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APVC

Altiplano–Puna volcanic complex

volcanic complex (Spanish: Complejo volcánico Altiplano-Puna), also known as APVC, is a complex of volcanic systems in the Puna of the Andes. It is located

Cerro Panizos

group of lava domes. It is part of the Altiplano-Puna volcanic complex (APVC), a group of calderas and associated ignimbrites (a form of volcanic rock)

El Tatio

volcanic belts in the Andes), and of the Altiplano–Puna volcanic complex (APVC) – a system of large calderas and associated ignimbrites which were the sources

Cerro Guacha

volcanic arcs of the Andes, and its associated Altiplano-Puna volcanic complex (APVC). A number of volcanic calderas occur within the latter. Cerro Guacha and

Kirtanananda Swami

to the APVC, not directly to the victims. He must undergo a psychological evaluation by a mental health professional pre-approved by the APVC, and he

Altiplano-Puna Magma Body

plateau approximately 10–20 km beneath the Altiplano-Puna Volcanic Complex (APVC) in the Central Andes. High resolution tomography shows that this magma body

Vision science

the Vision Sciences Society (VSS)[2] Asia Pacific Conference on Vision (APVC)[3] British Congress of Optometry and Vision Science(BCOVS)[4] Indian Contact

Tocorpuri

(AVZ). Tocorpuri is part of the CVZ. The Altiplano-Puna volcanic complex (APVC) has been episodically active between 10 and 1 million years ago. Surges

Aucanquilcha

northwest of the Altiplano–Puna volcanic complex (APVC), a local large igneous province. The APVC is underpinned below at a depth of 20 kilometres (12 mi)

Cerro Bitiche

Zone away from the volcanic arc within the Altiplano-Puna volcanic complex (APVC), close to Zapaleri volcano. The field is formed by seven scoria cones and