Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015

The first direct field measurement of the entire terminal moraine of the Werenskioldbreen glacier on Spitsbergen took place at the end of July and the beginning of August 2015. The results of the measurements were the basis for the development of the large-scale terminal moraine map. The article pre...

Full description

Bibliographic Details
Main Authors: Downar-Zapolska Laura, Głowacki Tadeusz
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20182900029
id doaj-5bf91734cdcb44bb8c4ae42ea7f2d2c4
record_format Article
spelling doaj-5bf91734cdcb44bb8c4ae42ea7f2d2c42021-02-02T00:56:44ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01290002910.1051/e3sconf/20182900029e3sconf_cpsys2018_00029Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015Downar-Zapolska LauraGłowacki TadeuszThe first direct field measurement of the entire terminal moraine of the Werenskioldbreen glacier on Spitsbergen took place at the end of July and the beginning of August 2015. The results of the measurements were the basis for the development of the large-scale terminal moraine map. The article presents the stages of map creation and editing based on measurement points established by the GNSS method. The map editing required knowledge of the morphologically complex terrain. Key documentation was field notes and documentary photographs, enabling the cartographic interpretation of the varied topographic features of the terrain's surface. Based on the documentation, the water bodies on the moraine were located, the outline of the structure and the boundary points were executed and the latter were excluded from the triangulation process. The glacial river was also excluded from triangulation, which allowed a DTM to be developed. An important step in point cloud mapping was to generate a topologically correct digital elevation model of satisfactory accuracy. On the basis of the DTM, contour lines were generated showing the topographic features of the terrain's surface. The printable resultant map's scale is 1: 5000; it is in the UTM coordinate system, in the 33X zone. Complementing the content of the map, a grid of geographic coordinates, a kilometer grid, and map key descriptions were added.https://doi.org/10.1051/e3sconf/20182900029
collection DOAJ
language English
format Article
sources DOAJ
author Downar-Zapolska Laura
Głowacki Tadeusz
spellingShingle Downar-Zapolska Laura
Głowacki Tadeusz
Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015
E3S Web of Conferences
author_facet Downar-Zapolska Laura
Głowacki Tadeusz
author_sort Downar-Zapolska Laura
title Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015
title_short Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015
title_full Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015
title_fullStr Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015
title_full_unstemmed Map of the terminal moraine of the Werenskioldbreen glacier (South-West Spitsbergen) from 2015
title_sort map of the terminal moraine of the werenskioldbreen glacier (south-west spitsbergen) from 2015
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2018-01-01
description The first direct field measurement of the entire terminal moraine of the Werenskioldbreen glacier on Spitsbergen took place at the end of July and the beginning of August 2015. The results of the measurements were the basis for the development of the large-scale terminal moraine map. The article presents the stages of map creation and editing based on measurement points established by the GNSS method. The map editing required knowledge of the morphologically complex terrain. Key documentation was field notes and documentary photographs, enabling the cartographic interpretation of the varied topographic features of the terrain's surface. Based on the documentation, the water bodies on the moraine were located, the outline of the structure and the boundary points were executed and the latter were excluded from the triangulation process. The glacial river was also excluded from triangulation, which allowed a DTM to be developed. An important step in point cloud mapping was to generate a topologically correct digital elevation model of satisfactory accuracy. On the basis of the DTM, contour lines were generated showing the topographic features of the terrain's surface. The printable resultant map's scale is 1: 5000; it is in the UTM coordinate system, in the 33X zone. Complementing the content of the map, a grid of geographic coordinates, a kilometer grid, and map key descriptions were added.
url https://doi.org/10.1051/e3sconf/20182900029
work_keys_str_mv AT downarzapolskalaura mapoftheterminalmoraineofthewerenskioldbreenglaciersouthwestspitsbergenfrom2015
AT głowackitadeusz mapoftheterminalmoraineofthewerenskioldbreenglaciersouthwestspitsbergenfrom2015
_version_ 1724312607327780864