UnivTrevesV1, PascalFrancis, Corpus, bibRecord, 000905

'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 Kilian

Source :

The Holocene : (Sevenoaks) [ 0959-6836 ] ; 2005.

RBID : Francis:08-0171532

Descripteurs français

Pascal (Inist)
- Moyen, Chili, Age, Holocène, Système, Nom, Forme, Calendrier, Méthode, Forêt, Sol, Etude, Andes, Patagonie, Terroir.

English descriptors

KwdEn :
- Age, Calendar, Chile, Floor, Forest, Form, Holocene, Method, Middle, Name, Soil, Study, System.

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.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A01	`01`	`1`		`@0 0959-6836`
A03		`1`		`@0 Holocene : (Sevenoaks)`
A05				`@2 15`
A06				`@2 1`
A08	`01`	`1`	`ENG`	`@1 'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile`
A11	`01`	`1`		`@1 KOCH (Johannes)`
A11	`02`	`1`		`@1 KILIAN (Rolf)`
A14	`01`			`@1 Department of Earth Sciences, Simon Fraser University @2 Burnaby, BC V5A 1S6 @3 CAN @Z 1 aut.`
A14	`02`			`@1 Lehrstuhl fur Geologie, FB VI, Universität Trier @2 54286 Trier @3 DEU @Z 2 aut.`
A20				`@1 20-28`
A21				`@1 2005`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 25948 @5 354000126630100020`
A44				`@0 0000 @1 © 2008 INIST-CNRS. All rights reserved.`
A45				`@0 43 ref.`
A47	`01`	`1`		`@0 08-0171532`
A60				`@1 P @3 PR`
A61				`@0 A`
A64	`01`	`1`		`@0 The Holocene : (Sevenoaks)`
A66	`01`			`@0 GBR`
C01	`01`		`ENG`	@0 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.
C02	`01`	`H`		`@0 52528 @1 II`
C02	`02`	`H`		`@0 52526 @1 II`
C02	`03`	`H`		`@0 525`
C03	`01`	`H`	`FRE`	`@0 Moyen @2 ND @5 01`
C03	`01`	`H`	`ENG`	`@0 Middle @2 ND @5 01`
C03	`02`	`H`	`FRE`	`@0 Chili @2 NG @5 05`
C03	`02`	`H`	`ENG`	`@0 Chile @2 NG @5 05`
C03	`03`	`H`	`FRE`	`@0 Age @2 NI @5 14`
C03	`03`	`H`	`ENG`	`@0 Age @2 NI @5 14`
C03	`04`	`H`	`FRE`	`@0 Holocène @2 NI @5 15`
C03	`04`	`H`	`ENG`	`@0 Holocene @2 NI @5 15`
C03	`05`	`A`	`FRE`	`@0 Système @5 19`
C03	`05`	`A`	`ENG`	`@0 System @5 19`
C03	`06`	`A`	`FRE`	`@0 Nom @5 20`
C03	`06`	`A`	`ENG`	`@0 Name @5 20`
C03	`07`	`H`	`FRE`	`@0 Forme @5 21`
C03	`07`	`H`	`ENG`	`@0 Form @5 21`
C03	`08`	`A`	`FRE`	`@0 Calendrier @5 22`
C03	`08`	`A`	`ENG`	`@0 Calendar @5 22`
C03	`09`	`H`	`FRE`	`@0 Méthode @5 23`
C03	`09`	`H`	`ENG`	`@0 Method @5 23`
C03	`10`	`H`	`FRE`	`@0 Forêt @5 24`
C03	`10`	`H`	`ENG`	`@0 Forest @5 24`
C03	`11`	`H`	`FRE`	`@0 Sol @5 25`
C03	`11`	`H`	`ENG`	`@0 Floor @5 25`
C03	`12`	`H`	`FRE`	`@0 Etude @5 26`
C03	`12`	`H`	`ENG`	`@0 Study @5 26`
C03	`13`	`H`	`FRE`	`@0 Andes @4 INC @5 31`
C03	`14`	`H`	`FRE`	`@0 Patagonie @4 INC @5 32`
C03	`15`	`H`	`FRE`	`@0 Terroir @4 CD @5 96`
C03	`15`	`H`	`ENG`	`@0 Soil @4 CD @5 96`
C07	`01`	`H`	`FRE`	`@0 Amérique @2 NG`
C07	`01`	`H`	`ENG`	`@0 America @2 NG`
C07	`02`	`H`	`FRE`	`@0 Amérique du Sud @2 NG @5 09`
C07	`02`	`H`	`ENG`	`@0 South America @2 NG @5 09`
N21				`@1 105`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

Format Inist (serveur)

NO :	FRANCIS 08-0171532 INIST
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:08-0171532

Le 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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<s2>Burnaby, BC V5A 1S6</s2>
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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile</title>
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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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<fA14 i1="01"><s1>Department of Earth Sciences, Simon Fraser University</s1>
<s2>Burnaby, BC V5A 1S6</s2>
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<sZ>1 aut.</sZ>
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<fA14 i1="02"><s1>Lehrstuhl fur Geologie, FB VI, Universität Trier</s1>
<s2>54286 Trier</s2>
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<fC01 i1="01" l="ENG"><s0>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.</s0>
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<s2>NI</s2>
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<fC03 i1="05" i2="A" l="FRE"><s0>Système</s0>
<s5>19</s5>
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<fC03 i1="05" i2="A" l="ENG"><s0>System</s0>
<s5>19</s5>
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<s5>21</s5>
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<s5>23</s5>
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<fC03 i1="10" i2="H" l="FRE"><s0>Forêt</s0>
<s5>24</s5>
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<fC03 i1="10" i2="H" l="ENG"><s0>Forest</s0>
<s5>24</s5>
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<fC03 i1="11" i2="H" l="FRE"><s0>Sol</s0>
<s5>25</s5>
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<fC03 i1="11" i2="H" l="ENG"><s0>Floor</s0>
<s5>25</s5>
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<fC03 i1="12" i2="H" l="FRE"><s0>Etude</s0>
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<s5>26</s5>
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<s5>31</s5>
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<s5>32</s5>
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<s5>96</s5>
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<s5>96</s5>
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<s2>NG</s2>
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<fC07 i1="02" i2="H" l="FRE"><s0>Amérique du Sud</s0>
<s2>NG</s2>
<s5>09</s5>
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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>
<CC>52528; 52526; 525</CC>
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<FG>Amérique; Amérique du Sud</FG>
<ED>Middle; Chile; Age; Holocene; System; Name; Form; Calendar; Method; Forest; Floor; Study; Soil</ED>
<EG>America; South America</EG>
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'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile

'Little Ice Age' glacier fluctuations, Gran Campo Nevado, southernmost Chile

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