Because the lava is so hot is heats the ocean water to the gas state (steam).
When pillow lava touches ocean water, the temperature of the water can increase significantly, sometimes reaching temperatures above 500 degrees Celsius. This can create steam and explosive reactions as the lava rapidly cools in the water.
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" 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.
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.
Water does cool lava, but not instantly. For one thing, lava is a poor conductor of heat, so when lava erupts underwater the outside cools fairly quickly to form solid crust, but the inside remains molten. Second, the water in contact with the lava or crust (which is still quite hot) boils and forms an insulating layer of steam.
Yes, the heat of the lava may well turn some of the water into steam, but the sea will cool & solidify the lava.
Victoria falls is made out of molten lava.
When pillow lava touches ocean water, the temperature of the water can increase significantly, sometimes reaching temperatures above 500 degrees Celsius. This can create steam and explosive reactions as the lava rapidly cools in the water.
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.
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.
Lava is very hot- it is melted rock. Hot rock + water= steam
Mid-ocean ridges typically produce basaltic magma, which is low in silica content and flows easily. This type of magma is associated with fast-spreading divergent plate boundaries and results in the formation of oceanic crust.
Lava
"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.
because hot thing that flow down in the cooler surface so they steamed up.
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.
red lava