vasily chuvardinsky (14 resultados)

Condición: New.

Taschenbuch. Condición: Neu. Latepaleozoic and Quaternary glacial periods. Discrown of glacial theory | Vasily Chuvardinsky | Taschenbuch | 68 S. | Englisch | 2018 | LAP LAMBERT Academic Publishing | EAN 9786139846955 | Verantwortliche Person für die EU: BoD - Books on Demand, In de Tarpen 42, 22848 Norderstedt, info[at]bod[dot]de | Anbieter: preigu.

Condición: New.

Taschenbuch. Condición: Neu. Quaternary relief on the Baltic Shield | Continental glacier or fault neotectonics? | Vasily Chuvardinsky | Taschenbuch | 132 S. | Englisch | 2014 | LAP LAMBERT Academic Publishing | EAN 9783659536250 | Verantwortliche Person für die EU: BoD - Books on Demand, In de Tarpen 42, 22848 Norderstedt, info[at]bod[dot]de | Anbieter: preigu.

paperback. Condición: New. NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Taschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The geological features of the Permo-Carboniferous glaciation are based on the same criteria as for the Quaternary glaciation. The author's many years of research have proved that the 'exaration' types of the relief of the Quaternary fiords, skerries, lake basins in bedrock, drumlins, foreheads, polished rocks, furrows on bedrock - all this formed by the disjunctive dislocations. They occupy their normal place in the ensemble of paragenetic structures that accompany faulting. Extremly favorable conditions for the development of terrestrial vegetation were created in the Carboniferous period. And the climate of the Permian period was generally the warmest of the formerly dominant Paleozoic. The results of the drilling land ice (up to subglacial surface) in Antarctica and Greenland are of special, unique importance. It turned out that instead of moraine-containing ice mass, as if filled with huge blocks and boulders,only inclusions of sandy-loamy and fine-earth substance are recorded in the continental ice. An important function of glaciers is the conservation of the subglacial geological-topographic surface. 68 pp. Englisch.

Taschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware 68 pp. Englisch.

Taschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The author proposes reconsidering some of the fundamental issues of the Quaternary period. Based on own many-year long research carried out on the Baltic Shield, the author proves the fault-tectonic origin of such forms of the glacial exaration relief as roches moutonnes, fjords, etc. Referred by many to glacial accumulation, these land forms have actually emerged due to fault-folding processes. As has been shown by deep drilling of glaciers in the Antarctic and Greenland, the continental ice does not contain any boulders, but only trace amounts of dust-like substance. Since the lower strata are not involved in the general movement of glaciers, they conserve the glacier beds. In order to reveal the mechanism of boulder deposits formation, one should consider the actual geological processes, fault tectonic ones in the first place. The book is intended for geologists, geomorphologists, geographers, as well as general readers. 132 pp. Englisch.

Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The geological features of the Permo-Carboniferous glaciation are based on the same criteria as for the Quaternary glaciation. The author's many years of research have proved that the 'exaration' types of the relief of the Quaternary fiords, skerries, lake basins in bedrock, drumlins, foreheads, polished rocks, furrows on bedrock - all this formed by the disjunctive dislocations. They occupy their normal place in the ensemble of paragenetic structures that accompany faulting. Extremly favorable conditions for the development of terrestrial vegetation were created in the Carboniferous period. And the climate of the Permian period was generally the warmest of the formerly dominant Paleozoic. The results of the drilling land ice (up to subglacial surface) in Antarctica and Greenland are of special, unique importance. It turned out that instead of moraine-containing ice mass, as if filled with huge blocks and boulders,only inclusions of sandy-loamy and fine-earth substance are recorded in the continental ice. An important function of glaciers is the conservation of the subglacial geological-topographic surface.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 68 pp. Englisch.

Taschenbuch. Condición: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The geological features of the Permo-Carboniferous glaciation are based on the same criteria as for the Quaternary glaciation. The author's many years of research have proved that the 'exaration' types of the relief of the Quaternary fiords, skerries, lake basins in bedrock, drumlins, foreheads, polished rocks, furrows on bedrock - all this formed by the disjunctive dislocations. They occupy their normal place in the ensemble of paragenetic structures that accompany faulting. Extremly favorable conditions for the development of terrestrial vegetation were created in the Carboniferous period. And the climate of the Permian period was generally the warmest of the formerly dominant Paleozoic. The results of the drilling land ice (up to subglacial surface) in Antarctica and Greenland are of special, unique importance. It turned out that instead of moraine-containing ice mass, as if filled with huge blocks and boulders,only inclusions of sandy-loamy and fine-earth substance are recorded in the continental ice. An important function of glaciers is the conservation of the subglacial geological-topographic surface.

Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The geological features of the Permo-Carboniferous glaciation are based on the same criteria as for the Quaternary glaciation. The author's many years of research have proved that the 'exaration' types of the relief of the Quaternary fiords, skerries, lake basins in bedrock, drumlins, foreheads, polished rocks, furrows on bedrock - all this formed by the disjunctive dislocations. They occupy their normal place in the ensemble of paragenetic structures that accompany faulting. Extremly favorable conditions for the development of terrestrial vegetation were created in the Carboniferous period. And the climate of the Permian period was generally the warmest of the formerly dominant Paleozoic. The results of the drilling land ice (up to subglacial surface) in Antarctica and Greenland are of special, unique importance. It turned out that instead of moraine-containing ice mass, as if filled with huge blocks and boulders,only inclusions of sandy-loamy and fine-earth substance are recorded in the continental ice. An important function of glaciers is the conservation of the subglacial geological-topographic surface.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 68 pp. Englisch.

Taschenbuch. Condición: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering.

Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The author proposes reconsidering some of the fundamental issues of the Quaternary period. Based on own many-year long research carried out on the Baltic Shield, the author proves the fault-tectonic origin of such forms of the 'glacial exaration' relief as roches moutonnes, fjords, etc. Referred by many to glacial accumulation, these land forms have actually emerged due to fault-folding processes. As has been shown by deep drilling of glaciers in the Antarctic and Greenland, the continental ice does not contain any boulders, but only trace amounts of dust-like substance. Since the lower strata are not involved in the general movement of glaciers, they conserve the glacier beds. In order to reveal the mechanism of boulder deposits formation, one should consider the actual geological processes, fault tectonic ones in the first place. The book is intended for geologists, geomorphologists, geographers, as well as general readers.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 132 pp. Englisch.

Taschenbuch. Condición: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The author proposes reconsidering some of the fundamental issues of the Quaternary period. Based on own many-year long research carried out on the Baltic Shield, the author proves the fault-tectonic origin of such forms of the glacial exaration relief as roches moutonnes, fjords, etc. Referred by many to glacial accumulation, these land forms have actually emerged due to fault-folding processes. As has been shown by deep drilling of glaciers in the Antarctic and Greenland, the continental ice does not contain any boulders, but only trace amounts of dust-like substance. Since the lower strata are not involved in the general movement of glaciers, they conserve the glacier beds. In order to reveal the mechanism of boulder deposits formation, one should consider the actual geological processes, fault tectonic ones in the first place. The book is intended for geologists, geomorphologists, geographers, as well as general readers.