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Speleology in Kazakhstan

Shakalov on 04 Jul, 2018
Hello everyone!   I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")   There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...

New publications on hypogene speleogenesis

Klimchouk on 26 Mar, 2012
Dear Colleagues, This is to draw your attention to several recent publications added to KarstBase, relevant to hypogenic karst/speleogenesis: Corrosion of limestone tablets in sulfidic ground-water: measurements and speleogenetic implications Galdenzi,

The deepest terrestrial animal

Klimchouk on 23 Feb, 2012
A recent publication of Spanish researchers describes the biology of Krubera Cave, including the deepest terrestrial animal ever found: Jordana, Rafael; Baquero, Enrique; Reboleira, Sofía and Sendra, Alberto. ...

Caves - landscapes without light

akop on 05 Feb, 2012
Exhibition dedicated to caves is taking place in the Vienna Natural History Museum   The exhibition at the Natural History Museum presents the surprising variety of caves and cave formations such as stalactites and various crystals. ...

Did you know?

That enthalpy is heat content [16].?

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KarstBase a bibliography database in karst and cave science.

Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
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Featured articles from other Geoscience Journals
Karst environment, Culver D.C.
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs, Bontognali, Tomaso R.R.; D’Angeli Ilenia M.; Tisato, Nicola; Vasconcelos, Crisogono; Bernasconi, Stefano M.; Gonzales, Esteban R. G.; De Waele, Jo
Calculating flux to predict future cave radon concentrations, Rowberry, Matt; Marti, Xavi; Frontera, Carlos; Van De Wiel, Marco; Briestensky, Milos
Microbial mediation of complex subterranean mineral structures, Tirato, Nicola; Torriano, Stefano F.F;, Monteux, Sylvain; Sauro, Francesco; De Waele, Jo; Lavagna, Maria Luisa; D’Angeli, Ilenia Maria; Chailloux, Daniel; Renda, Michel; Eglinton, Timothy I.; Bontognali, Tomaso Renzo Rezio
Evidence of a plate-wide tectonic pressure pulse provided by extensometric monitoring in the Balkan Mountains (Bulgaria), Briestensky, Milos; Rowberry, Matt; Stemberk, Josef; Stefanov, Petar; Vozar, Jozef; Sebela, Stanka; Petro, Lubomir; Bella, Pavel; Gaal, Ludovit; Ormukov, Cholponbek;
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Your search for database (Keyword) returned 44 results for the whole karstbase:
Showing 1 to 15 of 44
3-D seismic evidence of the effects of carbonate karst collapse on overlying clastic stratigraphy and reservoir compartmentalization, 1996, Hardage B. A. , Carr D. L. , Lancaster D. E. , Simmons J. L. , Elphick R. Y. , Pendleton V. M. , Johns R. A. ,
A multidisciplinary team, composed of stratigraphers, petrophysicists, reservoir engineers, and geophysicists, studied a portion of Boonsville gas field in the Fort Worth Basin of north-central Texas to determine how modern geophysical, geological, and engineering techniques can be combined to understand the mechanisms by which fluvio-deltaic depositional processes create reservoir compartmentalization in a low- to moderate-accommodation basin. An extensive database involving well logs: cores, production, and pressure data from more than 200 wells, 26 mi(2) (67 km(2)) of 3-D seismic data, vertical seismic profiles (VSPs), and checkshots was assembled to support this investigation. We found the mast Important geologic influence on stratigraphy and reservoir compartmentalization in this basin to be the existence of numerous karst collapse chimneys over the 26-mi(2) (67 km(2)) area covered by the 3-D seismic grid, These near-vertical karst collapses originated in, or near, the deep Ordovician-age Ellenburger carbonate section and created vertical chimneys extending as high as 2500 fl (610 m) above their point of origin causing significant disruptions in the overlying elastic strata. These karst disruptions lend to be circular in map view, having diameters ranging from approximately 500 ft (150 m) to as much as 3000 ft (915 m) in some cases. Within our study area, these karat features were spaced 2000 ft (610 m) to 6000 ft (1830 m) apart, on average. The tallest karst collapse zones reached into the Middle Pennsylvanian Strawn section, which is some 2500 ft (760 m) above the Ellenburger carbonate where the karst generation began. We used 3-D seismic imaging to show how these karst features affected the strata above the Ellenburger and how they have created a well-documented reservoir compartment in the Upper Caddo, an upper Atoka valley-fill sandstone that typically occurs 2000 ft (610 m) above the Ellenburger. By correlating these 3-D seismic images with outcrops of Ellenburger karat collapses, we document that the physical dimensions (height, diameter, cross-sectional area) of the seismic disruptions observed in the 3-D data equate to the karst dimensions seen in outcrops. We also document that this Ellenburger carbonate dissolution phenomenon extends over at least 500 mi (800 km), and by inference we suggest karst models like we describe here may occur in any basin that has a deep, relatively thick section of Paleozoic carbonates that underlie major unconformities

