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Science

Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard

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Pages 239-251 | Received 30 Aug 2016, Accepted 09 Feb 2017, Published online: 09 Mar 2017

Figures & data

Figure 1. Location of the study area with extent of the Main Map 1 marked in red. Basemap data and background satellite imagery provided by © Norsk Polar Institute (http://www.npolar.no).

Figure 1. Location of the study area with extent of the Main Map 1 marked in red. Basemap data and background satellite imagery provided by © Norsk Polar Institute (http://www.npolar.no).

Figure 2. Geological map of the study area. The map is based on Geological Map of Svalbard 1:250,000 provided by © Norsk Polar Institute (http://geodata.npolar.no).

Figure 2. Geological map of the study area. The map is based on Geological Map of Svalbard 1:250,000 provided by © Norsk Polar Institute (http://geodata.npolar.no).

Figure 3. Examples of fluvial-flow-dominated fan surface morphology: (a) ground-based view of active and older inactive braided channels visible on the fan surface; (b) orthophoto of braided pattern of fluvial channels; (c) fluvial-flow-dominated fan with incised channel in the most proximal part and a network of active and older inactive braided channels in a more distal one. Note also that large part of this fan is vegetated.

Figure 3. Examples of fluvial-flow-dominated fan surface morphology: (a) ground-based view of active and older inactive braided channels visible on the fan surface; (b) orthophoto of braided pattern of fluvial channels; (c) fluvial-flow-dominated fan with incised channel in the most proximal part and a network of active and older inactive braided channels in a more distal one. Note also that large part of this fan is vegetated.

Figure 4. Examples of debris-flow-dominated fan surface morphology: (a) ground view of recent debris flow channel; (b) orthophoto of the debris-flow-dominated fan depicting a dense network of recent (‘fresh’) and older debris flow channels and lobes (c) ground view of older, partly levelled, debris flow channels.

Figure 4. Examples of debris-flow-dominated fan surface morphology: (a) ground view of recent debris flow channel; (b) orthophoto of the debris-flow-dominated fan depicting a dense network of recent (‘fresh’) and older debris flow channels and lobes (c) ground view of older, partly levelled, debris flow channels.

Figure 5. Examples of colluvial fan surface morphology: (a) oblique view of short and steep colluvial fans located along the fjord margin; (b) an NIR (false colour: Near Infrared – Red – Green) composite satellite image of a colluvial fan with recently modified areas emphasized by a light grey colour. The older parts of the fan are shown in green. Note also that the inactive parts of the slope between fans are vegetated and therefore highlighted in near-infrared (red in the image). Source: © Digital Globe; (c) ground-view of coalescing colluvial fans.

Figure 5. Examples of colluvial fan surface morphology: (a) oblique view of short and steep colluvial fans located along the fjord margin; (b) an NIR (false colour: Near Infrared – Red – Green) composite satellite image of a colluvial fan with recently modified areas emphasized by a light grey colour. The older parts of the fan are shown in green. Note also that the inactive parts of the slope between fans are vegetated and therefore highlighted in near-infrared (red in the image). Source: © Digital Globe; (c) ground-view of coalescing colluvial fans.

Table 1. Definitions, types and units, range of values and source of calculated morphometric properties of fans and their catchment areas.

Table 2. Outcomes of morphometric features per fan type for fans located in Petuniabukta region, Svalbard – Part I.

Table 3. Outcomes of morphometric features per fan type for fans located in Petuniabukta region, Svalbard – Part II.

Figure 6. The lithology of the catchments of colluvial and alluvial fans in Petuniabukta.

Note: ‘dominated’ – means that the specified lithological unit occupied more than 50% of the catchment area; ‘and other’ – means that each of the specified lithological units occupied less than 50% of the catchment area.
Figure 6. The lithology of the catchments of colluvial and alluvial fans in Petuniabukta.
Supplemental material

Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard.pdf

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