You can die if you do not get away quickly. The radiant heat from a lava flow, especially a basaltic lava flow, is very intense. Being close to a large flow without protection can quickly kill a person. Fortunately, these flows are slow moving, and the same radiated heat will often make it unbearable to get any closer before you could get close enough for it to kill you.
it doesn't
Lava that erupts underwater and takes the form of round lumps is called pillow lava
This type of lava is known as pillow lava. When molten lava is erupted underwater, it quickly cools and solidifies into pillow-shaped structures due to the rapid cooling effect of the surrounding water. Over time, multiple layers of pillow lava can accumulate to form underwater volcanic structures.
Underwater eruptions cause tsunamis and cause lava to form and underwater ridge.
Underwater lava, also known as pillow lava, cools more rapidly due to the surrounding water, resulting in a characteristic pillow-like shape. Surface lava, on the other hand, tends to flow more freely and can form different structures like pahoehoe or aa lava flows. Additionally, underwater lava interactions with water can trigger explosive reactions due to rapid cooling and fragmentation.
it doesn't
Lava that erupts underwater and takes the form of round lumps is called pillow lava
This type of lava is known as pillow lava. When molten lava is erupted underwater, it quickly cools and solidifies into pillow-shaped structures due to the rapid cooling effect of the surrounding water. Over time, multiple layers of pillow lava can accumulate to form underwater volcanic structures.
Underwater eruptions cause tsunamis and cause lava to form and underwater ridge.
Pillow lava
because it is
Underwater lava, also known as pillow lava, cools more rapidly due to the surrounding water, resulting in a characteristic pillow-like shape. Surface lava, on the other hand, tends to flow more freely and can form different structures like pahoehoe or aa lava flows. Additionally, underwater lava interactions with water can trigger explosive reactions due to rapid cooling and fragmentation.
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.
It burns
Underwater lava, known as pillow lava, cools more rapidly than surface lava due to the rapid transfer of heat to the surrounding water. This results in the formation of rounded, pillow-shaped structures. Additionally, underwater lava may be more enriched in certain elements due to interactions with seawater.
The lava itself is not different, it is the environment that is different. Water is much denser than air and has a higher heat capacity, meaning it takes more energy to heat it up. As a result, lava will lose heat to water extremely quickly, and so will cool much faster than it can on land.
Volcanoes underwater erupt in much the same way as those on dry land. They erupt when pressure builds up. The difference between these two types of volcanoes is that the lava produced in an underwater volcano cools dramatically faster than the lava on land.