A shield volcano can range in size depending on scale, but in height they are relatively low compared to diameter. They have shallow slopes. They are shaped, as the name suggests, like round shields of the classical world.
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.
Shield volcanoes are in the shape of a shield. Hence, the name shield volcano! Shield volcanoes are tall and broad with flat rounded shapes. They have low slpes and almost always have large craters. Shield volcanoes form from eruptions of flowing lava. THe lava spreads out and builds up volcanoes with broad, gently, sloping sides. One example of a shield volcano is the Hawaiian Islands.
Not necessarily. Shield volcanoes are volcanoes, but not all volcanoes are shield volcanoes.
Shield volcanoes are different from the commonly imagined volcano because they have a broad, gently sloping shape resembling a shield rather than a tall, conical shape. They are formed by the eruption of low-viscosity lava that flows easily over long distances, creating the shield-like shape. This type of volcano typically has less explosive eruptions and is associated with more effusive, continuous lava flows.
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 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.
Shield volcanoes are in the shape of a shield. Hence, the name shield volcano! Shield volcanoes are tall and broad with flat rounded shapes. They have low slpes and almost always have large craters. Shield volcanoes form from eruptions of flowing lava. THe lava spreads out and builds up volcanoes with broad, gently, sloping sides. One example of a shield volcano is the Hawaiian Islands.
False. The magma of shield volcanoes is silica-poor.
Not necessarily. Shield volcanoes are volcanoes, but not all volcanoes are shield volcanoes.
They are shield volcanoes. This means that they are cone shaped but with very shallow slope angles forming the volcanoes flank.
Shield volcanoes are different from the commonly imagined volcano because they have a broad, gently sloping shape resembling a shield rather than a tall, conical shape. They are formed by the eruption of low-viscosity lava that flows easily over long distances, creating the shield-like shape. This type of volcano typically has less explosive eruptions and is associated with more effusive, continuous lava flows.
shield volcanos are basalt volcanoes and they are ussaly the smaller of the three tpes of volcanoes starting with rylotic then andesitic then basalt .so you cant put a actuall meausrement on the size of a shiel volcano. Answer #2: The shield volcanoes are produced by the accumulation of basaltic fluid and exhibit the shape of a broad, slightly domed structure that resembles a warrior's shield. Most shield volcanoes have grown from the deep ocean floor to form islands or seamounts. An example of a shield volcano is the Mauna Loa, which is Earth's largest volcano, from its base on the ocean floor of the Pacific Ocean to its summit, Mauna Loa is over 9 kilometers (6 miles) high.
There are three types of volcanoes which have different shapes and types of eruptions. * Shield Volcanoes - are low and flat and have small, flowing eruptions. * Composite Volcanoes - are a mixture between shield volcanoes and cone volcanoes, their eruptions are explosive. * Cone Volcanoes - are the tallest and largest volcanoes, and they have VERY explosive eruptions.
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 most obvious difference between the three types of volcanoes are their size. Shield volcanoes are the largest, followed by composite volcanoes, leaving cinder cone volcanoes as the smallest.
The Hawiian islands are formed by shield volcanoes.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.