Systme dinformation gographique et splologie : un outil pour la gestion de lespace karstique ?, 1997, Robbezmasson Jeanmarc, Huttel Olivier, Levinet Ciia, Plagnes David, Vaquer Cathy, Villaret Laurent
Geographical Information Systems (GIS) make up for this inadequacy by allowing simultaneous management and spatial query of point, line and polygon entities. It is shown on a limited example in southern France the potential importance of these techniques in the field of karstology.

Stable isotopes as natural tracers of the karst recharge to the tertiary clastic aquifers: a case study of southern part of Ljubljana marsh , 1998, Pezdič, Jož, E,

The main purpose of the research was to determine the recharge and storage of groundwater at the southern part of Ljubljana marsh where tertiary aquifers are filled mainly with karst water. Stable isotopes of hydrogen, oxygen and carbon in water or in dissolved species, as well as tritium content in water and precipitation were used as natural tracers to follow the recharge and discharge of surface streams and aquifers. Together with hydrogeological and other chemical evidence they provide useful information about water mass transport, storage, refilling of aquifers and mixing of groundwater. In the aquifers, springs and surface river water d18O varied from -9,65 to -8,82 š while dD has the range from -67,4 to -61,2 š. Tritium activities are measured from 1,6 to 13,4 T.U.. Long term averages (n = 13 years) for d18O (dD) in Ljubljana is -8,73 (-60,6) š and tritium content is 17,5 T.U.. The mean temperature in Ljubljana is 10,03ºC and average years precipitation amount is 1332 mm. Years 1992-93 have been characterised by low tritium content in precipitation (8,2 for 1992 and 10,6 for 1993) and so important for investigation. The average mean meteoric line for the last 14 years is defined as dD=8,188xd18O+10,66. Temperature correlation vs. oxygen is: d18O=0,254xt-10,78. The above database is discussed in order to evaluate thesis about karst influence on the recharge and storage of clastic sediment aquifers in the Iška delta sediment structure.

Predicting natural cavities in chalk, 2001, Edmonds Cn,
Introduction Chalk is a soluble carbonate rock with extensive karst development. Natural cavity occurrence initially appears to be random. In an area where the degree of influence of all cavity formational factors is similar, but dissolution is focused on one set of joints rather than another, then solution feature occurrence is perhaps random. This might be termed the microscale' view, measured at a scale of metres. However, if the pattern of natural cavity occurrence is considered at a macroscale' level, say measured in hundreds of metres or kilometres, then spatial patterns emerge suggesting dissolution is not as random as it might first appear. Spatial characteristics of natural cavity occurrence on the Chalk In order to analyse the spatial characteristics of natural cavity occurrence it was first necessary to collect as many records of solution feature occurrence as possible from published and unpublished sources including local authorities, Construction Industry Research and Information Association (CIRIA), Transport Research Laboratory (TRL), Building Research Establishment (BRE), National House Building Council (NHBC), the Environment Agency, water companies, and site investigation reports. Particular emphasis was placed on fieldwork to record new features revealed in a wide range of engineering works, road and motorway construction, and on visits to large numbers of working/disused chalk quarries and aggregate workings. A database of 2226 natural cavities was compiled, composed mainly of solution pipes, sinkholes (dolines) and swallow holes. The spatially related database (each cavity location being recorded by National Grid Reference) was carefully scrutinized to determine ... This 250-word extract was created in the absence of an abstract

