Zobrazeno 1 - 10
of 13
pro vyhledávání: '"John E. Foss"'
Autor:
Antonio V. Segovia, John E. Foss
Publikováno v:
Groundwater as a Geomorphic Agent ISBN: 9781003028833
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31b014c2f4b71b20c66473ce1806974a
https://doi.org/10.4324/9781003028833-1
https://doi.org/10.4324/9781003028833-1
Autor:
Antonio V. Segovia, John E. Foss
Publikováno v:
Groundwater as a Geomorphic Agent ISBN: 9781003028833
The relationship of landscapes and soils includes both dynamic and static components. Landscapes result from interaction of processes with materials that make up the uppermost part of the Earth’s crust. Climatic fluctuations, through their effects
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5cfb43ff2bc54a6047e47681f3419e6c
https://doi.org/10.4324/9781003028833-4
https://doi.org/10.4324/9781003028833-4
Autor:
John E. Foss, María del Rosario Domínguez Carrasco, Betty B. Faust, William J. Folan, Joel D. Gunn
Publikováno v:
Ancient Mesoamerica. 13:297-315
Maya Lowlands climate researchers have set aside earlier beliefs that Maya civilization flourished in an unchanging environment. Analyses of river discharge, weather patterns, lake-bottom sediments, and settlement patterns reveal a highly variable cl
Autor:
James J. Vorst, David L. Coffey, Vernon H. Reich, Trudy W. Banta, Duane C. Wolf, John E. Foss, John G. Graved
Publikováno v:
Journal of Agronomic Education. 19:25-28
Publikováno v:
Kavousi I ISBN: 9781623030360
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22c1b39f49634ce7dcd7e944c41e1bd5
https://doi.org/10.2307/j.ctt3fgv78.19
https://doi.org/10.2307/j.ctt3fgv78.19
Autor:
John E. Foss
Publikováno v:
Agronomy Journal. 88:119-121
Autor:
John E. Foss
Publikováno v:
Geoarchaeology. 24:111-112
Autor:
John E. Foss
Publikováno v:
Soil Science. 170:222-223
Autor:
John E. Foss
Publikováno v:
Soil Science. 169:398-399
Autor:
John E. Foss
Publikováno v:
Annals of the New York Academy of Sciences. 288:234-244
The morphological, physical and chemical characteristics of the major soils at the Flint Run (Virginia) and Shawnee-Minisink (Pennsylvania) sites were compared. The pedological data were then integrated with archaeological, geological and palynologic