{"id":2093,"date":"2016-06-06T22:38:20","date_gmt":"2016-06-06T22:38:20","guid":{"rendered":"https:\/\/courses.lumenlearning.com\/geologyxwaymakerxmaster\/?post_type=chapter&p=2093"},"modified":"2025-10-13T17:03:00","modified_gmt":"2025-10-13T17:03:00","slug":"reading-volcanic-landforms","status":"publish","type":"chapter","link":"https:\/\/courses.lumenlearning.com\/geo\/chapter\/reading-volcanic-landforms\/","title":{"raw":"Reading: Volcanic Landforms","rendered":"Reading: Volcanic Landforms"},"content":{"raw":"
\r\n\r\n\"A\r\n\r\nWhy is the Republic of Indonesia made of 17,508 islands?\r\n\r\nAround 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.\r\n\r\n<\/div>\r\n

Landforms from Lava<\/h2>\r\n

Volcanoes and Vents<\/h3>\r\nThe 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 1). The eruptions that created the entire ocean floor are essentially fissure eruptions.\r\n\r\n[caption id=\"attachment_2191\" align=\"aligncenter\" width=\"500\"]\"A Figure 1. A fissure eruption on Mauna Loa in Hawaii travels toward Mauna Kea on the Big Island.[\/caption]\r\n

Lava Domes<\/h3>\r\nViscous 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 2).\r\n\r\n[caption id=\"attachment_2190\" align=\"aligncenter\" width=\"500\"]\"Picture Figure 2. Lava domes are large, round landforms created by thick lava that does not travel far from the vent.[\/caption]\r\n\r\nLava flows often make mounds right in the middle of craters at the top of volcanoes, as seen in the Figure 3.\r\n\r\n[caption id=\"attachment_2189\" align=\"aligncenter\" width=\"500\"]\"Lava Figure 3. Lava domes may form in the crater of composite volcanoes as at Mount St. Helens.[\/caption]\r\n\r\n \r\n

Lava Plateaus<\/h3>\r\nA lava plateau forms when large amounts of fluid lava flow over an extensive area (Figure 4). When the lava solidifies, it creates a large, flat surface of igneous rock.\r\n\r\n[caption id=\"attachment_2188\" align=\"aligncenter\" width=\"500\"]\"Layers Figure 4. 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.[\/caption]\r\n\r\n \r\n

Land<\/h3>\r\nLava creates new land as it solidifies on the coast or emerges from beneath the water (Figure 5).\r\n\r\n[caption id=\"attachment_2187\" align=\"aligncenter\" width=\"500\"]\"Lava Figure 5. Lava flowing into the sea creates new land in Hawaii.[\/caption]\r\n\r\nOver 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 6).\r\n\r\n[caption id=\"attachment_2186\" align=\"aligncenter\" width=\"500\"]\"Satellite Figure 6. 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.[\/caption]\r\n\r\n \r\n

Landforms from Magma<\/h2>\r\nMagma intrusions can create landforms. Shiprock in New Mexico is the neck of an old volcano that has eroded away (Figure 7). The volcanic neck is the remnant of the conduit the magma traveled up to feed an eruption.\r\n\r\n[caption id=\"attachment_2185\" align=\"aligncenter\" width=\"500\"]\"Shiprock Figure 7. The aptly named Shiprock in New Mexico.[\/caption]\r\n\r\n \r\n

Summary<\/h2>\r\n