Showing posts with label Tibetan Plateau. Show all posts
Showing posts with label Tibetan Plateau. Show all posts

Monday, 8 June 2026

Magnitude 5.6 Earthquake in Bhutan.

The United States Geological Survey recorded a Magnitude 5.6 Earthquake at a depth of 10.0 km, about 15 km to the northwest of the city of Punākha, in Punākha District, Bhutan, slightly after 11.35 pm local time (slightly after 5.35 pm GMT) on Sunday 7 June 2026. There are no reports of any damage or casualties arising from this quake, but people have reported feeling it as far away as Tibet, India, and Bangladesh.

The approximate location of the 7 June 2026 Bhutan Earthquake. USGS.

Earthquake activity in the area is caused by the uplift of the Tibetan Plateau, due to the impact of India into Eurasia to the south. he Indian Plate is moving northwards at a rate of 5 cm per year, causing it to impact into Eurasia, which is also moving northward, but only at a rate of 2 cm per year. The collision of the Indian and Eurasian plates has lead to the formation of the Himalayan Mountains, the Tibetan Plateau, and the mountains of southwest China, Central Asia and the Hindu Kush.

Block diagram showing how the impact of the Indian Plate into Eurasia is causing uplift on the Tibetan Plateau. Jayne Doucette/Woods Hole Oceanographic Institution.

Much of northern India and neighbouring areas of Central Asia and the Himalayas, are prone to Earthquakes caused by the impact of the Indian Plate into Eurasia from the south. When two tectonic plates collide in this way and one or both are oceanic then one will be subducted beneath the other (if one of the plates is continental then the other will be subducted), but if both plates are continental then subduction will not fully occur, but instead the plates will crumple, leading to folding and uplift (and quite a lot of Earthquakes). 

The movement of India into Eurasia over the last 71 million years. USGS.

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Saturday, 27 September 2025

Magnitude 5.6 Earthquake in Gansu Province, China.

The China Earthquake Networks Center recorded a Magnitude 6.8 Earthquake at a depth of 10 km beneath Longxi County in southern Gansu Province, slightly before 5.50 am local time on Saturday 27 September 2025 (slightly before 9.50 pm on Friday 26 September, GMT). The Earthquake was felt across southeastern Gansu. Seventeen houses were destroyed by the event, with 4382 damaged, eleven people injured and 7812 in need of at least temporary rehousing. 

Emergency workers clearing debris following a Magnitude 5.6 Earthquake in Gansu Province, China, on Saturday 27 September 2025. Xinhau.

Much of western China and neighbouring areas of Central Asia and the Himalayas, are prone to Earthquakes caused by the impact of the Indian Plate into Eurasia from the south. The Indian Plate is moving northwards at a rate of 5 cm per year, causing it to impact into Eurasia, which is also moving northward, but only at a rate of 2 cm per year. When two tectonic plates collide in this way and one or both are oceanic then one will be subducted beneath the other (if one of the plates is continental then the other will be subducted), but if both plates are continental then subduction will not fully occur, but instead the plates will crumple, leading to folding and uplift (and quite a lot of Earthquakes). The collision of the Indian and Eurasian plates has lead to the formation of the Himalayan Mountains, the Tibetan Plateau, and the mountains of southwest China, Central Asia and the Hindu Kush.

Tectonic map of Asia, showing relationships between the India–Asia collision, escape of Indonesian and South China blocks seaward, and extension from Siberia to the Pacific margin. (Note also the opening of back-arc basins including the Sea of Japan and the South China Sea, and extension in the Bohai Basin and eastern part of the NCC.) The North China Craton is also strongly influenced by Pacific and palaeo-Pacific subduction, perhaps also inducing extension in the eastern NCC. The palaeo Pacific and Pacific subduction zones developed in the Mesozoic, and also contributed to the hydration of the subcontinental lithospheric mantle beneath the NCC. Kusky et al. (2007).

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Tuesday, 7 January 2025

Magnitude 6.8 earthquake in southern Tibet kills at least 126 people.

