2 edition of Geological investigations in East Greenland. found in the catalog.
Geological investigations in East Greenland.
Lawrence Richard Wager
|Other titles||The stratigraphy and tectonics of Knud Rasmussens Land and the Kangerdlugssuaq region.|
|Statement||by L.R. Wager.|
|Series||Meddelelser om Gr©ınland -- bd.134, nr.5|
|Contributions||Scoresby Sound Committee. East Greenland Expedition,, British East Greenland Expedition 1935-36.|
|The Physical Object|
|Number of Pages||64|
Wager, L.R., , Geological investigations in East Greenland IV: The Stratigraphy and tectonics of Knud Rasmussen Land and the Kangerdlugssuaq Region, Geol. Surv. of Greenland, (5): 1– Google ScholarCited by: GEOLOGICAL INVESTIGATIONS IN EAST GREENLAND. Part I. General Geology from Angmagsalik to Kap Dalton. By L. R. WAGER. (Meddelelser om Gr0nland, Bd. , Nr. 2.) Kobenhavn: C. A. Reitzels Forlag I XI X 7 inches; 46 pages; illustrations and maps This is an important contribution to the geological survey of Greenland. Its.
The new geological map of East Greenland The new geological map of East Greenland Brooks, Kent The ‘Caledonian Orogeny’ conjures up pictures of the Scottish Highlands: the Moine Thrust, the Dalradian metasediments and massive granites. However, although the Caledonian was first investigated and mapped in Scotland, hence the Author: Brooks, Kent. Darwin, C., On certain areas of elevation and subsidence in the Pacific and Indian Oceans, as deduced from the study of coral formations, J. Geol. Soc. London, 2, ,
Assessment of Undiscovered Oil and Gas Resources of the East Greenland Rift Basins Province. Introduction. In the U.S. Geological Survey (USGS) completed an assessment of the potential for undiscovered, techni-cally recoverable (assuming the absence of sea ice) oil and gas resources in the East Greenland Rift Basins Province (fig. 1).File Size: 3MB. Techniques of Water-Resources Investigations of the United States Geological Survey Chapter A20 SIMULATION OF SOLUBLE WASTE TRANSPORT AND BUILDUP IN SURFACE WATERS USING TRACERS By F.A. Kilpatrick Book 3 APPLICATION OF HYDRAULICS. Link back to USGS publications.
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Additional Physical Format: Online version: Wager, L. (Lawrence Rickard), Geological investigations in east Greenland. København: C.A. Reitzels forlag. Buy Geological Investigations in East Greenland, Part III - The Petrology of the Skaergaard Intrusion, Kangerdlusgssuaq, East Greenland on FREE SHIPPING on.
buy geological investigations in east greenland: part iii: the petrology of the skaergaard intrusion, kangerdlugssuaq, east greenland.
on free shipping on qualified orders. The book summarises the results of more than 60 years of geological investigations in Greenland and the surrounding shelf areas. It has been written with a professional background and is presented in a form that is suitable not only for the general, interested reader, but also for students and geologists without a specific knowledge of.
Trettin, H. / GEOLOGY OF THE INNUITIAN OROGEN AND ARCTIC PLATFORM OF CANADA AND GREENLAND, GSA DNAG Volume E, Ottawa, cl, pages, 9 figures in separate slipcase, - 1 - $ 50 Wagner, L.
and Deer, W. / GEOLOGICAL INVESTIGATIONS IN EAST GREENLAND, Part III. Geological investigations began in the late nineteenth century in this region, which was generally accessible by ship except in the worst ice years, and the region became the main focus of the long series of Danish geological expeditions to East Greenland led by Lauge Koch from to (see, e.g., Haller, ).
The area of East Greenland around Scoresby Sund, Kong Oscar and Kejser Geological investigations in East Greenland. book Joseph Fjords is the largest ice-free area in Greenland. It also has incredible geodiversity, with basement rocks as old as three billion years, an almost complete sedimentary record of the last byrs and huge volumes of flood basalts from the splitting of the Atlantic.
