Lava is a volcanic by-product. there are submarine volcanoes. It is not known whether they have caused or contributed to submarine ( the ships) accidents but it could happen. another possibililty is that a bomb or depth charge that is intended to attack a submarine falls into a sub-volcano- explodes, and sets of an eruption unplanned by the Destroyer or bomber that dropped the charge!
That would be the result of a submarine volcano. Pillow lava is a common type of lava that submarine volcanoes produce.
Submarine lava flows create unique shapes and formations due to rapid cooling and solidification in cold ocean water. These flows can result in features like pillow lavas, which form rounded shapes, and sheet flows, which can stretch over large areas due to their fluid nature. Submarine lava flows also release gases that can form bubbles which get trapped in the solidified lava, creating vesicles.
Both pillow lava and pahoehoe lava are types of basaltic lava that form during submarine volcanic eruptions. They both have smooth, ropy surfaces, caused by the flow of lava, and are relatively low in viscosity.
Pillow lava erupts underwater and forms rounded lumps or pillow-shaped structures due to the rapid cooling of molten lava when it comes into contact with water. This type of lava flow is commonly found at mid-ocean ridges and submarine volcanoes.
When lava cools underwater, it usually forms a type of igneous rock known as pillow lava. This occurs because the rapid cooling of lava in water causes it to solidify quickly and take on a rounded, pillow-like shape. Pillow lava formations are commonly found at mid-ocean ridges and undersea volcanoes.
Submarine volcanoes seldom erupt with an explosion because of the enormous pressure exerted by the weight of water above. This pressure prevents the buildup of gas bubbles that are necessary for explosive eruptions on land. Instead, submarine eruptions usually result in more gentle, effusive flows of lava.
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Pillow lava is a type of basaltic lava that forms underwater when lava erupts on the ocean floor. It cools quickly, creating pillow-shaped structures. These formations resemble stacked pillows due to the outer crust solidifying quickly while the lava inside continues to flow, resulting in rounded shapes. Pillow lava is commonly found in mid-ocean ridges and submarine volcanic environments.
Pillow lavas are associated with underwater volcanic eruptions, where lava cools rapidly upon contact with water, forming characteristic pillow-like shapes. These formations are common in submarine volcanic environments, such as mid-ocean ridges and seamounts. Pillow lavas provide valuable insights into the Earth's tectonic and volcanic processes.
Volcanoes that are underwater, known as submarine volcanoes. The deepest one is the Submarine 1922 in the Celebes Sea near the Sanghie Islands of Indonesia, and it is 16,000 feet (5,000 meters) below sea level.
You drag the word "submarine" itself onto the submarine. Then you wait for it to sink.
"Yellow Submarine"because my friend had to play it for a exam.