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Jingbo

Jingpohu

Medan gunung api · China · 1000 m

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Tipe
Medan gunung api
Negara
China
Wilayah
Eastern Asia Volcanic Regions / Central East Asia Volcanic Province
Ketinggian
1000 m
Koordinat
44.080, 128.830
Letusan terakhir
-520
Kondisi tektonik
Intraplate / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Trachybasalt / Tephrite Basanite
Ringkasan geologi

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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
3550 BCE~3361 BCE · 1 letusan · VEI maks. ?1656 BCE~1467 BCE · 1 letusan · VEI maks. ?709 BCE~520 BCE · 1 letusan · VEI maks. ?3550 BCE2792 BCE2035 BCE1467 BCE709 BCE

Garis waktu rinci

  1. 520 SM (±100 tahun)VEI ?Perkiraan geologi
    BCE 520 – Berlangsung
  2. 1540 SM (±150 tahun)VEI ?Perkiraan geologi
    BCE 1540 – Berlangsung
  3. 3550 SMVEI ?Perkiraan geologi
    BCE 3550 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.