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Articles

Geomorphological and Geoecological Controls and Processes Following Gully Development in Alpine Mires, Lesotho

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Pages 49-58 | Published online: 28 Jan 2018

Figures & data

FIGURE 1. Study sites in eastern Lesotho and topographic setting of mire 1

FIGURE 1. Study sites in eastern Lesotho and topographic setting of mire 1

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)

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)

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)

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

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

FIGURE 7. Soil moisture profiles across mire 1 during summer (Feb.) and winter (July) 2001

FIGURE 7. Soil moisture profiles across mire 1 during summer (Feb.) and winter (July) 2001

FIGURE 8. A biological transect across mire 1

FIGURE 8. A biological transect across mire 1

FIGURE 9. A vegetational transect across mire 2

FIGURE 9. A vegetational transect across mire 2

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

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