Emily M Taylor (Former Employee)
Science and Products
Filter Total Items: 28
Stop 16: Trench 14 Stop 16: Trench 14
No abstract available.
Authors
Emily M. Taylor, John S. Stuckless, S. S. Levy
Instructions for the soil development index template; Lotus 1-2-3; B, Program disk Instructions for the soil development index template; Lotus 1-2-3; B, Program disk
No abstract available.
Authors
Emily M. Taylor
A quantitative comparison of Soil Development in four climatic regimes A quantitative comparison of Soil Development in four climatic regimes
A new quantitative Soil Development Index based on field data has been applied to chronosequences formed under different climatic regimes. The four soil chronosequences, developed primarily on sandy deposits, have some numeric age control and are located in xeric-inland (Merced, Calif.), xeric-coastal (Ventura, Calif.), aridic (Las Cruces, N. Mex.), and udic (Susquehanna Valley, Pa.)...
Authors
J.W. Harden, E. M. Taylor
Science and Products
Filter Total Items: 28
Stop 16: Trench 14 Stop 16: Trench 14
No abstract available.
Authors
Emily M. Taylor, John S. Stuckless, S. S. Levy
Instructions for the soil development index template; Lotus 1-2-3; B, Program disk Instructions for the soil development index template; Lotus 1-2-3; B, Program disk
No abstract available.
Authors
Emily M. Taylor
A quantitative comparison of Soil Development in four climatic regimes A quantitative comparison of Soil Development in four climatic regimes
A new quantitative Soil Development Index based on field data has been applied to chronosequences formed under different climatic regimes. The four soil chronosequences, developed primarily on sandy deposits, have some numeric age control and are located in xeric-inland (Merced, Calif.), xeric-coastal (Ventura, Calif.), aridic (Las Cruces, N. Mex.), and udic (Susquehanna Valley, Pa.)...
Authors
J.W. Harden, E. M. Taylor