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Horizons in earth science research. Volume 7 /
| Clasificación: | Libro Electrónico |
|---|---|
| Otros Autores: | , |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
New York :
Nova Science Publishers, Inc.,
2012.
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| Temas: | |
| Acceso en línea: | Texto completo |
Tabla de Contenidos:
- HORIZONS IN EARTH SCIENCE RESEARCH. VOLUME 7; HORIZONS IN EARTH SCIENCE RESEARCH. VOLUME 7; Library of Congress Cataloging-in-Publication Data; CONTENTS; PREFACE; Chapter 1: GLACIAL EROSION AND KARST EVOLUTION (KARREN FORMATION ON THE SURFACES FORMED BY GLACIERS); ABSTRACT; 1. INTRODUCTION; 2. LANDFORMS CREATED BY GLACIERS; 3. LANDFORMS OF GLACIALLY TRANSFORMED AREAS; 4. RELATONSHIP BETWEEN ICE AND KARSTIFICATION; 4.1. The Influence of Karstification on Glaciersand Their Geomorphic Action; 4.2. The Impact of Ice on Karstification; 5. KARSTIC SURFACES TYPES TRANSFORMED BY GLACIERS.
- 5.1. Surfaces of Roches Moutonnées5.2. Planar Surfaces; 5.3. Surfaces with Dolines and Uvalas; 5.4. Surfaces Dissected by Glacial Troughs to a Smaller Degree; 5.5. Large Glacial trough with Rock Basins; 5.6. Glacial troughs with Giant Dolines and Uvalas; 5.7. Glacial Troughs; 5.8. Surfaces with Cirques; 5.9. Surfaces with Combe-Ridges; 6. KARSTIFICATION ON GLACIAL SURFACES AND LANDFORMS; 6.1. Karren Formation; 6.2. Karstification on Surfaces with Dolines and Uvalas; 6.3. Evolution of Depressions of the Superficial Deposit; 6.4. Karstification in a Cirque Valley.
- 6.5. Karstification in Glacier Valleys (Troughs)6.6. Cavity Formation; 7. GLACIOKARST ENVIRONMENTS; CONCLUSION; REFERENCES; Chapter 2: GEOMETRY OF CORONAL RAYS; ABSTRACT; 1. INTRODUCTION; 2. CORONAL STREAMERS IN THE COURSE OF THE SOLAR CYCLE; 3. GEOMETRY OF POLAR PLUMES; 4. SPIRALITY OF CORONAL RAYS; 5. DEFLECTION OF CORONAL RAYS BY REMOTECORONAL MASS EJECTIONS; 6. JETS; CONCLUSION; REFERENCES; Chapter 3: ESTONIAN DOLOMITES: OCCURRENCE, RESOURCES, CHARACTERISATION AND NEW PROSPECTS FOR APPLICATION; ABSTRACT.
- GEOLOGICAL OCCURRENCE AND CHARACTERISATION OFDOLOMITE RESOURCES IN ESTONIA AND THEIR APPLICATIONCHEMICAL AND THERMAL PROPERTIES OF DOLOMITES; DOLOMITES AS SORBENTS FOR SO2; CONCLUSION; DOLOMITES IN CALCINATION/CARBONATION LOOP FOR CCS; CONCLUSION; APPLICATION OF DOLOMITES IN THE MODIFICATION OFN-CONTAINING FERTILISERS BASED ON AMMONIUM NITRATE; CONCLUSION; SUMMARY; ACKNOWLEDGMENTS; REFERENCES.
- Chapter 4: THE EARLY AND LATE GLACIAL HIGHMOUNTAIN GLACIATION SURROUNDING TIBETAS TOPOGRAPHIC-CLIMATIC CAUSEOF HIGH-ENERGETIC GLACIAL LAKEOUTBURST FLOODS (GLOFS) AND THEIRSEDIMENTOLOGICAL CONSEQUENCESIN THE LOWER MOUNTAIN FORELANDSABSTRACT; 1. PRINCIPLE OF ACTUALISM VERSUS CONSTELLATIONAND THE PROPORTION OF SNOWLINE DEPRESSIONIN THE MOUNTAIN RELIEF AND EXTENT OF GLACIATION; 2. THE GLACIAL GLACIER HISTORY (LAST GLACIAL MAXIMUM(LGM) OR LAST GLACIAL PERIOD (LGP)) OF TIBET AND ITSSURROUNDING MOUNTAINS WITH THEIR IMPORTANCE TO ICEDAMMEDLAKES AND GLACIAL LAKE OUTBURST FLOODS (GLOFS)