Correct option is B
Lava domes form from the slow eruption of highly viscous felsic lava, resulting in a mound-shaped bulge near the volcanic vent.
Information Booster
- Lava domes are rich in silica, making the lava thick and slow-moving.
- These domes often collapse, leading to pyroclastic flows.
- Famous examples include Mount St. Helens and Mount Pelee.
- They form in both stratovolcanoes and independent eruptions.
- Felsic lava typically contains rhyolite or andesite.
- Lava domes indicate high-pressure magma chambers.
Additional Knowledge
- (a) Cinder cone: Small, steep-sided volcanoes formed from pyroclastic fragments.
- (b) Lava domes: Correct answer; mound-like features due to viscous lava.
- (c) Maars and tuff ring: Formed by explosive eruptions interacting with groundwater.
- (d) Caldera: Large volcanic crater formed by a collapsed magma chamber.