Types of Volcanic Vents

Updated on October 31, 2016
unvrso profile image

Unvrso has been writing varied topics of literature since 2005 and started writing for hubpages in 2009.

Fractures on Top of Volcanoes Through Where Lava is Ejected

Volcanic Vent on Top of a Volcano
Volcanic Vent on Top of a Volcano | Source

What is a Volcanic Vent?

Volcanic vents are openings in the Earth's crust from which lava and pyroclastic flows are ejected. Their forms determine the varied types of eruptions that gave them shape. Volcanic vents originate in the magma chamber - an underground pool of liquefied rock (magma) underneath the surface of the Earth. The liquefied rock in the magma chamber is subject to great increasing pressure, and over time, it fractures the Earth's crust, creating a volcanic vent.

Most volcanic eruptions find their way out to the surface through a central vent; however, some other volcanic eruptions may blast out portions of the side of a mountain, producing fractures on the Earth's crust known as fissures. When volcanic eruptions of blasting lava have ceased, volcanic vents continue releasing steam and gas fumes through small openings surrounding a volcano which are called fumaroles.

Central Volcanic Vent From Above

Volcanic Vents
Volcanic Vents | Source

Test your knowledge

view quiz statistics

Types of Volcanic Vents

Central vents are the most common types of volcanic vents. Central vents are the conduit pipes through which magma is forced upward to the surface of the Earth, and then ejected as gases, lava or pyroclastic fragments. A central vent connects the magma chamber to the open vent on top of a volcano, and is maintained open by the continuous release of volcanic material. A central vent sometimes can be enlarged by the collapse of its peripheral walls. Eruptions may also occur through fissures made in the volcanic conduit pipe and flowing out through a linear vent on the side of a shield volcano.

There are many types of volcanic vents and all of them are defined by the characteristics of their formation, such as the type of magma and eruption. They are located everywhere magma and gases are allowed to break through the earth´s crust; either in continental land and in the ocean floor.

Long openings on the Earth's Crust

Fissures | Source

Volcanic Fissure (Eruption fissure)

Fissures are linear volcanic vents through which lava and gases spew, although not as explosive as in a central vent eruption. Fissures on the ground can be of a few meters wide by many kilometers long. Lava ejected from fissures produce basalt flows and lava channels; the spills of lava in every direction produce ramparts on both sides of the channel.

This type of vents are usually seen from an airplane as fractures on the ground, and they lack a central caldera. Fissures are often found along rift zones, including the East African Rift and Iceland. They’re a common feature on the flanks of shield volcanoes through which they connect to magma reservoirs underground.


Fumaroles | Source

Opening on the Earth's Crust

Fumaroles are other type of volcanic vents that form around volcanoes as openings on the Earth's crust; sometimes in collections of fumaroles. They can be seen emitting gases, along with water vapor, which forms a white cloud of varied sizes. Although, fumaroles do not eject lava, they need the heating source from the underground in order to gain the necessary temperature for the water and pressure for the gases to scape to the outside atmosphere.

Fumaroles emit steam, which is created, when super-heated water turns into steam due to a drop in pressure as it emerges from the underground. Fumaroles also emit gases, including carbon dioxide, sulfur dioxide, hydrogen sulfide and hydrogen chloride. Some fumaroles may remain active for weeks or maybe months if they occur on top of a volcanic deposit that quickly cools, while others may persist for longer spans of time if they are atop a constant high temperature source.

Mount St. Helens

Mount St. Helens
Mount St. Helens | Source

Eruption of Mt. St. Helens

Some eruptions can be very destructive. Most eruptions detonate through a central vent; however, there have been occasions when powerful volcanic eruptions explode out through fissures on the flanks of a volcano. This usually happens when the forces underground, including the accumulation of gases, pressure and heat combine to create a tremendous force blasting away the side of a mountain. This is what occurred during the 1980 eruption of Mount St. Helens in Washington.

The tremendous pressure developed a bulge on the north side of Mount St. Helens. Suddenly! The pressure and heat contained in its interior, along with the gases dissolved in the magma, caused the escaping of these volcanic materials through the cracks and voids of the mountain, blasting out a large portion of the mount and creating a 1.2 by 1.8 miles volcanic crater. Days later, Mt. St. Helens was 396 meters (1,300 ft.) shorter and a huge crater 3.2 km (2 miles) across by 500 meters (3.1 miles) deep developed on its top.

Black Smoker

Black Smoker
Black Smoker | Source

Hydrothermal Vents (black smokers and white smokers)

There are other types of volcanic vents. Some are found along deep submarine mountain ridges in the ocean floor, and others on continental land, and they’re known as hydrothermal vents. These types of vents develop when underground water comes in contact with the hot magma; it becomes heated, and finally escapes through earth´s crust, rising as steam and gas into the ocean or the atmosphere.

On the ocean floor, hydrothermal vents are formed at spreading ridges and convergent plate boundaries, when jets of varied minerals come in contact with the freezing water of the ocean floor. Back smokers are formed when sulfide minerals mix with the cold ocean water and white smokers when deposits of calcium, barium and silicon come in contact with the freezing water.

Hot Spring

Hot Spring
Hot Spring | Source

Hot Springs

On continental land, water spouting from a hot spring is heated by the earth´s mantle (geochemically). Generally, in the earth’s mantle, temperature rises with increasing depth. When water penetrates deep enough into the earth´s interior, it may be heated to reach the boiling point; the steam formed escapes through the fissures made in the earth´s crust.

