Snow line of the rhine-linth glacier in the upper wurm
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| Autores principales: | , |
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
1993
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| Acceso en línea: | |
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| _version_ | 1867170486077620224 |
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| author | Keller, Oskar Krayss, Edgar |
| author_facet | Keller, Oskar Krayss, Edgar |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The Wurmian Glaciation of the Alpine Foreland has been reconstructed in different phases as a result of investigations in the Rhine-Bodan region as well as in the Linth area. The whole High Glacial is divided in four main phases: ice advance into the piedmont basins, building-up of the foreland glaciation, high stages and retreat into the inner Alps. This epoch took up perhaps less than 12,000 years. During the period of building, an average increase of ice thickness of about 12 cm per year was sufficient to form an extensive foreland glacier within 5000-7000 years. The snow lines of the stades of the piedmont glaciation as well as of the local glaciers are calculated. Snow lines at about 1500 m a.s.l. led to an inner alpine ice build-up and an advance of glaciers towards the piedmont basins. To produce the foreland ice sheet, low snow lines of 900-1000 m a.s.l. were necessary. An interstadial phase before the maximum glaciation is evidenced by sediment sequences and a 14C-date of 22,100 BP. The chronology of ice retreat after 18 ka BP is still uncertain. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_56773 |
| institution | PANGAEA |
| language | en |
| publishDate | 1993 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Snow line of the rhine-linth glacier in the upper wurm Keller, Oskar Krayss, Edgar AGE; Age, comment; Age, maximum/old; Age, minimum/young; Geographic name/locality; LATITUDE; LONGITUDE; OUTCROP; Outcrop sample; Paleoclimate Database of the Quaternary; PKDB; PKDB24327; Snow line elevation The Wurmian Glaciation of the Alpine Foreland has been reconstructed in different phases as a result of investigations in the Rhine-Bodan region as well as in the Linth area. The whole High Glacial is divided in four main phases: ice advance into the piedmont basins, building-up of the foreland glaciation, high stages and retreat into the inner Alps. This epoch took up perhaps less than 12,000 years. During the period of building, an average increase of ice thickness of about 12 cm per year was sufficient to form an extensive foreland glacier within 5000-7000 years. The snow lines of the stades of the piedmont glaciation as well as of the local glaciers are calculated. Snow lines at about 1500 m a.s.l. led to an inner alpine ice build-up and an advance of glaciers towards the piedmont basins. To produce the foreland ice sheet, low snow lines of 900-1000 m a.s.l. were necessary. An interstadial phase before the maximum glaciation is evidenced by sediment sequences and a 14C-date of 22,100 BP. The chronology of ice retreat after 18 ka BP is still uncertain. |
| title | Snow line of the rhine-linth glacier in the upper wurm |
| topic | AGE; Age, comment; Age, maximum/old; Age, minimum/young; Geographic name/locality; LATITUDE; LONGITUDE; OUTCROP; Outcrop sample; Paleoclimate Database of the Quaternary; PKDB; PKDB24327; Snow line elevation |
| url | https://doi.org/10.1594/PANGAEA.56773 |