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C D Spencer

Biographic Data

ID5380381
NAMEC D Spencer
GIVEN NAMESC D
FAMILY NAMESpencer
SIGNATURESPENCER C D
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS4
AUTHOR COUNT3
EDITOR COUNT0
FIRST PUBLICATION YEAR1978
LATEST PUBLICATION YEAR1998
H-INDEX1
  • Rapid coastal change during the mid- to late Holocene

    Open Access•C D Spencer, Chris Spencer et al.•ARTICLE•The Holocene•1998•Cited by: 4•References: 3

    A common problem facing sea-level researchers lies in determining the cause of rapid changes observed in coastal stratigraphic sequences. Such changes are commonly ascribed to the interaction of processes that operate over differing temporal and spatial scales, i.e. rapid local and regional sea-level trends and storm magnitude/frequency. At least some of the difficulty in distinguishing between these processes lies in the often limited stratigrap…

  • Two types of role playing

    C D Spencer•ARTICLE•American Psychologist•1978

  • Two types of role playing

    C D Spencer, Charlie Spencer•ARTICLE•American Psychologist•1978

  • Rapid coastal change during the mid- to late Holocene

    Open Access•C D Spencer, Chris Spencer et al.•ARTICLE•The Holocene•1998•Cited by: 4•References: 3

    A common problem facing sea-level researchers lies in determining the cause of rapid changes observed in coastal stratigraphic sequences. Such changes are commonly ascribed to the interaction of processes that operate over differing temporal and spatial scales, i.e. rapid local and regional sea-level trends and storm magnitude/frequency. At least some of the difficulty in distinguishing between these processes lies in the often limited stratigrap…

  • Two types of role playing

    C D Spencer•ARTICLE•American Psychologist•1978

  • Two types of role playing

    C D Spencer, Charlie Spencer•ARTICLE•American Psychologist•1978

  • Rapid coastal change during the mid- to late Holocene

    Open Access•C D Spencer, Chris Spencer et al.•ARTICLE•The Holocene•1998•Cited by: 4•References: 3

    A common problem facing sea-level researchers lies in determining the cause of rapid changes observed in coastal stratigraphic sequences. Such changes are commonly ascribed to the interaction of processes that operate over differing temporal and spatial scales, i.e. rapid local and regional sea-level trends and storm magnitude/frequency. At least some of the difficulty in distinguishing between these processes lies in the often limited stratigrap…

External validity (2 works) · Internal validity (2 works) · Psychology (2 works) · Social Psychology (2 works) · Accretion (finance (1 works) · Applied Psychology (1 works) · Archaeology (1 works) · Barrier island (1 works) · Coastal wetland ecosystem dynamics (1 works) · Ecology (1 works)

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