Titlebook: Landscapes and Landforms of Botswana; Frank D. Eckardt Book 2022 Springer Nature Switzerland AG 2022 Geomorphology of Botswana.Botswana la

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Julius Atlhopheng,Read Brown Mthanganyika Mapeo,Frank D. Eckardt

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Irka Schüller,Lukas Belz,Heinz Wilkes,Achim Wehrmann

Carcinogenesis

The Okavango Delta Peatlands,ts. Once thus colonised, peat production is accelerated due to the higher productivity and less easily decomposed tissue of emergent plants compared to submerged and floating-leaved plants. In backswamp settings, the floating mats are extensive (hundreds of square metres to hectares) and lead to the

愤怒事实

Landscape Evolution of the Lake Ngami and Mababe Depressions Within the Okavango Rift Zone, North-C palaeo-shorelines at ca. 936 m were formed on numerous occasions within the last 100 ka due to climatic conditions and feedback factors. Hence controversies revolve around possible dates and palaeo-climatic conditions for shoreline formation. Preliminary work on basin sediments suggests that palaeo

Flu表流动

Landscapes and Landforms of the Chobe Enclave, Northern Botswana,several ecoregions from tropical and subtropical grasslands to savannas and shrubland biomes. The hydrological cycle in the northern Chobe Enclave is governed by a complex interplay between the Okavango, Kwando, and Upper Zambezi drainage basins, which originate from tropical watersheds of the Angol

lipids

The Chobe-Zambezi Channel-Floodplain System: Anatomy of a Wetland in a Dryland,el-like depressions) all widespread. Collectively, these fluvial landforms create the physical template for shorter-term water, sediment and ecosystem dynamics. A strong flood and drying season dynamic is evident; river stages typically rise from January and peak around April, before subsequently fa

修饰语

Kalahari Pans: Quaternary Evolution and Processes of Ephemeral Lakes,stic feature of many small Kalahari pans, resulted from temporary phases of significant aeolian sediment transport. However, there is no hint of longer sedimentation gaps or significant periods of erosion. The prevailing depositional processes contradict the former assumption that deflation is the m

PET-scan

Landscape Evolution of the Stampriet Transboundary Basin and Relation to the Groundwater System: The of water at the surface and pan sediment chemistry and also reduces the potential for deflation and abrasion of the surface by the wind. The main geomorphological components of the STAS region are the dunes and sand sheet cover of the Kalahari Erg, dry valleys and ephemeral rivers, pans, and calcr

演讲

anachronistic

Geomorphology and Landscapes of the Limpopo River System,ory into the Limpopo are strongly affected by human activity, including river damming and groundwater abstraction. This significantly impacts on river discharge and thus sediment dynamics. The net outcome is that there is limited streamwise sediment connectivity through these tributaries and thus th