Mostly fiery death.
When lava comes out the side of the volcano, it is called a lava flow or lava eruption. This can happen as a result of pressure build-up within the volcano causing the lava to find alternative pathways to reach the surface, often leading to lava flowing out from the sides.
Mars does not currently have active volcanic eruptions, so there is no flowing lava on its surface. However, evidence suggests that Mars had volcanic activity in the past, and there are remnants of volcanic features such as mountains, valleys, and ancient lava flows.
They are a group of volcanic islands either side of the Equator in the Pacific Ocean. A province of Ecuador
This is known as a volcanic vent.Gas and lava exit a volcano are through a volcanic vent or fissure and cool rapidly at the surface. Eruptions can be fluid or explosive.
When Mount Fuji erupted in 1707, it spewed ash and volcanic debris, affecting crops and disrupting daily life in the region. The eruption caused ash fall in Edo (modern-day Tokyo) and led to the formation of a new volcanic crater on the southeastern side of the mountain. The eruption lasted for over two weeks but did not result in any casualties.
can trigger landslides, and mudflow :)
A volcanic cinder cone.
The moon appears smooth on one side, known as the near side, because it is covered by large, flat plains called maria, formed by ancient volcanic activity. In contrast, the far side is heavily cratered and rugged, with fewer maria, due to its thicker crust and less volcanic activity. This difference is a result of tidal locking, where the same side of the moon always faces Earth, allowing for varied geological processes on each side.
A side vent in a volcano is a smaller opening located on the flanks of the main volcanic cone or crater. Side vents can release lava, gases, and ash during volcanic eruptions, providing additional pathways for volcanic activity to occur.
Represents the volcanic elevations
a volcanic vent is a channel way or opening through which magma ascends to the surface
Represents the volcanic elevations
Represents the volcanic elevations
The Moon's near side has more Maria (dark, smooth plains) than the far side because the lunar crust is thinner on the near side, allowing for more volcanic activity in the past. This resulted in more volcanic eruptions and lava flows creating the Maria that we see today. The far side of the Moon has a thicker crust, which limited the amount of volcanic activity.
Two examples of volcanic countries outside of the Caribbean are Iceland and the Philippines.
The far side of the Moon is characterized by a notable absence of large, flat maria (basaltic plains) that are prevalent on the near side. Instead, it features a more rugged terrain with a higher density of impact craters and mountainous regions. This difference is attributed to the thicker crust on the far side, which inhibited volcanic activity and the formation of maria. As a result, the far side presents a starkly different landscape compared to the near side.
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