; friable; few very fine roots; many fine and medium prominent yellowish brown (10YR 5/6) masses of iron accumulation throughout; 4 percent gravel; strongly effervescent; slightly alkaline; gradual wavy boundary. [Combined thickness of the Bg horizon is 25 to 76 cm (10 to 30 inches).] BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

You should also verify how many wheel bearings they’re replacing. If it were me, I would go ahead and replace the bearing on the other side of the vehicle as well…chances are, it’s not far behind in terms of failure.

After I drilled out the defective sensor , I took a reamer to the hole. The shop that removed the other sensor (left front) was nice enough to let me go home without a sensor (I got one from an online Toyota dealer at a big discount). And my labor is free.

They need to be tight due to the super tight tolerance on positioning for proper operation. I did some work recently and had to R&R an ABS sensor. Long story short, a thousandth made a huge difference in signal level. Too close and it rubs, too far and weak signal. Rust forming on the spacer was enough to cause weak signal…removing them required diligent care not to damage them…

Dropped my car off at a mechanic to check into an issue I’ve been having (groaning in the front/left wheel). Turns out it is a wheel bearing that needs to be replaced and the mechanic quoted me $750 for the job, saying “the bearing needs to be pressed and it’s a fair amount of labor”.

DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

1020mmto m

202227 — What are wheel bearings, and what do wheel bearings do? Aiding in the optimal rotation of the wheel, the wheel hub plays an important role ...

Thanks all, appreciate the help. I did call a second and third shop and was quoted $350 by one and $380 from the other. Both shops gave me their estimate, and when they then asked what I was quoted when it was diagnosed they said the shop I went to was notorious for extremely high prices and that $750 was way too high… I’m surprised since the first shop had great reviews.

SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

700mm toinches

Candy Crush Saga Level 14960 played by Skillgaming Candy Crush Saga Walkthrough Playlist: ...

Ak--15 to 28 cm (6 to 11 inches); black (10YR 2/1) loam, dark gray (10YR 4/1) dry; weak fine and medium subangular blocky structure parting to weak fine granular; friable; common very fine roots; 1 percent gravel; strongly effervescent; slightly alkaline; clear smooth boundary. [Combined thickness of A horizon is 25 to 51 cm (10 to 20 inches).] Bg1--28 to 53 cm (11 to 21 inches); dark gray (2.5Y 4/1) loam; weak fine and medium subangular blocky structure; friable; few very fine roots; common fine prominent yellowish brown (10YR 5/4) masses of iron accumulation throughout; common fine and medium faint grayish brown (2.5Y 5/2) iron depletions throughout; 1 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg2--53 to 76 cm (21 to 30 inches); dark gray (2.5Y 4/1) loam; weak medium subangular blocky structure; friable; few very fine roots; common fine strong brown (7.5YR 4/6) very weakly cemented iron oxide concretions throughout; few black (2.5Y 2.5/1) krotovina; common fine and medium distinct light olive brown (2.5Y 5/4) masses of iron accumulation throughout; many medium and coarse faint dark grayish brown (2.5Y 4/2) and gray (2.5Y 5/1) iron depletions throughout; 4 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg3--76 to 97 cm (30 to 38 inches); grayish brown (2.5Y 5/2) loam; weak medium subangular blocky structure; friable; few very fine roots; many fine and medium prominent yellowish brown (10YR 5/6) masses of iron accumulation throughout; 4 percent gravel; strongly effervescent; slightly alkaline; gradual wavy boundary. [Combined thickness of the Bg horizon is 25 to 76 cm (10 to 30 inches).] BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

1000mm toinches

20121230 — Web sites like justanswer.com/legal ...leave nothing to chance. Tory Johnson, GMA Workplace Contributor, ...

TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

It requires that the material used in the manufacture of the fasteners in the United States be melted in the United States or a qualifying country. What are ...

L10 versus Competing Expressions of Expected Linear-Bearing Life ... Where L10 is how long 90% of all linear bearings put into the defined service will deliver. C ...

Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, calcareous, mesic Typic Endoaquolls TYPICAL PEDON: Kish loam - on a southwest-facing slope with less than 1 percent gradient in a cultivated field at an elevation of 264 meters (865 feet) above mean sea level. (Colors are for moist soil unless otherwise noted.) Apk--0 to 15 cm (0 to 6 inches); black (10YR 2/1) loam, dark grayish brown (10YR 4/2) dry; moderate medium granular structure; friable; common very fine roots; strongly effervescent; slightly alkaline; clear smooth boundary. Ak--15 to 28 cm (6 to 11 inches); black (10YR 2/1) loam, dark gray (10YR 4/1) dry; weak fine and medium subangular blocky structure parting to weak fine granular; friable; common very fine roots; 1 percent gravel; strongly effervescent; slightly alkaline; clear smooth boundary. [Combined thickness of A horizon is 25 to 51 cm (10 to 20 inches).] Bg1--28 to 53 cm (11 to 21 inches); dark gray (2.5Y 4/1) loam; weak fine and medium subangular blocky structure; friable; few very fine roots; common fine prominent yellowish brown (10YR 5/4) masses of iron accumulation throughout; common fine and medium faint grayish brown (2.5Y 5/2) iron depletions throughout; 1 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg2--53 to 76 cm (21 to 30 inches); dark gray (2.5Y 4/1) loam; weak medium subangular blocky structure; friable; few very fine roots; common fine strong brown (7.5YR 4/6) very weakly cemented iron oxide concretions throughout; few black (2.5Y 2.5/1) krotovina; common fine and medium distinct light olive brown (2.5Y 5/4) masses of iron accumulation throughout; many medium and coarse faint dark grayish brown (2.5Y 4/2) and gray (2.5Y 5/1) iron depletions throughout; 4 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg3--76 to 97 cm (30 to 38 inches); grayish brown (2.5Y 5/2) loam; weak medium subangular blocky structure; friable; few very fine roots; many fine and medium prominent yellowish brown (10YR 5/6) masses of iron accumulation throughout; 4 percent gravel; strongly effervescent; slightly alkaline; gradual wavy boundary. [Combined thickness of the Bg horizon is 25 to 76 cm (10 to 30 inches).] BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

Bg2--53 to 76 cm (21 to 30 inches); dark gray (2.5Y 4/1) loam; weak medium subangular blocky structure; friable; few very fine roots; common fine strong brown (7.5YR 4/6) very weakly cemented iron oxide concretions throughout; few black (2.5Y 2.5/1) krotovina; common fine and medium distinct light olive brown (2.5Y 5/4) masses of iron accumulation throughout; many medium and coarse faint dark grayish brown (2.5Y 4/2) and gray (2.5Y 5/1) iron depletions throughout; 4 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg3--76 to 97 cm (30 to 38 inches); grayish brown (2.5Y 5/2) loam; weak medium subangular blocky structure; friable; few very fine roots; many fine and medium prominent yellowish brown (10YR 5/6) masses of iron accumulation throughout; 4 percent gravel; strongly effervescent; slightly alkaline; gradual wavy boundary. [Combined thickness of the Bg horizon is 25 to 76 cm (10 to 30 inches).] BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

Item: 7203B Bearing; Type: Single row Angular contact ball bearings; SKU: 7203BBearing; Inner Ring Diameter (bore): 17mm; Inner Ring Tolerance: 0~-10m ...

Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

1020mm inchesto feet

Elantra has same bearing setup as Honda’s. A shop can lowball the cost and then have to replace more parts or remove knuckle to press out bearing. The bearing is pressed into the hub. So, assume the hub will be damaged or scored.image600×600 22.3 KB

