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I <br /> TABLE III-I-2 <br /> ECOLOGICAL LAND USE - THOMPSON CREEK LAND USE STUDY AREA <br /> E L U Description <br /> Geomorphology Erosion Mass Stream Reveg Prod <br /> ELU# Vegetation % Slope Soils Hazard Failure Order* Capabilities** <br /> Depth in —� ---Inches Origin <br /> Origin <br /> 1 Englemann Spruce-Sub- Basalt <br /> alpine fir 16-40 40+ Sandstone <br /> Shales Mod Mod 1 , 2 Mod High <br /> 2 Basalt <br /> Aspen Sandstone <br /> (ser.al) 16-40 40+ Shales Mod High 1 , 2 Mod High <br /> 3 Basalt <br /> Mountain Sandstone <br /> Meadow 16-40 40+ Shale Mod Mod 2, 3 Mod High <br /> 4 Mancos <br /> Aspen 40+ 20-40 Shale High High 1 , 2, 3 Low Mod <br /> 5 Englemann Spruce - <br /> ^, Subalpine fir 0-15 40+ Basalt Low Low 1 , 2 high High <br /> coo <br /> i <br /> 6 Mountain Meadow 0-15 40+ Alluvium* Low Low 1 , 2, 3 High High <br /> Englemann Spruce - <br /> Subalpine fir 40+ 20-40 Shales High High 1 , 2 , 3 Low Mod <br /> 8 Grass-shrub Basalt <br /> 16-40 20-40 Shale High High 1 , 2, 3 Mod Mod <br /> 9 Grass (Alpine) Sandstone <br /> Association 40+ 20-40 Shale High High 1 , 2 Low Low <br /> f <br /> 10 Meadow-Cottonwood 16-40 40+ Alluvium Low Law 1 , 2, 3 , 4 High High <br /> *The stream order system is a method to analyse drainage-basin characteristics . The orders <br /> in this planning unit are directly proportional to watershed area , channel dimension, and <br /> stream discharge at that point in the drainage network. <br /> . **Revegetation and Production potentials of high, moderate and low are based on climate, soil texture, <br /> soil depth, slope and geology . Soil textures were projected from geology , climate , vegetation and <br /> ated (_heck points . High-Moderate-Low are relative to each other on this unit . <br /> from i.sol. <br />