Clastic Sediments in Caves – Imperfect Recorders of Processes in Karst

Clastic sediments have played an important role in deciphering geologic history and processes since the inception of the discipline. Early studies of caves applied stratigraphic principles to karst deposits. The majority of cave deposits are breakdown and alluvium. The alluvial materials have been s...

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Main Author: Ira D. Sasowsky
Format: Article
Language:English
Published: Slovenian Academy of Sciences and Arts 2007-04-01
Series:Acta Carsologica
Online Access:https://ojs.zrc-sazu.si/carsologica/article/view/216
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author Ira D. Sasowsky
author_facet Ira D. Sasowsky
author_sort Ira D. Sasowsky
collection DOAJ
description Clastic sediments have played an important role in deciphering geologic history and processes since the inception of the discipline. Early studies of caves applied stratigraphic principles to karst deposits. The majority of cave deposits are breakdown and alluvium. The alluvial materials have been successfully investigated to determine ages of caves, landscape evolution, paleoenvironmental conditions, and paleobiota. Rapid stage changes and the possibility of pipe-full flow make cave deposits different than surface deposits. This and other factors present difficulties with interpreting the cave record, but extended preservation is afforded by the “roofing” of deposits. Dating by magnetism or isotopes has been successful in many locations. Caves can be expected to persist for 10 Ma in a single erosive cycle; most cave sediments should be no older than this.
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spelling doaj.art-8413c39cec1f4d72a5593ea078f88ddf2023-02-07T17:49:17ZengSlovenian Academy of Sciences and ArtsActa Carsologica0583-60501580-26122007-04-0136110.3986/ac.v36i1.216202Clastic Sediments in Caves – Imperfect Recorders of Processes in KarstIra D. Sasowsky0Office for Terrestrial Records of Environmental Change, Department of Geology and Environmental Science, University of Akron, Akron, OH 44325-4101Clastic sediments have played an important role in deciphering geologic history and processes since the inception of the discipline. Early studies of caves applied stratigraphic principles to karst deposits. The majority of cave deposits are breakdown and alluvium. The alluvial materials have been successfully investigated to determine ages of caves, landscape evolution, paleoenvironmental conditions, and paleobiota. Rapid stage changes and the possibility of pipe-full flow make cave deposits different than surface deposits. This and other factors present difficulties with interpreting the cave record, but extended preservation is afforded by the “roofing” of deposits. Dating by magnetism or isotopes has been successful in many locations. Caves can be expected to persist for 10 Ma in a single erosive cycle; most cave sediments should be no older than this.https://ojs.zrc-sazu.si/carsologica/article/view/216
spellingShingle Ira D. Sasowsky
Clastic Sediments in Caves – Imperfect Recorders of Processes in Karst
Acta Carsologica
title Clastic Sediments in Caves – Imperfect Recorders of Processes in Karst
title_full Clastic Sediments in Caves – Imperfect Recorders of Processes in Karst
title_fullStr Clastic Sediments in Caves – Imperfect Recorders of Processes in Karst
title_full_unstemmed Clastic Sediments in Caves – Imperfect Recorders of Processes in Karst
title_short Clastic Sediments in Caves – Imperfect Recorders of Processes in Karst
title_sort clastic sediments in caves imperfect recorders of processes in karst
url https://ojs.zrc-sazu.si/carsologica/article/view/216
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