The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

Apk--0 to 15 cm (0 to 6 inches); black (10YR 2/1) loam, dark grayish brown (10YR 4/2) dry; moderate medium granular structure; friable; common very fine roots; strongly effervescent; slightly alkaline; clear smooth boundary. Ak--15 to 28 cm (6 to 11 inches); black (10YR 2/1) loam, dark gray (10YR 4/1) dry; weak fine and medium subangular blocky structure parting to weak fine granular; friable; common very fine roots; 1 percent gravel; strongly effervescent; slightly alkaline; clear smooth boundary. [Combined thickness of A horizon is 25 to 51 cm (10 to 20 inches).] Bg1--28 to 53 cm (11 to 21 inches); dark gray (2.5Y 4/1) loam; weak fine and medium subangular blocky structure; friable; few very fine roots; common fine prominent yellowish brown (10YR 5/4) masses of iron accumulation throughout; common fine and medium faint grayish brown (2.5Y 5/2) iron depletions throughout; 1 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg2--53 to 76 cm (21 to 30 inches); dark gray (2.5Y 4/1) loam; weak medium subangular blocky structure; friable; few very fine roots; common fine strong brown (7.5YR 4/6) very weakly cemented iron oxide concretions throughout; few black (2.5Y 2.5/1) krotovina; common fine and medium distinct light olive brown (2.5Y 5/4) masses of iron accumulation throughout; many medium and coarse faint dark grayish brown (2.5Y 4/2) and gray (2.5Y 5/1) iron depletions throughout; 4 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg3--76 to 97 cm (30 to 38 inches); grayish brown (2.5Y 5/2) loam; weak medium subangular blocky structure; friable; few very fine roots; many fine and medium prominent yellowish brown (10YR 5/6) masses of iron accumulation throughout; 4 percent gravel; strongly effervescent; slightly alkaline; gradual wavy boundary. [Combined thickness of the Bg horizon is 25 to 76 cm (10 to 30 inches).] BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

As always when in doubt you get a second opinion . It could be that this shop does not have the right equipment for the job or there is a lot of labor involved .

Scope of work as per the first shop was to “replace the left/front wheel bearing and press the new one”, that’s all they mentioned.

I paid $250 parts and labor for the front wheel bearing of my previous Toyota Corolla. It had to be pressed in also. They put in a Timken bearing and it didn’t take much time…around 45 minutes and I was out of there.Shop around because your estimate seems on the high side.

1020 cm toinches

1020 mm toinchesand feet

20211111 — With them we can connect a rotating axle to a relatively stationary machine without any friction between them. So they're used everywhere.

I thought sometimes they just replace the whole hub part is a little more but less labor. That price sounds high you need to get a second quote.

Bg1--28 to 53 cm (11 to 21 inches); dark gray (2.5Y 4/1) loam; weak fine and medium subangular blocky structure; friable; few very fine roots; common fine prominent yellowish brown (10YR 5/4) masses of iron accumulation throughout; common fine and medium faint grayish brown (2.5Y 5/2) iron depletions throughout; 1 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg2--53 to 76 cm (21 to 30 inches); dark gray (2.5Y 4/1) loam; weak medium subangular blocky structure; friable; few very fine roots; common fine strong brown (7.5YR 4/6) very weakly cemented iron oxide concretions throughout; few black (2.5Y 2.5/1) krotovina; common fine and medium distinct light olive brown (2.5Y 5/4) masses of iron accumulation throughout; many medium and coarse faint dark grayish brown (2.5Y 4/2) and gray (2.5Y 5/1) iron depletions throughout; 4 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg3--76 to 97 cm (30 to 38 inches); grayish brown (2.5Y 5/2) loam; weak medium subangular blocky structure; friable; few very fine roots; many fine and medium prominent yellowish brown (10YR 5/6) masses of iron accumulation throughout; 4 percent gravel; strongly effervescent; slightly alkaline; gradual wavy boundary. [Combined thickness of the Bg horizon is 25 to 76 cm (10 to 30 inches).] BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

You did the right thing by getting other quotes and as an aside, never give a lot of credence to online reviews. Some may be fake and in some cases people may have been robbed blind and simply do not realize it. Their car is fixed for double what anyone else charges so they’re happy with it all.

