Geology of Spitsbergen, 1965

(in 2 vols).
  • 204 Pages
  • 1.67 MB
  • 9265 Downloads
  • English
by
National Lending Library for Science & Technology , Boston Spa
Geology -- Norway -- Spitsb
Statement(edited by V. N. Sokolov), translated (from the Russian) by J. E. Bradley, edited by W. B. Harland :
SeriesTranslations of Russian books
ContributionsBradley, John Ernest Stobart., Harland, W. B.
Classifications
LC ClassificationsQE281
The Physical Object
Pagination(204)p.(4fold) :
ID Numbers
Open LibraryOL18995618M

Additional Physical Format: Online version: Sokolov, Valentin Nikolaevich. Geology of Spitsbergen, Boston Spa, National Lending Library for Science & Technology,   adshelp[at] The ADS is operated by the Smithsonian Astrophysical Geology of Spitsbergen under NASA Cooperative Agreement NNX16AC86AAuthor: P.

Friend. Get this from a library. Geology of Spitsbergen, [W B Harland; Valentin Nikolaevich Sokolov]. The geology of Svalbard encompasses the geological description of rock types found in Svalbard, and the associated tectonics and sedimentological history of soils and rocks.

The geological exploration of Svalbard is an ongoing activity, and recent understandings may differ from earlier interpretations.

Spitsbergen Geology of Spitsbergen known as West Spitsbergen; Norwegian: Vest Spitsbergen or Vestspitsbergen, Urban East Norwegian: [ˈvɛ̂stˌspɪtsbærɡn̩], also sometimes spelled Spitzbergen) is the largest and only permanently populated island of the Svalbard archipelago in northern tuting the westernmost bulk of the archipelago, it borders the Arctic Ocean, the Norwegian Sea, and the Location: Arctic Ocean.

Authors are Karsten Piepjohn (Bundesanstalt für Geowissenschaften und Rohstoffe), Malte Jochmann (Store Norske Spitsbergen Kullkompani) and Rolf Stange (amongst others owner of this website).

Christiane Hübner (Longyearbyen Feltbiologiske Forening) is the editor of the booklet, which is available in English, Norwegian and German. The Geology of Svalbard (Geological Society Memoir) Hardcover – February 1, Spitsbergen, respectively about the size of Scotland and Switzerland, have the wealth in Geology of Spitsbergen and complexity in stratigraphy and structure no less than those classic areas.

Moreover with an international history and present treaty status many nations have Cited by:   Spitsbergen-Svalbard guidebook. A complete guidebook. Useful and important information, Nature and history, Places and regions.4/5(1). The Basement - The large-scale features of the Svalbard geology are relatively simple.

The oldest formations, the so-called Basement, including Pre­cambrian, Cambrian and Ordovician rocks, occur as a belt along the west-coast of Spits­bergen, in a large area between Wijde­fjorden and Hinlopenstretet in the north, as well as in the northern part of Nordaust­landet and in the southern Geology of Spitsbergen.

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The Svalbard archipelago is found in the Arctic Ocean, approximately km ( miles) north of the northernmost tip of Norway. It is a geologist’s paradise, having a rich geological history that can be traced back through the Mesozoic era ( million years ago), the Cambrian era ( million years ago), and all the way to the Archean era, over billion years ago.

a transect from west to east across Spitsbergen, reflecting very well the distribution of precipitation: on Prins Karls 1965 book and along the central west coast it lies at m a.s.l., but reaches > m in the highlands of north-eastern Spitsbergen.

North-eastern Spitsbergen is a very dry area, and can be described as a polar Size: 1MB. Spitsbergen and the Olga Basin, Western Barents Sea. Seismic data in the fjords of Svalbard. SVALEX cruises in Geology of Svalbard • Pre-Devonian Hecla Hoek Basement, variably reworked during the Caledonian orogeny • Devonian continental deposits (Old Red Sandstone).

The Hornsund area displays large variations in landscape and geology over short distances. The mountains, the valleys and the fjords combine to create huge local weather variations in the Hornsund area. There can, for example, be a strong easterly wind in Hornsund while along the west coast of Spitsbergen it is dead calm.

2 The geology of Longyearbyen Introduction Svalbard. Either no sediments were deposited at all or the deposited layers were eroded before the Tertiary sedimentation began – a time gap of 35 million years (marked by the double dotted line in the picture of Hiorthfjellet in middle of the book).

However, the whole mountainside of. The evolution of trees in the Middle and Late Devonian was a key stage in the biological evolution of the Earth system (e.g., Le Hir et al., ) affecting the atmosphere, pedogenic processes, sediment transport, and terrestrial main early tree types have been identified: archaeopteridaleans, pseudosporochnaleans, and lycopsids (Meyer-Berthaud et al., ).Cited by: About this book In this booklet, the authors take you on an exciting journey through the geological history of the surroundings of Lonyearbyen.

The Geology of Longyearbyen starts with a short description of the development of Spitsbergen in earth history, from the days of the dinosaurs to the recent ice age with present-day glaciers, traces of. contributions to glacial geology of spitsbergen and additional notes on the glacial phenomena of spitsbergen.

