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Friedrich Julius Theodor Kestner

Biographic Data

ID3752717
NAMEFriedrich Julius Theodor Kestner
GIVEN NAMESFriedrich Julius Theodor
FAMILY NAMEKestner
SIGNATUREKESTNER F J T
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS2
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1962
LATEST PUBLICATION YEAR1970
H-INDEX1
  • 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•Cited by: 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•Cited by: 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•Cited by: 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 works) · Geology (2 works) · Geology (2 works) · Oceanography (2 works) · Oceanography (2 works) · Aeolian processes and effects (1 work) · American Environmental and Regional History (1 work) · Archaeology (1 work) · Bay (1 work) · Coastal and Marine Dynamics (1 work)

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