Jingbo
Jingpohu
Medan gunung api · China · 1000 m
- 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)
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Garis waktu rinci
- 520 SM (±100 tahun)VEI ?Perkiraan geologiBCE 520 – Berlangsung
- 1540 SM (±150 tahun)VEI ?Perkiraan geologiBCE 1540 – Berlangsung
- 3550 SMVEI ?Perkiraan geologiBCE 3550 – Berlangsung
Tautan eksternal
- Belum ada di Wikipedia (Bahasa Indonesia). Anda dapat berkontribusi di Wikidata.
- 🔗 Halaman asli Smithsonian GVP
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.