Question

Identify the different parts of the volcano shown in the diagram. Write their names on the lines given near them.

$\huge\underline\mathfrak\green{Please \: answer \: the \: question}$
$\huge\underline\mathscr\purple{You \: will \: get \: 25 \: points}$
​

Answer 1

Answer:

niceeeeeeeeeeee brooooo

Answer 2

$\: \: \: \: \: \: \: \: \: \: \: \: \: \: \: \: \: \: \: \: \: \huge\mathscr{\underline{\underline{\red{Answer}}}}</p><p>$

Extra information

Vent

A volcanic vent is an opening exposed on the earth's surface where volcanic material is emitted. All volcanoes contain a central vent underlying the summit crater of the volcano.Fractures can also act as conduits for escaping volcanic gases, which are released at the surface through vent openings called fumaroles.

Parasitic cone

A parasitic cone is the cone-shaped accumulation of volcanic material not part of the central vent of a volcano. It forms from eruptions from fractures on the flank of the volcano. These fractures occur because the flank of the volcano is unstable.

Ash

Volcanic ash consists of fragments of rock, minerals, and volcanic glass, created during volcanic eruptions and measuring less than 2 mm in diameter. The term volcanic ash is also often loosely used to refer to all explosive eruption products, including particles larger than 2 mm.

Dike

Dikes are tabular or sheet-like bodies of magma that cut through and across the layering of adjacent rocks. They form when magma rises into an existing fracture, or creates a new crack by forcing its way through existing rock, and then solidifies.

Throat

Entrance of a volcano. The part of the conduit that ejects lava and volcanic ash.

Conduit

Some volcanoes have a single conduit, while others have a primary conduit with one or more additional conduits that branch off it.

Crater

A volcanic crater is an approximately circular depression in the ground caused by volcanic activity. It is typically a bowl-shaped feature within which occurs a vent or vents.

Summit

Highest point; apex. Throat - Entrance of a volcano. The part of the conduit that ejects lava and volcanic ash.

Lava

Magma is generated by the internal heat of the planet or moon and it is erupted as lava at volcanoes or through fractures in the crust, usually at temperatures from 700 to 1,200 °C (1,292 to 2,192 °F). The solid rock resulting from subsequent cooling is also often described as lava.

Sill

a sill is a tabular sheet intrusion that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or along the direction of foliation in metamorphic rock. A sill is a concordant intrusive sheet, meaning that a sill does not cut across preexisting rock beds.

Flank

A flank eruption is a volcanic eruption which occurs on the flanks of a volcano, instead of at its summit. Such eruptions occur when the conduit connecting the summit to the magma chamber below is blocked, forcing the magma to move laterally.

Base

A caldera is a basin-like feature formed by collapse of land after a volcanic eruption. This happens after a huge stratovolcano blows its top off. The base of the crater then sinks, leaving a caldera where the top of the volcano was before.