GEOLOGY

Detailed explanation-1: -The most majestic of the volcanoes are composite volcanoes, also known as strato-volcanoes. Composite volcanoes are tall, symetrically shaped, with steep sides, sometimes rising 10, 000 feet high. They are built of alternating layers of lava flows, volcanic ash, and cinders.

Detailed explanation-2: -Composite volcanoes are also called stratovolcanoes. Some geologists avoid the use of the term “stratovolcano” because these volcanoes typically are not stratified and do not consist of orderly layers of lava flows and pyroclastic deposits.

Detailed explanation-3: -Composite or Stratovolcanoes (Fig. 5.14) erupt both lava and pyroclastic deposits. The slopes of stratovolcanoes are therefore composed of lava flows alternating with layers of pyroclastic deposits. Stratovolcanoes have steeper slopes than shield volcanoes and are common along convergent plate boundaries (Fig.

Detailed explanation-4: -Stratovolcanoes, also known as composite cones, are the most picturesque and the most deadly of the volcano types. Their lower slopes are gentle, but they rise steeply near the summit to produce an overall morphology that is concave in an upward direction.

Detailed explanation-5: -Mount Vesuvius, a stratovolcano, last erupted in March 1944, located in southern Italy. In 79 AD, Mount Vesuvius erupted covering the city of Pompeii in molten lava, ash, pumice volcanic blocks, and toxic gases.