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Iskut-Unuk River Cones

Kerucut piroklastik · Canada · 1880 m

Shallow ponds are seen across the surface of valley-filling lava flows of the Iskut-Unuk volcanic field. The flows traveled south 5 km where they crossed the border into Alaska and dammed the Blue River, forming several small lakes and traveling a total of approximately 22 km. The Iskut-Unuk River Cone Group consists of eight small basaltic centers at the southern end of the Stikine volcanic belt that range in age from about 70,000 to only a few hundred years old and form one of the youngest volcanic fields in Canada.
Shallow ponds are seen across the surface of valley-filling lava flows of the Iskut-Unuk volcanic field. The flows traveled south 5 km where they crossed the border into Alaska and dammed the Blue River, forming several small lakes and traveling a total of approximately 22 km. The Iskut-Unuk River Cone Group consists of eight small basaltic centers at the southern end of the Stikine volcanic belt that range in age from about 70,000 to only a few hundred years old and form one of the youngest volcanic fields in Canada. · Foto: Photo by Ben Edwards, 1997 (Dickinson College, Pennsylvania). · Wikimedia Commons
Tipe
Kerucut piroklastik
Negara
Canada
Wilayah
North America Volcanic Regions / Northern Cordilleran Volcanic Province
Ketinggian
1880 m
Koordinat
56.567, -130.750
Letusan terakhir
1800
Kondisi tektonik
Intraplate / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

Eight small basaltic centers at the southern end of the Stikine volcanic belt near the Alaska border comprise the Iskut-Unuk River Cones group. Lava flows date back 70,000 years, but the subaerial vents produced cinder cones and lava flows that were probably all active between about 9,000 and a few hundred years ago. Five of the centers produced lava flows that traveled up to ~20 km down the Iskut and Unuk River valleys and their tributaries. The three remaining centers are products of ice-contact volcanism that formed pillow lava, hyaloclastite breccias, and scoria. The flows are similar in mineralogy and contain abundant crustal xenoliths. Vents in the Iskut River Canyon area produced at least 10 lava flows, and the Lava Fork vents at least three lava flows, the latest of which erupted within the past few hundred years.

Ringkasan Wikipedia

Ringkasan Inggris

The Iskut volcanic field is a group of volcanoes and lava flows on and adjacent to the Alaska–British Columbia border in the Boundary Ranges of the Coast Mountains. All the volcanoes in this volcanic field are situated in British Columbia along the Iskut and Unuk rivers and their tributaries, with lava flows having reached Alaska. The oldest volcanoes in the Iskut volcanic field are Little Bear Mountain and Hoodoo Mountain, which are 146,000 and 85,000 years old, respectively. Younger volcanic centres include Second Canyon, King Creek, Tom MacKay Creek, Snippaker Creek, Iskut Canyon, Cone Glacier, Cinder Mountain and Lava Fork, all of which formed in the last 70,000 years. All of the volcanoes are mafic in composition except for Hoodoo Mountain which consists of peralkaline rocks. The latest volcanic eruption took place from the Lava Fork volcano in 1800, although an uncertain 1904 eruption is also attributed to this volcano.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
6830 BCE~6539 BCE · 1 letusan · VEI maks. ?4792 BCE~4501 BCE · 1 letusan · VEI maks. ?3628 BCE~3336 BCE · 1 letusan · VEI maks. ?1881 BCE~1590 BCE · 1 letusan · VEI maks. ?716 BCE~425 BCE · 1 letusan · VEI maks. ?1322~1613 · 1 letusan · VEI maks. ?1613~1904 · 2 letusan · VEI maks. ?6830 BCE4792 BCE2463 BCE425 BCE1613

Garis waktu rinci

  1. 1904VEI ?Perkiraan geologi
    1904 – Berlangsung
    Lava Fork
  2. 1800VEI ?Perkiraan geologi
    1800 – Berlangsung
    Lava Fork
  3. 1590 (±50 tahun)VEI ?Perkiraan geologi
    1590 – Berlangsung
    Lava Fork
  4. 620 SM (±150 tahun)VEI ?Perkiraan geologi
    BCE 620 – Berlangsung
    Iskut River
  5. 1830 SM (±300 tahun)VEI ?Perkiraan geologi
    BCE 1830 – Berlangsung
    Iskut River
  6. 3450 SM (±150 tahun)VEI ?Perkiraan geologi
    BCE 3450 – Berlangsung
    Iskut River
  7. 4700 SM (±300 tahun)VEI ?Perkiraan geologi
    BCE 4700 – Berlangsung
    Iskut River
  8. 6830 SM (±150 tahun)VEI ?Perkiraan geologi
    BCE 6830 – Berlangsung
    Iskut River

Tautan eksternal

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