Last edited by Faegrel
Sunday, May 17, 2020 | History

2 edition of Quaternary Geology of the Narssaq Area, South Greenland. found in the catalog.

Quaternary Geology of the Narssaq Area, South Greenland.

Geological Survey of Greenland.

Quaternary Geology of the Narssaq Area, South Greenland.

by Geological Survey of Greenland.

  • 168 Want to read
  • 24 Currently reading

Published by s.n in S.l .
Written in English


Edition Notes

1

SeriesGeological Survey of Greenland Report -- 86
ContributionsFunder, S.
ID Numbers
Open LibraryOL21791012M

Evolution of the Tugtutôq Central Complex, South Greenland: A high-level, rift-axial, late-Gardar centre Author links open overlay panel B.G.J. Upton a A.R. Martin a D. Stephenson b Show moreCited by: Climate change and the Viking-age fjord environment of the Eastern Settlement, South Greenland January Geologic survey of Denmark and Greenland bulletin

LITHOS ELSEVIER Lithos 40 () Crust-mantle interaction m the evolution of the Ilimaussaq Complex, South Greenland: Nd isotopic studies Ross Stevenson a'*, B.G.J. Upton b, A. Steenfeltc ' Geological Survey of Canada, Booth St. Ottawa, Ont., Canada K1A OE8 b Department of Geology and Geophysics, University of Edinburgh, Edinburgh, EH9 3JW, UK c Cited by: WELCOME, LET THE FUN BEGIN! Get e-Books "Greenland Geoscience" on Pdf, ePub, Tuebl, Mobi and Audiobook for are more than 1 Million Books that have been enjoyed by people from all over the world. Always update books hourly, if not looking, search in the book search column. Enjoy % FREE.

Three principal episodes (at c. , and Ma.) of faulting and associated alkaline magmatism are recognised in the evolution of the Gardar province in south Greenland. Terrestrial sediments and lavas, accumulated in fault-bounded troughs and cut by Early Gardar alkaline complexes, constitute evidence for continental rifting and Cited by: Quaternary geology The Earth's youngest period, the Quaternary, includes the last 2–3 million years and is characterized by several glaciations and warmer interglacial intervals. The cause of the climatic changes is probably to be found in the Earth's orbital parameters, which result in lower summer insolation in the northern hemisphere.


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Quaternary Geology of the Narssaq Area, South Greenland by Geological Survey of Greenland. Download PDF EPUB FB2

The Quaternary geology of the Narssaq area, South Greenland (Contribution to the Narssaq Project) [Funder, Svend] on *FREE* shipping on qualifying offers. The Quaternary geology of the Narssaq area, South Greenland (Contribution to the Narssaq Project)Author: Svend Funder.

The Quaternary geology of the Narssaq area, South Greenland [Svend. Funder] on *FREE* shipping on qualifying : Svend. Funder. Geological Guide South Greenland: The Narsarsuaq-Narsqa-Qaqortoq region: The Narsarsuaq - Narsaq - Qaqortoq Region by Henning Sørensen () on *FREE* shipping on qualifying offers.

Geological Guide South Greenland: The Narsarsuaq-Narsqa-Qaqortoq region: The Narsarsuaq - Narsaq - Qaqortoq Region by Henning Sørensen ()Manufacturer: Geological Survey of Denmark & Greenland. Get this from a library. The Quaternary geology of the Narssaq area, South Greenland.

[Svend Funder]. Geological Guide - South Greenland. The Narsarsuaq - Narsaq - Qaqortoq region. This book is a handy guide book to the fascinating geology of South Greenland which houses some world-famous mineral localities.

It focuses on the description of the main geological features of the region and of localities and is planned as a handy guide book to be used in the field.

This volume is in the Decade of North American Geology Project series, it is Geology of North America volume K Small ink name-stamp of 'Rhodes', dated Decemberon the front endpaper. No signs of : Roger B.

Morrison. Buy The Quaternary geology of the Narssaq area, South Greenland (Contribution to the Narssaq Project) by Funder, Svend (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Svend Funder.

The three major sections of this volume include six chapters describing the regional Quaternary geology of Canada, two describing the Quaternary geology and climatic history of Greenland, and six that review applied Quaternary geology in Canada, including chapters on paleobotanical analysis, geodynamics, geomorphic processes, terrain geochemistry, Quaternary resources, and the influence of the Quaternary.

