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Dryland alluvial fans developed along the northern flanks of the Sierra Lisbona in the north-western Vera basin (Almería region, southeast Spain) display negligible amounts of incision despite distal base-level lowering of >30 m by the modern drainage network. The fans are of early-middle Quaternary age and are graded to a coeval river terrace, now isolated from the modern drainage network. The...
Nonpedogenic channel calcretes of up to 3.5 m thick occur in a number of locations across the Tabernas Basin in Almera Province, southeast Spain. They represent the last major phase of late Quaternary calcium carbonate cementation to affect this semiarid drainage basin. Channel calcretes are situated within the basal parts of sequences of <12-m-thick, poorly sorted, coarse-grained and schist-dominated...
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