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Full-Text Articles in Earth Sciences

Unusual Polygenetic Void And Cave Development In Dolomitized Miocene Chalks On Barbados, West Indies, Jonathan B. Sumrall, John E. Mylroie, Hans G. Machel Sep 2013

Unusual Polygenetic Void And Cave Development In Dolomitized Miocene Chalks On Barbados, West Indies, Jonathan B. Sumrall, John E. Mylroie, Hans G. Machel

International Journal of Speleology

Barbados provides an unusual case of polygenetic cave development within dolomitized chalks and marls of the Miocene Oceanics Group. These diagenetic processes are driven by a succession and interplay of tectonic uplift, fracturing, hypogene fluid injection, overprinting by mixing zone diagenesis, and mechanical and biological erosion in the current littoral zone. The significance of the voids and caves within the chalks on Barbados are: 1) these appear to be the first dissolution caves documented in dolomitized chalk, and 2) these features show a polygenetic origin documenting the diagenetic changes in lithology that allowed the development and preservation of these cave …


Hypogenic Origin Of Provalata Cave, Republic Of Macedonia: A Distinct Case Of Successive Thermal Carbonic And Sulfuric Acid Speleogenesis, Marjan Temovski, Philippe Audra, Andrej Mihevc, Jorge E. Spangenberg, Victor Polyak, William Mcintosh, Jean-Yves Bigot Sep 2013

Hypogenic Origin Of Provalata Cave, Republic Of Macedonia: A Distinct Case Of Successive Thermal Carbonic And Sulfuric Acid Speleogenesis, Marjan Temovski, Philippe Audra, Andrej Mihevc, Jorge E. Spangenberg, Victor Polyak, William Mcintosh, Jean-Yves Bigot

International Journal of Speleology

Provalata Cave (Republic of Macedonia) is a small but remarkable hypogenic cave, developed in Cambrian marbles by successive thermal carbonic and sulfuric acid speleogenesis. The cave has a thick partly corroded calcite crust, abundant gypsum deposits, with cupolas, ceiling and wall channels, feeders and replacement pockets as some of the most characteristic morphological features. Distribution of morphology and deposits suggest a hypogenic origin in two distinct speleogenetic phases: the first by thermal CO2 rich waters, the second by sulfuric acid dissolution, which were separated by complete infilling of cave passages with pyroclastic-derived clays. In the first phase of speleogenesis, …


Concentration And Stable Carbon Isotopic Composition Of Co2 In Cave Air Of Postojnska Jama, Slovenia, Magda Mandić, Andrej Mihevc, Albrecht Leis, Ines Krajcar Bronić Sep 2013

Concentration And Stable Carbon Isotopic Composition Of Co2 In Cave Air Of Postojnska Jama, Slovenia, Magda Mandić, Andrej Mihevc, Albrecht Leis, Ines Krajcar Bronić

International Journal of Speleology

Partial pressure of CO2 (pCO2) and its isotopic composition (δ13CairCO2) were measured in Postojnska jama, Slovenia, at 10 locations inside the cave and outside the cave during a one-year period. At all interior locations the pCO2 was higher and δ13CairCO2 lower than in the outside atmosphere. Strong seasonal fluctuations in both parameters were observed at locations deeper in the cave, which are isolated from the cave air circulation. By using a binary mixing model of two sources of CO2, one of them being the atmospheric CO2 …


Incision History Of Glenwood Canyon, Colorado, Usa, From The Uranium-Series Analyses Of Water-Table Speleothems, Victor J. Polyak, Harvey R. Duchene, Donald G. Davis, Arthur N. Palmer, Margaret V. Palmer, Yemane Asmerom Jul 2013

Incision History Of Glenwood Canyon, Colorado, Usa, From The Uranium-Series Analyses Of Water-Table Speleothems, Victor J. Polyak, Harvey R. Duchene, Donald G. Davis, Arthur N. Palmer, Margaret V. Palmer, Yemane Asmerom

International Journal of Speleology

Uranium-series analyses of water-table-type speleothems from Glenwood Cavern and “cavelets” near the town of Glenwood Springs, Colorado, USA, yield incision rates of the Colorado River in Glenwood Canyon for the last ~1.4 My. The incision rates, calculated from dating cave mammillary and cave folia calcite situated 65 and 90 m above the Colorado River, are 174 ± 30 m/My for the last 0.46 My and 144 ± 30 m/My for the last 0.62 My, respectively. These are consistent with incision rates determined from nearby volcanic deposits. In contrast, δ234U model ages (1.39 ± 0.25 My; 1.36 ± 0.25 …


Appropriate Terminology For Karst-Like Phenomena: The Problem With ‘Pseudokarst’, Rolan S. Eberhard, Chris Sharples Jan 2013

Appropriate Terminology For Karst-Like Phenomena: The Problem With ‘Pseudokarst’, Rolan S. Eberhard, Chris Sharples

International Journal of Speleology

The practice of referring to certain morphologically karst-like phenomena as ‘pseudokarst’ is problematic, because it ignores basic principles of sound classification, logical naming conventions and accepted geomorphic classifications and terminology. These problems have compounded the difficulty in establishing an accepted classification of ‘pseudokarst’ types. The practice embodies a karst-centric perspective which should be avoided in favour of using conventional geomorphic terminology for non-karstic features. We illustrate this by providing existing conventional terms for many ‘pseudokarst’ types reported in the literature.


