Glacial and periglacial geomorphology of central Troms and Finnmark county, Arctic Norway

被引:7
作者
Leigh, J. R. [1 ]
Evans, D. J. A. [1 ]
Stokes, C. R. [1 ]
Andreassen, L. M. [2 ]
Carr, R. J. [3 ]
机构
[1] Univ Durham, Dept Geog, Durham, England
[2] Norwegian Water Resources & Energy Directorate NV, Oslo, Norway
[3] Newcastle Univ, Sch Geog Polit & Sociol, Newcastle Upon Tyne, Tyne & Wear, England
基金
英国自然环境研究理事会;
关键词
Glacial geomorphology; periglacial geomorphology; remote sensing; Arctic; Norway; Scandinavian Ice Sheet; ROCK GLACIERS; HOLOCENE GLACIER; PROTALUS RAMPARTS; SOUTHERN NORWAY; NORTHERN NORWAY; ICE-SHEET; DIAGNOSTIC-CRITERIA; CENTRAL JOTUNHEIMEN; MELTWATER DRAINAGE; PLATEAU ICEFIELD;
D O I
10.1080/17445647.2021.1950580
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
Here we present a glacial and periglacial geomorphological map of a similar to 6800 km(2) region of central Troms and Finnmark county, Arctic Norway. The map is presented at a 1:115,000 scale with the aim of characterising the spatial distribution of glacial and periglacial landforms and facilitating the reconstruction of the glacial history of the region during the latter stages of deglaciation from the Last Glacial Maximum and into the Holocene. Mapping was conducted predominantly by manual digitisation of landforms using a combination of Sentinel-2A/2B satellite imagery (10 m pixel resolution), vertical aerial photographs (<1 m pixel resolution), and Digital Elevation Models (10 and 2 m pixel resolution). Over 20,000 individual features have been mapped and include moraines (subdivided into major and minor moraines), ridges within areas of discrete debris accumulations (DDAs), flutings, eskers, irregular mounded terrain, lineations, glacially streamlined bedrock, possible glacially streamlined terrain, pronival ramparts, rock glaciers (subdivided into valley wall and valley floor, and rock glacierised moraines), lithalsas, contemporary glaciers and lakes. The map records several noteworthy large moraine assemblages within individual valleys, forming inset sequences from pre-Younger Dryas limits up to the 2018/19 ice margins and represents a valuable dataset for reconstructing Holocene glacial and periglacial activity.
引用
收藏
页码:348 / 366
页数:19
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