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- W4381955193 abstract "Dry valleys and dells are abundant and well developed in regions of past periglaciation such as the Polish lowlands and English chalklands. Many valleys formed by water flowing on frozen ground or when water tables were higher, whereas dells probably formed by snowpatch erosion. Dry valleys often contain sediments attributed to solifluction, slopewash, fluvial, fluvio–colluvial or postglacial processes. In Poland, dry valleys formed on terrains glaciated during the penultimate (Saalian) to last (Weichselian) cold stage of the Pleistocene, whereas many chalkland valleys in England have likely developed over longer periods with repeated climate changes between periglacial and temperate conditions." @default.
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- W4381955193 date "2023-01-01" @default.
- W4381955193 modified "2023-09-23" @default.
- W4381955193 title "Dry valleys and dells" @default.
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