Kueishantao, Taiwan

Volcano Type: Stratovolcano
Volcano Status: Historical
Last Known Eruption: 1785 ± 10 years
Summit Elevation: 401 m    1,316 feet
Latitude: 24.85°N   24°51’0″N
Longitude: 121.92°E   121°55’0″E

Kueishantao Island, whose summit is 401 m above sea level, is the southernmost of five small volcanic islands off the NE coast of Taiwan. Kueishantao, also known as Guieshan Island, consists of andesitic lava flows and volcaniclastic material. Kueishantao is the southwesternmost volcano along the axis of the Okinawa Trough back-arc basin that extends to the NE from Taiwan to Unzen volcano in Kyushu.

The SW tip of the Okinawa Trough extends past Kueishantao onto the Ilao Plain on the island of Taiwan. The island is known as “Turtle Mountain Island” due to its profile as seen from some points on the coast of Taiwan. Historical accounts during the time of King Qianlong of the Qing Dynasty (1775-1795 AD) noted the Guieshan mountain split open with a blood-red lava flow. Kueishantao displays vigorous active submarine fumaroles and solfataras that discolor seawater over wide areas.

Originally posted 2010-10-08 06:18:06.

Tengchong, Taiwan

Tengchong

Volcano Type: Pyroclastic cones
Volcano Status: Uranium-series
Last Known Eruption: 5750 BC ± 1000 years
Summit Elevation: 2865 m   9,399 feet
Latitude: 25.23°N *   25°14’0″N
Longitude: 98.50°E    98°30’0″E

The Tengchong volcanic district, located in southern China near the border with Burma (Myanmar), was active during five periods ranging from the early Pliocene to the Holocene. Three main stages prroduced Pliocene to mid-Pleistocene basaltic rocks, mid- to late-Pleistocene silicic pyroclastic rocks, and Holocene basaltic andesites.

Tengchong

Tengchong

Click Here For The Rest Of Tengchong, Taiwan

Originally posted 2010-10-08 06:35:15.

Tatun Volcano Group, Taiwan

Volcano Type: Lava domes
Volcano Status: Radiocarbon
Last Known Eruption: 4100 BC ± 40 years
Summit Elevation: 1120 m   3,674 feet
Latitude: 25.17°N *   25°10’0″N
Longitude: 121.52°E   121°31’0″E

The Tatun (Datun) volcano group consists predominately of a series of andesitic lava domes in the northernmost part of Taiwan. About 20 volcanoes, the southernmost of which is only 15 km north of the capital city of Taipei, are included in the Tatun group, which was constructed along E-W and NE-SW trending ridges. The highest and youngest volcano is the 1120-m-high Cising (Chisingshan) lava dome.

Path to Mt. Tatun

Path to Mt. Tatun

Several magmatic eruptions took place at the Tatun volcano group about 23,000 to 13,000 years ago, and a phreatic eruption assocciated with collapse of the lava dome, possibly closely following lava effusion, took place about 6000 years ago. Hot springs, fumaroles, and solfataras are found over wide areas along a zone parallel to the SW-NE-trending Chinshan fault and extending to the NE coast of Taiwan, and extensive geothermal exploration has occurred at the Daiton geothermal area.

Stream on Mt. Tatun (Allen Hsu)

Stream on Mt. Tatun (Allen Hsu)

Stream on Mt. Tatun (Allen Hsu)

Stream on Mt. Tatun (Allen Hsu)

Sunset on Mt. Tatun (Allen Hsu)

Sunset on Mt. Tatun (Allen Hsu)

Sunset on Mt. Tatun (Allen Hsu)

Sunset on Mt. Tatun (Allen Hsu)

Sunset on Mt. Tatun (Allen Hsu)

Sunset on Mt. Tatun (Allen Hsu)

Overview of Tatun Volcano (Juin's Album)

Overview of Tatun Volcano (Juin's Album)

Sunset on Mt. Tatun (Kenji Chen)

Sunset on Mt. Tatun (Kenji Chen)

Bird's Eye View of Tatun Mountain (Dans Photo)

Bird's Eye View of Tatun Mountain (Dans Photo)

Mt. Tatun's South Peak

Mt. Tatun's South Peak

Originally posted 2010-10-08 06:09:45.