Natural And Anthropogenic Factors Which Influence Aerosol Distribution In Ingleborough Show Cave, Uk, Andrew C. Smith B.S.C, Peter M. Wynn, Philip A. Barker Professor Jan 2013

Natural And Anthropogenic Factors Which Influence Aerosol Distribution In Ingleborough Show Cave, Uk, Andrew C. Smith B.S.C, Peter M. Wynn, Philip A. Barker Professor

International Journal of Speleology

Monitoring in Ingleborough Show Cave (N. Yorkshire, UK) reveals the influence of tourism and cave management techniques on different parameters of the cave atmosphere. Exploratory aerosol monitoring identified a 0.015 ± 0.03 mg/m³ (≈70%) reduction in airborne particulates within the first 75 meters of cave passage and two major aerosol sources within this artificially ventilated show cave. Autogenic aerosol production was identified close to active stream ways (increases of


A Model For The Formation Of Layered Soda-Straw Stalactites, Bence Paul, Russell Drysdale, Helen Green, Jon Woodhead, John Hellstrom, Rolan Eberhard Jan 2013

A Model For The Formation Of Layered Soda-Straw Stalactites, Bence Paul, Russell Drysdale, Helen Green, Jon Woodhead, John Hellstrom, Rolan Eberhard

International Journal of Speleology

Climate records based upon instrumental data such as rainfall measurements are usually only available for approximately the last 150 years at most. To fully investigate decadal-scale climate variation, however, these records must be extended by the use of climate proxies. Soda-straw stalactites (straws) are a previously under-utilised potential source of such data. In this contribution we investigate the structure and formation of straws and look at some issues that may affect the reliability of straw-based palaeoclimate records. We use laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) trace element analysis to document surface contamination features that have the potential to obscure annual …


Book Review: Water In Karst: Management, Vulnerability, And Restoration, Arthur N. Palmer Jan 2013

Book Review: Water In Karst: Management, Vulnerability, And Restoration, Arthur N. Palmer

International Journal of Speleology

Neven Kresic.
Water in Karst: Management, Vulnerability, and Restoration
New York, McGraw-Hill, 2013. ISBN 978-0-07-175333.3, 19×24 cm, 736 p. + 14 p. of color plates, hardbound,
US $125 (also available as e-book)


Table Of Contents Jan 2013

Table Of Contents

International Journal of Speleology

No abstract provided.


Layer-Bounding Surfaces In Stalagmites As Keys To Better Paleoclimatological Histories And Chronologies, Loren Bruce Railsback, Pete D. Akers, Lixin Wang, Genevieve A. Holdridge, Ny Riavo Voarintsoa Jan 2013

Layer-Bounding Surfaces In Stalagmites As Keys To Better Paleoclimatological Histories And Chronologies, Loren Bruce Railsback, Pete D. Akers, Lixin Wang, Genevieve A. Holdridge, Ny Riavo Voarintsoa

International Journal of Speleology

Petrographic recognition of layer-bounding surfaces in stalagmites offers an important tool in constructing paleoclimate records. Previous petrographic efforts have examined thickness of layers (a possible proxy for annual rainfall) and alternation of layers in couplets (a possible indicator of seasonality). Layer-bounding surfaces, in contrast, delimit series of layers and represent periods of non-deposition, either because of exceptionally wet or exceptionally dry conditions.

Two types of layer-bounding surfaces can be recognized according to explicitly defined petrographic criteria. Type E layer-bounding surfaces are surfaces at which layers have been truncated or eroded at the crest of a stalagmite. Keys to their recognition …


Front Cover Jan 2013

Front Cover

International Journal of Speleology

No abstract provided.


Mixing Of Water In A Carbonate Aquifer, Southern Italy, Analysed Through Stable Isotope Investigations, Emma Petrella, Fulvio Celico Jan 2013

Mixing Of Water In A Carbonate Aquifer, Southern Italy, Analysed Through Stable Isotope Investigations, Emma Petrella, Fulvio Celico

International Journal of Speleology

Mixing of water was analysed in a carbonate aquifer, southern Italy, through stable isotope investigations (18O,δ2H). The input signal (rainwater) was compared with the isotopic content of a 35-meter groundwater vertical profile, over a 1-year period. Within the studied aquifer, recharge and flow are diffuse in a well-connected fissure network.

At the test site, the comparison between input and groundwater isotopic signals illustrates that no efficient mixing takes place in the whole unsaturated zone, between the fresh infiltration water and the stored water.

When analysing the stable isotopes composition of groundwater, significant variations were observed above …


Table Of Contents Jan 2013

Table Of Contents

International Journal of Speleology

No abstract provided.


