Figures & data
FIGURE 2. Gully denudation and aggradation for peat and mineral sediment surfaces (January 2000 to July 2001)
![FIGURE 2. Gully denudation and aggradation for peat and mineral sediment surfaces (January 2000 to July 2001)](/cms/asset/53998e3d-deae-4439-a740-b8949818b5ca/uaar_a_11956970_f0002.gif)
FIGURE 3. Otomys burrows and pathways within the peat horizon of a north-facing gully sidewall (gully depth ∼120 cm)
![FIGURE 3. Otomys burrows and pathways within the peat horizon of a north-facing gully sidewall (gully depth ∼120 cm)](/cms/asset/4a09c24a-409c-405b-bacd-5553831f664f/uaar_a_11956970_f0003.gif)
FIGURE 4. Cracked peat surfaces along gully sidewalls and adjacent areas. The cracks are infilled with sediment transported by wind and water (gully depth ∼3 m; width = 3–4 m)
![FIGURE 4. Cracked peat surfaces along gully sidewalls and adjacent areas. The cracks are infilled with sediment transported by wind and water (gully depth ∼3 m; width = 3–4 m)](/cms/asset/3cfbf048-47b7-403a-8391-e2cd4ac89b6d/uaar_a_11956970_f0004.gif)
FIGURE 5. Particle size distribution for peat and mineral sediment and for a desiccation crack infill
![FIGURE 5. Particle size distribution for peat and mineral sediment and for a desiccation crack infill](/cms/asset/a0439e11-72d5-4ab1-8665-4df2dbfa0881/uaar_a_11956970_f0005.gif)
FIGURE 6. Ground thermal regime and associated horizontal particle movement for a north- and south-facing gully sidewall over 5 d in July 1999
![FIGURE 6. Ground thermal regime and associated horizontal particle movement for a north- and south-facing gully sidewall over 5 d in July 1999](/cms/asset/8897a50b-055f-4b12-9aff-499d7420fc2d/uaar_a_11956970_f0006.gif)
Table 1 Comparing shear strength values during February (summer) and July (winter) 1999 for various sedimentological settings (n = 30 per site). Percentage moisture and organics were measured in February