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The M�yrdalsj�okull Ice Cap, Iceland : glacial processes, sediments and landforms on an active volcano /

Existing lowland ice caps are usually considered the best analogues for formerly glaciated areas and as such Icelandic glaciers have been intensively investigated with regard to process-orientated sediment-landform interrelationships. Much work has been directed towards understanding the interaction...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Otros Autores: Schomacker, Anders (Editor ), Kr�uger, Johannes (Editor ), Kj�r, Kurt H. (Editor )
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Amsterdam : Elsevier, 2010.
Colección:Developments in Quaternary science ; 13.
Temas:
Acceso en línea:Texto completo

MARC

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245 0 4 |a The M�yrdalsj�okull Ice Cap, Iceland :  |b glacial processes, sediments and landforms on an active volcano /  |c edited by Anders Schomacker, Johannes Kr�uger, Kurt H. Kj�r. 
260 |a Amsterdam :  |b Elsevier,  |c 2010. 
300 |a 1 online resource (vii, 211 pages) :  |b illustrations (some color), maps (some color). 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
490 1 |a Developments in Quaternary sciences,  |x 1571-0866 ;  |v 13 
520 |a Existing lowland ice caps are usually considered the best analogues for formerly glaciated areas and as such Icelandic glaciers have been intensively investigated with regard to process-orientated sediment-landform interrelationships. Much work has been directed towards understanding the interaction between volcanic activity and glacier response i.e. water outbursts - j�okulhlaups and sudden events of rapid flowing glacier ice, i.e. surges. The M�yrdalsj�okull ice cap has served as an excellent 'ice-age' laboratory and publications are found in all major peer-reviewed journals. The M�yrdalsj�okull ice cap is located in south central Iceland and covers some 600 km2 and is centered over a large caldera hosting the Katla central volcano that encircles an area of 100 km2. Eruptions from the Katla volcanic system occur on average twice a century and belong to the most violent geological events observed associated with an enormous outburst of water with strong influence on the ice cap and surrounding areas. During eruptions, huge quantities of tephra and volcanic gasses are also emitted. The ice cap drains into several basins via a series of outlet glaciers that terminate onto different forefields. Since the turn of the previous century M�yrdalsj�okull has retreated from its Little Ice Age maximum by frontal or areal retreat only punctuated by abrupt minor advances or temporary stagnation. Either way this does provide a unique opportunity to investigate a diversity of glacial environments and its coupling to volcanic activity. Book covers all aspects of the ice cap and volcano dynamics Comprehensive reviews with updated results Editors and authors are well established scientists with research experience from M�yrdalsj�okull Standard reference work for M�yrdalsj�okull. 
504 |a Includes bibliographical references and indexes. 
505 0 0 |t Katla and Eyjafjallaj�okull volcanoes /  |r Erik Sturkell [and others] --  |t Katla : tephrochronology and eruption history /  |r Gu�r�un Larsen --  |t Deglaciation and Holocene glacial history of Iceland /  |r �Olafur Ing�olfsson, Hreggvi�ur Nor�dahl and Anders Schomacker --  |t Variations of M�yrdalsj�okull during postglacial and historical times /  |r Oddur Sigur�sson --  |t Ice-marginal environments : geomorphic and structural genesis of marginal moraines at M�yrdalsj�okull /  |r Johannes Kr�uger, Anders Schomacker and �Ivar �Orn Benediktsson --  |t Dead-ice environments : a landsystems model for a debris-charged, stagnant lowland glacier margin, K�otluj�okull /  |r Johannes Kr�uger, Kurt H. Kj�r and Anders Schomacker --  |t Subglacial environments, sediments and landforms at the margins of M�yrdalsj�okull /  |r Amders Schomacker, Kurt H. Kj�r and Johannes Kr�uger --  |t Evidence for subglacial deformation and deposition during a complete advance-stagnation cycle of Kotluj�okull, Iceland : a case study /  |r Knud Erik S. Klint, Niels Richardt and Johannes Kr�uger --  |t M�yrdalsj�okull's forefields under the microscope : the micromorphology of meltout and subglacial tills /  |r Jaap J.M. van der Meer, Simon J. Carr and Kurt H. Kj�r) --  |t Volcanogenic j�okulhlaups (glacier outburst floods) from M�yrdalsj�okull : impacts on proglacial environments /  |r Andrew J. Russell, Robert Duller and Nigel P. Mountney. 
588 0 |a Print version record. 
506 |a Licensed for access by U. of T. users. 
651 0 |a M�yrdalsj�okull (Iceland) 
650 0 |a Ice caps  |z Iceland. 
650 0 |a Volcanoes  |z Iceland. 
650 0 |a Sedimentation and deposition  |z Iceland. 
650 0 |a Glaciology. 
651 0 |a Katla (Iceland) 
651 6 |a M�yrdalsj�okull (Islande)  |0 (CaQQLa)000268417 
650 6 |a Calottes glaciaires  |z Islande.  |0 (CaQQLa)201-0236557 
650 6 |a Volcans  |z Islande.  |0 (CaQQLa)201-0205956 
650 6 |a S�edimentation (G�eologie)  |0 (CaQQLa)201-0020441  |z Islande.  |0 (CaQQLa)201-0427214 
650 6 |a Glaciologie.  |0 (CaQQLa)201-0026581 
650 7 |a SCIENCE  |x Earth Sciences  |x Geology.  |2 bisacsh 
650 7 |a Glaciology  |2 fast  |0 (OCoLC)fst00942986 
650 7 |a Ice caps  |2 fast  |0 (OCoLC)fst00966538 
650 7 |a Sedimentation and deposition  |2 fast  |0 (OCoLC)fst01110984 
650 7 |a Volcanoes  |2 fast  |0 (OCoLC)fst01168844 
651 7 |a Iceland  |2 fast  |0 (OCoLC)fst01210572 
651 7 |a Iceland  |z M�yrdalsj�okull  |2 fast  |0 (OCoLC)fst01241093 
650 7 |a Glazialgeologie  |2 gnd  |0 (DE-588)4157506-4 
650 7 |a Glazialmorphologie  |2 gnd  |0 (DE-588)4021212-9 
650 7 |a Vulkanismus  |2 gnd  |0 (DE-588)4064081-4 
651 7 |a Myrdalsj�okull  |2 gnd  |0 (DE-588)4355153-1 
700 1 |a Schomacker, Anders,  |e editor. 
700 1 |a Kr�uger, Johannes,  |e editor. 
700 1 |a Kj�r, Kurt H.,  |e editor. 
776 0 8 |i Print version:  |t M�yrdalsj�okull Ice Cap, Iceland.  |d Amsterdam : Elsevier, 2010  |z 9780444530455  |w (DLC) 2013474145  |w (OCoLC)465362630 
830 0 |a Developments in Quaternary science ;  |v 13. 
856 4 0 |u https://sciencedirect.uam.elogim.com/science/book/9780444530455  |z Texto completo