'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile
Identifieur interne : 000905 ( PascalFrancis/Corpus ); précédent : 000904; suivant : 000906'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile
Auteurs : Johannes Koch ; Rolf KilianSource :
- The Holocene : (Sevenoaks) [ 0959-6836 ] ; 2005.
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
Moraine systems of Glaciar Lengua (unofficial name) and neighbouring glaciers of Gran Campo Nevado (53°S) in the southernmost Andes were mapped and dated by dendrochronological means. They were formed around AD 1628, 1872/1875, 1886, 1902, 1912 and 1941 with the advance in the 1870s being calendar dated. Recessional moraines within each moraine system correspond to brief standstills or minor readvances. A significantly older moraine could not be directly dated by dendrochronological methods as the forest on it was assumed to be second-generation or older. From soil-formation rates, it is assumed that this moraine was formed at some time between AD 1280 and 1460, a time in which many other glaciers in Patagonia formed moraines. Overall, fluctuations of Glaciar Lengua show a strong synchronicity to other glaciers in the Patagonian Andes between 41°S and 55°S. This study suggests that Glaciar Lengua and possibly all glaciers of Gran Campo Nevado reached their Holocene maximum during the 'Little Ice Age.
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Pour connaître la documentation sur le format Inist Standard.
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Format Inist (serveur)
NO : | FRANCIS 08-0171532 INIST |
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ET : | 'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile |
AU : | KOCH (Johannes); KILIAN (Rolf) |
AF : | Department of Earth Sciences, Simon Fraser University/Burnaby, BC V5A 1S6/Canada (1 aut.); Lehrstuhl fur Geologie, FB VI, Universität Trier/54286 Trier/Allemagne (2 aut.) |
DT : | Publication en série; Papier de recherche; Niveau analytique |
SO : | The Holocene : (Sevenoaks); ISSN 0959-6836; Royaume-Uni; Da. 2005; Vol. 15; No. 1; Pp. 20-28; Bibl. 43 ref. |
LA : | Anglais |
EA : | Moraine systems of Glaciar Lengua (unofficial name) and neighbouring glaciers of Gran Campo Nevado (53°S) in the southernmost Andes were mapped and dated by dendrochronological means. They were formed around AD 1628, 1872/1875, 1886, 1902, 1912 and 1941 with the advance in the 1870s being calendar dated. Recessional moraines within each moraine system correspond to brief standstills or minor readvances. A significantly older moraine could not be directly dated by dendrochronological methods as the forest on it was assumed to be second-generation or older. From soil-formation rates, it is assumed that this moraine was formed at some time between AD 1280 and 1460, a time in which many other glaciers in Patagonia formed moraines. Overall, fluctuations of Glaciar Lengua show a strong synchronicity to other glaciers in the Patagonian Andes between 41°S and 55°S. This study suggests that Glaciar Lengua and possibly all glaciers of Gran Campo Nevado reached their Holocene maximum during the 'Little Ice Age. |
CC : | 52528; 52526; 525 |
FD : | Moyen; Chili; Age; Holocène; Système; Nom; Forme; Calendrier; Méthode; Forêt; Sol; Etude; Andes; Patagonie; Terroir |
FG : | Amérique; Amérique du Sud |
ED : | Middle; Chile; Age; Holocene; System; Name; Form; Calendar; Method; Forest; Floor; Study; Soil |
EG : | America; South America |
LO : | INIST-25948.354000126630100020 |
ID : | 08-0171532 |
Links to Exploration step
Francis:08-0171532Le document en format XML
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<author><name sortKey="Koch, Johannes" sort="Koch, Johannes" uniqKey="Koch J" first="Johannes" last="Koch">Johannes Koch</name>
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<author><name sortKey="Kilian, Rolf" sort="Kilian, Rolf" uniqKey="Kilian R" first="Rolf" last="Kilian">Rolf Kilian</name>
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<front><div type="abstract" xml:lang="en">Moraine systems of Glaciar Lengua (unofficial name) and neighbouring glaciers of Gran Campo Nevado (53°S) in the southernmost Andes were mapped and dated by dendrochronological means. They were formed around AD 1628, 1872/1875, 1886, 1902, 1912 and 1941 with the advance in the 1870s being calendar dated. Recessional moraines within each moraine system correspond to brief standstills or minor readvances. A significantly older moraine could not be directly dated by dendrochronological methods as the forest on it was assumed to be second-generation or older. From soil-formation rates, it is assumed that this moraine was formed at some time between AD 1280 and 1460, a time in which many other glaciers in Patagonia formed moraines. Overall, fluctuations of Glaciar Lengua show a strong synchronicity to other glaciers in the Patagonian Andes between 41°S and 55°S. This study suggests that Glaciar Lengua and possibly all glaciers of Gran Campo Nevado reached their Holocene maximum during the 'Little Ice Age.</div>
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<server><NO>FRANCIS 08-0171532 INIST</NO>
<ET>'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile</ET>
<AU>KOCH (Johannes); KILIAN (Rolf)</AU>
<AF>Department of Earth Sciences, Simon Fraser University/Burnaby, BC V5A 1S6/Canada (1 aut.); Lehrstuhl fur Geologie, FB VI, Universität Trier/54286 Trier/Allemagne (2 aut.)</AF>
<DT>Publication en série; Papier de recherche; Niveau analytique</DT>
<SO>The Holocene : (Sevenoaks); ISSN 0959-6836; Royaume-Uni; Da. 2005; Vol. 15; No. 1; Pp. 20-28; Bibl. 43 ref.</SO>
<LA>Anglais</LA>
<EA>Moraine systems of Glaciar Lengua (unofficial name) and neighbouring glaciers of Gran Campo Nevado (53°S) in the southernmost Andes were mapped and dated by dendrochronological means. They were formed around AD 1628, 1872/1875, 1886, 1902, 1912 and 1941 with the advance in the 1870s being calendar dated. Recessional moraines within each moraine system correspond to brief standstills or minor readvances. A significantly older moraine could not be directly dated by dendrochronological methods as the forest on it was assumed to be second-generation or older. From soil-formation rates, it is assumed that this moraine was formed at some time between AD 1280 and 1460, a time in which many other glaciers in Patagonia formed moraines. Overall, fluctuations of Glaciar Lengua show a strong synchronicity to other glaciers in the Patagonian Andes between 41°S and 55°S. This study suggests that Glaciar Lengua and possibly all glaciers of Gran Campo Nevado reached their Holocene maximum during the 'Little Ice Age.</EA>
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<ED>Middle; Chile; Age; Holocene; System; Name; Form; Calendar; Method; Forest; Floor; Study; Soil</ED>
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