Tephra is stuff that comes out of the volcano, it is mainly disposed as rocks.
A combination volcano develops from repeated lava eruptions and the accompanying tephra deposits Tephra is the debris from the eruption..
Mount Terror is a stratovolcano, which is a tall, conical volcano composed of layers of hardened lava, tephra, and volcanic ash. It is located in Antarctica and is part of the active volcano chain known as the Terror Rift.
The summit of a shield volcano is typically characterized by a broad, gently sloping dome shape formed by the eruption of low-viscosity basaltic lava that can flow over long distances. At the summit, there may be a central crater or caldera, which can result from explosive eruptions or the collapse of the volcano after magma withdrawal. The overall structure allows for the accumulation of layers of lava flows, contributing to the volcano's shield-like appearance. Examples of shield volcanoes include Mauna Loa and Kilauea in Hawaii.
cinder cone volcano
Nevado del Ruiz is a stratovolcano, not a shield volcano. Shield volcanoes are typically broad and have gentle slopes created by low-viscosity lava flows, while stratovolcanoes have steep slopes and are composed of alternating layers of hardened lava, tephra, and volcanic ash.
A combination volcano develops from repeated lava eruptions and the accompanying tephra deposits Tephra is the debris from the eruption..
Mount Terror is a stratovolcano, which is a tall, conical volcano composed of layers of hardened lava, tephra, and volcanic ash. It is located in Antarctica and is part of the active volcano chain known as the Terror Rift.
The summit of a shield volcano is typically characterized by a broad, gently sloping dome shape formed by the eruption of low-viscosity basaltic lava that can flow over long distances. At the summit, there may be a central crater or caldera, which can result from explosive eruptions or the collapse of the volcano after magma withdrawal. The overall structure allows for the accumulation of layers of lava flows, contributing to the volcano's shield-like appearance. Examples of shield volcanoes include Mauna Loa and Kilauea in Hawaii.
Cinder Cone Volcano
Tephra
cinder cone volcano
Nevado del Ruiz is a stratovolcano, not a shield volcano. Shield volcanoes are typically broad and have gentle slopes created by low-viscosity lava flows, while stratovolcanoes have steep slopes and are composed of alternating layers of hardened lava, tephra, and volcanic ash.
Cindercone
Tephra
Tephra is basically ash, rock, cinders, and solidified lava spurted from a volcano.
Mt. Okmok is a stratovolcano, which is a conical volcano built up by many layers (strata) of hardened lava, tephra, pumice, and volcanic ash. It is located in the Aleutian Islands of Alaska and is known for its explosive eruptions.
Mount Bailey is a tephra cone and shield volcano, and is located in Oregon.