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Recent developments in geomorphology research /

"Geomorphology is defined as the study of the physical features of the surface of the earth and their relation to its geological structures. Geomorphology is useful not only for understanding the surface evolution of Earth, but of other solid planetary bodies as well. This monograph comprises t...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Otros Autores: Reale, Ronald M. (Editor )
Formato: Electrónico eBook
Idioma:Inglés
Publicado: New York : Nova Science Publishers, [2020]
Colección:Earth sciences in the 21st century
Temas:
Acceso en línea:Texto completo

MARC

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245 0 0 |a Recent developments in geomorphology research /  |c Ronald M. Reale (editor). 
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264 1 |a New York :  |b Nova Science Publishers,  |c [2020] 
300 |a 1 online resource. 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
490 0 |a Earth sciences in the 21st century 
504 |a Includes bibliographical references and index. 
505 0 |a Geomorphology of the Campo de Calatrava volcanic field / Miguel Ángel Poblete Piedrabuena, Salvador Beato Bergua and José Luis Marino Alfonso -- Snow avalanches in the middle mountains of the Asturian Central Massif (Cantanbrian Mountains, nw of Spain) : an active nivoperiglacial process / Miguel Ángel Poblete Piedrabuena, Salvador Beato Bergua and José Luis Marino Alfonso -- Geomorphological analysis and erosion modelling of a Martian fluvial system / Vilmos Steinmann. 
520 |a "Geomorphology is defined as the study of the physical features of the surface of the earth and their relation to its geological structures. Geomorphology is useful not only for understanding the surface evolution of Earth, but of other solid planetary bodies as well. This monograph comprises three chapters, each detailing a specific recent development in geomorphology research. Chapter 1 describes the geomorphology of the Campo de Calatrava Volcanic Field in Central Spain, focusing on its volcanoes and the interference that any volcanic activity has produced in other forms of modeling and quaternary deposits. Chapter 2 analyzes the triggering of snow avalanches in the middle mountains of the Asturian Central Massif and their morphogenetic role in the dynamics and modeling of its slopes, a phenomenon that is impacted by the changing global climate. Chapter 3 analyzes the former fluvial erosion on Mars, adopting a model called SIMWE (SImulated Water Erosion) to recreate the geomorphological features observed on the planet today in an effort to understand its ancient climatic conditions"--  |c Provided by publisher. 
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700 1 |a Reale, Ronald M.,  |e editor. 
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