Mount Nyamuragira is a shield volcano located in the Democratic Republic of the Congo. It is primarily composed of basaltic rock, which is a type of igneous rock formed from cooled lava flows.
Mount Vesuvius is composed mainly of andesite rock, which is a type of volcanic rock that forms from the cooling of lava. Andesite is a common rock type in stratovolcanoes like Mount Vesuvius, which is a composite volcano known for its explosive eruptions.
methamorphic rock?
Mount Nyamuragira was formed by volcanic activity along the East African Rift. It is a shield volcano, characterized by its broad, gentle slopes, which are built up by successive flows of low-viscosity lava. Over time, repeated eruptions have contributed to the growth of the volcano.
Mount Cristo Rey is a laccolith, which is a type of intrusive igneous rock formation that occurs when magma is injected between layers of sedimentary rock and causes the overlying rock layers to arch upward.
Mount Stromboli is an active volcano located on the island of Stromboli in Italy. The rock type of Mount Stromboli is predominantly basaltic.
Mount Nyamuragira is on a convergent boundry
The Nyamuragira Volcano, or Mount Nyamuragira, is located on the continent of Africa in the Virunga Mountains in the Democratic Republic of the Congo.
it is a shield volcano.... i think. i hope that helps, if thats your question.
this mt. has a rock type of rock
Mount Vesuvius is composed mainly of andesite rock, which is a type of volcanic rock that forms from the cooling of lava. Andesite is a common rock type in stratovolcanoes like Mount Vesuvius, which is a composite volcano known for its explosive eruptions.
methamorphic rock?
it is made of sedementry
Sedimentary!
Mount Pinatubo is predominantly composed of andesite, which is an intermediate volcanic rock type. This rock type is typically associated with explosive volcanic activity due to its high silica content.
It is granite
Mount Nyamuragira was formed by volcanic activity along the East African Rift. It is a shield volcano, characterized by its broad, gentle slopes, which are built up by successive flows of low-viscosity lava. Over time, repeated eruptions have contributed to the growth of the volcano.
Mount Cristo Rey is a laccolith, which is a type of intrusive igneous rock formation that occurs when magma is injected between layers of sedimentary rock and causes the overlying rock layers to arch upward.