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Publication Date

2008

Publication Title

Acta Carsologica

Volume Number

37

Issue Number

1

Abstract

Throughout the center of Saudi Arabia the anhydrite upper Jurassic Heeth formation can be followed N to S. Locally it is punctured by hypogene karst sinkholes. The most prominent are the former Layla Lakes at 22.17N 46.70E. The lakes (17 originally) have been drained in the late 1980's, revealing 19 sinkholes, some of them composites of several subsidence centers. The largest is 1.1 km long, 0.4 km wide and about 40 m deep. Others are less than 10 m across and rather recent. The bottom of the former lakes and the flats around them are composed of thick layers of fine-grained lake chalks. The most striking feature of these sinkholes is the several meters thick tufa covering the vertical walls of the sinkholes. It formed subaqueous and is entirely composed of gypsum. Morphologically the tufa displays thick bulbous forms at the bottom changing to conical forms at middle depth to gour-, gutter-, or shovel-like forms near to the former lake surface. The mineralogy and morphology of this tufa appear to be singular world-wide.

Keywords

Heeth Formation, Hypogene karst, Sinkholes, Tufa, Gypsum tufa, Paleolakes

Geographic Subject

Layla Lakes (Saudi Arabia)

Document Type

Article

Language

English and Slovenian

Identifier

K26-00159

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Article Location

 
COinS

Latitude

22.1362925

Longitude

46.6986302
 
 

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