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Jingbo

Jingpohu

Volcanic field · China · 1000m

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Type
Volcanic field
Country
China
Region
Eastern Asia Volcanic Regions / 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 basantic 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

Summary (VEI over time)
Click a bar to see individual eruptions
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
    BCE 520 – Ongoing
  2. 1540 BCE (±150 yrs)VEI ?Geological estimate
    BCE 1540 – Ongoing
  3. 3550 BCEVEI ?Geological estimate
    BCE 3550 – Ongoing

External links

⚠ For reference only. Not for emergency response.