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all geography including DSDP/ODP Sites and Legs
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elements, isotopes
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carbon
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Primary terms
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absolute age (1)
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Africa
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East Africa
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Namib Desert (1)
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carbon
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Cenozoic
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Quaternary
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Holocene (1)
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upper Quaternary (1)
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clay mineralogy (4)
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isotopes
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minerals (4)
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sediments
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peat (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Dryland dunes and other dryland environmental archives as proxies for Late Quaternary stratigraphy and environmental and climate change in southern Africa Available to Purchase
Micromagnetic seep detection in the Sudan Available to Purchase
Stratigraphy, sedimentology, and tectonic development of the southeastern Pliocene Loreto Basin, Baja California Sur, Mexico Available to Purchase
Full article available in PDF version.
Influence of hydrazine on the vibrational modes of kaolinite Available to Purchase
Interlayer structures of the two-layer hydrates of Na- and Ca-vermiculites Available to Purchase
Three-dimensional order and the structure of aniline-vermiculite Available to Purchase
Structure of a vermiculite-aniline intercalate Available to Purchase
Radiometric evidence for involvement of floating islands in the formation of Florida Everglades tree islands Available to Purchase
Characteristics and Peat Stratigraphy of Tree Islands in Certain Wetland Environments Available to Purchase
Abstract (Heinselman, 1963, 1970; Hofstetter, 1999), and the Seney region of Mitchigan (Heinselman, 1965). The origin of these features has never been satisfactorily explained, and workers have concentrated on regictlal descriptions rather than on a continental awareness and comparison of these biophysiographic features. The objective of tbis study was to survey similarities and differences between islands in northern and southern regions of the contineht, largely from the .. literature, but also from the. experience of the authors, in the hope of shedding light on their genesis and the factors controlling their development. This study includes a compa~ison of morphology, vegetation, and stratigraphy of the peats underlying the islands. The islands that were investigated here were those located on uniformly deep peats in northern minnesota, the northern Florida Everglades, and the Okefenokee Swamp of Georgia. This study did not consider islands associated with the shallow peats (less than 1.5 CD) or sinkhole peats'in the soufhern Everglades.