By Michael J. Lace, John E. Mylroie

Carbonate rock coasts are chanced on world-wide, from continental beaches of the Adriatic Sea of Europe to the Yucatan Peninsula of North the US, and on tropical islands from Rodrigues Island within the Indian Ocean, to the Mariana Islands within the Pacific Ocean, to the Bahama Islands within the Atlantic Ocean. Such coasts are popular for his or her strange and special karst landforms. Karst procedures, relatively these linked to coastal landforms, are proving to be strangely detailed and intricate.

This quantity provides a complete evaluation of the methods linked to coastal karst improvement evaluating examples from a wide geographical and geomorphological diversity of island and continental shoreline/paleoshoreline settings, together with a overview of pseudokarst strategies that could compete with and overprint dynamic coastal karst landscapes.

As potent administration of hydrologic assets grows extra advanced, coastal caves and karst symbolize basic parts in linked coastal aquifers, which within the rock checklist may also shape major petroleum reservoirs.

Audience through supplying a clearer figuring out of the geological, organic, archaeological and cultural worth of coastal caves and karst assets, this quantity deals a severe device to coastal researchers and geoscientists in similar fields and to coastal land managers because it illustrates the range of coastal karst landforms, the original procedures which shaped them, the variety of assets they harbor and their dating to coastal quarter protection techniques and the advance of sustainable administration approaches.

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Extra info for Coastal Karst Landforms

Example text

Both the centimeter-scale karren and meter-scale pinnacles have been assigned many different terms over the past few decades. Some of the synonyms include champignon surface (Stoddart et al. 1971), phytokarst (Folk et al. 1973), lacework morphology (Bull and Laverty 1982), etc. The term spitzkarren (Trudgill 1979) was also suggested, despite little similarity with spitzkarren originally described by B¨ogli (1960) (compare Trudgill’s Fig. 1 and B¨ogli’s Fig. 15). In recent years, the term eogenetic karren (Taboroˇsi et al.

Acceptance (Mylroie and Mylroie 2009; Lundberg 2009). This is based on an understanding that this type of karren is polygenetic and arises from a number of processes (including biocorrosion, wetting and drying, salt weathering and hydration, and salt spray and rain water mixing) that are superimposed on the highly heterogeneous texture and high primary porosity of diagenetically immature limestone. Eogenetic lithology is deemed to be the crucial factor controlling the development of this type of karren by making the rocks predisposed to the development of multitudes of irregular hollows and residual forms that accompany them (Taboroˇsi et al.

This is familiar from fractured coastal limestones, where cracks in the rock develop a darker hue due to being preferentially colonized by microbes (which respond to microenvironmental variations in shade and water availability) and give a web-like appearance to the rock surface (Fig. 5a). On more uniform rock surfaces, microbial colonization can be more haphazard and creates random dark patches that coalesce over time. Darker patches are often accompanied by a difference in microrelief, with depressions forming in places where the top layer of rock was colonized and gradually destroyed by microbes (Fig.

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Coastal Karst Landforms by Michael J. Lace, John E. Mylroie
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