In volcanology, a lava dome is a circular, mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano. Dome-building eruptions are common, particularly in convergent plate boundary settings. [1] Around 6% of eruptions on Earth form lava domes. [1]

2024年1月2日 · Lava domes are circular, steep-sided mounds of volcanic rocks formed from the extrusion of viscous lava that piles around a volcanic vent.

2025年4月9日 · lava dome The lava dome of Mount St. Helens, May 16, 1984. Following the great eruption of May 18, 1980, a dome of lava grew intermittently in the crater of the volcano. By the time of this photograph, the dome measured 850 metres (2,800 feet) …

2024年7月9日 · Domes are sometimes called lava domes. At least 12 units of the National Park System contain volcanic domes, including: Lassen Volcanic National Park contains multiple lava domes. Lassen Peak is the world’s largest dome with a peak elevation of 10,457 feet (3,187 m). It was emplaced 27,000 years ago.

Lava domes are formed by viscous magma being erupted effusively onto the surface and then piling up around the vent. Like lava flows, they typically do not have enough gas or pressure to erupt explosively, although they may sometimes be preceded or followed by explosive activity.

Some lava domes grow in a matter of hours or day, while others may take years – some taking upwards of 100 years to reach their full extent. The stages of development seen below, the Mount St. Helens 1980-1986 lava dome is an example of a composite lava dome that grew episodically.

Lava domes are common features on volcanoes around the world. Lava domes are volcanoes to exist on plate margins as well as in intra-arc hotspots, and on heights above 6000 m and in the sea floor. [1] Individual lava domes and volcanoes featuring lava domes are listed below.

Volcanic dome, any steep-sided mound that is formed when lava reaching the Earth’s surface is so viscous that it cannot flow away readily and accumulates around the vent. Sometimes domes are produced by repeated outpourings of short flows from a summit vent, and, occasionally, extremely viscous.

Lava domes are hemispherical to irregularly shaped mounds of volcanic rock (Blake, 1990). They form from lava that is too viscous to flow very far from the vent that extruded it (Husain et al., 2014). The composition is typically andesitic to rhyolitic.

Lava domes demonstrate a large variety of textures and features, depending largely on composition and the ability of the lava dome to deform and flow. Listed below are a few of these features and breid descriptions of each.