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EarthCache

STOLOVA HORA KOZELKA

A cache by CIRA Send Message to Owner Message this owner
Hidden : 8/12/2008
Difficulty:
2 out of 5
Terrain:
3 out of 5

Size: Size: not chosen (not chosen)

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Geocache Description:


http://img.geocaching.com/cache/40caf912-9f95-44f8-af2a-67878e5a1c06.jpg

[CZ]

Prírodní rezervace Kozelka rozloha 33ha

Zalesnená hora vystupuje 100 - 150m nad okolni krajinu Manetínské kotliny a predstavuje zbytek mladotretihorního  trachybazaltoveho lávového príkrovu.  Vrcholová plošina je zretelne poznamenaná procesy pleistocenního (starší ctvrtohory) periglaciálního (mrazového) zvetrávání.Stolová hora, též tabulová hora, je pojem z  geologieci geomorfologie , kterým se oznacuje osamocená vyvýšenina, která typicky vystupuje strmými svahy nad okolní krajinu. Vrchol hory tvorí ploché temeno, které je ruzného tvaru a velikosti. Svými rozmery jsou stolové hory prechodem mezi svedeckými vrchya tabulemi. Tento zajímavý geomorfologickýtvar vzniká erozne denudacnícinností exogenních sil (vody, vetru, mrazu) pusobících na tabule a plošiny s  horizontálneci subhorizontálne uloženými sedimenty. Nejcastejší výskyt stolových hor je vázán na aridnía sopecnéoblasti, kde po zvetrání vrcholu hory vznikne plošina odolnejšího ztuhlého magmatu. Díky príkrým svahum, které oddelují ploché temeno od okolní krajiny, je pomerne casté, že se na temeni hory nachází uzavrený ekosystéms odlišnou flórou a faunou

 

 

[EN]

Reservation mesa Kozelka  stretch33ha

Kozelka mountain rises in range from 100 to 150 metre above surrounding landscape of Manetin’s fold. This mountain was formed in young tertiary which we can know thanks to the occurrence of rest of tertiary’s trachyte extrusive sheet. Kozelka was created by chemical and mechanical erosion. In the first phase fantastic rocky forms were created in bare parts of joint extrusive sheet on the top of mountain. In the second phase depression of short canyon rose and rock pillars and towers were created.In the third phase formations of rock stone broke up and dumped and currently borders of mountain’s foot, slopes and cliffs were shaped. During the process of mountain’s shaping very important erosial factor was water. Except of surface’s erosion, water influenced mountain’s underground. Nowadays it means Kozelka is very rich in subterranean waters.

http://img.geocaching.com/cache/86f1f24e-f6cf-4ed7-b7a0-ba077eeacc01.jpg

 

 http://img.geocaching.com/cache/34525e46-f71f-40b9-a725-65e8d05020dc.jpg

 

[CZ]

Pro zalogování cache musite splnit tyto podminky:

Pripojte k logu fotografii Vas s GPS z vrcholu Kozelky u cedule  

Kolik milionu let trvaly Ctvrtohory?

 

[EN]

You must fulfill the requirements for log this cache:

Insert your photo with GPS picture to log from on the top of the mountain

How be of long duration antropozoikum alias kvartér?

 

Additional Hints (No hints available.)



 

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Current Time:
Last Updated: on 5/13/2018 3:10:21 AM Pacific Daylight Time (10:10 AM GMT)
Rendered From:Unknown
Coordinates are in the WGS84 datum

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