Origin of atoll lagoons, 2001, Purdy Edward G. , Winterer Edward L. ,
A database of 301 atolls from the Pacific, Indian, and Atlantic Oceans has been analyzed with respect to factors governing maximum atoll lagoon depth. Statistically significant correlations between maximum atoll lagoon depth and both atoll area and present-day rainfall are viewed as the combined effect of paleorainfall precipitation and catchment area in contributing to overall atoll morphology. This interpretation is supported by the gross saucer-shaped morphology of several of the Lau group of the Fiji Islands, and the subsurface Cretaceous Golden Lane atoll of Mexico, where evidence of reef rim construction is lacking but evidence for significant solution relief is compelling. The contribution of reefs to atoll rim construction appears to be limited generally to [~]10 m, leaving more than 20 m of relief to be explained at most atolls. At a number of these, the last interglacial highstand surface is [~]15-20 m beneath Holocene rim sediments. Subsidence rates of even 5 cm/ k.y. do not suffice to explain the subsea depth of this unconformity, suggesting the dominating influence of solution on relief expression. Calculations of solution rates relative to the residence time of sea level below given depths during the past 700 k.y. suggest that the observed atoll relief is in part inherited from more than one Pleistocene, or perhaps earlier, glacial stage. Whatever the precise time of origin, the data available strongly suggest that atoll morphology is solution determined rather than growth predicated

The Development of a Karst Feature Database for Southeastern Minnesota, 2002, Gao, Y. , Alexander Jr. , E. C. , Tipping, R. G.
A karst feature database of southeastern Minnesota has been developed that allows sinkhole and other karst feature distributions to be displayed and analyzed across existing county boundaries in a geographic information system (GIS) environment. The central Database Management System (DBMS) is a relational GIS-based system interacting with three modules: GIS, statistical, and hydrogeologic modules. Data tables are stored in a Microsoft Access 2000 DBMS and linked to corresponding ArcView shape files. The current Karst Feature Database of Southeastern Minnesota was put on a Windows NT server accessible to researchers and planners through networked interfaces. Initial spatial analyses and visualizations of karst feature distributions in Southeastern Minnesota were conducted using data extracted from the karst feature database. A series of nearest-neighbor analyses indicates that sinkholes in southeastern Minnesota are not evenly distributed (i.e., they tend to be clustered). ArcInfo, ArcView and IRIS ExplorerTM were used to generate a series of 2D and 3D maps depicting karst feature distributions in southeastern Minnesota using data exported from the GIS-based karst feature database. The resulting maps allow regional trends to be visualized and extend county-scale trends to larger state-wide scales.

Groundwater modelling in aquifers with highly karstic and heterogeneous characteristics (KHC) in Palestine, 2002, Froukh Lj,
Groundwater modelling is hindered by the lack of adequate information about the groundwater system and hence the need for an interactive and efficient system for data preparation and results analysis. Such a lack of information usually necessitates the use of tedious iterative methodology within a sensitivity analysis scheme. The heterogeneous aquifer systems complicate the issue since more data is required to simulate the system. This study demonstrates the integrated approach to bridge the gap between data handling and modelling. The karst cretaceous aquifer system (complex aquifer system) of the Eastern Basin in the West Bank is used to illustrate this approach. The groundwater modelling approach integrates the outputs from different programs for data preparation and analysis. These include (1) Groundwater Database (GWW) (2) Geographic Information System (GIS) (3) Groundwater Modelling System (GMS). In addition, the paper will summarize the data collection efforts, problems faced and experience gained working with heterogeneous media. This involves linking the results from various field investigations for groundwater development programs in the West Bank

Thesis Abstract: Karst feature distribution in South-eastern Minnesota: Extending a GIS-based database for spatial analysis and rescouce management, 2003, Gao Yongli

Symposium Abstract: A digital database of the [UK] Biological Records: A demonstration and preliminary analysis, 2003, Proudlove G. S.

Faune aquatique souterraine de France : base de donnes et elments de biogographie, 2003, Ferreira David, Doleolivier Mariejos, Malard Florian, Deharveng Louis, Gibert Janine
SUBTERRANEAN AQUATIC FAUNA OF FRANCE: DATABASE AND BIOGEOGRAPHY - Many data exist on the aquatic subterranean fauna of France but they are scattered. Thus, large-scale patterns of ground water biodiversity are still poorly documented due mainly to the lack of synthesis. Since 2002, we are currently gathering existing information on the distribution of stygobite species in France. A first inventory is presented in this paper. The present database contains 381 species and subspecies corresponding to more than 5700 records. This diversity indicates that the stygobite fauna of France is among one of the richest ground water fauna in Europe. Our current knowledge of groundwater biodiversity varies markedly among zoological groups and regions. We are currently implementing the present data set in order to provide a distribution pattern as complete as possible of stygobite richness in France. The database will be used for delineating hot spots of biodiversity (specific richness, endemism), for identifying priority areas for conservation and for formulating and testing hypotheses on the origin and drivers of groundwater biodiversity.