TYPICAL PEDON: Kish loam - on a southwest-facing slope with less than 1 percent gradient in a cultivated field at an elevation of 264 meters (865 feet) above mean sea level. (Colors are for moist soil unless otherwise noted.) Apk--0 to 15 cm (0 to 6 inches); black (10YR 2/1) loam, dark grayish brown (10YR 4/2) dry; moderate medium granular structure; friable; common very fine roots; strongly effervescent; slightly alkaline; clear smooth boundary. Ak--15 to 28 cm (6 to 11 inches); black (10YR 2/1) loam, dark gray (10YR 4/1) dry; weak fine and medium subangular blocky structure parting to weak fine granular; friable; common very fine roots; 1 percent gravel; strongly effervescent; slightly alkaline; clear smooth boundary. [Combined thickness of A horizon is 25 to 51 cm (10 to 20 inches).] Bg1--28 to 53 cm (11 to 21 inches); dark gray (2.5Y 4/1) loam; weak fine and medium subangular blocky structure; friable; few very fine roots; common fine prominent yellowish brown (10YR 5/4) masses of iron accumulation throughout; common fine and medium faint grayish brown (2.5Y 5/2) iron depletions throughout; 1 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg2--53 to 76 cm (21 to 30 inches); dark gray (2.5Y 4/1) loam; weak medium subangular blocky structure; friable; few very fine roots; common fine strong brown (7.5YR 4/6) very weakly cemented iron oxide concretions throughout; few black (2.5Y 2.5/1) krotovina; common fine and medium distinct light olive brown (2.5Y 5/4) masses of iron accumulation throughout; many medium and coarse faint dark grayish brown (2.5Y 4/2) and gray (2.5Y 5/1) iron depletions throughout; 4 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Bg3--76 to 97 cm (30 to 38 inches); grayish brown (2.5Y 5/2) loam; weak medium subangular blocky structure; friable; few very fine roots; many fine and medium prominent yellowish brown (10YR 5/6) masses of iron accumulation throughout; 4 percent gravel; strongly effervescent; slightly alkaline; gradual wavy boundary. [Combined thickness of the Bg horizon is 25 to 76 cm (10 to 30 inches).] BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

1020mmto feet

Cool. With that said, you really should consider getting the other one replaced at the same time…see if the shop will give you a break on the labor.