Hot spring´s temperatures may range from warm, good enough for a bath, to super-heated, in which case, it may represent a hazard for people.


Pyroclastic flow
fragments of superheated gas and rock
fractures on the Earth's crust through where gas fumes and steam are ejected
long fracture through which lava erupts
Central vent
Magma chamber
Liquefied lava
conductive channel through where magma is ejected
underground pool of liquid rock

Questions & Answers

  • Can vent tube walls consist of metamorphic rocks and shells?

    There are three main types of rocks; igneous, sedimentary and metamorphic. The differences among them rely on the way in which they are formed. Sedimentary rocks are formed of sand, pebbles, and shells of living organisms. Igneous rocks are formed when molten lava has cooled after an eruption.

    Metamorphic rock forms when sedimentary, igneous or metamorphic rock is subjected to high pressures under the earth´s crust or at extremely high temperatures inside the earth or close contact with molten magma; this is called contact metamorphism and occurs when the molten magma travels through the orifice of a volcano.

© 2012 Jose Juan Gutierrez


Submit a Comment
  • profile image

    Luke Hemmings 

    5 years ago



This website uses cookies

As a user in the EEA, your approval is needed on a few things. To provide a better website experience, owlcation.com uses cookies (and other similar technologies) and may collect, process, and share personal data. Please choose which areas of our service you consent to our doing so.

For more information on managing or withdrawing consents and how we handle data, visit our Privacy Policy at: https://maven.io/company/pages/privacy

Show Details
HubPages Device IDThis is used to identify particular browsers or devices when the access the service, and is used for security reasons.
LoginThis is necessary to sign in to the HubPages Service.
Google RecaptchaThis is used to prevent bots and spam. (Privacy Policy)
AkismetThis is used to detect comment spam. (Privacy Policy)
HubPages Google AnalyticsThis is used to provide data on traffic to our website, all personally identifyable data is anonymized. (Privacy Policy)
HubPages Traffic PixelThis is used to collect data on traffic to articles and other pages on our site. Unless you are signed in to a HubPages account, all personally identifiable information is anonymized.
Amazon Web ServicesThis is a cloud services platform that we used to host our service. (Privacy Policy)
CloudflareThis is a cloud CDN service that we use to efficiently deliver files required for our service to operate such as javascript, cascading style sheets, images, and videos. (Privacy Policy)
Google Hosted LibrariesJavascript software libraries such as jQuery are loaded at endpoints on the googleapis.com or gstatic.com domains, for performance and efficiency reasons. (Privacy Policy)
Google Custom SearchThis is feature allows you to search the site. (Privacy Policy)
Google MapsSome articles have Google Maps embedded in them. (Privacy Policy)
Google ChartsThis is used to display charts and graphs on articles and the author center. (Privacy Policy)
Google AdSense Host APIThis service allows you to sign up for or associate a Google AdSense account with HubPages, so that you can earn money from ads on your articles. No data is shared unless you engage with this feature. (Privacy Policy)
Google YouTubeSome articles have YouTube videos embedded in them. (Privacy Policy)
VimeoSome articles have Vimeo videos embedded in them. (Privacy Policy)
PaypalThis is used for a registered author who enrolls in the HubPages Earnings program and requests to be paid via PayPal. No data is shared with Paypal unless you engage with this feature. (Privacy Policy)
Facebook LoginYou can use this to streamline signing up for, or signing in to your Hubpages account. No data is shared with Facebook unless you engage with this feature. (Privacy Policy)
MavenThis supports the Maven widget and search functionality. (Privacy Policy)
Google AdSenseThis is an ad network. (Privacy Policy)
Google DoubleClickGoogle provides ad serving technology and runs an ad network. (Privacy Policy)
Index ExchangeThis is an ad network. (Privacy Policy)
SovrnThis is an ad network. (Privacy Policy)
Facebook AdsThis is an ad network. (Privacy Policy)
Amazon Unified Ad MarketplaceThis is an ad network. (Privacy Policy)
AppNexusThis is an ad network. (Privacy Policy)
OpenxThis is an ad network. (Privacy Policy)
Rubicon ProjectThis is an ad network. (Privacy Policy)
TripleLiftThis is an ad network. (Privacy Policy)
Say MediaWe partner with Say Media to deliver ad campaigns on our sites. (Privacy Policy)
Remarketing PixelsWe may use remarketing pixels from advertising networks such as Google AdWords, Bing Ads, and Facebook in order to advertise the HubPages Service to people that have visited our sites.
Conversion Tracking PixelsWe may use conversion tracking pixels from advertising networks such as Google AdWords, Bing Ads, and Facebook in order to identify when an advertisement has successfully resulted in the desired action, such as signing up for the HubPages Service or publishing an article on the HubPages Service.
Author Google AnalyticsThis is used to provide traffic data and reports to the authors of articles on the HubPages Service. (Privacy Policy)
ComscoreComScore is a media measurement and analytics company providing marketing data and analytics to enterprises, media and advertising agencies, and publishers. Non-consent will result in ComScore only processing obfuscated personal data. (Privacy Policy)
Amazon Tracking PixelSome articles display amazon products as part of the Amazon Affiliate program, this pixel provides traffic statistics for those products (Privacy Policy)
ClickscoThis is a data management platform studying reader behavior (Privacy Policy)