Jingbo
Jingpohu
Volcanic field · China · 1000m
- 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
Detailed timeline
- 520 BCE (±100 yrs)VEI ?Geological estimateBCE 520 – Ongoing
- 1540 BCE (±150 yrs)VEI ?Geological estimateBCE 1540 – Ongoing
- 3550 BCEVEI ?Geological estimateBCE 3550 – Ongoing
External links
- Not yet on Wikipedia (English). You can contribute on Wikidata.
- 🔗 Smithsonian GVP source page
⚠ For reference only. Not for emergency response.