For persistent hikers the trek over the mountain to Qassiarsuk is a typical journey through the South Greenlandic countryside with sheep farms, green river valleys, raw mountains and ice-filled fjords.

If you are interested in some of the many mineral deposits in Greenland, then you may be familiar with the Dyrnæs-Narsaq complex. Narsaq Heliport operates year-round, linking Narsaq with Qaqortoq on the shores of Labrador Sea, and thus with Arctic Umiaq off-season route also links Narsaq with the large Narsarsuaq Airport, and indirectly with the rest of Greenland and Europe.

Sea. The harbor of Narsaq is a natural coastal harbor with steep depth. Narsaq is a port of call for the Arctic Municipality: Kujalleq. This volume contains 14 chapters covering regional Quaternary geology of Canada, applied Quaternary geology of Canada and Quaternary geology of Greenland.

The maps cover the paleogeography of North America 8, years ago (3 sheets:years ago andyears ago), the Quaternary geology mapping in Canada and the late Wisconsinan and Holocene Retreat of the Laurentide Ice Sheet.

This book is the second of three volumes in which the recent knowledge of the extent and chronology of Quaternary glaciations has been compiled on a global scale.

This information is seen as a fundamental requirement, not only for the glacial community, but for the wider user-community of general Quaternary workers. In particular the need for accurate ice. Funder, S. () CI4-dating of samples collected during the expedition to North Greenland.

Rapport GrCnlands Geologiske UndersCgelseFunder, S. (co-ordinator) () Quaternary geology of the ice- free areas and adjacent shelves of Greenland. In: Fulton, R.J.

(ed), Quaternary Geology of Canada and Greenland, pp. Cited by: and m, except off South-East Greenland where large shelfs areas are found at – m below sea level. The total area of the continental shelf is estimated to be c. / QUATERNARY GEOLOGY OF CANADA AND GREENLAND, GSA DNAG Volume K1, Boulder,cl, pages, five plates in separate J.

/ PLUTONIC DEVELOPMENT OF THE Ilordleg Area, South Greenland, Part 2, Late Kinematic basic dykes, København,pb, pages, 39 figs., 4 plates, 4 tables, - 3 - $ 25 G eology Books U.S. State Geology Maps. Lake sediment coring in South Greenland in Quaternary geology and biology of the Jørgen A sediment core from a lake in the Kap Farvel area on South Greenland.

Quaternary geology. The Quaternary is the most recent period in the Earth’s history: the last million years.

It is marked by the appearance of man as well as repeated glacial/interglacial cycles, which strongly influenced the mountains and their environment. Sampling sites (indicated by numbers) and geology of the Eriksfjord Formation and Gardar lavas, South Greenland, slightly simplified after 1:maps of Greenland 60V 2 Nord (Julianehaab) and 61 V 3 Syd (Narssarssuaq), and based on geological mapping of Stewart [ belongs to the Ketilidian mobile belt with a final cooling age of ca Cited by: QUATERNARY GEOLOGIC MAP OF THE SAN JOSE EAST QUADRANGLE, SANTA CLARA COUNTY, CALIFORNIA by E.

Helley1 and J. Wesling2 Open-File Report This map is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade,Cited by: 3. The ice sheet only retreated behind the present ice extent from c.

to cal ka BP and c. to cal ka BP in the mountainous southern Greenland, whereas the more sensitive low-lying Qassimiut lobe was behind its present margin from c. 9 ka until the Little Ice by:. Glacier surface mass-balance measurements on Greenland started more than a century ago, but no compilation exists of the observations from the ablation area of the ice sheet and local glaciers.

Such data could be used in the evaluation of modelled surface mass balance, or to document changes in glacier melt independently from model by: The final compilation of data is being released by the Washington State’s Division of Geology and Earth Resources (WDGER). Geologic and landslide mapping of km of coastline yielded landslides for the database that we constructed for WDGER (Figure 7).A stimulating (but uneven) textbook on Ice Age Earth.

June ; Quaternary Geology of Canada and Greenland. A warming of 7 °C in South Greenland was .