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| San Pablo | |
|---|---|
Volcan San Pablo from just below the summit on San Pedro volcano | |
| Highest point | |
| Elevation | 6,110 m (20,050 ft)[1] |
| Prominence | 808 m (2,651 ft)[2] |
| Parent peak | San Pedro |
| Coordinates | 21°53′02″S 68°20′33″W / 21.88389°S 68.34250°W[1] |
| Geography | |
| Location | Chile |
| Parent range | Andes |
| Geology | |
| Mountain type | Stratovolcano |
| Climbing | |
| First ascent | September 1910 by Hans Berger (Germany)[3][4][5] |
| Easiest route | North side to col then west slopes |
San Pablo is a dormant volcano located in the Antofagasta Region of Chile, near the Bolivia border. It is joined to the younger San Pedro volcano by a high col. It is located in the Chilean province of El Loa, city of Calama and Ollagüe.[6]
San Pablo was active in pre-glacial times. After that period, glaciations formed a girdle of moraines and the mountain was covered by ash fall from neighbouring San Pedro.[7] Its central crater was eroded and a glacier formed inside. The volcano itself is formed by three groups of andesite lavas which variously contain pyroxene or hornblende; these groups are known as the Lower Group, the Middle Group and the Summit Group.[8]
San Pablo was first climbed by Hans Berger (Germany) in September 1910.[3][4]
It has an official height of 6050 meters.[9] Other data from available digital elevation models: SRTM yields 6098 metres,[10] ASTER 6076 metres[11] and TanDEM-X 6143 metres.[12] The height of the nearest key col is 5302 meters, leading to a topographic prominence of 808 meters.[13] San Pablo is considered a Mountain Subgroup according to the Dominance System [14] and its dominance is 13.22%. Its parent peak is San Pedro and the Topographic isolation is 5.1 kilometers.[13]