Its definently "Pillow Lava".
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.
Lava that erupts underwater and takes the form of round lumps is called pillow 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.
Pillow lava is basaltic lava that forms rounded pillow like lumps. It forms when a volcano erupts fairly deep underwater. Lava erupts bu quickly crusts over, creating a bulbous formation. The crust then breaks and more lava spills out, continuing the process.See the link below for a video of pillow lava.
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
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.
Lava that erupts underwater and takes the form of round lumps is called pillow 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.
Pillow lava
Pillow lava is basaltic lava that forms rounded pillow like lumps. It forms when a volcano erupts fairly deep underwater. Lava erupts bu quickly crusts over, creating a bulbous formation. The crust then breaks and more lava spills out, continuing the process.See the link below for a video of pillow lava.
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 got its name because of its distinctive pillow-like shapes that form when lava flows underwater and cools rapidly. As the outer layer of lava cools and solidifies quickly upon contact with water, it forms a rounded mound resembling a pillow. This unique shape is characteristic of lava flows in underwater volcanic environments.
This is called a lava dome.
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.
it doesn't
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.