Alitar
Alitar is constructed on Miocene-Pliocene La Pacana and Atana ignimbrite. The volcano is composed from andesites and dacites of Pliocene-Pleistocene age. A 500 metres (1,600 ft) wide, 50 metres (160 ft) deep maar lies at the southwest foot of the volcano. Fumarolic activity occurs both in the northern sector of the maar and another area 400 metres (1,300 ft) northwest of it. 200 metres (660 ft) west of the maar a hydrothermal well system comprising six pools and gas discharges is located in a creek.
primaryTopic
Alitar
Alitar is constructed on Miocene-Pliocene La Pacana and Atana ignimbrite. The volcano is composed from andesites and dacites of Pliocene-Pleistocene age. A 500 metres (1,600 ft) wide, 50 metres (160 ft) deep maar lies at the southwest foot of the volcano. Fumarolic activity occurs both in the northern sector of the maar and another area 400 metres (1,300 ft) northwest of it. 200 metres (660 ft) west of the maar a hydrothermal well system comprising six pools and gas discharges is located in a creek.
has abstract
Alitar is constructed on Mioce ...... charges is located in a creek.
@en
elevation (μ)
mountain range
Wikipage page ID
47,586,921
Wikipage revision ID
744,735,712
age
point
-23.15 -67.63333333333334
comment
Alitar is constructed on Mioce ...... charges is located in a creek.
@en
label
Alitar
@en
lat
long
-6.763333333333334e+1
wasDerivedFrom
isPrimaryTopicOf
name
Alitar
@en