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Evolution of karst in the lower part...

Temovski, Marjan.

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Evolution of karst in the lower part of Crna Reka River Basin

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Evolution of karst in the lower part of Crna Reka River Basin/ by Marjan Temovski.
作者:	Temovski, Marjan.
出版者:	Cham :Springer International Publishing : : 2016.,
面頁冊數:	xiii, 265 p. :ill., map, digital ;24 cm.
內容註:	Introduction -- General overview of the research area -- Methodology -- Hypogenic cave development -- Epigenic cave development -- Characteristics of karst surface -- General conclusions -- Appendix A -- Appendix B.
Contained By:	Springer eBooks
標題:	Karst - Macedonia. -
電子資源:	http://dx.doi.org/10.1007/978-3-319-24547-8
ISBN:	9783319245478$q(electronic bk.)

Evolution of karst in the lower part of Crna Reka River Basin
Temovski, Marjan.

Evolution of karst in the lower part of Crna Reka River Basin[electronic resource] /by Marjan Temovski. - Cham :Springer International Publishing :2016. - xiii, 265 p. :ill., map, digital ;24 cm. - Springer theses,2190-5053. - Springer theses..

Introduction -- General overview of the research area -- Methodology -- Hypogenic cave development -- Epigenic cave development -- Characteristics of karst surface -- General conclusions -- Appendix A -- Appendix B.

This thesis addresses karst development in a terrain characterized by a highly complex geological and geomorphological evolution. It tackles the extent and complexity of both epigenic and hypogenic karst development, based on morphological analyses of caves, combined with analyses and datations of cave sediments and their correlation to regional geological and geomorphological evolution. Hypogenic karst registered is mainly the result of hydrothermal speleogenesis due to increased geothermal gradient in connection with nearby Pliocene-Pleistocene volcanic centers, with occurrence of sulfuric acid speleogenesis and ghost-rock weathering due to local geological or lithological control. Epigenic speleogenesis is strongly controlled by base level oscillations, with also examples of deep phreatic (now fossil) caves connected to regional base level rise, and per-ascensum speleogenesis. Another important finding is the constraining of the timing of Mariovo Lake draining in the Pleistocene, an important event in order to understand the geomorphological evolution in Macedonia, as it led to the onset of fluvial development and incision of valleys, shaping most of the present morphology.

ISBN: 9783319245478$q(electronic bk.)

Standard No.: 10.1007/978-3-319-24547-8doiSubjects--Topical Terms:

2179581
Karst
--Macedonia.

LC Class. No.: GB600.4.M33

Dewey Class. No.: 551.447094976

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