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What side effect can result from volcanic activity?

can trigger landslides, and mudflow :)


What is a steep side?

A volcanic cinder cone.


Why does the moon look smooth on one side and rough on the other side?

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.


What is the definition of a side vent in a volcano?

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.


What do the side in the model represent?

Represents the volcanic elevations


What are volcanic vents and side vents?

a volcanic vent is a channel way or opening through which magma ascends to the surface


What do the side slits in the model represent?

Represents the volcanic elevations


What do the side slit in the model represent?

Represents the volcanic elevations


Why are more Maria found on the side of the moon facing earth than on the opposite side?

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.


Name of two volcanic islands out side of the Caribbean?

Two examples of volcanic countries outside of the Caribbean are Iceland and the Philippines.


What surface features are almost completely absent on the far side?

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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