Around the Pacific Rim is Indonesia, a nation built from the dotted volcanoes of an island arc. Indonesia is distinctive for its rich volcanic soil, tropical climate, tremendous biodiversity, and volcanoes. These volcanoes are in Java, Indonesia.
The most obvious landforms created by lava are volcanoes, most commonly as cinder cones, composite volcanoes, and shield volcanoes. Eruptions also take place through other types of vents, commonly from fissures (Figure below). The eruptions that created the entire ocean floor are essentially fissure eruptions.
A fissure eruption on Mauna Loa in Hawaii travels toward Mauna Kea on the Big Island.
Viscous lava flows slowly. If there is not enough magma or enough pressure to create an explosive eruption, the magma may form a lava dome. Because it is so thick, the lava does not flow far from the vent. (Figure below).
Lava domes are large, round landforms created by thick lava that does not travel far from the vent.
Lava flows often make mounds right in the middle of craters at the top of volcanoes, as seen in the Figure below.
Lava domes may form in the crater of composite volcanoes as at Mount St. Helens.
A lava plateau forms when large amounts of fluid lava flow over an extensive area (Figure below). When the lava solidifies, it creates a large, flat surface of igneous rock.
Layer upon layer of basalt have created the Columbia Plateau, which covers more than 161,000 square kilometers (63,000 square miles) in Washington, Oregon, and Idaho.
Lava creates new land as it solidifies on the coast or emerges from beneath the water (Figure below).
Lava flowing into the sea creates new land in Hawaii.
Over time the eruptions can create whole islands. The Hawaiian Islands are formed from shield volcano eruptions that have grown over the last 5 million years (Figure below).
The island of Hawaii was created by hotspot volcanism. You can see some of the volcanoes (both active and extinct) in this mosaic of false-color composite satellite images.
Magma intrusions can create landforms. Shiprock in New Mexico is the neck of an old volcano that has eroded away (Figure below). The volcanic neck is the remnant of the conduit the magma traveled up to feed an eruption.
The aptly named Shiprock in New Mexico.
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NOTES / HIGHLIGHTS
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| Image | Reference | Attributions |
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| Credit: 16028122 Source: https://pixabay.com/photos/indonesia-java-bromo-volcano-5217694/ License: Pixabay License | ||
| Credit: Courtesy of DW Peterson/US Geological Survey;Zappy's Source: http://volcanoes.usgs.gov/images/pglossary/FissureEruption_examps.php License: Public Domain; CC BY-NC 3.0 | ||
| Credit: User:Brian0918/Wikipedia;Zappy's Source: http://commons.wikimedia.org/wiki/File:Valle_Grande_dome.jpg License: Public Domain; CC BY-NC 3.0 | ||
| Credit: Courtesy of Willie Scott/US Geological Survey;Zappy's Source: http://commons.wikimedia.org/wiki/File:MSH06_aerial_crater_from_north_high_angle_09-12-06.jpg License: Public Domain; CC BY-NC 3.0 | ||
| Credit: Kelvin Kay (User:Kkmd/Wikipedia);Zappy's Source: http://commons.wikimedia.org/wiki/File:Vistahouse.jpg License: Public Domain; CC BY-NC 3.0 | ||
| Credit: Vlad and Marina Butsky;Zappy's Source: http://www.flickr.com/photos/butsky/357672637/ License: CC BY 2.0; CC BY-NC 3.0 | ||
| Credit: Courtesy of NOAA Coastal Services Center Hawaii Land Cover Analysis project;Zappy's Source: http://earthobservatory.nasa.gov/IOTD/view.php?id=2449 License: Public Domain; CC BY-NC 3.0 | ||
| Credit: Bowie Snodgrass;Zappy's Source: http://commons.wikimedia.org/wiki/File:Shiprock.snodgrass3.jpg License: CC BY 2.0; CC BY-NC 3.0 |
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