Volcanic particles about the size of rice grains are called volcanic ash. Ash is made up of small rock and mineral fragments that are expelled during a volcanic eruption.
When lava stops erupting out of the central vent, it solidifies and forms a volcanic rock structure called a volcanic plug or volcanic dome at the top of the vent. These structures can vary in size and shape depending on the type of lava that was erupted and the eruption style.
Eruption products are the materials expelled during a volcanic eruption. They can include various forms of rock, ash, lava flows, gas, and volcanic dust. These products vary in composition and size, ranging from fine ash to large volcanic rocks, and they contribute to the formation of new geological features and can impact the surrounding environment and climate. Eruption products play a key role in understanding volcanic activity and its effects on ecosystems and human settlements.
Large volcanoes that rise from the sea floor are called seamounts or underwater volcanoes. These formations are created by volcanic activity beneath the ocean's surface and can vary in size and shape.
VEI is the volcanic explosivity index. It rates the severity of explosive volcanic eruptions based on the volume of material ejected and the height of the eruption plume. The scale ranges from VEI 0, indicating a non-explosive eruption, to VEI 8, indicating a super eruption. Each step up the scale represents a tenfold increase in the size of the eruption.
Pyroclastic fall is the volcanic hazard made up of rocky particles about the size of a grain of sand. These particles are ejected during an explosive eruption and can pose a threat to both life and property.
The worlds youngest island is Surtsey, one of the islands in Iceland. After a volcanic eruption in 1963. after the eruption subsided in 1967, erosion had caused it to become smaller in size.
Volcanic mountains are formed when magma rises towards the Earth's surface through a weak spot in the Earth's crust, causing a volcanic eruption. Over time, repeated eruptions build up layers of solidified lava and volcanic ash, creating a mountain. The shape and size of the mountain depend on the type of eruption and the characteristics of the magma.
Volcanic bombs are formed when lava is ejected from a volcanic vent in a semi-molten state. The lava is then shaped into a projectile by the force of the eruption and it solidifies before hitting the ground. The shape and size of volcanic bombs depend on the viscosity of the lava and the intensity of the eruption.
The various types of material ejected by a volcano are called volcanic products, which can include ash, lava flows, pyroclastic flows, volcanic gases, and volcanic bombs. These materials vary in size, composition, and behavior depending on the type of volcano and the eruption style.
Tephra is the term used to describe bits of material, such as ash, rocks, and other debris, that fall to the Earth after a volcanic eruption. Tephra can vary in size and composition depending on the nature of the eruption.
The ash from volcanic eruptions can reach altitudes of up to 20-30 kilometers into the atmosphere. The exact height can vary depending on the size and intensity of the eruption.