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 ====== Faults of the Bohemian Massif ======
+<sub> // ** %% https://doi.org/10.48790/MWF4-SH44 %% ** // </sub>
-This page reviews some main features of the most important faults in the Bohemian Massif and its close neighbourhood.
+This web reviews some main features of the most important faults in the Bohemian Massif and its close neighbourhood. It uses a structured database of active faults and related local observations made or compiled by the It will use a structured database of active faults and related local observations made or compiled by the **[[authors_and_credits#authors|editors]]** between 2019 and 2022 and occasionally updated with new contributions. The current map is incomplete (e.g. faults in Šumava Mountains, Eger rift, Krkonoše Mountains, are largely missing) and even the work on the main faults is still ongoing.
-It uses a structured database of active faults and related observations as edited by Petr Špaček, Petra Štěpančíková and Ivan Prachař and occasionally updated based on new contributions.
-Emphasis is given to those faults which were demonstrably active in Cenozoic and which are assumed to potentially slip during the following thousands of years.
-//Active faults can relax the crustal stress by a sudden slip, generating earthquakes which may cause damage at fragile building structures.
-In the Czech Republic strong earthquakes happen rarely but it is assumed from what we observe in geologically similar parts of the world that they may happen indeed - once after a very long time of quiescence.
-Learning about whether and where such earthquakes occurred in geological history, how often and how strong they were - these are the main reasons we study faults and related geological features in detail. The information learnd is then used together with the known earthquakes of the last centuries for better quantitative assessment of seismic hazard.
-//
-{{url>https://www.arcgis.com/home/webmap/viewer.html?url=http%3A%2F%2Fmaps1.arcgisonline.com%2Farcgis%2Frest%2Fservices%2FUSGS_Earthquake_Faults%2FMapServer&source=sd 1600,800 noscroll noborder alignment|alt-text}}
+The emphasis here is on those faults which were demonstrably active in Cenozoic and/or which are assumed to pose increased seismic hazard for the following thousands of years. For the sake of completeness, some other significant (or notorious) faults are added, beyond these criteria.
+You may navigate to the targets either via **map below** (it downloads slowly!) or via encyclopedic entries in the sidebar.\\
+Read more on **[[database_and_how_to_use_it|usage and technicals]]** if you need it.\\
+Making the database available for your GIS is in the pipeline.
+----
+{{url>https://faults.ipe.muni.cz/loader.html 1600,800 noscroll noborder alignment|alt-text}}
-[[technicals|Technicals]]
-[[start:sidebar|dbf]]
-=== Diendorf-Boskovice fault ===
-=== Haná fault zone ===
-=== Železné hory fault ===
-=== Mariánské lázně fault ===
-=== Hluboká fault ===
-=== Sudetic marginal fault ===

Faults of the Bohemian Massif

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