2 edition of Geomorphic and vegetational studies in the Mesters Vig district, northeast Greenland found in the catalog.
Geomorphic and vegetational studies in the Mesters Vig district, northeast Greenland
Washburn, A. L.
Includes bibliographical references: p. -60.
|Statement||by A.L. Washburn.|
|Series||Meddelelser om Grønland -- Bd. 166, nr. 1|
|LC Classifications||Q115 .D39 bd. 166, nr. 1|
|The Physical Object|
|Pagination||60 p., 5 leaves of plates (1 folded) :|
|Number of Pages||60|
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Get this from a library. Geomorphic and vegetational studies in the Mesters Vig district, Northeast Greenland. General introduction. [A L Washburn]. Book Reviews. book review. The Arctic Basin, Pleistocene and Recent Environments of the Great Plains, Geomorphic and Vegetational Studies in the Mesters Vig District, Northeast Greenland.
General Introduction, The Flowering Plants and Ferns of the Mesters Vig District, Northeast Greenland, The Structure and Development of Turf Hummocks in the. Geomorphic and Vegetational Studies in the Mesters Vig District, Northeast Greenland.
General Introduction by A. Washburn; The Flowering Plants and Ferns of the Mesters Vig District, Northeast Greenland by Hugh M. Raup; The Structure and Development of Turf Hummocks in the Mesters Vig District, Northeast Greenland by Hugh M. Raup; Instrumental Observations of Mass-Wasting in the Mesters Vig.
Aspects of the Weichselian chronology in central East Greenland. Geomorphic and Vegetational Studies in the Mesters Vig District, Northeast Greenland. General IntroductionAuthor: Svend Funder. Geomorphic and Vegetational Studies in the Mesters Vig District, Northeast Greenland.
General Introduction and glacial landforms in the. Of high interest are also the instrumental observations of mass-wasting carried out by Wahburn in the Mesters Vig district of NE Greenland from to (Washburn ). Experimental sites ranging in mean gradient from to were established in various conditions regarding grain size, moisture and vegetational characteristics.
Increased understanding of coastal soils is, however, only possible from the purview of specific examples that illustrate soil distribution patterns in terms of sequences based on soil-forming factors of topography (toposequences), time (chronosequences), climate change (climosequence), and biological factors (biosequence).
(From Hugh M. Raup b The relation of the vascular flora and some factors of site in the Mesters Vig district, Northeast Greenland. Meddel om Gronl. (5)p.). - - - Organized ideas on the vegetation of the whole of Greenland began with Warming.
He published an account of this vegetation inand an English version appeared in The occurrence of soil in coastal zones is not a simple matter to resolve. Summarized coastal zones form a global perspective that only briefly indicates potential occurrence of soil in relation to coastal landforms, maritime climates, drainage, vegetation, and time available for formation.
References REFERENCES Aalto, K.R.,Glacial marine sedimentation and stratigraphy of the Toby Conglomerate (upper Proterozoic), southeastern British Columbia, northwester. Quaternary geology of Boothia Peninsula, District of Franklin and northern District of Keewatin, central Canadian Arctic.
Geological Survey of Canada, Memoir 26 pp. Ediger II, R., and Barkley, T.M. The first trips went to Mesters Vig in Northeast Greenland, where there was an airstrip that had served a lead mine, but soon the programme included a cruise around Svalbard in a chartered boat, visits to several parts of the Canadian Arctic, and the first "tourist party" to Qaanaaq in Northwest Greenland.
"Changes in vegetation following reduction in grazing pressure on the National Trust Kinder Estate, Peak District, Derbyshire, England." Biological Conservation: 69(1): Anderson, R. The Periglacial Environment, Permafrost, And Man_Price_ - Free download as PDF File .pdf), Text File .txt) or read online for free.
A classic geological work on periglacial landscape. In the case of the periglacial environment, the transition is usually to, or from, a glacial or temperate environment, the so-called glacial and interglacial periods of the Pleistocene.
The proglacial environment, which refers specifically to ice-marginal conditions, is a periglacial environment in the original sense of Lozinski. Knowledge on Holocene sea-level changes in the U.K. improved appreciably in the s and s, essentially due to the creation of an important national working group contributing to the IGCP Projects 61 and 2 0 0 and to the careful compilation and screening of sea-level data undertaken by M.J.
Tooley and I. Shennan. Full text of "Biosphere Reserves, Compilation 4, October programme on man and the biosphere (MAB)" See other formats.