File:Lom Kosov Pohled Na Jezero D.jpg
Jump to navigation
Jump to search
Size of this preview: 450 × 600 pixels. Other resolutions: 180 × 240 pixels | 360 × 480 pixels | 576 × 768 pixels | 768 × 1,024 pixels | 2,304 × 3,072 pixels.
Original file (2,304 × 3,072 pixels, file size: 1.18 MB, MIME type: image/jpeg)
Captions
Captions
View of the interior of the Kosov quarry (the lake at the bottom of the quarry) from the western upper edge of the quarry.
Summary
[edit]
| Description |
Čeština: Lom Kosov je opuštěný vytěžený vápencovo–břidlicový lom nacházející ve středočeském kraji (v CHKO Český Kras) asi 3,5 kilometrů od vlakového nádraží v Berouně nedaleko od osady Jarov. Lokalita je tvořena několika lomovými patry a silně elipticky protaženým (v severojižním směru) jezerem na dně. Ačkoliv zde byla těžba kamene ukončena (a postupně dochází k zavážení lomu), vstup do lokality není široké veřejnosti povolen a v jezírku platí zákaz koupání. Lom byl založen nedalekou cementárnou v Králově Dvoře v roce 1909 a její provoz dlouhou dobu zásoboval zde těženými silurskými vápenci a břidlicemi, které byly používány jako korekční surovina při výrobě cementu. Vápence se nacházely v horních etážích lomu, zatímco břidlice se vyskytovala převážně v okolí jezera. Lokalita je paleontologicky známá výskytem zkamenělin hlavonožců a pravěké mořské fauny.
English: The Kosov quarry is an abandoned limestone and slate quarry located in the Central Bohemian Region (in the Bohemian Karst Protected Landscape Area) about 3.5 kilometres from the train station in Beroun, not far from the settlement of Jarov. The site consists of several quarry levels and a strongly elliptical (in the north-south direction) lake at the bottom. Although the quarrying of stone has been stopped here (and the quarry is gradually being closed), the general public is not allowed to enter the site and swimming in the lake is prohibited. The quarry was established by the nearby cement factory in Kralova Dvůr in 1909 and its operations have long supplied the Silurian limestone and shale mined here, which was used as a corrective raw material in cement production. The limestone was found in the upper stages of the quarry, while the shale was mainly found around the lake. The site is palaeontologically known for its cephalopod fossils and prehistoric marine fauna. |
| Date | |
| Source | Own work |
| Author | Mojmir Churavy |
| Camera location |  | View this and other nearby images on: OpenStreetMap |  |
|---|
Licensing
[edit]
I, the copyright holder of this work, hereby publish it under the following license:
This file is licensed under the Creative Commons Attribution-Share Alike 4.0 International license.
- You are free:
- to share – to copy, distribute and transmit the work
- to remix – to adapt the work
- Under the following conditions:
- attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
- share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the same or compatible license as the original.
File history
Click on a date/time to view the file as it appeared at that time.
| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:19, 24 June 2023 | | 2,304 × 3,072 (1.18 MB) | Mojmir Churavy (talk | contribs) | Uploaded own work with UploadWizard |
You cannot overwrite this file.
File usage on Commons
There are no pages that use this file.
