Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ...
Field investigations of the Laptev Sea shoreface morphology were carried out (1) off erosional shores composed of unconsolidated sediments, (2) off the modern delta shores of the Lena River, and (3) off rocky shores.It was found that profiles off erosional shores had a concave shape. This shape is n...
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ftdatacite:10.1594/pangaea.425282 2024-09-15T18:17:31+00:00 Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ... Are, Felix Grigoriev, Mikhail N Hubberten, Hans-Wolfgang Rachold, Volker Razumov, Sergey O Schneider, Waldemar 2002 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.425282 https://doi.pangaea.de/10.1594/PANGAEA.425282 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 LATITUDE LONGITUDE Lithology/composition/facies Area/locality Inclination Shoreface depth Width Visual description Measured Laptev Sea System LSS dataset Supplementary Dataset Dataset 2002 ftdatacite https://doi.org/10.1594/pangaea.425282 2024-08-01T11:01:20Z Field investigations of the Laptev Sea shoreface morphology were carried out (1) off erosional shores composed of unconsolidated sediments, (2) off the modern delta shores of the Lena River, and (3) off rocky shores.It was found that profiles off erosional shores had a concave shape. This shape is not well described by commonly applied power functions, a feature, which is in disagreement with the generally accepted concept of the equilibrium shape of shoreface profiles. The position of the lower shoreface boundary is determined by the elevation of the coastal lowland inundated during the last transgression (at -5 to -10 m) and may easily be recognized by a sharp, an order of magnitude decrease in the mean inclination of the sea floor. The mean shoreface inclination depends on sediment grain-size and ranges from 0.0022 to 0.033. The concave shape of the shoreface did not change substantially during the last 20-30 years, which indicates that shoreline retreat did not slow down and hence suggests continued ... : Supplement to: Are, Felix; Grigoriev, Mikhail N; Hubberten, Hans-Wolfgang; Rachold, Volker; Razumov, Sergey O; Schneider, Waldemar (2002): Comparative shoreface evolution along the Laptev Sea coast. Polarforschung, 70, 135-150 ... Dataset laptev Laptev Sea lena river DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
LATITUDE LONGITUDE Lithology/composition/facies Area/locality Inclination Shoreface depth Width Visual description Measured Laptev Sea System LSS |
spellingShingle |
LATITUDE LONGITUDE Lithology/composition/facies Area/locality Inclination Shoreface depth Width Visual description Measured Laptev Sea System LSS Are, Felix Grigoriev, Mikhail N Hubberten, Hans-Wolfgang Rachold, Volker Razumov, Sergey O Schneider, Waldemar Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ... |
topic_facet |
LATITUDE LONGITUDE Lithology/composition/facies Area/locality Inclination Shoreface depth Width Visual description Measured Laptev Sea System LSS |
description |
Field investigations of the Laptev Sea shoreface morphology were carried out (1) off erosional shores composed of unconsolidated sediments, (2) off the modern delta shores of the Lena River, and (3) off rocky shores.It was found that profiles off erosional shores had a concave shape. This shape is not well described by commonly applied power functions, a feature, which is in disagreement with the generally accepted concept of the equilibrium shape of shoreface profiles. The position of the lower shoreface boundary is determined by the elevation of the coastal lowland inundated during the last transgression (at -5 to -10 m) and may easily be recognized by a sharp, an order of magnitude decrease in the mean inclination of the sea floor. The mean shoreface inclination depends on sediment grain-size and ranges from 0.0022 to 0.033. The concave shape of the shoreface did not change substantially during the last 20-30 years, which indicates that shoreline retreat did not slow down and hence suggests continued ... : Supplement to: Are, Felix; Grigoriev, Mikhail N; Hubberten, Hans-Wolfgang; Rachold, Volker; Razumov, Sergey O; Schneider, Waldemar (2002): Comparative shoreface evolution along the Laptev Sea coast. Polarforschung, 70, 135-150 ... |
format |
Dataset |
author |
Are, Felix Grigoriev, Mikhail N Hubberten, Hans-Wolfgang Rachold, Volker Razumov, Sergey O Schneider, Waldemar |
author_facet |
Are, Felix Grigoriev, Mikhail N Hubberten, Hans-Wolfgang Rachold, Volker Razumov, Sergey O Schneider, Waldemar |
author_sort |
Are, Felix |
title |
Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ... |
title_short |
Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ... |
title_full |
Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ... |
title_fullStr |
Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ... |
title_full_unstemmed |
Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1) ... |
title_sort |
geometric parameters of shoreface profiles of laptev sea erosion coast (table 1) ... |
publisher |
PANGAEA |
publishDate |
2002 |
url |
https://dx.doi.org/10.1594/pangaea.425282 https://doi.pangaea.de/10.1594/PANGAEA.425282 |
genre |
laptev Laptev Sea lena river |
genre_facet |
laptev Laptev Sea lena river |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.425282 |
_version_ |
1810455533116719104 |