well actually the water never gets hot
An underwater lava flow is called "pillow lava" when it forms from the rapid cooling of lava upon contact with water. This type of lava takes on a rounded, pillow-like shape due to the formation of a crust that traps the molten lava inside, which then expands and breaks through the surface. Pillow lava is commonly found at mid-ocean ridges and volcanic ocean floors.
When lava cools in the ocean, it forms a type of rock called pillow basalt. This distinctive rock gets its name from its pillow-like shape that results from the rapid cooling of lava in water. Pillow basalt is commonly found in areas where underwater volcanic eruptions occur.
Pillow basalt forms when basaltic lava erupts underwater and cools rapidly, creating pillow-shaped structures. Water cools the lava quickly, causing it to solidify into distinctive pillow-like shapes as it is extruded.
"Pillow basalt" formations, which are round or tubular structures that result from the rapid cooling of lava under water. This process occurs when hot lava erupts into the ocean and solidifies quickly, forming these distinctive shapes.
Pillow lava is the result of underwater volcanic eruptions. When hot magma is extruded onto the ocean floor, it cools rapidly and forms pillow-shaped structures due to the rapid cooling process in the water.
An underwater lava flow is called "pillow lava" when it forms from the rapid cooling of lava upon contact with water. This type of lava takes on a rounded, pillow-like shape due to the formation of a crust that traps the molten lava inside, which then expands and breaks through the surface. Pillow lava is commonly found at mid-ocean ridges and volcanic ocean floors.
When lava cools in the ocean, it forms a type of rock called pillow basalt. This distinctive rock gets its name from its pillow-like shape that results from the rapid cooling of lava in water. Pillow basalt is commonly found in areas where underwater volcanic eruptions occur.
Pillow basalt forms when basaltic lava erupts underwater and cools rapidly, creating pillow-shaped structures. Water cools the lava quickly, causing it to solidify into distinctive pillow-like shapes as it is extruded.
"Pillow basalt" formations, which are round or tubular structures that result from the rapid cooling of lava under water. This process occurs when hot lava erupts into the ocean and solidifies quickly, forming these distinctive shapes.
Pillow lava is the result of underwater volcanic eruptions. When hot magma is extruded onto the ocean floor, it cools rapidly and forms pillow-shaped structures due to the rapid cooling process in the water.
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.
Pillow lava is formed when hot basaltic lava erupts underwater, typically at mid-ocean ridges or volcanic islands. As the lava flows out and comes into contact with the cold ocean water, it rapidly cools and solidifies, creating a rounded, pillow-like shape. The outer surface solidifies quickly while the interior remains molten, leading to the formation of these distinctive structures. As more lava is expelled, additional layers of pillow lava are created, often resulting in a stacked appearance.
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.
False. Basaltic lava sometimes is erupted under water or flows into the ocean. It makes a formation like a pile of pillows on the sea bottom. Pillow lava crystallizes quickly from the outside to the inside of each "pillow." Lava of this type forms only under water. Pillow lavas are found on many mountains throughout the world.
When a volcano ejects lava from the ocean floor, the lava cools very rapidly. This causes the outside of the lava plume to solidify. Pressure builds inside this lava pillow, as it is usually described, until it breaks through a weak area in the pillow "shell" and forms a new lava pillow. The process repeats until the lava source is exhausted or the pressure wanes.
in a volcano Pillow lava forms only when lava emerges from a place that is submerged under water.
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.