GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Physical geography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (903 pages)
    Edition: 1st ed.
    ISBN: 9783319533483
    Series Statement: Cave and Karst Systems of the World Series
    DDC: 551.447
    Language: English
    Note: Intro -- Preface -- Contents -- Contributors -- 1 Types and Settings of Hypogene Karst -- Abstract -- 1 Introduction -- 1.1 Genetic Types of Karst -- 1.2 Definitions of Hypogene Speleogenesis -- 1.3 Diversity of Hypogene Speleogenesis -- 2 Hydrogeologic Context of Hypogene Speleogenesis -- 2.1 Origin of Aqueous Fluids -- 2.2 Flow Regimes -- 2.2.1 Compactional Regime -- 2.2.2 Thermobaric Regime -- 2.2.3 Deep Endogenous Regime -- 2.2.4 Meteoric Regime -- 2.2.5 Other Flow Drives -- 2.2.6 The Nature, Evolution and Interaction of the Regimes -- 2.3 Endogenic Fluids in the Deep Crustal Settings and Their Connection to the Upper Crust -- 2.4 Hydrodynamic Zoning of the Upper Crust in Continents -- 2.4.1 Hydrogeologic Stories -- 2.4.2 Hierarchy of Gravitational Flow Systems -- 2.4.3 Hydrodynamic Zoning According to Circulation Intensity -- 2.4.4 Hydrodynamic Zoning According to Distribution of Fluid Pressure -- 2.4.5 Hydrodynamic Zoning According to Dominating Flow Regimes -- 3 Genetic Divisions of Hypogene Karst -- 3.1 Genetic Types According to Hydrodynamic Environments -- 3.2 Endokarst -- 4 Hypogene Karstification, Metasomatism and Weathering -- 4.1 Metasomatism -- 4.2 Metasomatism and Karstification -- 4.3 Ghost-Rock Karstification -- 4.4 Cavernous Decay Features: Tafoni and Honeycomb Structures -- 5 Settings of Hypogene Karst -- 5.1 Basin's Marginal Discharge Areas -- 5.2 Basin's Internal Areas -- 5.3 Anticlinal Folds and Uplifted Blocks -- 5.4 Zones of Deep-Rooted Faults -- 5.5 Young Disrupted Basins -- 5.6 Large Carbonate Platforms, Side-Open to the Ocean -- 5.7 Areas of Young Volcanism -- 6 Lithogeodynamic Perspective of Endogenous Hypogene Karstification -- 7 Outlook -- References -- Europe -- 2 Hypogenic Caves in the UK -- Abstract -- 1 Introduction -- 2 Northern England -- 2.1 The Alston Block -- 2.2 The Askrigg Block -- 3 The Peak District. , 4 Wales and the Forest of Dean -- 5 The Bristol District -- 6 Transverse Hypogenic Gypsum Karst of Northern England and the East Midlands -- References -- 3 Hypogene Caves in France -- Abstract -- 1 Introduction -- 2 Hypogene Speleogenesis: Definition and Characteristics -- 2.1 Hypogene Solutional Processes -- 2.2 The Ghost-Rock Karstification -- 3 Hydrogeological Setting -- 3.1 Marginal Basin Areas -- 3.2 Internal Basin Areas -- 3.3 Basin Deep Zone -- 3.4 Coastal Basins -- 3.5 Deformed Strata -- 3.6 Disrupted Basins -- 3.7 Volcanic and Magmatic Intrusions -- 4 Types of Hypogene Caves in France -- 4.1 Hypogene Cave Pattern in Phreatic Conditions -- 4.1.1 Isolated Geodes -- 4.1.2 3D Multistory Maze Caves -- 4.1.3 2D Maze Caves -- 4.1.4 Giant Ascending and Collapse Shafts -- 4.1.5 Caves Associated with Ore Deposits -- 4.2 Hypogene Cave Pattern Along or Above the Water Table -- 4.2.1 Upward Developing Dendritic Caves -- 4.2.2 Isolated Chambers -- 4.2.3 Sulfuric Water Table Caves -- 4.2.4 "Smoking" Shafts in the Vadose Zone -- 5 Conclusions -- Acknowledgements -- References -- 4 Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) -- Abstract -- 1 Introduction -- 2 Regional Geological and Hydrogeological Setting -- 3 Hypogenic Caves in the Murcia Region -- 3.1 Caves of Sierra Espuña Mountain Range -- 3.2 The Caves of the Hydrothermal Field of Cartagena -- 3.3 Caves of the North-Western Sector -- 3.4 Other Hypogenic Caves in the Murcia Region -- 4 Conclusions -- Acknowledgements -- References -- 5 Hypogene Imprints in Coastal Karst Caves from Mallorca Island (Western Mediterranean): Morphological