Shield volcanoes almost always emit very fluid or runny lava that spreads over a wide distance, so these volcanoes are not steep.
Yes and no, it depends where and how the volcano forms, when it discombobulates, and so on.
No they are not steep
shield volcanoes have gentle sides and aren't very tall
Not necessarily. Shield volcanoes are volcanoes, but not all volcanoes are shield volcanoes.
There are similarities and differences. Cinder cones are generally much smaller than shield volcanoes or stratovolcanoes. Like shield volcanoes, they primarily erupt basaltic lava. However, like stratovolcanoes they have steep slopes and are composed of material that has erupted into the air and been welded together.
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.
No they are not steep
shield volcanoes have gentle sides and aren't very tall
shield volcanoes have gentle sides and aren't very tall
No. Shield volcanoes have gentle slopes composed almost entirely of cooled lava flows.
Not necessarily. Shield volcanoes are volcanoes, but not all volcanoes are shield volcanoes.
There are similarities and differences. Cinder cones are generally much smaller than shield volcanoes or stratovolcanoes. Like shield volcanoes, they primarily erupt basaltic lava. However, like stratovolcanoes they have steep slopes and are composed of material that has erupted into the air and been welded together.
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.
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 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.
Both shield volcanoes and cinder cones erupt low-viscosity basaltic lava and have eruptions that are only mildly explosive if at all.Cinder cones are small, steep-sloped volcanoes composed primarily of a chunky variety of basalt called scoria.Shield volcanoes are large, gently sloping volcanoes composed primarily of layers of lava flows.
The Hawiian islands are formed by shield volcanoes.
There are three kinds of cone volcanoes shield cones, composite cones, and cinder cones. Shield cones have very fluid lava. They erupt with a quiet lava flow. An example of a shield cone volcano is Mauna Loa. A shield cone is pretty much a little dome that has been flattened. Composite cones have sticky lava and rock bits. They have the most explosive eruptions An example of a composite cone volcano is Vesuvius. Composite cones are steep at the top but gentle at the bottom. Cinder cones have cinders. They have explosive eruptions An example is Paricutin. A cinder cone is very steep.