2 edition of Report on the 1968 Geological Expedition to Scores by Sund, East Greenland. found in the catalog.
Report on the 1968 Geological Expedition to Scores by Sund, East Greenland.
Geological Survey of Greenland.
|Series||Geological Survey of Greenland Report -- 21|
Birkenmajer, K., , Report on investigations of Tertiary sediments at Kap Brewster, Scoresby Sund, East Greenland, Rapp. Grønland geol. Unders E. G., , “Report on geological investigations at Jokulsa in Fljotsdal Valley, Summer ” [in Icelandic], Natl. Energy Authority (Orkustofnun), Reykjavik. Geological. USCGC EASTWIND (WAGB) ARCTIC WEST St. John's Newfoundland, Montreal Canada Argentina laying cable for the American Telephone and Telegraph company USCGC EASTWIND (WAGB) ARCTIC EAST Gronnedal Greenland, USAirBase Thule, Umanak Island, Ata Sund, Jacobshavn Harbor Argentina, Karrats Fjord.
Kangerlussuaq Fjord (Greenlandic: Kangerlussuaq, meaning 'large fjord'; old spelling Kangerdlugssuaq; Danish: Stor Fjord) is a fjord in eastern is part of the Sermersooq municipality.. The fjord was named by the East-Greenland Coast Expedition led by Georg Carl Amdrup in Currently drilling explorations are being carried out for the possible . It has been some time coming but I am pleased to now formally announce my expeditions to the spectacular Scoresby Sund fjord system on the east coast of Greenland with good friend Daniel Bergmann. For Daniel and I will be leading two back-to-back 'fly-in, fly-out' expeditions that will depart from Reykjavik via charter.
Earth and Planetary Science Letters, 32 () Elsevier Scientific Publishing Company, Amsterdam - Printed in The Netherlands [41 BIOSTRATIGRAPHIC AGES OF TERTIARY BASALTS ON THE EAST GREENLAND CONTINENTAL MARGIN AND THEIR RELATIONSHIP TO PLATE SEPARATION IN THE NORTHEAST ATLANTIC N.J. SOPER, C. DOWNIE, A.C. HIGGINS and L.I. COSTA Department of Geology. The first expedition departed from Longyearbyen in Svalbard early in August and sailed up the coast of Svalbard before crossing the Greenland Sea (Arctic ocean) to Greenland. We then sailed down the east coast of Greenland exploring many of the incredible fjords (including the breathtaking Scoresby Sund and Kaiser Franz Josef fjords) before.
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Get this from a library. Report on the geological expedition to Scoresby Sund, East Greenland. Following the – work in the Scoresby Sund region, GGU planned to extend the geological mapping program to both North Greenland and North-East Greenland, a vast region for which modern topographic base maps were lacking (Henriksen and Higgins, ).
In cooperation with the Geodetic Institute in Copenhagen, a new topographic mapping project. The wealth of new observations and data accumulated between and during regional mapping by the Geological Survey of Greenland and other organizations has radically changed our understanding of virtually all aspects of the East Greenland segment of the orogen extends for km between 70°N (Scoresby Sund) and 82°N (Kronprins Christian.
Report on the geological expedition to Scoresby Sund, East Greenland. Book: OCLC Number: Notes: Cover title. Description: pages illustrations, maps (4 folded in pocket) 24 cm.
# Geological survey of Greenland. Report\/span> \u00A0\u00A0\u00A0 schema. Chadwick, B. () The structure of south Renland, Scoresby Sund, with special reference to the tectonometamorphic evolution of a southern internal part of the Caledonides of East Greenland. Bull. Grgnlands Geol.
Unders. (also Meddr Gr4nland. Figure 4. Geological map of the East Greenland Caledonian orogen from 72°N to 74°30′N, showing location of the Charcot Land, Eleonore Sø, and Målebjerg windows, and the Hamberg Gletscher foreland.
E–F–G and H–J are the lines of the cross sections shown in Figures 13 and A klippe of Eleonore Bay Supergroup sedimentary rocks in. Tertiary lavas from the Scoresby Sund area of East Greenland are found to have moderately stable remanent magnetization which is reversed with respect to the present earth's magnetic field.
The mean direction () is similar to that of Trap Diabase dykes in S.W. Greeland. Review of Palaeobotany and Palynology, 31 (): 1 Elsevier Scientific Publishing Company, Amsterdam -- Printed in The Netherlands PALYNOLOGY OF THE PLANT-BEARING RHAETIAN TO HETrANGIAN KAP STEWART FORMATION, SCORESBY SUND, EAST GREENLAND K.
RAUNSGAARD PEDERSEN and JENS J. LUND Geological. THIS paper deals with some investigations of the Quaternary geology of the Scoresby Sund region, north-east Greenland, carried out by the author in the summers of and for the Geological.
The sedimentary record around outer Scoresby Sund begins with the Scoresby Sund glaciation (≃isotope stage 6), but is incomplete.
Both at Kap Hope, headward of. Surrounding the settlement of Ittoqqortoormiit, at the mouth of Scoresby Sund in North-East Greenland, is the Liverpool Land Terrain—a geological terrain that records evidence of subduction to ultra-high pressures (depths of over km).
EAST GREENLAND. Join us on a Greenland photo tour with our expert team. East Greenland is one of the best places in the Arctic to photograph breathtaking landscapes and massive icebergs.
We will use the expedition ship MS Freya to explore the Scoresbysund fjord system and visit the Inuit village Ittoqqortoormiit. The fjord system of Scoresby Sund on the east coast of Greenland has been the subject of two research cruises by RV Polarstern in and Most of.
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.
East Greenland is an outstanding example of a passive continental margin of the type characterized by voluminous basaltic activity such as is common to the North Atlantic margins, but is also found in many other areas.
It is divided into three provinces on the basis of geology, structure and morphology. The structure of south Renland, Scoresby Sund with special reference to the tectono-metamorphic evolution of a southern internal part of the Caledonides of East Greenland.
Chadwick. 67 pp., 27 fig., 2 plts. From central East Greenland, C14 ages betw > 40, years B.P. have been obtained for six samples of marine bivalve shells.
The ages seem to be consistent with geological observations. Copenhagen. Denmark: Geological Survey of' Denmark and Greenland (GEUS). GEUS Bulletin p., maps (including 2 pocket maps), colour and b&w illus. glossary, references. Hardbound. DKK. and Open Access Online. The place names of northern East Greenland tell the story of exploration of this remote part of the world.
Geological Survey of Denmark and Greenland, Øster V oldg DK Copenhagen K, Denmark. E-mail: [email protected]; [email protected] Bulletin GSBIndhold 04/12/07 Side 5. Exploration history and place names of northern East Greenland.
Anthony K. Higgins. 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. In late September of I will lead an expedition to photograph the incredible landscapes of the Scoresby Sund fjord system on the remote East Coast of Greenland.
Greenland is an incredible place to inspire the imagination and fuel your photographic desires.Abstract. Our knowledge of the sea bottom of the North Polar Sea, the Greenland-Norwegian Sea, and the North Atlantic was for a long period based on bathymetric maps by Nansen () and bottom-sample investigations by Bøggild (, ).East Greenland View GeoRef Thesaurus > Close mobile search navigation Modify Your Advanced Search.
Update search Book Chapter Scoresby Sund (3) Skaergaard Intrusion (14) South Greenland (1).