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ABSTRACT. In this article I examine a range of issues raised in recent geographical studies of land reform. I briefly discuss the career of land reform, review a selection of geographical publications on land reform in a range of places in the global south and even the global north, note some prominent themes and silences, and raise points for discussion and debate about the direction a geography‐of‐land‐reform literature might take. My aim is to help geographers who are interested in land reform identify ways in which they might more purposively develop a literature that heretofore has not been considered a whole.  相似文献   
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A sequence of Middle Pleistocene (approximately early 'Cromerian Complex') sediments has been subdivided into subglacial, proximal glaciomarine, distal glaciomarine and marine facies. The subglacial facies represents lodgement till deposited during the final stages of ice-sheet advance. At the onset of ice-sheet retreat, streams deposited their load into a shallow-water; glaciomarine environment; gravelly sediments immediately in front of the ice-grounding line and finer material, in suspension, to more distal areas. Ice-rafting, slumping and traction currents were also active within the glaciomarine environment. The lithofacies characteristics of this sequence are consistent with deposition from a grounded tidewater ice-sheet. The glacigenic succession is restricted to the Forth Approaches area, which implies that the ice-sheet had a limited offshore extent.  相似文献   
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