BCg--97 to 119 cm (38 to 47 inches); light brownish gray (2.5Y 6/2) loam; weak medium and coarse subangular blocky structure; friable; many medium and coarse prominent dark yellowish brown (10YR 4/6) masses of iron accumulation throughout; 7 percent gravel; strongly effervescent; slightly alkaline; clear wavy boundary. [0 to 25 cm (0 to 10 inches) thick] Cg--119 to 152 cm (47 to 60 inches); 45 percent light brownish gray (2.5Y 6/2), 40 percent brown (7.5YR 5/3), and 15 percent grayish brown (2.5Y 5/2) stratified loam, sandy loam, and loamy coarse sand; massive; very friable; 14 percent gravel; violently effervescent; moderately alkaline. TYPE LOCATION: McHenry County, Illinois; about 1.6 km (1 mile) northwest of Huntley; 617 m (2,025 feet) south and 37 m (120 feet) east of the northwest corner of sec. 29, T. 43 N., R. 7 E; USGS Huntley, Illinois, topographic quadrangle; lat. 42 degrees 10 minutes 37 seconds N. and long. 88 degrees 27 minutes 05 seconds W., NAD 27; UTM Zone 16, 380125 easting and 4670445 northing, NAD 83. RANGE IN CHARACTERISTICS: The depth to the base of soil development ranges from 76 to 127 cm (30 to 50 inches). The mollic epipedon ranges from 25 to 51 cm (10 to 20 inches) in thickness. Carbonates are in all parts of the fine-earth fraction between 25 to 51 cm (10 and 20 inches). Reaction is slightly alkaline or moderately alkaline throughout the series control section. The calcium carbonate equivalent ranges from 5 to 30 percent. The particle-size control section has between 18 and 34 percent clay and 15 to 50 percent fine and coarser sand. The sand fraction is well sorted (poorly graded) throughout the series control section. The Apk, Ap, Ak, or A horizon has hue of 10YR, 2.5Y, or is neutral; value of 2 to 3, and chroma of 0 to 2. It is loam, silt loam, clay loam, or silty clay loam. Some pedons have an AB horizon. The Bg or BCg horizon has hue of 10YR, 2.5Y, 5Y, or is neutral; value of 4 to 6; and chroma of 0 to 2. It is loam, clay loam, silt loam, silty clay loam, or sandy loam. Gravel content ranges from 0 to 10 percent. The Cg horizon has hue of 7.5YR, 10YR, 2.5Y or 5Y; value of 5 or 6; and chroma of 1 to 4. It is loam, sandy loam, or silt loam with strata of coarser textures a common feature. Gravel content ranges from 2 to 15 percent. The calcium carbonate equivalent is generally higher in this section than in the upper two-thirds of the series control section. COMPETING SERIES: These are the Canisteo, Hetz, Hooppole, Jeffers, and Tilfer series in the same family. Canisteo soils have a poorly sorted (well graded) sand fraction in the lower two-thirds of the series control section. Hetz soils have less than 410 mm (16 inches) of average annual precipitation and are at elevations above 1829 m (6,000 feet). Hooppole soils contain more than 75 percent sand in the lower part of the series control section. Jeffers soils have appreciable amounts of gypsum and have horizons with firm consistence in the series control section. Tilfer soils have a lithic contact at depths between 51 to 102 cm (20 and 40 inches). GEOGRAPHIC SETTING: The Kish soils have concave to slightly convex slopes with gradient of 0 to 2 percent in shallow depressions and on rims of depressions. They have formed in loamy glacial outwash or in a thin, silty mantle and outwash. Mean annual air temperature ranges from 7 to 12 degrees C (44 to 53 degrees F), mean annual precipitation ranges from 740 to 1020 mm (29 to 40 inches), frost free days range from 140 to 180 days, and elevation ranges from 183 to 311 meters (600 to 1020 feet) above mean sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Brenton, Elburn, Harpster, Lena, and Pella soils. The somewhat poorly drained Brenton and Elburn soils are on slightly higher landform positions. Harpster and Pella soils are fine-silty and are on similar landform positions nearby. The very poorly drained Lena soils are on slightly lower landform positions. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Poorly drained. An apparent seasonal high water table is 15 cm (0.5 foot) above the surface to 46 cm (1.5 feet) below the surface in normal years. The potential for surface runoff is negligible to low. Saturated hydraulic conductivity is moderately high or high (4.23 to 14.11 micrometers per second). Permeability is moderate. USE AND VEGETATION: Mostly under cultivation; corn and soybeans are the principal crops. Native vegetation is hydrophytic grasses, reeds, and sedges. DISTRIBUTION AND EXTENT: Northern Illinois. Extent is small in MLRA 95B. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana SERIES ESTABLISHED: McHenry County, Illinois, 1996. Name is derived from the Kishwaukee River, which is near the type location. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon - zone from the surface of the soil to a depth of 28 cm (11 inches) (Apk and Ak horizons); cambic horizon - the zone from approximately 28 to 119 cm (11 to 47 inches) (Bg1, Bg2, Bg3, and BCg horizons); calcareous family - carbonates at 25 to 51 cm (10 to 20 inches); aquic moisture regime - low chroma below mollic epipedon. National Cooperative Soil Survey U.S.A.

You didn’t mention the year of your Elantra, but when I plugged in a 2015 into repairpal.com for an estimate, my local zip code brought up an estimate for $173-266 to change a single wheel bearing…you definitely need to get a 2nd and 3rd quote

Not necessarily. I had this setup on my old Mazda Protege. You press the hub out of the bearing, and the inner race of the bearing is stuck in the hub. You then carefully score the outside of the inner race, and strike it once or twice with a chisel…the inner race splits in too, and you’re left with the hub, which you can press into the new bearing.

you can get the whole hub and bearing for like $150 , so your mechanic is telling you it is going to take him 5 hours to do the job on a bearing ?? I doubt it , i would run from that guy .

This doesn’t include the cost of replacing one perfectly good ABS sensor that had to be destroyed in the process. (tech told me that the sensor would be in the way of the press, and they couldn’t remove it without destroying it. ). I believed him, as I replaced the ABS sensor on the other side a year earlier. It was defective. I too had to destroy the old one to remove it, as Toyota machined the hole too small. Talk about a tight fit! There was TSB about this, I believe.

1 Corinthians 7:28 But if you do marry, you have not sinned; and if a virgin marries, she has not sinned. But those who marry will face many troubles in ...

I took my knuckle to a shop and they pressed out my bearing and he said hub was scored but he had 1 used. For $20. I tried to pay with my card and tech said hub was his and cash only. Had to run to atm for $20 cash. Bet tech had a few hubs in his toolbox. From other jobs?