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What type of volcano is Gede?
stratovolcano
Gede is a stratovolcano with at least 21 eruptions between 1747 and 1957. Eruptions have been moderate to moderate-large in size (VEI=2-3). The eruption in 1840 was the largest and generated pyroclastic flows. The 1947-1948 and 1955 eruptions were phreatic.
How high is Mount Gede?
9,869′
Mount Gede/Elevation
Is Mount Gede active?
Seven craters are located in the complex: Baru, Gumuruh (2,927 m), Lanang (2,800 m), Kawah Leutik, Ratu (2,800 m), Sela (2,709 m) and Wadon (2,600 m). Historical volcanic activity has been recorded since the 16th century….
| Mount Gede | |
|---|---|
| Mountain type | Stratovolcano |
| Last eruption | March 1957 |
| Climbing | |
| Easiest route | Gunung Putri |
What type of volcano is Mauna Loa?
shield volcano
Mauna Loa is the largest active volcano on the planet. Meaning “long mountain” in Hawaiian, it is the quintessential shield volcano in its shape— signified by broad, rounded slopes. The volcano makes up roughly 51% of Hawaiʻi Island and stands 13,678 feet (4,170 m) above sea level.
What type of volcano is Salak?
Salak is a stratovolcano with at least five eruptions between 1780 and 1938.
Is Mauna Loa extinct?
The slow drift of the Pacific Plate will eventually carry Mauna Loa away from the hotspot within 500,000 to one million years from now, at which point it will become extinct. Mauna Loa’s most recent eruption occurred from March 24 to April 15, 1984….
| Mauna Loa | |
|---|---|
| Easiest route | Ainapo Trail |
When did Mauna Loa first erupt?
Mauna Loa is among Earth’s most active volcanoes, having erupted 33 times since its first well-documented historical eruption in 1843. It has produced large, voluminous flows of basalt that have reached the ocean eight times since 1868.
Is Mount Salak still active?
It has several satellite cones on its southeast flank and the northern foot, along with two additional craters at the summit. Mount Salak has been evaluated for geothermal power development….
| Mount Salak | |
|---|---|
| Location | Java, Indonesia |
| Geology | |
| Mountain type | Stratovolcano |
| Last eruption | January 1938 |
How tall is Mount Salak?
7,254′
Mount Salak/Elevation
Why did Mauna Loa erupted in 1984?
Six large vent structures eventually formed in this area around the active vents. Lava channel blockage caused an overflow of the main lava channel leading from the “2,900-m vents” of the 1984 Mauna Loa eruption. Lava spills over the collapsed side levee to feed new flows.
What caused Mauna Loa to erupt in 1984?
Lava channel blockage caused an overflow of the main lava channel leading from the “2,900-m vents” of the 1984 Mauna Loa eruption. Lava spills over the collapsed side levee to feed new flows.
When was the last eruption from Mauna Loa?
April 15, 1984
Mauna Loa/Last eruption
Where is Mount Gede Pangrango national park located?
Mount Gede Pangrango National Park is a national park in West Java, Indonesia. The park is centred on two volcanoes— Mount Gede and Mount Pangrango —and is 150 km² in area.
What kind of animals live in Gunung Gede Pangrango?
Gunung Gede-Pangrango is inhabited by 251 of the 450 bird species found in Java. Among these are endangered species like the Javan hawk-eagle and the Javan scops owl. Among the endangered mammal species in the Park there are several primates such as the silvery gibbon, Javan surili and Javan lutung.
Where did the cimungkat National Park come from?
It evolved from already existing conservation areas, such as Cibodas Botanical Gardens, Cimungkat Nature Reserve, Situgunung Recreational Park and Mount Gede Pangrango Nature Reserve, and has been the site of important biological and conservation research over the last century.
What is the Pangrango pillar?
At 3,020m, Pangrango is just 58 metres higher than neighbouring Gunung Gede. The pillar is from the Dutch colonial era and constructed as part of early efforts to properly map Java and other islands. If you look on the back of it you will see it has a numbered marker – 142.