Interaction between the Epikarst and Surface Karstification (Case Studies): Advances in Karst Science
Autor Márton Veressen Limba Engleză Hardback – 23 oct 2024
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Specificații
ISBN-13: 9783031699351
ISBN-10: 3031699351
Pagini: 150
Ilustrații: Approx. 150 p. 130 illus., 50 illus. in color.
Dimensiuni: 210 x 279 mm
Ediția:2024
Editura: Springer Nature Switzerland
Colecția Springer
Seria Advances in Karst Science
Locul publicării:Cham, Switzerland
ISBN-10: 3031699351
Pagini: 150
Ilustrații: Approx. 150 p. 130 illus., 50 illus. in color.
Dimensiuni: 210 x 279 mm
Ediția:2024
Editura: Springer Nature Switzerland
Colecția Springer
Seria Advances in Karst Science
Locul publicării:Cham, Switzerland
Cuprins
Chapter 1: The Epikarst.- Chapter 2: Sediment Structure Of Subsidence Dolines (Sinkholes).- Chapter 3: The Development Of Epikarst And Dolines In The Bakony Region (Hungary).- Chapter 4: Truncated Epikarst On Glaciokarst.- Chapter 5: Karstification Of Plate-Shaped Dolines (Răchite, Padis, Romania).- Chapter 6: Denuding Epikarst On Dolomite (Environs Of Veszprém, The Bakony Region).- Chapter 7: Epikarst With Grikes – Tropical Karren Of Bemaraha Type.
Notă biografică
Márton Veress
He is a biology-geography secondary school teacher. Between 1969 and 1984 he worked in public education and from 1984 to 2016 (until retirement) at Berzsenyi Dániel College (and at its institutions of legal successor). He obtained PhD in 1997 and DsC in 2004 and habilitated in 2001. He was the head of the Department of Geography and Department of Physical Geography for several periods. He was the head of the Institute of Geography and Environmental Science and the dean of the Faculty of Natural Sciences for several periods. For some years he was the head of the Doctorate School of Environmental Science. At present he is Professor Emeritus.
His research area is karst, he studied mainly covered karst, karren and glaciokarst. In addition, he also deals with the modelling of karst. His field researches involved the Bakony Mountains (Hungary), the karsts of the Alps and the Dinarides. During his expeditions he also investigated the karsts of South China, Turkey, Madagascar, Chile (the island of Diego de almagro) and Russia (Lena). The number of his articles is 180, the number of his monographs and book chapters is 45 (23 are in English language). He is a member of the Editorial Board at Springer Publisher and Editor-in Chief of the Journal of Karsztfejlődés.
He is a biology-geography secondary school teacher. Between 1969 and 1984 he worked in public education and from 1984 to 2016 (until retirement) at Berzsenyi Dániel College (and at its institutions of legal successor). He obtained PhD in 1997 and DsC in 2004 and habilitated in 2001. He was the head of the Department of Geography and Department of Physical Geography for several periods. He was the head of the Institute of Geography and Environmental Science and the dean of the Faculty of Natural Sciences for several periods. For some years he was the head of the Doctorate School of Environmental Science. At present he is Professor Emeritus.
His research area is karst, he studied mainly covered karst, karren and glaciokarst. In addition, he also deals with the modelling of karst. His field researches involved the Bakony Mountains (Hungary), the karsts of the Alps and the Dinarides. During his expeditions he also investigated the karsts of South China, Turkey, Madagascar, Chile (the island of Diego de almagro) and Russia (Lena). The number of his articles is 180, the number of his monographs and book chapters is 45 (23 are in English language). He is a member of the Editorial Board at Springer Publisher and Editor-in Chief of the Journal of Karsztfejlődés.
Textul de pe ultima copertă
The book deals with the relationship and interaction between epikarst and surface karstification in seven chapters. The focus of the book is the development of the epikarst of different karst types and the genetics between the epikarst and landscape features. Chapter 1 gives a general description on the epikarst. Chapter 2 describes the sediment structure of subsidence dolines and interprets their development. It illustrates the interaction between the epikarst and surface karstification in different environments and rocks, which is primarily based on geoelectric resistance data of the bedrock of the karst. The investigations include covered karsts (Chapters 3 and 4), glaciokarsts (Chapter 4), a dolomite terrain (Chapter 6) and tropical karren (Chapter 7).
Caracteristici
Illustrates with real examples in different environments and rocks Presents new interpretation of the development of karst features Provide useful guidance for environmental protection