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P F Karrow

Biographic Data

ID4800432
NAMEP F Karrow
GIVEN NAMESP F
FAMILY NAMEKarrow
SIGNATUREKARROW P F
AFFILIATIONSUniversity of Waterloo
VERIFIEDNo
TOTAL WORKS5
TOTAL CITATIONS0
WORKS AS AUTHOR5
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1964
LATEST PUBLICATION YEAR1984
H-INDEX0
  • Corry Bog, Pennsylvania

    Open Access•P F Karrow, Barry G Warner et al.•ARTICLE•Quaternary Research•1984

    New radiocarbon dates, carbon and oxygen isotope analyses of mollusks and marl, and palynologic analysis have clarified age relationships at the Corry kettle bog in northwestern Pennsylvania. A 4000-yr difference in radiocarbon dates between basal peat and marl top, previously interpreted as caused by the presence of an unconformity, is reinterpreted as due to “hard-water effects” from carbonate bedrock and glacial deposits. A radiocarbon date of…

  • Late Quaternary Mollusks from Glacial Lake Algonquin, Nipissing, and Transitional Sediments from Southwestern Ontario, Canada

    Open Access•Barry B Miller, P F Karrow et al.•ARTICLE•Quaternary Research•1979

    Mollusks were studied from six sites in Lake Algonquin deposits (12,000-10,000 yr B.P.), five transitional (Lake Stanley low stage; 10,000 – 6000 yr B.P.), and six Nipissing stage sites (6000-4000 yr B.P.) east of Lake Huron in southwestern Ontario. The sites represent a variety of near-shore, lagoonal, estuarine, and fluvial environments. Eighteen species were limited to occurrences in Algonquin stage deposits; 8 were found only in the transitio…

  • Comment on “Greatlakean Substage

    Open Access•P F Karrow•ARTICLE•Quaternary Research•1978

  • Stratigraphy, Paleontology, and Age of Lake Algonquin Sediments in Southwestern Ontario, Canada

    Open Access•P F Karrow, T W Anderson et al.•ARTICLE•Quaternary Research•1975

    Molluscs, ostracodes, diatoms, pollen, plant macrofossils, peat, and wood have been found in glacial Lake Algonquin sediments, and estuarine-alluvial sediments of the same age, in southern Ontario. Molluscs and ostracodes are particularly abundant and widespread. Pollen analysis of Lake Algonquin sediments, bogs on the Algonquin terrace, and upland bogs above the Algonquin terrace, indicate that Lake Algonquin was still in existence at the time o…

  • Niagara Falls (Geology)

    Walter M Tovell, P F Karrow•CHAPTER•Naturalist's Guide to Ontario•1964

No prominent works on this page.

  • Niagara Falls (Geology)

    Walter M Tovell, P F Karrow•CHAPTER•Naturalist's Guide to Ontario•1964

  • Stratigraphy, Paleontology, and Age of Lake Algonquin Sediments in Southwestern Ontario, Canada

    Open Access•P F Karrow, T W Anderson et al.•ARTICLE•Quaternary Research•1975

    Molluscs, ostracodes, diatoms, pollen, plant macrofossils, peat, and wood have been found in glacial Lake Algonquin sediments, and estuarine-alluvial sediments of the same age, in southern Ontario. Molluscs and ostracodes are particularly abundant and widespread. Pollen analysis of Lake Algonquin sediments, bogs on the Algonquin terrace, and upland bogs above the Algonquin terrace, indicate that Lake Algonquin was still in existence at the time o…

  • Comment on “Greatlakean Substage

    Open Access•P F Karrow•ARTICLE•Quaternary Research•1978

  • Late Quaternary Mollusks from Glacial Lake Algonquin, Nipissing, and Transitional Sediments from Southwestern Ontario, Canada

    Open Access•Barry B Miller, P F Karrow et al.•ARTICLE•Quaternary Research•1979

    Mollusks were studied from six sites in Lake Algonquin deposits (12,000-10,000 yr B.P.), five transitional (Lake Stanley low stage; 10,000 – 6000 yr B.P.), and six Nipissing stage sites (6000-4000 yr B.P.) east of Lake Huron in southwestern Ontario. The sites represent a variety of near-shore, lagoonal, estuarine, and fluvial environments. Eighteen species were limited to occurrences in Algonquin stage deposits; 8 were found only in the transitio…

  • Corry Bog, Pennsylvania

    Open Access•P F Karrow, Barry G Warner et al.•ARTICLE•Quaternary Research•1984

    New radiocarbon dates, carbon and oxygen isotope analyses of mollusks and marl, and palynologic analysis have clarified age relationships at the Corry kettle bog in northwestern Pennsylvania. A 4000-yr difference in radiocarbon dates between basal peat and marl top, previously interpreted as caused by the presence of an unconformity, is reinterpreted as due to “hard-water effects” from carbonate bedrock and glacial deposits. A radiocarbon date of…

Geology (5 works) · Geography (4 works) · Geology and Paleoclimatology Research (4 works) · Paleontology (4 works) · Archaeology (3 works) · Glacial period (3 works) · Bog (2 works) · Geological formations and processes (2 works) · Hydrology and Sediment Transport Processes (2 works) · Oceanography (2 works)

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