The China Earthquake Networks Center recorded a Magnitude 6.8 Earthquake at a depth of 10 km beneath Tingri County in southern Tibet, close to Mount Everest and the border with Tibet at about 9.05 am local time on Tuesday 7 January 2025 (about 1.05 am, GMT). The Earthquake was felt across southern Tibet, eastern Nepal, western Bhutan, northeastern India and northern Bangladesh. More than 150 aftershocks have been recorded since the original event.

The approximate location of the 7 January 2025 Tibet Earthquake. USGS.

At the time of writing rescue workers have reported 126 deaths and 188 people injured in Tibet and another five injuries in Nepal. However, the number of casualties is likely to rise significantly, as the population in the area around the epicentre of the Earthquake largely live in small, remote villages, largely cut off from the outside world, and which are subsequently difficult for rescue workers to reach. To make matters worse, daytime temperatures in the area average -8°C at this time of year, falling to -18°C at night. More than a thousand homes have been damaged or destroyed in areas that rescue workers have managed to reach, so is likely that in other areas people may have lost  their homes or be trapped beneath debris, vulnerable to the cold.

Rescue workers in Tingri County, Tibet, following a Magnitude 6.8 Earthquake on Tuesday 7 January 2024. Xinhua/AP.

Earthquake activity in the area is caused by the uplift of the Tibetan Plateau, due to the impact of India into Eurasia to the south. he Indian Plate is moving northwards at a rate of 5 cm per year, causing it to impact into Eurasia, which is also moving northward, but only at a rate of 2 cm per year. The collision of the Indian and Eurasian plates has led to the formation of the Himalayan Mountains, the Tibetan Plateau, and the mountains of southwest China, Central Asia and the Hindu Kush.

Block diagram showing how the impact of the Indian Plate into Eurasia is causing uplift on the Tibetan Plateau. Jayne Doucette/Woods Hole Oceanographic Institution.

Much of Tibet and neighbouring areas of Central Asia and the Himalayas, are prone to Earthquakes caused by the impact of the Indian Plate into Eurasia from the south. When two tectonic plates collide in this way and one or both are oceanic then one will be subducted beneath the other (if one of the plates is continental then the other will be subducted), but if both plates are continental then subduction will not fully occur, but instead the plates will crumple, leading to folding and uplift (and quite a lot of Earthquakes). The collision of the Indian and Eurasian plates has lead to the formation of the Himalayan Mountains, the Tibetan Plateau, and the mountains of southwest China, Central Asia and the Hindu Kush.

The movement of India into Eurasia over the last 71 million years. USGS.

See also...

Wednesday, 30 October 2024

Murina yushuensis: A new species of Tube-nosed Bat from a high altitude cave on the Tibetan Plateau.

Tube-nosed Bats, Murina spp., are a large group of Vespertilionid Bats found from northeastern Russia to Papua New Guinea. There are currently 40 described species in the genus about half of which have been described in the past decade, largely from genetic studies which have uncovered many cryptic species, predominantly in South and Southeast China. These Bats are insectivorous, and generally found in lowland forests, with the maximum known diversity in South China and Southeast Asia, although this may be due to a lack of sampling in more northerly parts of China.

In a paper published in the Journal of Mammalogy on 23 October 2024, Xiaoyun Wang of the Key Laboratory of Conservation and Application in Biodiversity of South China at Guangzhou University, Xuesong Han of the Shan Shui Conservation Center and the Center for Nature and Society at Peking University, Gábor Csorba of the Department of Zoology at the Hungarian Natural History Museum, Yi Wu, also of the Key Laboratory of Conservation and Application in Biodiversity of South China at Guangzhou University, Huaiqing Chen also of the Center for Nature and Society at Peking University, Xiang Zhao and  Zhengyi Dong, also of the Shan Shui Conservation Center, Wenhua Yu,again of the Key Laboratory of Conservation and Application in Biodiversity of South China at Guangzhou University, and Zhi Lu, again of the Center for Nature and Society at Peking University, describe a new species of Murina from a high altitude cave on the Tibetan Plateau in Qinghai Province in Northeast China.