Book Review: Speleothem Science: From Process To Past Environments, Giovanni Zanchetta Jan 2013

Book Review: Speleothem Science: From Process To Past Environments, Giovanni Zanchetta

International Journal of Speleology

Ian J. Fairchild and Andy Baker.
Speleothem Science: From Process to Past Environments
Wiley Blackwell, 2012. Hardcover, 450 p.,
ISBN-10: 1405196203, ISBN-13: 978-1405196208, €57


World Karst Reviews Jan 2013

World Karst Reviews

International Journal of Speleology

No abstract provided.


Book Review: Trevor Shaw And Alenka Čuk Slovene Caves & Karst, Pictured 1545-1914, Arrigo A. Cigna Jan 2013

Book Review: Trevor Shaw And Alenka Čuk Slovene Caves & Karst, Pictured 1545-1914, Arrigo A. Cigna

International Journal of Speleology

Trevor Shaw and Alenka Čuk.
Slovene Caves & Karst, pictured 1545-1914
Založba ZRC, Ljubljana, 2012.
ISBN 978-961-254-369-3, 230 p. 200x290, 258 b/w and colour illustrations, paper cover, € 25.00


World Karst Reviews Jan 2013

World Karst Reviews

International Journal of Speleology

No abstract provided.


Full Issue 42(1) Jan 2013

Full Issue 42(1)

International Journal of Speleology

All articles in Volume 42 Issue 1. Does not include cover image.


The Use Of Passive Seismological Imaging In Speleogenetic Studies; An Example From Kanaan Cave, Lebanon, Carole Nehme, Christophe Voisin, Armand Mariscal, Pierre-Charles Gérard, Cécile Cornou, Badr Jabbour-Gédéon, Samer Amhaz, Nancy Salloum, Nada Badaro-Saliba, Jocelyne Adjizian-Gérard, Jean-Jacques Delannoy Jan 2013

The Use Of Passive Seismological Imaging In Speleogenetic Studies; An Example From Kanaan Cave, Lebanon, Carole Nehme, Christophe Voisin, Armand Mariscal, Pierre-Charles Gérard, Cécile Cornou, Badr Jabbour-Gédéon, Samer Amhaz, Nancy Salloum, Nada Badaro-Saliba, Jocelyne Adjizian-Gérard, Jean-Jacques Delannoy

International Journal of Speleology

Among many parameters that control the evolution of caves stands the volume of unconsolidated clay sediments generally produced by the alteration of the calcareous rocks. Here we introduce the use of a passive seismological imaging technique to investigate the clay deposits and estimate its total volume in a cave. Applied for the first time for speleogenesis studies, the HVSR (Horizontal / Vertical Spectral Ration) is a geophysical technique that can help better interpret cave geomorphology. We apply seismological spectral techniques (H/V ratio) on ambient noise vibrations to derive the clay volume, as well as its shape. This technique applied on …


Variances In Airflows During Different Ventilation Modes In A Dynamic U-Shaped Cave, Jiří Faimon, Marek Lang Jan 2013

Variances In Airflows During Different Ventilation Modes In A Dynamic U-Shaped Cave, Jiří Faimon, Marek Lang

International Journal of Speleology

Airflow dynamics were studied in Císařská Cave (Moravian Karst, Czech Republic) under different seasonal conditions. The dependence of airflows on the difference between external and cave temperatures is nonlinear and roughly obeys the Darcy-Weisbach equation. The upward airflows were found to be systematically higher than the downward airflows under comparable driving forces. The principle reason is nonlinearity between air temperature and air density. U-shaped cave geometry magnifies this effect by feedback between external temperature and airflow driving forces. Whereas this feedback is positive during the upward airflow ventilation mode, it is negative during the downward airflow mode. To discuss the …


Front Cover Jan 2013

Front Cover

International Journal of Speleology

No abstract provided.


Editorial, Jo De Waele Jan 2013

Editorial, Jo De Waele

International Journal of Speleology

No abstract provided.


Full Issue 42(2) Jan 2013

Full Issue 42(2)

International Journal of Speleology

All articles in Volume 42 Issue 2. Does not include cover image.


Cave Ventilation Is Influenced By Variations In The Co2-Dependent Virtual Temperature, Enrique P. Sánchez-Cañete, Penélope Serrano-Ortiz, Francisco Domingo, Andrew S. Kowalski Jan 2013

Cave Ventilation Is Influenced By Variations In The Co2-Dependent Virtual Temperature, Enrique P. Sánchez-Cañete, Penélope Serrano-Ortiz, Francisco Domingo, Andrew S. Kowalski

International Journal of Speleology

Dynamics and drivers of ventilation in caves are of growing interest for different fields of science. Accumulated CO2 in caves can be exchanged with the atmosphere, modifying the internal CO2 content, affecting stalagmite growth rates, deteriorating rupestrian paintings or creating new minerals. Current estimates of cave ventilation neglect the role of high CO2 concentrations in determining air density – approximated via the virtual temperature (Tv) –, affecting buoyancy and therefore the release or storage of CO2. Here we try to improve knowledge and understanding of cave ventilation through the use of T …