Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

W A Rockie

Biographic Data

ID1685696
NAMEW A Rockie
GIVEN NAMESW A
FAMILY NAMERockie
SIGNATUREROCKIE W A
VERIFIEDNo
TOTAL WORKS9
TOTAL CITATIONS2
AUTHOR COUNT9
EDITOR COUNT0
FIRST PUBLICATION YEAR1934
LATEST PUBLICATION YEAR1951
H-INDEX1
  • Alaskan Group Settlement: The Matanuska Colony

    W A Rockie, Kirk H Stone•ARTICLE•Economic Geography•1951

  • Snowdrift Erosion in the Palouse

    Open Access•W A Rockie•ARTICLE•Geographical Review•1951•Cited by: 1

    on the agriculture are the theme of this paper. The Palouse is an almost completely dissected plateau, which rises in elevation from 1200 feet at its southwestern tip to about 2800 feet along its eastern border. It has virtually no undissected upland but also is almost without alluvial bottomland. The surface is practically all sloping. The south and west slopes of the hills are universally of more gentle gradient, averaging less than 20 per cent…

  • Investigations in Erosion Control and the Reclamation of Eroded Land at the Palouse Conservation Experiment Station, Pullman, Wash., 1931-42

    Open Access•W A Rockie, Glenn M Horner et al.•ARTICLE•Geographical Review•1945

  • The Soils That Support Us. An Introduction to the Study of Soils and Their Use by Men

    Open Access•W A Rockie, Charles E Kellogg•ARTICLE•Geographical Review•1942

  • Pitting on Alaskan Farm Lands: A New Erosion Problem

    Open Access•W A Rockie•ARTICLE•Geographical Review•1942•Cited by: 1

    C ERTAIN areas of cleared land in central Alaska have, in the course of time, changed from smooth-surfaced tracts to pitted, pocked, or honeycombed surfaces. The exact cause of the change has not been adequately investigated, though there is need for such a study. A more detailed knowledge of the potential and actual frequency of this phenomenon is important because of the persistent efforts that are being made to promote agriculture in this regi…

  • Soils and Soil Management

    Open Access•W A Rockie, A F Gustafson•ARTICLE•Geographical Review•1942

  • A Picture of Matanuska

    Open Access•W A Rockie•ARTICLE•Geographical Review•1942

  • Man's Effects on the Palouse

    Open Access•W A Rockie•ARTICLE•Geographical Review•1939

  • Snowdrifts and the Palouse Topography

    Open Access•W A Rockie•ARTICLE•Geographical Review•1934

    GRICULTURE in the Palouse region of the Pacific Northwest presents some radical differences from that in most parts of the country. Farmers attempting to transplant their previous experience to the Palouse have learned with sorrow that they cannot farm here as they did back east or down south. Even as agriculture differs, erosion differs. One peculiar phase of the regional erosion problem is presented here-that of snowdrifting and associated form…

  • Snowdrift Erosion in the Palouse

    Open Access•W A Rockie•ARTICLE•Geographical Review•1951•Cited by: 1

    on the agriculture are the theme of this paper. The Palouse is an almost completely dissected plateau, which rises in elevation from 1200 feet at its southwestern tip to about 2800 feet along its eastern border. It has virtually no undissected upland but also is almost without alluvial bottomland. The surface is practically all sloping. The south and west slopes of the hills are universally of more gentle gradient, averaging less than 20 per cent…

  • Pitting on Alaskan Farm Lands: A New Erosion Problem

    Open Access•W A Rockie•ARTICLE•Geographical Review•1942•Cited by: 1

    C ERTAIN areas of cleared land in central Alaska have, in the course of time, changed from smooth-surfaced tracts to pitted, pocked, or honeycombed surfaces. The exact cause of the change has not been adequately investigated, though there is need for such a study. A more detailed knowledge of the potential and actual frequency of this phenomenon is important because of the persistent efforts that are being made to promote agriculture in this regi…

  • Snowdrifts and the Palouse Topography

    Open Access•W A Rockie•ARTICLE•Geographical Review•1934

    GRICULTURE in the Palouse region of the Pacific Northwest presents some radical differences from that in most parts of the country. Farmers attempting to transplant their previous experience to the Palouse have learned with sorrow that they cannot farm here as they did back east or down south. Even as agriculture differs, erosion differs. One peculiar phase of the regional erosion problem is presented here-that of snowdrifting and associated form…

  • Man's Effects on the Palouse

    Open Access•W A Rockie•ARTICLE•Geographical Review•1939

  • The Soils That Support Us. An Introduction to the Study of Soils and Their Use by Men

    Open Access•W A Rockie, Charles E Kellogg•ARTICLE•Geographical Review•1942

  • Pitting on Alaskan Farm Lands: A New Erosion Problem

    Open Access•W A Rockie•ARTICLE•Geographical Review•1942•Cited by: 1

    C ERTAIN areas of cleared land in central Alaska have, in the course of time, changed from smooth-surfaced tracts to pitted, pocked, or honeycombed surfaces. The exact cause of the change has not been adequately investigated, though there is need for such a study. A more detailed knowledge of the potential and actual frequency of this phenomenon is important because of the persistent efforts that are being made to promote agriculture in this regi…

  • Soils and Soil Management

    Open Access•W A Rockie, A F Gustafson•ARTICLE•Geographical Review•1942

  • A Picture of Matanuska

    Open Access•W A Rockie•ARTICLE•Geographical Review•1942

  • Investigations in Erosion Control and the Reclamation of Eroded Land at the Palouse Conservation Experiment Station, Pullman, Wash., 1931-42

    Open Access•W A Rockie, Glenn M Horner et al.•ARTICLE•Geographical Review•1945

  • Alaskan Group Settlement: The Matanuska Colony

    W A Rockie, Kirk H Stone•ARTICLE•Economic Geography•1951

  • Snowdrift Erosion in the Palouse

    Open Access•W A Rockie•ARTICLE•Geographical Review•1951•Cited by: 1

    on the agriculture are the theme of this paper. The Palouse is an almost completely dissected plateau, which rises in elevation from 1200 feet at its southwestern tip to about 2800 feet along its eastern border. It has virtually no undissected upland but also is almost without alluvial bottomland. The surface is practically all sloping. The south and west slopes of the hills are universally of more gentle gradient, averaging less than 20 per cent…

Geography (6 works) · Geology (6 works) · Geology (6 works) · Environmental Science (4 works) · Earth science (3 works) · Erosion (3 works) · Archaeology (2 works) · Climate change and permafrost (2 works) · Cryospheric studies and observations (2 works) · Geomorphology (2 works)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae