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About 8 kilometres (5.0 mi) northeast of Cerro Blanco lies a 1.2-kilometre (0.75 mi) wide and 20-metre (66 ft) deep vent known as El Escondido[27] or El Oculto.[16] It does not have a strong topographic expression but is conspicuous on satellite images as a semi-circular patch of darker material.[27] Gravimetric analysis has found a number of gravity anomalies around the caldera.[34] Surrounding terrain The terrain northeast-east from Cerro Blanco is covered by its ignimbrites and by Plinian fallout deposits[35] which radiate away from the calderas.[14] Cerro Blanco lies at the southwestern end of the Carachipampa valley,[36] a volcano-tectonic depression flanked by normal faults which extends to Carachipampa. This depression appears to have formed in response to north-south tectonic extension of the Puna[37] and is covered by volcanic deposits from Cerro Blanco.[16] These volcanic deposits form the "Campo de Pedra Pomez"[38] and extend 50 kilometres (31 mi) away from the volcano.[39] To the north, the El Niño scarp[40] of the El Niño caldera[41] separates the Cerro Blanco caldera from the Purulla valley.[40] Other valleys are the Purulla valley northwest from Cerro Blanco and Incahuasi due north; all three contain both volcanic deposits from Cerro Blanco and salt flats[36] or lakes.[42] In the Incahuasi valley an ignimbrite also known as the "white ignimbrite" reaches a distance of over 25 kilometres (16 mi).[22] Wind has carved 20-to-25-metre (66 to 82 ft) deep channels into the ignimbrit















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