Very tall volcanoes with sharp peaks are stratovolcanoes.
Volcanoes with a sharp peak are typically stratovolcanoes, also known as composite volcanoes. These volcanoes are characterized by their steep, conical shape formed by alternating layers of lava flows, ash, and volcanic rock. Notable examples include Mount St. Helens in the United States and Mount Fuji in Japan. Their steep profiles are the result of more explosive eruptions, which create a prominent summit.
shield volcanoes.
Mt. Lassen is a lava dome type of volcano. The domes of lava dome volcanoes grows from within, and commonly occur within the craters or on the flanks of large composite volcanoes.
Volcanoes are usually cone shaped mountains or hills.
They are dormant volcanoes.
kettle
horn
Glacial horn
CONE
Glacial horn
Glacial horn
The geological process responsible for the formation of a pyramidal peak is glacial erosion. This occurs when glaciers carve away at the sides of a mountain, creating a sharp, pyramid-shaped peak.
Volcanoes are cone shaped.
Different shaped volcanoes occur because of the way the magma flows. Three types of volcanoes are shield, composite, and caldera.
shield volcanoes.
It is important to know the definition of new terms. The broad slightly dome-shaped volcanoes in Hawaii are Shield Volcanoes.
Mt. Lassen is a lava dome type of volcano. The domes of lava dome volcanoes grows from within, and commonly occur within the craters or on the flanks of large composite volcanoes.