Stanley A Schumm

Dados Biográficos

ID1980729
NOMEStanley A Schumm
PRENOMESStanley A
SOBRENOMESchumm
ASSINATURASCHUMM S A
AFILIAÇÕESColorado State University
VERIFICADONão
TOTAL DE OBRAS11
TOTAL DE CITAÇÕES41
TOTAL COMO AUTOR11
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO1956
ANO MAIS RECENTE DE PUBLICAÇÃO2004
ÍNDICE H1

  • Arthur Newell Strahler (1918–2002)

    Stanley A SchummARTICLEAnnals of the Association of…2004Referências: 12

    Arthur Newell Strahler was born in Kolhapur, India, on February 20, 1918, the son of missionary parents, Milton and Harriet Strahler. He died on December 6, 2002. His interest in geology was develo

  • To Interpret the Earth

    Open AccessDouglas J Sherman, Stanley A SchummARTICLEGeographical Review1993Citada por: 1

  • To Interpret the Earth

    C Vita-Finzi, Claudio Vita‐finzi et al.ARTICLEGeographical Journal1992

  • Geomorphology

    Stephen Trudgill, Richard J Chorley et al.ARTICLETransactions of the Institute of…1986

  • Gradational Thresholds and Landform Singularity

    Open AccessZe’ev B Begin, Stanley A SchummARTICLEQuaternary Research1985

  • Gradational Thresholds and Landform Singularity

    Open AccessZe'ev B Begin, Ze’ev B Begin et al.ARTICLEQuaternary Research1984

    Geomorphic threshold conditions have been identifed at which stream patterns change and gully initiation occurs. For both, the threshold conditions are defined by the parameter of “relative shear stress” which is a measure of the energy state of the system and is based on known values of stream slope and mean annual discharge (for patterns) or drainage area (for gullies). The probability of passing from a stream pattern to another, or from stable…

  • Ephemeral-Stream Processes

    Open AccessPeter C Patton, Stanley A SchummARTICLEQuaternary Research1981

    Three unstable ephemeral-stream channels (arroyos), which drain source areas that have high sediment yields ranging from predominantly sand (Arroyo Calabasas) to a mixture of sand, silt, and clay (Sand Creek) to largely silt and clay (Sage Creek), were resurveyed to provide data on the rates and mechanics of erosion and sedimentation processes during periods ranging from 14 to 22 yr. Channel morphology changed significantly. Erosion occurred thro…

  • The Physical Geography (Geomorphology) of William Morris Davis

    Robert P Beckinsale, Philip B King et al.ARTICLEGeographical Journal1981Citada por: 1

    Canadian north and centre, an area larger than that of Quebec and the Maritime Provinces combined. Their depth is variable but may extend to about 100 feet (c. 30 m). Muskeg is thus a significant feature of the landscape and is also an important organic resource, so that the problem of its wise development is associated with many other aspects of the northern environment, such as water supplies, forest resources and the exploitation of petroleum,…

  • Geomorphic Thresholds

    Stanley A SchummARTICLETransactions of the Institute of…1979Citada por: 39Referências: 4

    Geomorphic thresholds were defined initially as the condition at which there is a significant landform change without a change of external controls such as base level, climate and land use. Landforms evolve to a condition of incipient instability following which change or failure occurs. Subsequently, through usage, the definition has been broadened to include abrupt landform change as a result of progressive change of external controls. Therefor…

  • Time, space, and causality in geomorphology

    Stanley A Schumm, R W LichtyARTICLEAmerican Journal of Science1965

    Distinctions between cause and effect in landform development depend on the span of time involved and the size of the geomorphic system under consideration. Depending upon the temporal and areal frame of reference, variables such as channel morphology may be either dependent or independent. In terms of geologic time, landforms represent a stage in an erosion cycle and are dependent on time. On a short-term basis, components of geomorphic systems …

  • Evolution of Drainage Systems and Slopes in Badlands at Perth Amboy, New Jersey

    Stanley A SchummARTICLEGeological Society of America…1956

    Research Article| May 01, 1956 EVOLUTION OF DRAINAGE SYSTEMS AND SLOPES IN BADLANDS AT PERTH AMBOY, NEW JERSEY STANLEY A SCHUMM STANLEY A SCHUMM BUILDING 25, FEDERAL CENTER, DENVER, COLORADO Search for other works by this author on: GSW Google Scholar GSA Bulletin (1956) 67 (5): 597–646. https://doi.org/10.1130/0016-7606(1956)67[597:EODSAS]2.0.CO;2 Article history received: 24 Mar 1955 first online: 02 Mar 2017 Cite View This Citation Add to Cita…