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China · Volcanic field

Jingbo

Jingpohu

Type
Volcanic field
Elevation
1000m
Last eruption
-520
Type
Volcanic field
Country
China
Region
Eastern Asia / Central East Asia Volcanic Province
Elevation
1000m
Coordinates
44.080, 128.830
Last eruption
-520
Tectonic setting
Intraplate / Continental crust (> 25 km)
Landform
Cluster
Major rock type
Trachybasalt / Tephrite basanite
Geological summary

Jingpohu is a Pliocene-to-Holocene volcanic field in the Jingpo Lake area of Heilongjiang Province, NE China. The lake formed when lava flows blocked the Mudan River (Mudanjiang). The NE-striking Dunhua-Mishan fault controls the location of many vents. One alkali basaltic lava flow traveled 100 km down a canyon NW of the lake. Many Holocene trachybasaltic or basanitic cones and lava flows lie on plateaus along the Mudan River, which also contain basanitic and tephriphonolitic rocks. Mantle xenoliths are common. A period of major activity about 5,500-5,200 years ago produced extensive lava flows that covered an area of about 500 km2.

Eruption history

3 recordedGlossary
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
3550 BCE~3361 BCE · 1 eruptions · max VEI ?1656 BCE~1467 BCE · 1 eruptions · max VEI ?709 BCE~520 BCE · 1 eruptions · max VEI ?3550 BCE2792 BCE2035 BCE1467 BCE709 BCE

Detailed timeline

  1. 520 BCE (±100 yrs)VEI ?Geological estimate
    520 BCE – end unknown
  2. 1540 BCE (±150 yrs)VEI ?Geological estimate
    1540 BCE – end unknown
  3. 3550 BCEVEI ?Geological estimate
    3550 BCE – end unknown

Nearby volcanoes

External links

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