Hualālai
Hualalai
Gunung api perisai · United States · 2523 m

- Tipe
- Gunung api perisai
- Negara
- United States
- Wilayah
- Eastern Pacific Volcanic Regions / Hawaiian-Emperor Hotspot Volcano Group
- Ketinggian
- 2523 m
- Koordinat
- 19.692, -155.870
- Letusan terakhir
- 1801
- Kondisi tektonik
- Intraplate / Oceanic crust (< 15 km)
- Bentuk lahan
- Shield
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
The basaltic Hualalai, at the western end of the island, is the third youngest shield volcano on Hawaii. Three rift zones, with numerous cinder cones and spatter cones, trend N, NW, and SE, and converge about 5 km E of the summit. Detailed mapping has shown that 95% of the surface area is of Holocene age, more than half is less than 3,000 years old, and a quarter is less than 1,000 years old. Eruptions at the end of the 18th century and in 1801 produced lava flows from vents on the NW rift zone that reached the sea and buried villages; the 1801 Huehue lava flow underlies part of the airport at Kona. The earlier of the two flows, the Kaupulehu lava flow, is notable for its large quantities of lava-encrusted mafic and ultramafic nodular xenoliths.
Ringkasan Wikipedia
Ringkasan InggrisHualālai is an active shield volcano on the island of Hawaiʻi in the Hawaiian Islands. It is the westernmost, third-youngest and the third-most active of the five volcanoes that form the island of Hawaiʻi, following Kīlauea and the much larger Mauna Loa. Its peak stands 8,271 feet (2,521 m) above sea level. Hualālai is estimated to have risen above sea level about 300,000 years ago. Despite maintaining a very low level of activity since its last eruption in 1801, and being unusually inactive for the last 2,000 years, Hualālai is still considered active, and is expected to erupt again sometime in the next 100 years. The relative unpreparedness of the residents in the area caused by the lull in activity would worsen an eruption's consequences.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 1800VEI 0Teramati1800 – 1801NW rift zone (520 m)
- 1784 (±7 tahun)VEI 0Teramati1784 – BerlangsungNW rift zone (1400-1900 m)
- 1650 (±50 tahun)VEI 1Perkiraan geologi1650 – BerlangsungNW rift zone (Luamakami)
- 1240 (±150 tahun)VEI 2Perkiraan geologi1240 – BerlangsungSSE rift zone (Waha Pele)
- 1150VEI 0Perkiraan geologi1150 – BerlangsungNW rift zone (Puu Alauawa, Nahaha)
- 1050 (±100 tahun)VEI 1Perkiraan geologi1050 – BerlangsungSSE rift zone (3 km NE of Waha Pele)
- 920 (±50 tahun)VEI 0Perkiraan geologi920 – BerlangsungNW rift zone (2 km NW of Luamakami)
- 770 (±200 tahun)VEI 1Perkiraan geologi770 – BerlangsungSSE rift zone (4.5 km NW of Waha Pele
- 80 SM (±75 tahun)VEI 0Perkiraan geologiBCE 80 – BerlangsungNorth rift zone (1130-1830 m)
- 350 SM (±75 tahun)VEI 0Perkiraan geologiBCE 350 – BerlangsungSE flank (1 km west of Waha Pehe)
- 400 SM (±75 tahun)VEI 0Perkiraan geologiBCE 400 – BerlangsungNW rift zone (Luamakami)
- 440 SM (±50 tahun)VEI 0Perkiraan geologiBCE 440 – BerlangsungNorth rift zone (3 km NE of Hainoa)
- 720 SM (±75 tahun)VEI 0Perkiraan geologiBCE 720 – BerlangsungNorth rift zone (700 m ENE of Hainoa)
- 1080 SM (±200 tahun)VEI 0Perkiraan geologiBCE 1080 – Berlangsung
- 1150 SM (±75 tahun)VEI 0Perkiraan geologiBCE 1150 – BerlangsungNW rift zone (0.7 km NW of Luamakami)
- 1650 SM (±200 tahun)VEI 0Perkiraan geologiBCE 1650 – Berlangsung
- 2040 SM (±75 tahun)VEI 0Perkiraan geologiBCE 2040 – BerlangsungNW rift zone (0.3 km NW of Hainoa)
- 2440 SM (±75 tahun)VEI 0Perkiraan geologiBCE 2440 – BerlangsungNW rift zone (1 km W of Hainoa Crater)
- 2770 SM (±75 tahun)VEI 0Perkiraan geologiBCE 2770 – Berlangsung
- 4410 SM (±100 tahun)VEI 0Perkiraan geologiBCE 4410 – BerlangsungSE rift zone (1.6 km SE of Hainoa)
- 6820 SM (±200 tahun)VEI 0Perkiraan geologiBCE 6820 – BerlangsungCone 60 m north of Hainoa Crater
- 7540 SM (±200 tahun)VEI 0Perkiraan geologiBCE 7540 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.