| El Negrillar | |
|---|---|
| Negros de Aras | |
 The cones in the image centre and associated black lava flows form the El Negrillar volcanic field, which covers about 220 square kilometres. | |
| Highest point | |
| Elevation | 3,500 m (11,500 ft)[1] |
| Coordinates | 24°11′S 68°15′W / 24.18°S 68.25°W[1] |
| Geography | |
  El Negrillar | |
El Negrillar is a volcanic field in the Andes. Located south of the Salar de Atacama and west of the Cordón de Púlar, it generated cinder cones and lava flows. Covering a surface area of 220 square kilometres (85 sq mi), it is the largest volcanic field in northern Chile, with almost a hundred vents that produced mainly lava flows. Owing to the arid climate, landforms are well preserved. Radiometric dating has yielded ages of less than 1.5 million years, with the most recent eruption occurring about 141,000 years ago. Parts of the Holocene Socompa debris avalanche overlie the field. A groundwater system underlies the volcanic field and some cones formed through phreatomagmatic eruptions. El Negrillar is located in a complex tectonic regime, characterized by numerous faults. The town of Tilomonte and various power lines, mines and water wells are in the area.