If they are the same shapes but differ only in size, then they are SIMILAR shapes. Otherwise, they are simply different shapes.
Yes - even shapes with different area.
Yes many different shapes can have the same volume
Organic shapes are shapes with a natural look and a flowing and curving appearance.
even shapes diffrent area
There are three main shapes of volcanoes: shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Each type has distinct characteristics based on its eruption style, lava composition, and shape.
Cinder cone volcanoes differ from shield and stratovolcanoes in terms of their shape, size, and eruption style. Cinder cones are typically smaller, with steep sides created by the accumulation of volcanic rock fragments. Shield volcanoes are large and have gentle slopes due to the fluid lava flows, while stratovolcanoes are characterized by their tall, conical shape and explosive eruptions caused by the interaction of magma with water.
Yes, Mount Aso is a caldera complex in Japan, comprising several stratovolcanoes. It is not a shield volcano, as shield volcanoes are typically characterized by gentle slopes and broad, flattened shapes, whereas Mount Aso has a more complex and irregular topography due to its formation as a caldera.
Both shield volcanoes and stratovolcanoes can form islands.
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Volcanoes can have various shapes depending on their eruption style and the material they are made of. Common shapes include shield volcanoes with gentle sloping sides, stratovolcanoes with steep-sided cones, cinder cone volcanoes with a circular or oval shape, and calderas which form when a volcano collapses into its emptied magma chamber.
Yes, the volcanoes in Iceland are primarily shield volcanoes. They are characterized by gentle sloping sides and a large central crater. The most famous shield volcano in Iceland is Snæfellsjökull.
Stratovolcanoes, shield volcanoes, and complex volcanoes have all formed islands.
No. Mount Vesuvius is a stratovolcano, but Kilauea is a shield volcano.
The different shapes of volcanoes include shield volcanoes, which have gentle slopes and are formed by fluid lava flows; stratovolcanoes, which have steep-sided slopes and are formed by alternating layers of lava and ash; and cinder cone volcanoes, which have steep slopes and are formed by explosive eruptions of ash and rock 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 six types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), cinder cone volcanoes, supervolcanoes, submarine volcanoes, and fissure vents. Each type of volcano is characterized by different eruption styles, shapes, and compositions.