Table of Contents
- 1 What type of plate boundary causes volcanic eruptions?
- 2 What type of plate boundary caused the White Island eruption?
- 3 What plate boundary is Indonesia on?
- 4 What type of boundary is found between the Australian plate and the Pacific plate?
- 5 Which type of plate boundary does not cause volcanoes?
- 6 What plates were involved in the Indonesian earthquake?
- 7 Where is Mount Galunggung located in the world?
- 8 How are plate boundaries related to volcanic activity?
What type of plate boundary causes volcanic eruptions?
Volcanoes are most common in these geologically active boundaries. The two types of plate boundaries that are most likely to produce volcanic activity are divergent plate boundaries and convergent plate boundaries. At a divergent boundary, tectonic plates move apart from one another.
What type of plate boundary caused the White Island eruption?
They happen quickly and sharply and usually without warning. The operating force on White Island, like a lot of New Zealand’s most dramatic landscapes, is tectonic. The volcano is part of the Taupō Volcanic Zone, which is on the boundary of the Pacific and Australian plates, clashing and grinding together endlessly.
What two plate boundaries can cause an earthquake?
About 80% of earthquakes occur where plates are pushed together, called convergent boundaries. Another form of convergent boundary is a collision where two continental plates meet head-on.
What plate boundary is Indonesia on?
The tectonics of Indonesia are very complex, as it is a meeting point of several tectonic plates. Indonesia is located between two continental plates: the Australian Plate (Sahul Shelf) and the Eurasian Plate (Sunda Shelf); and between two oceanic plates: the Pacific Plate and the Philippine Sea Plate.
What type of boundary is found between the Australian plate and the Pacific plate?
convergent boundary
The Hikurangi tectonic plate boundary is a convergent boundary. This means that the Australian and Pacific plates are pushing against each other.
What type of eruption was White Island?
The lava flows, ash, and pyroclastic flows produced by historic and prehistoric eruptions are andesitic and dacitic in composition. These eruptions also produce discrete craters within crater-fill deposits of the Central Cone. Since 1826, there has been a minimum of 28 phreatic or phreatomagmatic eruptions.
Which type of plate boundary does not cause volcanoes?
Volcanoes do not typically occur at transform boundaries. One of the reasons for this is that there is little or no magma available at the plate boundary. The most common magmas at constructive plate margins are the iron/magnesium-rich magmas that produce basalts.
What plates were involved in the Indonesian earthquake?
The January 15 event was a shallow crustal earthquake at the boundary between the Sunda plate and the Banda Sea microplate at a focal depth of 18 km. The earthquake occurred along the Mamuju–Majene thrust fault, which is known to be an active seismic source that has caused several deadly earthquakes in the recent past.
How did the Galunggung volcano have a landslide?
Like these mountains, Galunggung has a horseshoe -shaped crater indicating a massive landslide, and examination of shattered lava blocks revealed them to be similar to deposits on the other two volcanoes. According to radiocarbon dating of samples taken from a lava flow, the landslide happened within the last 23,000 years.
Where is Mount Galunggung located in the world?
Mount Galunggung is part of the Sunda Arc extending through Sumatra, Java and the Lesser Sunda Islands, which has resulted from the subduction of the Australian plate beneath the Eurasian plate .
Sometimes, the plates collide with one another or move apart. Volcanoes are most common in these geologically active boundaries. The two types of plate boundaries that are most likely to produce volcanic activity are divergent plate boundaries and convergent plate boundaries. Divergent Plate Boundaries.
Which is part of the Sunda Arc is Galunggung?
Galunggung. Mount Galunggung is part of the Sunda Arc extending through Sumatra, Java and Bali, which has resulted from the subduction of the Australian plate beneath the Eurasian plate .