An improved method for determination of holocene coastline changes around two ancient settlements in southern Anatolia: A geoarchaeological approach to historical land degradation studies, 2003, Bal Y, Kelling G, Kapur S, Akca E, Cetin H, Erol O,
Two well-known ancient sites in southern Anatolia were selected to investigate and quantify the impact of historical land degradation on the Mediterranean coast of Turkey. These sites are the Luwian settlements of Kelenderis (modern Aydincik) and nearby Nagidos (Bozyazi), both in Mersin Province and both occupied since around 4000 BP. Changes in local climatic conditions over this period have produced variations in the rates of fluvial transport of sediment/soil from the hinterland into the relevant deltaic regions, thus influencing rates of coastal progradation and aggradation. In addition, both eustatic and neotectonic movements have contributed to deltaic subsidence and/or hinterland uplift, with consequential impact on coastal evolution (positive or negative). The novel gcoarchaeological methodology adopted in this study involves the creation of a graphical archive from detailed and standardised measurements taken from rectified mono- and stereoscopic aerial photographs. These archival data were then integrated with data from several types of historical map and field measurements in order to develop a geographical information system (GIS) database that could be interrogated, enabling graphical models of past coastal change to be constructed and calculations then made of the coastal configurations at successive historical periods. These calculations reveal that over the past 6000 years there has been only limited erosion/degradation in the karstic hinterland supplying the sediment to these two study sites (contrary to some previous statements concerning the high degradation risk of Mediterranean karst terrains). Furthermore, rates of progradation in each delta appear to have become diminished or even reversed in the past several decades as a result of both natural and anthropogenic factors. The precise contribution of neotectonic movements in this seismically active zone remains unquantified and is a topic requiring further interdisciplinary study.

Zum Stand der Spelotherapie in sterreich., 2004, Bengesser R. , Pavuza R.
The successful medical utilisation of the subsurface climate in caves and abandoned mines in Austria is currently limited to a few speleotherapeutic stations. Despite the fact that this kind of treatment is widespread and successfully applied in Eastern Europe its profile and public interest remains comparatively low. Furthermore, certain safety related legal problems have emerged recently. The large number of appropriate natural caves and mines, the increasing size of a comprehensive speleoclimatic database as well as promising results of small scale tests in different caves and mines could help to establish additional speleotherapeutic stations. [Koppenbrllerhhle (1549/1), Schwarzenbachloch (1612/7), Josefistollen]

Degradates provide insight to spatial and temporal trends of herbicides in ground water, 2004, Kolpin D. K. , Schnoebelen D. J. , Thurman E. M. ,
Since 1995, a network of municipal wells in Iowa, representing all major aquifer types (alluvial, bedrock/karst region, glacial drift, bedrock/nonkarst region), has been repeatedly sampled for a broad suite of herbicide compounds yielding one of the most comprehensive statewide databases of such compounds currently available in the United States. This dataset is ideal for documenting the insight that herbicide degradates provide to the spatial and temporal distribution of herbicides in ground water. During 2001, 86 municipal wells in Iowa were sampled and analyzed for 21 herbicide parent compounds and 24 herbicide degradates. The frequency of detection increased from 17% when only herbicide parent compounds were considered to 53% when both herbicide parents and degradates were considered. Thus, the transport of herbicide compounds to ground water is substantially underestimated when herbicide degradates are not considered. A significant difference in the results among the major aquifer types was apparent only when both herbicide parent compounds and their degradates were considered. In addition, including herbicide degradates greatly improved the statistical relation to the age of the water being sampled. When herbicide parent compounds are considered, only 40% of the wells lacking a herbicide detection could be explained by the age of the water predating herbicide use. However, when herbicide degradates were also considered, 80% of the ground water samples lacking a detection could be explained by the age of the water predating herbicide use. Finally, a temporal pattern in alachlor concentrations in ground water could only be identified when alachlor degradates were considered

Zum Stand der Spelotherapie in sterreich, 2004, Bengesser R. , Pavuza R.
The successful medical utilisation of the subsurface climate in caves and abandoned mines in Austria is currently limited to a few speleotherapeutic stations. Despite the fact that this kind of treatment is widespread and successfully applied in Eastern Europe its profile and public interest remains comparatively low. Furthermore, certain safety related legal problems have emerged recently. The large number of appropriate natural caves and mines, the increasing size of a comprehensive speleoclimatic database as well as promising results of small scale tests in different caves and mines could help to establish additional speleotherapeutic stations.

