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95 (0,058s)

Výsledek výzkumu

Malacostratigraphy of the holocene tufa deposit at Kalivody (Nature park Džbán Tableland, north-western Bohemia)

The malacocoenoses of the lower complex are characteristic of the late Climatic Optimum (Epiatlantic Period), whereas their later retreat probably reflects the cultivation of the adjacent landscape during the final Bronze Age as well as the climatic ...

EG - Zoologie

  • 2009
  • Jx
Výsledek výzkumu

Tufa deposit near Račice in the Křivoklát Area (Central Bohemia).

In the vicinity of the gamekeeper's lodge kolouch near Račice a tufa deposit was investigated malacostratigraphically. The tufa sequence is separated by a scree horizon into two complexes. The lower one consists of fine-grained alm-...

DB - Geologie a mineralogie

  • 2003
  • Jx
Výsledek výzkumu

Malacostratigraphical studies on Holocene depositional and erosional processes in the White Carpathians.

Pure tufa deposition corresponds to a standstill phase in colluvial/proluvial sedimentation during the Holocene Climatic Optimum. By contrast, the Late Holocene with coarse scree. The tufa precipitation declined and the scree often ...

DB - Geologie a mineralogie

  • 2002
  • Jx
Výsledek výzkumu

Climate-induced changes in Holocene calcareous tufa formations, Bohemian Karst, Czech Republic.

A 17 m thick tufa accumulation at Svatý Jan pod Skalou was selected and thorougly studied as a typical, well developed representative of local tufa deposits. Tufa formation started at about 9500 BP. Termination of the t...

DB - Geologie a mineralogie

  • 2002
  • Jx
Výsledek výzkumu

Malacostratigraphical onvestigation of tufas at the Pivný Brook in the White Carpathians

The studied tufa deposit is situated in the spring area of Pivný brook and forms a step in the NW-facing slope of the central part of White Carpathians (SE Moravia). its main body consists of pure whitish tufa, whereas the lower and...

DB - Geologie a mineralogie

  • 2004
  • Jx
Výsledek výzkumu

The recent tufa body in Čimice Gorge in Prague 8.

Recent acceleration of tufa forming processes is recorded in Central Bohemia at various sites of Bohemian Karst and in the other areas built up by calcareous rocks. The tufa body developed since 50-ties and possibly in the last 20 y...

DB - Geologie a mineralogie

  • 2000
  • Jx
Výsledek výzkumu

Molluscs of a tufa-, marl- and alm-dominated slope cascade located north of Liptovská Lužná in the Low Tatra Mts.

Molluscs of a tufa-, marl- and alm-dominated slope cascade located north of Liptovská Lužná in the Low Tatra Mts.

EG - Zoologie

  • 2007
  • Jx
Výsledek výzkumu

Bílina: a window on Early Miocene marshland environments

DB - Geologie a mineralogie

  • 1998
  • Jx
Výsledek výzkumu

Holocene calcareous tufa cascades in the Bohemian Karst, International Conference on Past Global Changes, Excursion Guide

The excursion guide gives information about several localities of Holocene calcareous tufa of the Bohemian Karst...

DB - Geologie a mineralogie

  • 2000
  • B
Výsledek výzkumu

Holocene calcareous tufa accumulation and karstic spring in Svatý Jan pod Skalou (Bohemian Karst).

The monograph is focused ona deep-seated karst spring whitch deposited during Holocene some 17m of tufa deposits. The extensive paleoclimate and paleoenvironmental study was performed....

DB - Geologie a mineralogie

  • 2001
  • B
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