Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts
Using ground‐penetrating radar (GPR), we studied an entire 2.2 km long rock glacier (3780–4350 m asl) in the dry Andes of Chile with the aim of inferring its composition. In the high‐quality, unmigrated data, we identified the active layer base and the rock glacier floor. In between, hyperbolae gene...
Published in: | Permafrost and Periglacial Processes |
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Language: | unknown |
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Online Access: | https://doi.org/10.1002/ppp.1846 |
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ftrepec:oai:RePEc:wly:perpro:v:26:y:2015:i:4:p:335-346 2023-05-15T17:08:22+02:00 Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts Sébastien Monnier Christophe Kinnard https://doi.org/10.1002/ppp.1846 unknown https://doi.org/10.1002/ppp.1846 article ftrepec https://doi.org/10.1002/ppp.1846 2020-12-04T13:31:25Z Using ground‐penetrating radar (GPR), we studied an entire 2.2 km long rock glacier (3780–4350 m asl) in the dry Andes of Chile with the aim of inferring its composition. In the high‐quality, unmigrated data, we identified the active layer base and the rock glacier floor. In between, hyperbolae generated by diffracting boulders were inventoried; the ones along the rock glacier floor (n = 51) allowed determination of the average electromagnetic (EM) velocity in the rock glacier, the latter being further used for migration. Within the rock glacier (16–39 m thick), the EM velocity varies between 0.076 and 0.167 m.ns‐1; the main stratigraphic features observed are upward‐dipping reflectors. The low EM velocities ( Article in Journal/Newspaper Long Rock RePEc (Research Papers in Economics) Long Rock ENVELOPE(-61.198,-61.198,-62.689,-62.689) Permafrost and Periglacial Processes 26 4 335 346 |
institution |
Open Polar |
collection |
RePEc (Research Papers in Economics) |
op_collection_id |
ftrepec |
language |
unknown |
description |
Using ground‐penetrating radar (GPR), we studied an entire 2.2 km long rock glacier (3780–4350 m asl) in the dry Andes of Chile with the aim of inferring its composition. In the high‐quality, unmigrated data, we identified the active layer base and the rock glacier floor. In between, hyperbolae generated by diffracting boulders were inventoried; the ones along the rock glacier floor (n = 51) allowed determination of the average electromagnetic (EM) velocity in the rock glacier, the latter being further used for migration. Within the rock glacier (16–39 m thick), the EM velocity varies between 0.076 and 0.167 m.ns‐1; the main stratigraphic features observed are upward‐dipping reflectors. The low EM velocities ( |
format |
Article in Journal/Newspaper |
author |
Sébastien Monnier Christophe Kinnard |
spellingShingle |
Sébastien Monnier Christophe Kinnard Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts |
author_facet |
Sébastien Monnier Christophe Kinnard |
author_sort |
Sébastien Monnier |
title |
Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts |
title_short |
Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts |
title_full |
Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts |
title_fullStr |
Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts |
title_full_unstemmed |
Internal Structure and Composition of a Rock Glacier in the Dry Andes, Inferred from Ground‐penetrating Radar Data and its Artefacts |
title_sort |
internal structure and composition of a rock glacier in the dry andes, inferred from ground‐penetrating radar data and its artefacts |
url |
https://doi.org/10.1002/ppp.1846 |
long_lat |
ENVELOPE(-61.198,-61.198,-62.689,-62.689) |
geographic |
Long Rock |
geographic_facet |
Long Rock |
genre |
Long Rock |
genre_facet |
Long Rock |
op_relation |
https://doi.org/10.1002/ppp.1846 |
op_doi |
https://doi.org/10.1002/ppp.1846 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
26 |
container_issue |
4 |
container_start_page |
335 |
op_container_end_page |
346 |
_version_ |
1766064112644653056 |