Features and Speleogenetic Approach -- Abstract -- 1 Introduction -- 2 Geographical and Geological Setting -- 3 Caves Containing Hypogene Features -- 3.1 Llucmajor Upper Miocene Platform -- 3.1.1 Cova des Pas de Vallgornera. , 3.2 Campos Plio-Pleistocene Basin -- 3.2.1 Pou de Can Carro -- 3.2.2 Es Dolç -- 3.3 Portocristo Upper Miocene Littoral Fringe -- 3.3.1 Cova de s'Ònix -- 3.3.2 Coves del Drac -- 4 Final Discussion -- Acknowledgements -- References -- 6 Hypogene Karst in Austria -- Abstract -- 1 Introduction -- 2 Hypogene Karst in Austria -- 3 Examples of Hypogene Karst in Austria -- 3.1 Margin of the Vienna Basin -- 3.2 Salzach Fault System -- 3.3 Periadriatic Lineament -- 3.4 Northern Calcareous Alps -- 4 Summary and Outlook -- References -- 7 Hypogenic Caves in the Apennine Mountains (Italy) -- Abstract -- 1 Introduction -- 2 Geological Setting -- 2.1 Geological Structures of the Apennines -- 2.2 Hydrogeology and Geochemistry -- 3 Karst -- 3.1 Northern Apennines -- 3.2 Mt. Cucco Caves -- 3.3 Western Umbria -- 3.4 Carbonate Platforms of the Central-Southern Apennines -- 3.4.1 Capo Palinuro -- 3.4.2 Latium Mountains -- 3.5 North Calabria -- 4 Conclusions -- References -- 8 The Frasassi Caves: A "Classical" Active Hypogenic Cave -- Abstract -- 1 Introduction -- 2 Geological Setting -- 3 The Groundwater -- 3.1 Chemistry -- 3.2 Hydrodynamics -- 4 Cave Morphology -- 5 Cave Deposits -- 6 Active Speleogenetic Processes -- 6.1 H2S Degassing -- 6.2 Limestone Dissolution Measurements -- 7 Life -- 8 Speleogenesis -- References -- 9 The Coastal Sulfuric Acid Cave System of Santa Cesarea Terme (Southern Italy) -- Abstract -- 1 Introduction -- 2 Geology and Karst Geomorphology -- 3 The Santa Cesarea Terme Caves -- 4 Conclusions -- Acknowledgements -- References -- 10 The Thermal Hypogenic Caves of Acquasanta Terme (Central Italy) -- Abstract -- 1 Introduction -- 2 Geological Setting -- 2.1 Location and Climate -- 2.2 Geology -- 2.3 Hydrogeology -- 3 The Karst Area of Acquasanta Terme -- 3.1 Grotta di Acquasanta -- 3.2 The Rio Garrafo Caves -- 3.2.1 Sub-Horizontal Caves. , 3.2.2 Fault Caves -- 4 The Cave Environment -- 4.1 The Cave Water -- 4.2 Cave Atmosphere Composition -- 4.3 Active Cave Processes -- 5 Origin and Evolution of the Caves -- References -- 11 Inactive Hydrothermal Hypogenic Karst in SW Sardinia (Italy) -- Abstract -- 1 Introduction -- 2 Geographical and Geological Outline -- 3 The Main Hypogenic Caves -- 3.1 Mount San Giovanni -- 3.1.1 Santa Barbara Cave System -- 3.1.2 Crovassa Ricchi in Argento-Grotta Pisani-Grotta Quarziti -- 3.1.3 Crovassa Azzurra -- 3.1.4 Massa Riccardo-Albert -- 3.2 Campo Pisano-Monteponi -- 3.3 Mount Onixeddu-Mount Barega -- 3.4 Masua -- 3.5 Monte Guisi Cave -- 3.6 Corona 'e Sa Craba Quartzite Cave -- 4 Morphological, Mineralogical and Geochemical Evidence for Hypogene Processes -- 5 Conclusions -- Acknowledgements -- References -- 12 An Overview of the Hypogene Caves of Sicily -- Abstract -- 1 Introduction -- 2 Geology -- 3 Hypogene Caves -- 3.1 The Monte Inici Cave System -- 3.2 The Monte Kronio Cave System -- 3.3 Grotta dell'Acqua Fitusa -- 3.4 Grotta dei Personaggi -- 3.5 Grotta dell'Acqua Mintina -- 4 Conclusions -- Acknowledgements -- References -- 13 Hypogene Gypsum Caves in Piedmont (N-Italy) -- Abstract -- 1 Introduction -- 2 Geological and Structural Setting of the Gypsum Areas -- 2.1 Pre-evaporitic Messinian Deposits -- 2.2 Messinian Evaporitic and Syn-Evaporitic Deposits -- 2.3 Deposits of the Post-Evaporitic Messinian -- 3 Relationship Between the Geological and Structural Framework and Deep Karstification -- 4 The Caves of Moncalvo d'Asti -- 4.1 Groundwater Chemistry -- 4.2 Speleogenetic Hypothesis -- 5 The Cave of Monticello d'Alba -- 5.1 Speleogenetic Hypothesis -- 6 Conclusions -- References -- 14 Hypogene Speleogenesis in Greece -- Abstract -- 1 Introduction -- 2 Hypogene Caves of Greece -- 2.1 Hinterland -- 2.2 Internal Hellenides -- 2.2.1 Circum-Rhodope Belt. , 2.2.2 Paeonia Zone -- 2.2.3 Paiko Zone -- 2.2.4 Almopia Zone -- 2.2.5 Pelagonian Zone -- 2.2.6 Subpelagonian Zone -- 2.2.7 Cycladic Zone -- 2.3 External Hellenides -- 2.3.1 Pindos Zone -- 2.3.2 Gavrovo Zone -- 2.3.3 Ionian Zone -- 3 Speleogenetic Remarks -- 4 Conclusions -- 5 Acknowledgements -- References -- 15 Hypogene Karst in Macedonia -- Abstract -- 1 Introduction -- 2 Geological and Geomorphological Context -- 2.1 Pre-Cenozoic Structure -- 2.2 Cenozoic Evolution as Part of the South Balkan Extensional System -- 2.2.1 Possible Impact of the Messinian Salinity Crisis -- 2.2.2 Quaternary Uplift, Draining of Lakes and Fluvial Evolution -- 3 Hypogene Karst Systems in Macedonia -- 3.1 Mariovo -- 3.2 Katlanovo -- 3.3 Krčin (Banjište-Krasta and Kosovrasti) -- 3.4 Other Examples -- 4 General Conclusions on Hypogene Karst in Macedonia -- 4.1 Speleogenetic Mechanisms -- 4.2 Geodynamic Control on the Development of Hypogene Karst Systems -- 4.2.1 Hypogene Karst Development and the South Balkan Extensional System in Macedonia -- 4.2.2 Geomorphological Control on Hypogene Karst Evolution -- Acknowledgement -- References -- 16 Hypogene Caves of Romania -- Abstract -- 1 Introduction -- 2 Cerna Valley -- 3 Dobrogea -- 4 Mine Caves -- 5 Conclusions -- References -- 17 Fluid Flow Systems and Hypogene Karst of the Transdanubian Range, Hungary-With Special Emphasis on Buda Thermal Karst -- Abstract -- 1 Introduction -- 2 Fluid Flow Systems and Hypogene Karstification in Confined and Unconfined Carbonate Ranges-Theoretical Considerations -- 2.1 Cross-Formational Flow and Confinement of Carbonates -- 2.2 Heterogeneity of Permeability on Basin Scale -- 2.3 Hydraulic Continuity in Carbonates -- 2.4 Significance of Springs -- 2.5 Conceptual Flow Model and Connected Manifestations for an Unconfined and Confined Carbonate Basin. , 3 Fluid Flow Systems and Hypogene and Epigene Karst of the Transdanubian Range.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Keywords: Earth sciences ; Geophysics ; Hydrogeology ; Physical geography ; Earth Sciences ; Karst ; Höhle ; Entstehung ; Karsthydrographie ; Hydrogeochemie ; Hydrogeologie ; Erde ; Karsthöhle ; Karst ; Höhle ; Entstehung ; Karsthydrographie ; Hydrogeochemie ; Hydrogeologie ; Erde ; Karsthöhle
    Description / Table of Contents: This book illustrates the diversity of hypogene speleogenetic processes and void-conduit patterns depending on variations of the geological environments by presenting regional and cave-specific case studies. The cases include both well-known and newly recognized hypogene karst regions and caves of the world. They all focus on geological, hydrogeological, geodynamical and evolutionary contexts of hypogene speleogenesis. The last decade has witnessed the boost in recognition of the possibility, global occurrence, and practical importance of hypogene karstification (speleogenesis), i.e. the development of solutional porosity and permeability by upwelling flow, independent of recharge from the overlying or immediately adjacent surface. Hypogene karst has been identified and documented in many regions where it was previously overlooked or misinterpreted. The book enriches the basis for generalization and categorization of hypogene karst and thus improves our ability to adequately model hypogene karstification and predict related porosity and permeability. It is a book which benefits every researcher, student, and practitioner dealing with karst
    Type of Medium: Online Resource
    Pages: Online-Ressource (XX, 911 p. 647 illus., 509 illus. in color, online resource)
    ISBN: 9783319533483
