Natural mineral formations are a window into important processes leading to carbon storage
and mineralized carbonate structures formed through abiotic and biotic processes. In the …

The cumulative incision rates of~ 50–70 m/Ma integrating over the last~ 3 Ma have been
derived from published terrace-chronological data of the Danube river in the Western …

Abstract Montecchio cave (Grosseto province, Tuscany, Italy) opens at 320 m asl, in a small
outcrop of Jurassic limestone (Calcare Massiccio Fm.), close to the Albegna river. This area …

The Buda thermal karst is one of the most characteristic hypogene karst systems of the world
developed in Triassic and Eocene limestone and marl in Budapest, on the right side of the …

Here we track the water-table position and temperature of the Mount San Giovanni aquifer
(Iglesiente-Sulcis mining district, SW Sardinia, Italy) during the past 600 ka by determining …

The genesis of calcite coralloid speleothems from Lamalunga cave (Southern Italy) is here
investigated from a purely petrographic perspective, which constitutes the basis for any …

Exotic carbonate–siliceous coralloid speleothems of the Koněprusy Caves, which consist of
dominant aggregates of feather‐like, radial fibrous, dogtooth and gothic‐arch calcite …

Abstract The Buda Thermal Karst System is located under the densely populated hills of
Budapest. One of its caves (Pál-völgy Cave System) is the longest cave of Hungary with 30.1 …

Current knowledge about the formation of calcite rafts was summarized and expanded with
new data from the environment of a technical adit excavated in the 1950s in the central part …

Several thermal karstic caves are known in the Rózsadomb area of Budapest, Hungary. On
a small, 5–6 km2 territory more than 50 km of cave passages were mapped and …