Search KARSTBASE:
KarstBase a bibliography database in karst and cave science.
Featured articles from Cave & Karst Science Journals
Characterization of minothems at Libiola (NW Italy): morphological, mineralogical, and geochemical study, Carbone Cristina; Dinelli Enrico; De Waele Jo
Chemistry and Karst, White, William B.
Engineering challenges in Karst, Stevanović, Zoran; Milanović, Petar
The karst paradigm: changes, trends and perspectives, Klimchouk, Alexander
Long-term erosion rate measurements in gypsum caves of Sorbas (SE Spain) by the Micro-Erosion Meter method, Sanna, Laura; De Waele, Jo; Calaforra, José Maria; Forti, Paolo
Featured articles from other Geoscience Journals
Geochemical and mineralogical fingerprints to distinguish the exploited ferruginous mineralisations of Grotta della Monaca (Calabria, Italy), Dimuccio, L.A.; Rodrigues, N.; Larocca, F.; Pratas, J.; Amado, A.M.; Batista de Carvalho, L.A.
Karst processes and landforms, De Waele, J.
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
Helictite, 1973, Vol 10, Issue 4, p. 75-90
Sedimentary and Morphological Development of the Borenore Caves, New South Wales, Part I
Frank, R. M.
Abstract:
(of parts I and II) The Borenore Caves, west of Orange, occur in a partly metamorphosed Silurian limestone outcrop of about 5.5km2 which forms an impounded karst. Both of the main caves, the Arch Cave and the Tunnel Cave, contain large quantities of clastic sediments. Evidence from the position and kind of sediments and from the bedrock features show that both caves have undergone a predominantly fluvial development by a sequence of stream captures. The same type of evidence indicates a dry climatic phase for the Borenore area about 28,000 BP.
(of parts I and II) The Borenore Caves, west of Orange, occur in a partly metamorphosed Silurian limestone outcrop of about 5.5km2 which forms an impounded karst. Both of the main caves, the Arch Cave and the Tunnel Cave, contain large quantities of clastic sediments. Evidence from the position and kind of sediments and from the bedrock features show that both caves have undergone a predominantly fluvial development by a sequence of stream captures. The same type of evidence indicates a dry climatic phase for the Borenore area about 28,000 BP.