Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F13%3A00000197" target="_blank" >RIV/00025798:_____/13:00000197 - isvavai.cz</a>

Výsledek na webu

<a href="http://sp.lyellcollection.org/content/381/1/353" target="_blank" >http://sp.lyellcollection.org/content/381/1/353</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1144/SP381.1" target="_blank" >10.1144/SP381.1</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula

Popis výsledku v původním jazyce

This study of landscape evolution presents both new modern and palaeo processlandform data, and analyses the behaviour of the Antarctic Peninsula Ice Sheet through the Last Glacial Maximum (LGM), the Holocene and to the present day. Six sediment-landformassemblages are described and interpreted for Ulu Peninsula, James Ross Island, NE Antarctic Peninsula: (1) the Glacier Ice and Snow Assemblage; (2) the Glacigenic Assemblage, which relates to LGM sediments and comprises both erratic-poor and erratic-rich drift, deposited by cold-based and wetbased ice and ice streams respectively; (3) the Boulder Train Assemblage, deposited during a Mid-Holocene glacier readvance; (4) the Ice-cored Moraine Assemblage, found in front of small cirque glaciers; (5) the Paraglacial Assemblage including scree, pebble-boulder lags, and littoral and fluvial processes; and (6) the Periglacial Assemblage including rock glaciers, protalus ramparts, blockfields, solifluction lobes and extensive patterned ground.

Název v anglickém jazyce

Landscape evolution and ice-sheet behaviour in a semi-arid polar environment: James Ross Island, NE Antarctic Peninsula

Popis výsledku anglicky

This study of landscape evolution presents both new modern and palaeo processlandform data, and analyses the behaviour of the Antarctic Peninsula Ice Sheet through the Last Glacial Maximum (LGM), the Holocene and to the present day. Six sediment-landformassemblages are described and interpreted for Ulu Peninsula, James Ross Island, NE Antarctic Peninsula: (1) the Glacier Ice and Snow Assemblage; (2) the Glacigenic Assemblage, which relates to LGM sediments and comprises both erratic-poor and erratic-rich drift, deposited by cold-based and wetbased ice and ice streams respectively; (3) the Boulder Train Assemblage, deposited during a Mid-Holocene glacier readvance; (4) the Ice-cored Moraine Assemblage, found in front of small cirque glaciers; (5) the Paraglacial Assemblage including scree, pebble-boulder lags, and littoral and fluvial processes; and (6) the Periglacial Assemblage including rock glaciers, protalus ramparts, blockfields, solifluction lobes and extensive patterned ground.

Druh

C - Kapitola v odborné knize

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

—

Projekt

<a href="/cs/project/SPII1A9%2F23%2F07" target="_blank" >SPII1A9/23/07: Příspěvek ČR ke zajištění stavu ozonové vrstvy Země a slunečního UV záření v Antarktidě, paleoklimatická a paleogeografická rekonstrukce vybraného území Antarktidy a související geologické studium a mapování</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název knihy nebo sborníku

Antarctic Palaeoenvironments and Earth-Surface Processes

ISBN

978-1-86239-363-9

Počet stran výsledku

44

Strana od-do

353-395

Počet stran knihy

520

Název nakladatele

Geological Society, London

Místo vydání

London

Kód UT WoS kapitoly

—