{"database":"biostudies-literature","file_versions":[],"scores":null,"additional":{"submitter":["Sanders D"],"funding":["Austrian Science Fund FWF"],"pagination":["2099-2130"],"full_dataset_link":["https://www.ebi.ac.uk/biostudies/studies/S-EPMC9541593"],"repository":["biostudies-literature"],"omics_type":["Unknown"],"volume":["69(5)"],"pubmed_abstract":["Whereas deposits of extremely-rapid, 'catastrophic' mass wastings >10<sup>5</sup> m<sup>3</sup> in volume (for example, the Marocche di Dro rock avalanche in the Southern Alps and the Flims rockslide in the Western Alps) are easily recognized by their sheer mass and blocky surface, the identification of <i>fossil</i> catastrophic mass wastings partly removed by erosion must be based on deposit characteristics. Herein, a 'fossil' (pre-last glacial) rock avalanche, previously interpreted as either a till or debris flow, is described. The deposit, informally called 'Rubble Breccia', is located in the intramontane Campo Imperatore halfgraben that is bounded by a master fault with up to <i>ca</i> 900 m topographic throw. Based on documentation from field to thin section, and by comparative anal"],"journal":["Sedimentology"],"pubmed_title":["Identification of a Quaternary rock avalanche deposit (Central Apennines, Italy): Significance for recognition of fossil catastrophic mass-wasting."],"pmcid":["PMC9541593"],"funding_grant_id":["Y 1162"],"pubmed_authors":["Ortner H","Dendorfer T","Moseley GE","Steidle S","Sanders D","Edwards RL"],"additional_accession":[]},"is_claimable":false,"name":"Identification of a Quaternary rock avalanche deposit (Central Apennines, Italy): Significance for recognition of fossil catastrophic mass-wasting.","description":"Whereas deposits of extremely-rapid, 'catastrophic' mass wastings >10<sup>5</sup> m<sup>3</sup> in volume (for example, the Marocche di Dro rock avalanche in the Southern Alps and the Flims rockslide in the Western Alps) are easily recognized by their sheer mass and blocky surface, the identification of <i>fossil</i> catastrophic mass wastings partly removed by erosion must be based on deposit characteristics. Herein, a 'fossil' (pre-last glacial) rock avalanche, previously interpreted as either a till or debris flow, is described. The deposit, informally called 'Rubble Breccia', is located in the intramontane Campo Imperatore halfgraben that is bounded by a master fault with up to <i>ca</i> 900 m topographic throw. Based on documentation from field to thin section, and by comparative anal","dates":{"release":"2022-01-01T00:00:00Z","publication":"2022 Aug","modification":"2025-04-19T06:45:07.492Z","creation":"2025-04-19T06:45:07.492Z"},"accession":"S-EPMC9541593","cross_references":{"pubmed":["36248773"],"doi":["10.1111/sed.12984"]}}