    Series Statement: Cave and Karst Systems of the World
    Language: English
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2012-05-01
    Description: Deeply incised river networks are generally regarded as robust features that are not easily modified by erosion or tectonics. Although the reorganization of deeply incised drainage systems has been documented, the corresponding importance with regard to the overall landscape evolution of mountain ranges and the factors that permit such reorganizations are poorly understood. To address this problem, we have explored the rapid drainage reorganization that affected the Cahabón River in Guatemala during the Quaternary. Sediment-provenance analysis, field mapping, and electrical resistivity tomography (ERT) imaging are used to reconstruct the geometry of the valley before the river was captured. Dating of the abandoned valley sediments by the 10Be-26Al burial method and geomagnetic polarity analysis allow us to determine the age of the capture events and then to quantify several processes, such as the rate of tectonic deformation of the paleovalley, the rate of propagation of post-capture drainage reversal, and the rate at which canyons that formed at the capture sites have propagated along the paleovalley. Transtensional faulting started 1 to 3 million years ago, produced ground tilting and ground faulting along the Cahabón River, and thus generated differential uplift rate of 0.3 ± 0.1 up to 0.7 ±0.4 mm · y−1 along the river's course. The river responded to faulting by incising the areas of relative uplift and depositing a few tens of meters of sediment above the areas of relative subsidence. Then, the river experienced two captures and one avulsion between 700 ky and 100 ky. The captures breached high-standing ridges that separate the Cahabón River from its captors. Captures occurred at specific points where ridges are made permeable by fault damage zones and/or soluble rocks. Groundwater flow from the Cahabón River down to its captors likely increased the erosive power of the captors thus promoting focused erosion of the ridges. Valley-fill formation and capture occurred in close temporal succession, suggesting a genetic link between the two. We suggest that the aquifers accumulated within the valley-fills, increased the head along the subterraneous system connecting the Cahabón River to its captors, and promoted their development. Upon capture, the breached valley experienced widespread drainage reversal toward the capture sites. We attribute the generalized reversal to combined effects of groundwater sapping in the valley-fill, axial drainage obstruction by lateral fans, and tectonic tilting. Drainage reversal increased the size of the captured areas by a factor of 4 to 6. At the capture sites, 500 m deep canyons have been incised into the bedrock and are propagating upstream at a rate of 3 to 11 mm · y−1 while deepening at a rate of 0.7 to 1.5 mm · y−1. At this rate, 1 to 2 million years will be necessary for headward erosion to completely erase the topographic expression of the paleovalley. It is concluded that the rapid reorganization of this drainage system was made possible by the way the river adjusted to the new tectonic strain field, which involved transient sedimentation along the river's course. If the river had escaped its early reorganization and had been given the time necessary to reach a new dynamic equilibrium, then the transient conditions that promoted capture would have vanished and its vulnerability to capture would have been strongly reduced.
    Print ISSN: 0002-9599
    Electronic ISSN: 1945-452X
    Topics: Geosciences
    Published by HighWire Press on behalf of The American Journal of Science.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...