shield volcanoes have gentle sides and aren't very tall
It depends on viscosity of the lava. the runnier the lava, the farther it flows before solidifying, so it cannot pile up as fast.
The three major types of volcanoes are shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Shield volcanoes have broad, gently sloping sides and are primarily composed of basaltic lava. Cinder cone volcanoes are small, steep-sided volcanoes that erupt primarily cinder-sized fragments. Stratovolcanoes are tall, conical volcanoes composed of alternating layers of lava flows, volcanic ash, and other materials.
No, shield volcanoes are not steep mountains. They have gently sloping sides due to the relatively low viscosity of the lava that flows from them, which allows the lava to spread out and create a wide, shield-like shape.
These volcanoes are called stratovolcanoes or composite volcanoes. They are characterized by their steep slopes and alternating layers of cinders, ash, and lava flows, typically made of basaltic and andesitic compositions.
shield volcanoes have gentle sides and aren't very tall
shield volcanoes have gentle sides and aren't very tall
It depends on viscosity of the lava. the runnier the lava, the farther it flows before solidifying, so it cannot pile up as fast.
The three major types of volcanoes are shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Shield volcanoes have broad, gently sloping sides and are primarily composed of basaltic lava. Cinder cone volcanoes are small, steep-sided volcanoes that erupt primarily cinder-sized fragments. Stratovolcanoes are tall, conical volcanoes composed of alternating layers of lava flows, volcanic ash, and other materials.
No, shield volcanoes are not steep mountains. They have gently sloping sides due to the relatively low viscosity of the lava that flows from them, which allows the lava to spread out and create a wide, shield-like shape.
These volcanoes are called stratovolcanoes or composite volcanoes. They are characterized by their steep slopes and alternating layers of cinders, ash, and lava flows, typically made of basaltic and andesitic compositions.
The three main types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have broad, gently sloping sides and are mainly composed of basaltic lava flows. Stratovolcanoes are tall, steep-sided cones formed by alternating layers of lava flows and pyroclastic materials. Cinder cone volcanoes are small, steep-sided cones composed of pyroclastic material, often with a central vent.
Volcanoes can be classified based on their eruption style, shape, and location. Common types include shield volcanoes with broad, gently sloping sides, stratovolcanoes with steep sides and explosive eruptions, and cinder cone volcanoes with steep sides and a small crater. They are often found along tectonic plate boundaries or hot spots in the Earth's crust.
when lava flows down it the lava that stayed on it gets hard
What are the characterististicsc of the three types of volcanoes?
Gentle-sided volcanoes, also known as shield volcanoes, have broad and sloping sides with gently sloping eruptions of basaltic lava. Steep-sided volcanoes, also called stratovolcanoes, have steeper sides due to the buildup of layers of hardened lava, ash, and volcanic rocks from explosive eruptions. Examples of gentle-sided volcanoes include Mauna Loa in Hawaii, while examples of steep-sided volcanoes include Mount St. Helens in the United States.
The three main types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gently sloping sides and are formed by layers of lava flows. Stratovolcanoes are characterized by steep sides and explosive eruptions. Cinder cone volcanoes are small, steep-sided volcanoes built from explosive eruptions that eject fragmented rock.