Jom-Bolok volcanic field

The Jom-Bolok volcanic field lies in the over 3,100 metres (10,200 ft) high East Sayan Mountains^[3] and is far removed from the major plate boundaries around Asia. It may be under the influence of the subducting Pacific Plate regardless,^[4] as well as of the India-Asia collision,^[5] but more likely volcanism there is a consequence of a mantle plume^[6] and there are seismic velocity anomalies in the mantle under Jom-Bolok.^[7] Other volcanic fields within 1,000 kilometres (620 mi) of Jom-Bolok are the Hangai, Khamar-Daban, Oka, Tuva and Vitim fields. These volcanic fields extend into Mongolia.^[8]

Like the Udokan plateau, Jom-Bolok is a volcanic field part of the Baikal rift which has been volcanically active during the Holocene. Volcanism there may be the consequence either of passive rifting or mantle plume activity and has been ongoing since the Mesozoic.^[9] The basement of this area was heavily folded and altered during the Tertiary, which was also affected by river incision and earlier eruptive activity.^[10] During the late Pleistocene, 300–400 metres (980–1,310 ft) thick glaciers formed in the Jom-Bolok valley and other adjacent valleys.^[11]

The field contains scoria cones, lava flows^[3] and small cinder cones. Pyroclastic cones in the field include Atkinson, Kropotkin (2,077 metres (6,814 ft) and 52°42′0″N 98°59′0″E / 52.70000°N 98.98333°E / 52.70000; 98.98333),^[2][12] Medvedev,^[13] Ostanets Group ("remnants" in Russian), Peretolchin (2,050 metres (6,730 ft) and 52°43′0″N 98°58′0″E / 52.71667°N 98.96667°E / 52.71667; 98.96667), Pertolichina (2,050 metres (6,730 ft) and 52°43′0″N 98°58′0″E / 52.71667°N 98.96667°E / 52.71667; 98.96667), Pogranichniy ("border" in Russian, being located between two other flows), Stariy ("old" in Russian, 2,030 metres (6,660 ft) and 52°36′0″N 98°54′0″E / 52.60000°N 98.90000°E / 52.60000; 98.90000), Treshina ("fissure" in Russian) and Troynoy ("triplet" in Russian, three 10 metres (33 ft) high domes).^[2][12] Most of these cones are located within the Hee-Gol valley rather than the Jom-Bolok valley itself.^[14] These cones are constructed on top of three different faults.^[12]

An alkali basalt lava flow erupted during the Holocene has a volume of 7.9 cubic kilometres (1.9 cu mi) and reached a length of 70 kilometres (43 mi) along Jom-Bolok river,^[2] reaching the Oka river in a large fan and damming it.^[11] This volume is comparable to the volume of lavas emitted during the 1973 Tolbachik eruption, albeit smaller than the Eldgja and Laki eruptions.^[15] This volume is unusual for a volcanic field of this size. This large eruptive volume may be linked to the effects of the ending ice age; the melting of the glaciers and resulting unloading of the crust would have resulted in a pre-existing subcrustal pond of magma to drain in a high volume eruption. The extreme length of the flow was likely also helped by the formation of lava tubes within the flow.^[14] The northern lava flow during its formation displayed some excellent thermal insulation,^[8] and it propagated by a process named sheet inflation where lava flows form thin sheets that subsequently grow to larger flows with a solid crust.^[16]

The Kropotkin and Peretolchin cones are the largest ones and grew to heights of 100 metres (330 ft) above lava flows, Atkinson cone later formed on Peretolchin's side but is heavily degraded.^[12] The Atkinson cone was probably formed during at least two separate stages, as did the Stariy cone which was destroyed during the early phase of activity and subsequently grew a secondary cone.^[17]

A shorter, 6 kilometres (3.7 mi) long lava flow forms the southern lava field,^[18] within the upper Kadyr-Os and Khi-Gol valleys.^[16] This field with a volume of 0.2 cubic kilometres (0.048 cu mi) is comparable to some large Hawaiian lava flows such as the 1950 Mauna Loa lava flow.^[15] The Medvedev mound is associated with its own lava flow and peculiar lava features named "stony-flowers".^[13] This flow has a much smaller volume of 0.00007 cubic kilometres (1.7×10⁻⁵ cu mi), covering a surface of 0.03 square kilometres (0.012 sq mi).^[15] The youngest lavas were erupted in the upper Khi-Gol valley from the Oka-Jombolok convergence where it assumes an aa morphology. That they don't appear in the intervening region may be because it was channeled through older lava tubes beneath the older lava flows.^[16] Lava flows from Jom-Bolok formed a lava dam that generated Lake Khara-Nur about 6,400 years ago.^[19]

All the lavas at Jom-Bolok are hawaiites and comparable to the close but older Oka and Tuva field lavas;^[15] the total volume of volcanic rocks is about 16 cubic kilometres (3.8 cu mi).^[1] Other fields around the Baikal rift have also hawaiites but are also associated with other volcanic rocks.^[20]

• 
  A lava flow
• 
  Peretolchin

The climate is dominated by the westerlies from the Atlantic Ocean and by the Siberian High, with a mean annual temperature of −4 °C (25 °F)^[21] and a continental climate, with annual precipitation in the region being about 430 millimetres per year (17 in/year); during marine isotope stages 5 and 4 glaciation was widespread.^[22] The vegetation is classified as "bald vegetation", which is a montane vegetation type; here it is characterized by birch, larch, Siberian fir willow. The volcanoes rise from Paleozoic intrusive rocks and various Pleistocene to Holocene sediments occur in the region; at higher elevation there is permafrost.^[19] The "Tannuola complex" is a Paleozoic rock assembly that forms the mountains around the volcanic field. Sediment cores taken in lakes of the area have been used to reconstruct the history of vegetation and climate during the Holocene.^[23]