Inpetroleum geological activities were continued in East Greenland in order to increase existing knowl- edge on the sedimentology and biostratigraphy of the Upper Permian. B) The Scoresbysund-area in East Greenland The Scoresbysund area has a long and varied Earth history, which spans almost 3 billion years.
Simplified, the geological framework can be subdivided into six parts, on top of which then comes the ice age. In time, there were about 5, settlers in Greenland.
The official records indicate that two sizable Norse settlements had been founded in fjords on the southwestern coast of the island. Other smaller ones were located on the same coast as far north as present day Nuuk. In and –, the Geological Survey of Denmark and Greenland undertook mineralization investigations during geological expeditions to central East and North-East Greenland, with particular focus on major regional faults, thrusts, and detachment zones (Jensen,a, ; Pedersen, ; Stendal and Wendorff, ; Pedersen and.
Paper read at the IAV scientific session of Aug. 30, (XIII General Assembly, I.U.G.G.).Cited by: Greenland is the largest island on one-fifth of its surface area is exposed bedrock, the rest being covered by exposed surface is approximatelykm The geology of Greenland is dominated by crystalline rocks of the Precambrian Shield.
The crystalline rocks of the Nuuk/Qeqertarsuatsiaat area comprise some of the oldest bedrock in Greenland which.
Henriksen, N. Geological history of Greenland, pp. Copen hagen: Geological Survey of Denmark and Greenland. Evolution of a Surge-Type Glacier in its. Geologists from different universities in Norway undertook an expedition to Wollaston Forland, East Greenland, in the summer of The objective was to map and study coarse-grained sediments.
Geological investigations in East Greenland Part IV: The stratigraphy and tectonics of Knud Rasmussen Land and the Kangerdlugssuaq Region The Scoresby Sound Committee’s 2ND East Greenland Expedition in to King Christian IX’s Land Leader: E Mikkelsen Plus The British East Greenland Expedition Leader: L.R.
Wager. east Greenland, where they reach heights of about 2, meters, to north– Geology of Greenland occupy four-fifths of the country beneath the great interior ice sheet, and little is known concerning the coasts facing the Arctic Sea. Through geological investigations carried on during the last few decades.
Geological Investigations Boulder Canyon Project Pt 3-Examinations-Investigation. A book that does not look new and has been read but is in excellent condition.
No obvious damage to the cover, with the dust jacket (if applicable) included for hard covers. Central America and Caribbean, Europe, Middle East, Greenland, Mexico, Canada Seller Rating: % positive. Stemmerik, L. & Stouge, S. (eds) The Jurassic of North-East Greenland. Geological Survey of Denmark and Greenland Bulletin 5, pp.
The Jurassic sedimentary succession in East and North-East Greenland reflects deposition during the. "This Bulletin records the exploration history of northern East Greenland in three phases: the pioneer exploration and discovery from c.
BC to ; commercial activities, early mountaineering and geological mapping from to ; and modern scientific investigations, adventure and sporting expeditions from to. Methods of Geological Investigation These may be divided into two main groups: the surface investigations and the subsurface investigations.
A. Surface Investigations These include preparation of topographic maps (if these are not already available) using the normal mapping techniques.
In fact all field surveys begin with the preparation (or.Coordinates The Skaergaard intrusion is a layered igneous intrusion in the Kangerlussuaq area, East GreenlandIt comprises various rock types including gabbro, ferro diorite, anorthosite and granophyre.
Discovered by Lawrence Wager in during the British Arctic Air Route Expedition led by Gino Watkins, the intrusion has been important to the development of key .In Greenland, the ice age is not over yet: it is still 85% covered with ice. Moraine at the rim of the inland ice (Kangerlussuaq, West Greenland) The onset of glaciatíon in Greenland may have started about million years ago.