The lava is very runny so it spreads out over a wide area. Over time the layers of lava create a volcanic mountain that has gently sloping sides.
shield volcanoes have gentle sides and aren't very tall
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.
Shield volcanoes are made from runny lava and steep sides. Cinder cone volcanoes are made from lava layers that alternate with layers of cinder. composite volcanoes shoot lav into the air.
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.
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.
shield volcanoes have gentle sides and aren't very tall
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.
shield volcanoes have gentle sides and aren't very tall
Shield volcanoes are made from runny lava and steep sides. Cinder cone volcanoes are made from lava layers that alternate with layers of cinder. composite volcanoes shoot lav into the air.
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.
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.
gently sloping volcanoes are called shield volcanoes and they are formed from many eruptions of lava that is relatively low in silica, so it spreads out in many thin layers and creates the gently sloping sides of a shield volcano.
The three types of volcanoes are shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Shield volcanoes have broad, gently sloping sides, cinder cone volcanoes are steep-sided with a circular or oval shape, and stratovolcanoes are tall, conical volcanoes built up by many layers of hardened lava, tephra, pumice, and volcanic ash.
Shield volcanoes, stratovolcanoes, and cinder cone volcanoes are three types of volcano forms. Shield volcanoes have broad, gently sloping sides, stratovolcanoes are characterized by their steep-sided cones, and cinder cone volcanoes are made of pyroclastic fragments.
Three basic shapes of volcanoes are shield volcanoes, which have broad and gentle slopes, stratovolcanoes (composite volcanoes), which have steep sides and are typically made of multiple layers of hardened lava, ash, and volcanic rocks, and cinder cone volcanoes, which are small and steep-sided with a crater at the summit formed from ejected volcanic fragments.
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.
The three main types of volcanoes are shield volcanoes, cinder cone volcanoes, and composite (or stratovolcanoes) volcanoes. Shield volcanoes have gently sloping sides and are formed by layers of lava, while cinder cone volcanoes are steep-sided with a conical shape and are made of pyroclastic material. Composite volcanoes are a mix of both lava and pyroclastic material, with a classic symmetrical cone shape.