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Friedrich Julius Theodor Kestner

Datos Biográficos

ID3752717
NOMBREFriedrich Julius Theodor Kestner
NOMBRESFriedrich Julius Theodor
APELLIDOKestner
FIRMAKESTNER F J T
VERIFICADONo
TOTAL DE OBRAS3
TOTAL DE CITAS2
OBRAS COMO AUTOR3
OBRAS COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN1962
AÑO MÁS RECIENTE DE PUBLICACIÓN1970
ÍNDICE H1
  • Cyclic Changes in Morecambe Bay

    Friedrich Julius Theodor Kestner•ARTICLE•Geographical Journal•1970

  • The Old Coastline of the Wash

    J A Steers, W E Doran et al.•ARTICLE•Geographical Journal•1962

  • The Old Coastline of the Wash

    Friedrich Julius Theodor Kestner•ARTICLE•Geographical Journal•1962•Citada por: 2

    THE paper describes how various old salt-marsh edges around the Wash were traced s part of a field study into the processes of salt-marsh advance in this area. It is sought to establish that salt-marsh advance is not a continuous process, but that foreshore saltings tend to become stabilized when they are a 13-1z 2l mile wide, with a wider belt of mud flats in front of them. In the mud-flat areas accretion, caused by continuous deposition of sedi…

  • The Old Coastline of the Wash

    Friedrich Julius Theodor Kestner•ARTICLE•Geographical Journal•1962•Citada por: 2

    THE paper describes how various old salt-marsh edges around the Wash were traced s part of a field study into the processes of salt-marsh advance in this area. It is sought to establish that salt-marsh advance is not a continuous process, but that foreshore saltings tend to become stabilized when they are a 13-1z 2l mile wide, with a wider belt of mud flats in front of them. In the mud-flat areas accretion, caused by continuous deposition of sedi…

  • The Old Coastline of the Wash

    J A Steers, W E Doran et al.•ARTICLE•Geographical Journal•1962

  • The Old Coastline of the Wash

    Friedrich Julius Theodor Kestner•ARTICLE•Geographical Journal•1962•Citada por: 2

    THE paper describes how various old salt-marsh edges around the Wash were traced s part of a field study into the processes of salt-marsh advance in this area. It is sought to establish that salt-marsh advance is not a continuous process, but that foreshore saltings tend to become stabilized when they are a 13-1z 2l mile wide, with a wider belt of mud flats in front of them. In the mud-flat areas accretion, caused by continuous deposition of sedi…

  • Cyclic Changes in Morecambe Bay

    Friedrich Julius Theodor Kestner•ARTICLE•Geographical Journal•1970

Geography (3 obras) · Geology (2 obras) · Geology (2 obras) · Oceanography (2 obras) · Oceanography (2 obras) · Aeolian processes and effects (1 obra) · American Environmental and Regional History (1 obra) · Archaeology (1 obra) · Bay (1 obra) · Coastal and Marine Dynamics (1 obra)

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