[garwood, e. (signed) j. gregory.] on *free* shipping on qualifying offers. contributions to glacial geology of spitsbergen and additional notes on Author: E. (SIGNED) J. Gregory. GARWOOD. The Geology 6f Edge0ya and Barents0ya, Svalbard By B. Lock, C. Pickton, D. Smith, D. Batten and W.

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Harland Abstract This paper reviews the geology of Edge0ya and Barents0ya in the light of an investigation undertaken in A review of the history of research, with comprehensive reference list, is given. Geared toward optimum wildlife viewing, this expedition provides plenty of opportunities to witness polar bears, walrus and reindeer, and the occasions to capture some amazing photographs in the continuous daylight are as bountiful as the landscape itself.

While exploring the remarkable scenery and colorful tundra, you’ll also learn about the history and geology of Spitsbergen. LET US HELP YOU BOOK YOUR FLIGHTS. To book flights to complement your expedition, contact a Polar Travel Adviser () for seamless, worry-free booking of all ERGEN EXPLORER: WILDLIFE CAPITAL OF THE ARCTIC EXPEDITION DOSSIER | 5 Hotel Accommodations.

Also available: The Making of a Land - The Geology of Norway - ISBN Holocene Land-Ocean Interaction and Environmental Change Around the North Sea (Geological Society Special Publication, No. ) - ISBN The Geological Society of LondonFounded inthe Geological Society of London is the oldest geological society in the.

Forwick, M. & Vorren, T.O.: Stratigraphy and deglaciation of the Isfjorden area, Spitsbergen. Norwegian Journal of Geology, Vol. 90, pp Trondheim ISSN X High-resolution seismic data from the Isfjorden area, Spitsbergen, have been analysed in order to 1) establish a File Size: 9MB.

Harland - Volume Issue 5 - N. HughesAuthor: N. Hughes. Washington & Lee University, Assistant Professor of Geology, - American Overseas Petroleum, Limited, – Senior Geologist. Libya (4 yrs.), Spitsbergen (1 yr.), Netherlands and North Sea(2 yrs). Field: Geologic and structure mapping (plane table), stratigraphic studies, well-site geology.

Office: Regional. The north-western corner of Europe was torn from Greenland along an enormous fault, and during this process western Spitsbergen was folded up to form a new mountain chain.

Description Geology of Spitsbergen, 1965 PDF

The present geological era is called the Quaternary and this is the first period since the Permian, million years ago, when there have been real ice ages. Introduction to the Geology of Svalbard. Maher (9/21/98) draft version. Major geologic units: Svalbard has a very rich, a diverse and long, geologic history that makes it somewhat of a 'mecca' for geologists, a place where a great variety of geology is on display and where much can be richness is partly evident in the outlines below of major stratigraphic groups and.

Welcome to the new New features include: Split screen display — allows users to scroll the journal article and the article figures simultaneously; Faceted searching — added facets for journal, journal section, article type, book series and GeoRef keywords; Integrated OpenGeoSci Map view search results — allows users to limit search by geographic location.

Fig. 1: Cretaceous sill in Carboniferous strata of Lomfjorden area, NW Spitsbergen with about m of relief. Background on the High Arctic Large Igneous Manifestation on Svalbard: Major upper Cretaceous LIPs (e.g. the Kerguelen and Ontong Java Plateaus) show Aptian magmatic peaks, and are linked to global mantle overturning and anomalous.

Svalbard (‘cold coasts; in Norwegian) is the official name since for the archipelago in the Norwegian administrative area between longitude 10° and 35° E, and latitude 74° and 81° N. It was originally referred to as Spitsbergen from and in the Treaty of Paris of Spitsbergen, Dutch for ‘pointed peaks’, has a human population and a Polar bear population that is roughly the same.

It is one of the most unspoiled wilderness areas in the world. Although 60% of the land is covered with flowing glaciers, it has incredibly diverse scenery, including tundra, fjords and mountains from which it gets its name. Table of Contents January ; (1) Articles.

Select this article. P. F. Williams; Development of metamorphic layering and cleavage in low grade metamorphic rocks at Bermagui, Australia Geology of Spitsbergen, [book review] Am J Sci January 1, 96; doi: /ajs Full Text (PDF) Citation/Abstract.Baron Nils Adolf Erik NORDENSKJOLD, Sketch of the Geology of Spitsbergen () (includes a color lithographed fold-out geological map) Valentin Nikolaevich SOKOLOV, Geology of Spitsbergen, ; translated from the Russian by J.

E. Bradley, edited by W. B. Harland. Boston Spa, National Lending Library for Science & Technology, ).“rebirth” of the continental-drift theory about ), Dunbar inserted a land barrier to separate the Cambrian sea of Nova Scotia from that of New Bruns-wick (Figure T).

2 Of the five tectonostratigraphic zones into which Williams divided the Appalachians inthe Avalon Zone corresponds approximately.