Wudalianchi

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  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 48.72°N
  • 126.12°E

  • 597 m
    1958 ft

  • 305030
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Wudalianchi.

The Global Volcanism Program has no Weekly Reports available for Wudalianchi.

The Global Volcanism Program has no Bulletin Reports available for Wudalianchi.

The Wudalianchi volcanic field, named for a string of five scenic lava-dammed lakes, consists of 14 cinder cones capping a 500 sq km shield-like lava plateau in NE China. The volcanic field, whose name means "Five Connected Pools" was formed during five eruptive cycles from the early Pleistocene to historical time. Its ancient name was "Nine Hills," which after the historical eruptions now number 14 hills. The cinder cones were erupted through basement sedimentary and granitic rocks and show a preferred alignment along three chains at the intersection of NE- and NW-trending lineaments. In addition to the historical cinder cones of Laoheishan and Huoshaoshan, Xilongmenshan and Donglongmenshan are Holocene in age. The freshly preserved cones of Laoheishan and Huoshaoshan were formed during eruptions in 1720-21. Fissures at the base of the two new cinder cones fed glassy pahoehoe and aa lava flows that covered 65 sq km and formed the five lakes of Wudalianchi at their eastern and northern margins. Renewed eruptions took place in 1776.

Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1776 Unknown Confirmed 2 Historical Observations Laoheishan
1720 Jan 14 1721 Jun Confirmed 3 Historical Observations Laoheishan and Huoshaoshan

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.


Synonyms

Uyun-Kholdongi | Uyunhordongi | Uiun-Kholdongi | Wu-ta-Lien-Ch'ih | Nadug-Kholdonger | Kokhera | Ujun-Holdongi | Bo-shan

Cones

Feature Name Feature Type Elevation Latitude Longitude
Beigelaqiushan Cone 538 m
Bijiashan
    Pi-Chia-shan
    Sanjianshan
Cone 505 m
Dongjiaodebushan
    Tung-Chiao-te-Pu-shan
Cone 514 m
Donglongmenshan
    Tung-Lung-Men-shan
Cone 577 m
Huoshaoshan
    Liangbanshan
    Kocher
    Lianbanshan
Cone 390 m 48° 43' 30" N 126° 21' 0" E
Laoheishan
    Wassiljew
Cone 516 m 48° 41' 0" N 126° 20' 0" E
Molabushan Cone 523 m
Nangelaqiushan
    Nan-Ko-la-shan
Cone 597 m
Nomoer Cone 48° 36' 0" N 126° 15' 0" E
Weishan Cone 517 m
Wohushan Cone 496 m
Xiaogushan
    Yingbeishan
    Yen-Pei-shan
Cone 454 m
Xijiaodebushan
    Hsi-Chiao-te-Pu-shan
Cone 480 m
Xilongmenshan Cone 581 m
Yaoquanshan
    Yao-Chuan-shan
Cone 356 m
The Pleistocene Nangelaquishan cinder cone, capped by a 500-m-wide flat-bottomed crater, is one of 14 cones forming the Wudalianchi volcanic field in Manchuria, NE China. The cinder cones, four of which are Holocene in age, show a preferred alignment along three parallel NE-SW trends. The Wudalianchi volcanic field was named for five scenic lakes dammed by lava flows during a 1719-21 eruption, which formed two new cinder cones and produced a 65 sq km lava field.

Photo courtesy of Jim Whitford-Stark, Sul Ross State University, Texas (published in Feng et al., 1979).

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.

Chen H, Ren J, Wu X, 1999. Volcanic eruptive processes and characteristics of the current volcanoes in the Wudalianchi volcano clusters known from Manchurian-language historical archives discovered at present (in Chinese with English abs). Geol Rev, 45(Suppl): 409-413.

Feng M, 1982. The eruptions of Wudalianchi volcanoes of China. Volcano News, 10: 4-5.

Feng M, Keyi G, Wang F, 1979. Wudalianchi Volcanoes in China. Shanghai: Shanghai Sci Tech Publishers, 85 p.

Feng M, Whitford-Stark J L, 1986. The 1719-1721 eruptions of potassium-rich lavas at Wudalianchi, China. J Volc Geotherm Res, 30: 130-148.

Liu J, Taniguchi H, 2001. Active volcanoes in China. Tohoku Asian Studies, 6: 173-189.

Ogura T, 1969. Volcanoes in Manchuria. In: Ogura T (ed) {Geology and Mineral Resources of the Far East}, Tokyo: Univ Tokyo Press, 2: 373-413.

Vlodavetz V I, Piip B I, 1959. Kamchatka and Continental Areas of Asia. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 8: 1-110.

Wei H, Sparks R S J, Liu R, Fan Q, Wang Y, Hong H, Zhang H, Chen H, Jiang C, Dong J, Zheng Y, Pan Y, 2003. Three active volcanoes in China and their hazards. J Asian Earth Sci, 21: 515-526.

Whitford-Stark J L, 1987. A survey of Cenozoic volcanism on mainland Asia. Geol Soc Amer Spec Pap, 213: 1-74.

Whitford-Stark J L, 1987. . (pers. comm.).

Zhang M, 1989. . (pers. comm.).

Zhang M, Suddaby P, Thompson R N, Thirwall M F, Menzies M A, 1995. Potassic volcanic rocks in NE China: geochemical constraints on mantle sources and magma genesis. J Petr, 36: 1275-1303.

Volcano Types

Volcanic field

Tectonic Setting

Intraplate
Continental crust (> 25 km)

Rock Types

Major
Trachybasalt / Tephrite Basanite

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
57,885
57,885
136,201
2,164,526

Affiliated Databases

Large Eruptions of Wudalianchi Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
WOVOdat WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.
EarthChem EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).
Smithsonian Collections Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.