shield volcanoes have gentle sides and aren't very tall
shield volcanoes have gentle sides and aren't very tall
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.
The three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by lava flows, stratovolcanoes are tall, steep-sided volcanoes built up by layers of hardened lava, rock, and ash, and cinder cone volcanoes are relatively small, steep-sided volcanoes made of pyroclastic material.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Because if you look at them from above, they look like a warrior's shield.
No, shield volcanoes are a specific type of volcano characterized by their broad, gentle slopes and low viscosity lava flows. "Volcano" is a general term that refers to any landform where volcanic activity occurs, encompassing a variety of volcano types such as shield, composite, and cinder cone volcanoes.
The Hawaiian islands are made of two types of volcanoes, shield volcanoes and cinder cone volcanoes. Shield volcanoes have broad bases with gentle slopes. Cinder cone volcanoes have steeper sides, are made from fragments of lava, and are usually located at the base of shield volcanoes.
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.
Kilauea is an example of a (shield) volcano.
A shield volcano typically has a broad, gently sloping dome shape with a large base and low profile. This shape is formed by numerous eruptions of low-viscosity basaltic lava that flow easily over long distances, building up the volcano gradually over time. The Hawaiian Islands are good examples of shield volcanoes.
The three different types of volcanoes include the following; shield volcanoes, composite volcanoes, and the cinder cone volcanoes. These all have their names because of the size and shape of the out rocks of the actual volcano itself.