The Volcanic History of the UNESCO Global Geopark Bohemian Paradise

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F23%3A10168944" target="_blank" >RIV/00025798:_____/23:10168944 - isvavai.cz</a>

Výsledek na webu

<a href="https://doi.org/10.30486/gcr.2023.1979804.1121" target="_blank" >https://doi.org/10.30486/gcr.2023.1979804.1121</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.30486/gcr.2023.1979804.1121" target="_blank" >10.30486/gcr.2023.1979804.1121</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The Volcanic History of the UNESCO Global Geopark Bohemian Paradise

Popis výsledku v původním jazyce

Central Europe and the area of the UNESCO Global Geopark Bohemian Paradise have been affected by global tectonic events, especially during the last 500 million years. Volcanic phenomena are the most striking traces today of such past tectonic events. At the end of the Paleozoic, there were a number of volcanic eruptions connected to the waxing and waning of the Variscan Orogeny. Further volcanic activity came in the Neogene as a distal reaction to Alpine Orogenic processes. All volcanic phases show the variability of volcanic processes and have been studied intensively. In addition, these volcanic events and the production of various volcanic products enabled the emergence of local world-famous mineral deposits. The extraordinarily varied geology and the large number of volcanic features is a great tourist attraction and an excellent opportunity for a vivid interpretation of the geoheritage of Central Europe.

Název v anglickém jazyce

The Volcanic History of the UNESCO Global Geopark Bohemian Paradise

Popis výsledku anglicky

Central Europe and the area of the UNESCO Global Geopark Bohemian Paradise have been affected by global tectonic events, especially during the last 500 million years. Volcanic phenomena are the most striking traces today of such past tectonic events. At the end of the Paleozoic, there were a number of volcanic eruptions connected to the waxing and waning of the Variscan Orogeny. Further volcanic activity came in the Neogene as a distal reaction to Alpine Orogenic processes. All volcanic phases show the variability of volcanic processes and have been studied intensively. In addition, these volcanic events and the production of various volcanic products enabled the emergence of local world-famous mineral deposits. The extraordinarily varied geology and the large number of volcanic features is a great tourist attraction and an excellent opportunity for a vivid interpretation of the geoheritage of Central Europe.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10507 - Volcanology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2023

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

GEOCONSERVATION RESEARCH

ISSN

2645-4661

e-ISSN

2588-7343

Svazek periodika

6

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

IR - Íránská islámská republika

Počet stran výsledku

16

Strana od-do

98-113

Kód UT WoS článku

001004861100006

EID výsledku v databázi Scopus

2-s2.0-85162798385