Three Cavern Pictures
Limestone caverns are natural subterranean runway voids which have been selectively formed below upland areas at one or more levels in limestone strata. Fundamentally they are forms resulting from water drainage through limestone beneath the surface. They had their origin in the insidious percolatio...
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1928
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ftusouthflorida:oai:digitalcommons.usf.edu:kip_articles-6409 2023-09-05T13:18:46+02:00 Three Cavern Pictures Malott, Clyde A. 1928-01-01T08:00:00Z https://digitalcommons.usf.edu/kip_articles/5410 https://journals.iupui.edu/index.php/ias/article/view/5002 unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/kip_articles/5410 https://journals.iupui.edu/index.php/ias/article/view/5002 KIP Articles Limestone Caverns Pictures Groundwater text 1928 ftusouthflorida 2023-08-13T16:27:33Z Limestone caverns are natural subterranean runway voids which have been selectively formed below upland areas at one or more levels in limestone strata. Fundamentally they are forms resulting from water drainage through limestone beneath the surface. They had their origin in the insidious percolation of groundwaters along structural controllines, such as joints and bedding planes. These waters, charged with carbonic acid, dissolved runways sufficiently large to permit streams to freely follow them, and the runways thus initiated have been further dissolved out and eroded by the streams which coursed through them. Text Carbonic acid University of South Florida St. Petersburg: Digital USFSP |
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Open Polar |
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University of South Florida St. Petersburg: Digital USFSP |
op_collection_id |
ftusouthflorida |
language |
unknown |
topic |
Limestone Caverns Pictures Groundwater |
spellingShingle |
Limestone Caverns Pictures Groundwater Malott, Clyde A. Three Cavern Pictures |
topic_facet |
Limestone Caverns Pictures Groundwater |
description |
Limestone caverns are natural subterranean runway voids which have been selectively formed below upland areas at one or more levels in limestone strata. Fundamentally they are forms resulting from water drainage through limestone beneath the surface. They had their origin in the insidious percolation of groundwaters along structural controllines, such as joints and bedding planes. These waters, charged with carbonic acid, dissolved runways sufficiently large to permit streams to freely follow them, and the runways thus initiated have been further dissolved out and eroded by the streams which coursed through them. |
format |
Text |
author |
Malott, Clyde A. |
author_facet |
Malott, Clyde A. |
author_sort |
Malott, Clyde A. |
title |
Three Cavern Pictures |
title_short |
Three Cavern Pictures |
title_full |
Three Cavern Pictures |
title_fullStr |
Three Cavern Pictures |
title_full_unstemmed |
Three Cavern Pictures |
title_sort |
three cavern pictures |
publisher |
Digital Commons @ University of South Florida |
publishDate |
1928 |
url |
https://digitalcommons.usf.edu/kip_articles/5410 https://journals.iupui.edu/index.php/ias/article/view/5002 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_source |
KIP Articles |
op_relation |
https://digitalcommons.usf.edu/kip_articles/5410 https://journals.iupui.edu/index.php/ias/article/view/5002 |
_version_ |
1776199650737389568 |