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Penck's major work on landform evolution was Die morphologischen Analyse (1924; Morphological Analysis of Land Forms, 1953).
However, biological communities may significantly control geomorphic processes and have strong impacts on landform dynamics.
Typical weathering profiles based on landform and climate are deduced, denoting typical engineering and hydrogeological behaviour.
At larger regional and continental scales, climatic imprints on landform development produce palimpsest landscapes that challenge interpretation.
The study area is divided into different Physiographic Land Units (PLU) based on landform, landuse and slope.
Thus, the magnitudes of SOC change across temperature gradients were non-uniform and depended on landform type.
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Relief shown by shading on landforms map.
The results are consistent with field observations on landforms and geology.
The in situ soils get their distinguishing features from the parent rocks, which are sieved by flowing water, sliding glaciers, and drifting wind and are deposited on landforms such as river valleys and coastal plains.
Impacts on landforms and habitats vary depending on the type of structure and its size, shape, orientation, type of materials used, age and state of repair.
Impacts on landforms include thermokarst subsidence, increased hillslope instability, enhanced fluvial and lacustrine erosion, ice wedge degradation, frost mound thawing, thaw lake expansion, and degradation of palsas.
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