On 15 March 2018, a Bat roosting in the entrance to a cave on the bank of the Batang River about 8 km from the city of Yushu and 3770 m above sealevel was disturbed, responding by making a long, high-pitched noise. At the time the significance of this was not realised, but when the significance was realised, several repeat visits were made, with the Bat being found again on 25 December 2018.

The new species is described from this single male specimen, and is named Murina yushuensis, where 'yushuensis' means 'from Yushu'. The single specimen is 30.44 mm long (small for a member of the genus). with dark skin and small round ears, lacking the notch seen in some members of the genus. The fur of the dorsal surface is about 10 mm in length, with the basal 7 mm being black in colour, and the 3 mm at the tip being a golden brown. The fur of the ventral surface is slightly shorter, which the basal black portion being about 6 mm, and the 3 mm of the tip being pale. 

Holotype specimen of Murina yushuensis, GZHU 20077. Wang et al. (2024).

The Batang River is a tributary of the Yangtze running across the Tibetan Plateau, at altitudes of between 3860 m and 3530 m above sealevel. The area where Murina yushuensis was discovered has a mean annual temperature of only 2.9°C, and an annual average precipitation of 487 mm. The vegetation is largely meadows of Feathergrass with scattered shrubs and patches of Juniper woodland. This is a distinctly unusual environment for a member of a genus usually found in lowland tropical and subtropical forests. Murina yushuensis was discovered at the highest altitude any member of the genus has ever been recorded at, with the previous record being a specimen of the Little Tube-nosed But, Murina aurata, found at 2500 m. However, Wang et al. consider that while Murina yushuensis may seem exceptional, it is also potentially an indicator that other species of the genus may be living at high and intermediate altitudes, and not yet discovered due to a lack of sampling.

Surrounding environment of the cave where Murina yushuensis was discovered in March 2018. Wang et al. (2024).

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Wednesday, 4 October 2023

Magnitude 5.7 Earthquake in Bajhang District, Nepal.

The United States Geological Survey recorded a Magnitude 5.7 Earthquake at a depth of 20.1 km, in Bajhang District, Nepal slightly after 2.20 pm local time, (slightly after 9.20 am GMT) on Tuesday 3 October 2023. The event was felt as far away as New Delhi in India, and is reported to have injured at least seventeen people, with one more missing and presumed dead after being engulphed by a rockfall. A number of homes are reported to have collapsed in the town of Chainpur, and a major highway is reported to have been blocked by a landslide triggered by the event. The initial event has been followed by at least two significant aftershocks. 

The approximate location of the 3 October 2023 Bajhang District Earthquake. USGS.

Earthquake activity in Nepal is caused by the uplift of the Tibetan Plateau, due to the impact of India into Eurasia to the south. The Indian Plate is moving northwards at a rate of 5 cm per year, causing it to impact into Eurasia, which is also moving northward, but only at a rate of 2 cm per year. The collision of the Indian and Eurasian plates has led to the formation of the Himalayan Mountains, the Tibetan Plateau, and the mountains of southwest China, Central Asia and the Hindu Kush.

Block diagram showing how the impact of the Indian Plate into Eurasia is causing uplift on the Tibetan Plateau. Jayne Doucette/Woods Hole Oceanographic Institution.

Much of northern India and neighbouring areas of Central Asia and the Himalayas, are prone to Earthquakes, caused by the impact of the Indian Plate into Eurasia from the south. When two tectonic plates collide in this way and one or both are oceanic then one will be subducted beneath the other (if one of the plates is continental then the other will be subducted), but if both plates are continental then subduction will not fully occur, but instead the plates will crumple, leading to folding and uplift (and quite a lot of Earthquakes). The collision of the Indian and Eurasian plates has led to the formation of the Himalayan Mountains, the Tibetan Plateau, and the mountains of southwest China, Central Asia and the Hindu Kush.

The movement of India into Eurasia over the last 71 million years. USGS.

See also...

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