Magmatic and Hydrothermal Chronology of the Giant Rio Blanco Porphyry Copper Deposit, Central Chile: Implications of an Integrated U-Pb and 40Ar/39Ar Database, 2005, Deckart K, Clark Ah, Celso Aa, Ricardo Vr, Bertens An, Mortensen Jk, Fanning M,
The history of hypabyssal intrusion and hydrothermal activity in the northeastern and central parts of the be-hemothian (sensu Clark, 1993) Rio Blanco-Los Bronces porphyry copper-molybdenum deposit is clarified on the basis of integrated U-Pb and 40Ar/39Ar geochronology. Isotope dilution thermal ion mass spectrometry (ID-TIMS) U-Pb dates for zircon separates and ID-TIMS and sensitive high resolution ion microprobe (SHRIMP) dates for single zircon grains in pre-, syn- and late-mineralization volcanic and intrusive host rocks in the Rio Blanco, Don Luis, and Sur-Sur mining sectors provide a temporal framework for interpretation of incremental-heating and spot-fusion 40Ar/39Ar dates for, respectively, magmatic biotite and hydrothermal biotite, muscovite, and orthoclase. The ore deposit is hosted in part by 16.77 {} 0.25 to 17.20 {} 0.05 (2{sigma}) Ma andesitic volcanic strata of the Farellones Formation, but the major host rocks are units of the San Francisco batholith, including the 11.96 {} 0.40 Ma Rio Blanco granodiorite (mine terminology), the 8.40 {} 0.23 Ma Cascada granodiorite, and the 8.16 {} 0.45 Ma diorite. Hypabyssal dacitic intrusions (late porphyries) emplaced into the batholith yield 206Pb/238U ID-TIMS dates ranging from 6.32 {} 0.09 Ma (quartz monzonite porphyry), through 5.84 {} 0.03 Ma (feldspar porphyry) to 5.23 {} 0.07 Ma (Don Luis porphyry). The late-mineralization Rio Blanco dacite plug yields a SHRIMP zircon age of 4.92 {} 0.09 Ma. The 40Ar/39Ar plateau ages for phenocrystic biotites in quartz monzonite porphyry, feldspar porphyry, and Don Luis porphyry, as well as the preore diorite, range only from 5.12 {} 0.07 to 4.57 {} 0.06 Ma. All are significantly younger than the corresponding zircons and exhibit no correlation with intrusive sequence. The 40Ar/39Ar ages for hydrothermal biotite and orthoclase veins within the San Francisco batholith units fall in a narrow interval from 5.32 {} 0.27 to 4.59 {} 0.11 Ma. Hydrothermal sericites (muscovite), one associated with chalcopyrite, yielded spot-fusion ages of 4.40 {} 0.15 Ma (Rio Blanco granodiorite hosted) and 4.37 {} 0.06 Ma (Don Luis porphyry hosted). Comparison with the ID-TIMS and SHRIMP zircon ages indicates that most of the 40Ar/39Ar ages, even 95 percent plateaus, do not record initial magmatic cooling or hydrothermal alteration-mineralization events, evidence for quasipervasive reheating to at least 300{degrees}C by successive intrusions. Published Re-Os ages for two molybdenite samples range from 5.4 to 6.3 Ma and overlap extensively with the zircon U-Pb ages for the late porphyries. They imply that Cu-Mo mineralization overlapped temporally with the emplacement of, at least, quartz monzonite porphyry and feldspar porphyry units of the late porphyry suite and was, therefore, contemporaneous with the rise of dacitic melts to subvolcanic levels. Hydrothermal activity is inferred to have continued until 4.37 {} 0.06 Ma, following intrusion of the Don Luis porphyry and the early stages of emplacement of the Rio Blanco dacite plug complex. Hypogene Cu-Mo mineralization therefore probably persisted for 2 m.y. The geochronologic data do not resolve whether ore formation was continuous or episodic, but the observed crosscutting relationships between intensely altered and mineralized country rocks and less altered and mineralized late porphyry bodies support a model in which the ascent of metal-rich brines from an unexposed zone of the parental magma chamber was periodically stimulated by magma perturbation and hypabyssal intrusion

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