South Chalk Mountains
If viewed in terms of topography (state of the earth's surface), Wonogiri largely a Hilly area. Rocky limestone area is located in the south and west. These hills are part of the sequence Thousand Mountains in the southern part of Java Island. Mostly layer of soil is limestone. Allegedly, in the hills of gold ore Explored the which have not been until now.
In Central Java and East Java's mountain ranges Called the Mountains of South Limestone. Mountains in the northern part of Central Java and East Java extends to the so-called North Limestone Mountains and Mountains Kendeng.
According to the history of the earth, the mountains are limestone rock used to be the former seabed. Historically, geological, this area is lifted from the ocean floor and then up onto the land surface. This event is expected to occur in the days Neosen, about 20 million years ago. Land of lime formed by the events of metamorphosis of marine organisms have been settled That. This land is usually less fertile as it can not store water.
Wonogiri south the topography is Hilly and well-known as a sequence of limestone mountains south there are 109 natural lakes with an area of approximately 117.5 hectares. The potential of this natural lake used as a footstool needs daily water for the residents. Wonogiri the condition of the land most of the hills contain many limestone. This type of rock is very potential to be cultivated into limestone and calcite.
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