Print Date: Jul 22 2015 | Country: |
Description Date: May 31 2013 | State: Colorado |
Describer: Andy Steinert | County: Larimer |
Site ID: 2013CO069001 | MLRA: 48A -- Southern Rocky Mountains |
Site Note: Castnet NEON Soil Pit; This pedon has a seasonal, perched water table on top of the Cr horizon. This seasonal water table is from snow melt. There is no hydrophytic vegetation to suggest this is a permanent water table. | Soil Survey Area: 4-FTC -- Fort Collins, Colorado CO642 -- Estes Park Area, Colorado, Parts of Boulder and Larimer Counties |
Pedon ID: S2013CO069001 | Map Unit: 7702B -- Frisco-Catamount, moist families complex, 5 to 40 percent slopes |
Pedon Note: The backhoe was able to scrape/dig through the Cr horizon, but not dig straight down. | Quad Name: Longs Peak, Colorado |
Lab Source ID: SSL | Std Latitude: 40.2770556 |
Lab Pedon #: 13N61307 | Std Longitude: -105.5452500 |
User Transect ID: | |
Soil Name as Described/Sampled: Ustic Haplocryolls | |
Classification: Loamy-skeletal, mixed, superactive Ustic Haplocryolls | Latitude: 40 degrees 16 minutes 37.40 seconds north |
Soil Name as Correlated: | Longitude: 105 degrees 32 minutes 42.90 seconds west |
Classification: | Datum: WGS84 |
Pedon Type: | UTM Zone: 13 |
Pedon Purpose: laboratory sampling site | UTM Easting: 453647 meters |
Taxon Kind: family | UTM Northing: 4458653 meters |
Associated Soils: |
Physiographic Division: Rocky Mountain System | Primary Earth Cover: Tree cover |
Physiographic Province: Southern Rocky Mountains | Secondary Earth Cover: Conifers |
Physiographic Section: | Existing Vegetation: Arizona fescue, common juniper, Engelmann spruce, kinnikinnick, lodgepole pine, quaking aspen |
State Physiographic Area: | Parent Material: residuum weathered from granite |
Local Physiographic Area: | Bedrock Kind: granite |
Geomorphic Setting: on mountainflank, lower third of mountains on mountain slope | Bedrock Depth: 123 centimeters |
Upslope Shape: convex | Bedrock Hardness: moderately cemented |
Cross Slope Shape: linear | Bedrock Fracture Interval: less than 10 centimeters |
Particle Size Control Section: 25 to 100 cm. | Surface Fragments: 2.0 percent nonflat subangular indurated 2- to 75-millimeter granite fragments and 3.0 percent nonflat subangular indurated 75- to 250-millimeter granite fragments |
Description origin: NASIS | Description database: KSSL |