Soil polygenesis as a function of Quaternary climate change, northern Great Basin, USA
- 1 September 1995
- Vol. 68 (1-2), 1-26
- https://doi.org/10.1016/0016-7061(95)00025-j
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- Late Quaternary Environments in Ruby Valley, NevadaQuaternary Research, 1992
- Rates of Soil Development from Four Soil Chronosequences in the Southern Great BasinQuaternary Research, 1991
- Influence of climate and eolian dust on the major-element chemistry and clay mineralogy of soils in the northern Bighorn basin, U.S.A.CATENA, 1990
- SOIL TEMPERATURE AND MOISTURE REGIME RELATIONSHIPS WITHIN SOME RANGELANDS OF THE GREAT BASINSoil Science, 1989
- The use of hornblende etching, clast weathering, and soils to date alpine glacial and periglacial deposits: A study from southwestern MontanaGSA Bulletin, 1988
- Distribution of calcium carbonate in desert soils: A modelGeology, 1988
- Some properties of smectite and mica in clays of soils in dry regionsGeoderma, 1975
- Proposal for a micromorphological classification of soil materials. I. A classification of the related distributions of fine and coarse particlesGeoderma, 1975
- Clay Mineralogy of Soils Developed from Quaternary Deposits of the Eastern Sierra Nevada, CaliforniaGSA Bulletin, 1971
- Quaternary Paleoclimatic Implications of Soil Clay Mineral Distribution in a Sierra Nevada-Great Basin TransectThe Journal of Geology, 1969