Karst areas in Java island

BANTEN RANGKASBITUNG District Ujungkulon - Ujungkulon Sub Bayah - Cijengkol, Cilograng, Darmasari, Cikatomas, and bojongmanik Natural Landforms characteristic: not Morfolagi karst developed, except Cijengkol and darmasari karst, unique geomorphology. Other Description: Sea Caves and cave biota WEST JAVA SUKABUMI District: Cikembar - Gunungwalat District: Plabuhanratu - Bukit Cipatuguran District: Segaranten - CIDOLOG Sub: CIPEUNDEUY - CIPEUNDEUY Sub: Nyalindung - Jampangtengah. Natural Landforms characteristics: geomorphology and hydrology unique, except cipatuguran karst hills and Jampangtengah, less developed morphology of the cave. Other information: Biota cave. identified caves: cave monsters CIANJUR Sub: Takokak Natural Landforms characteristics: karst is not developed BOGOR Sub: ciampea - Cibodas Sub: Citeureup _ Citeureup District: Cilengsi - Cilengsi - Bojong Sub; Gudawang - Cigudeg Natural Landforms characteristics: a unique geomorphology and hydrology, except karst Citeureup and Cilengsi-Bojong, morphology of the ... [readmore]

Poetry Life of Caves

[caption id="attachment_211" align="alignleft" width="300" caption="Cave Jatijajar, famous tourism object in Central Java."][/caption] Coral reefs and caves turned out to have blood ties. Coral reefs are ancient surface of the earth rising over thousands of years ago was the origin of the cave. In the same year thousands of ornaments beautiful cave formed. Ancient coral reefs. Cave ornament admired because of its beauty, stalagmites and stalactites grow lengthwise. When the plants grow because of nutritional supply of nutrients and the result of photosynthesis, "Nutrition" in stalagmites and stalactites is nothing but the result of precipitation of calcium (Ca) in the process of dissolving or karst limestone (CaCO). Deposition of calcium that form water droplets that initially settled in the cave langt-forming inverted cone-stalactites. Instead of water droplets sink into the ... [readmore]

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