Gorely
Caldera · Russia · 1799m

- Type
- Caldera
- Country
- Russia
- Region
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Elevation
- 1799m
- Coordinates
- 52.555, 158.036
- Last eruption
- 2010
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Basalt / Picro-Basalt
Geological summary
Gorely volcano consists of five small overlapping stratovolcanoes constructed along a WNW-ESE line within a large 9 x 13 km caldera. The caldera formed about 38,000-40,000 years ago accompanied by the eruption of about 100 km3 of tephra. The massive complex includes about 40 cinder cones, some of which contain acid or freshwater crater lakes; three major rift zones cut the complex. Another Holocene stratovolcano is located on the SW flank. Activity during the Holocene was characterized by frequent mild-to-moderate explosive eruptions along with a half dozen episodes of major lava extrusion. Early Holocene explosive activity, along with lava flows filled in much of the caldera. Quiescent periods became longer between 6,000 and 2,000 years ago, after which the activity was mainly explosive. About 600-650 years ago intermittent strong explosions and lava flow effusion accompanied frequent eruptions. Historical eruptions have consisted of moderate Vulcanian and phreatic explosions.
From Wikipedia
Gorely is a volcano located in the southern part of the Kamchatka Peninsula, Russia. It consists of five overlapping stratovolcanoes and is one of the most active in southern Kamchatka. Gorely is a large, long-lived shield-type volcano that is currently in an eruptive phase. Prior eruptions occurred in 1980-81 and 1984–86.Several complexes compose the overall volcanic structure:ancient Pra-Gorely volcano which measures 20–25 km in diameter; a 12 km diameter caldera; thick stratum of ignimbrites totaling a volume of 100 km3; post-caldera eruption cinder cones; modern edifice – “Young Gorely” composed of three large superimposed cones and 11 associated craters forming a NW-SE trending intra-caldera ridgeline; a complex of 40 modern subsidiary cones on the slopes of “Young Gorely”.
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Eruption history
Detailed timeline
- 2010VEI 1Observed2010-06-06 – 2010-06-22Summit crater
- 1984VEI 2Observed1984-08-04 – 1986-09-21
- 1980VEI 3Observed1980-06-15 – 1981-07-03
- 1961VEI 2Observed1961-01-16 – Ongoing
- 1947VEI 2Observed1947-12 – Ongoing
- 1932VEI ?Geological estimate1932 – Ongoing
- 1931VEI 2Observed1931-05 – 1931-07-15
- 1930VEI 3Observed1930-09 – 1931-01-17
- 1929VEI 3Observed1929-09-01 – 1930-04
- 1869VEI 2Observed1869 – Ongoing
- 1855VEI 2Geological estimate1855-04 – Ongoing
- 1832VEI 3Observed1832-02 – Ongoing
- 1828VEI 3Observed1828-06 – Ongoing
- 1821VEI ?Geological estimate1821 – Ongoing
- 1750 (±50 yrs)VEI 2Geological estimate1750 – Ongoing
- 1330 (±25 yrs)VEI 2Geological estimate1330 – Ongoing
- 1030 (±25 yrs)VEI 3Geological estimate1030 – Ongoing
- 550VEI 3Geological estimate550 – Ongoing
- 250VEI 3Geological estimate250 – Ongoing
- 200VEI 3Geological estimate200 – Ongoing
- 50VEI 3Geological estimate50 – Ongoing
- 350 BCEVEI 3Geological estimateBCE 350 – Ongoing
- 700 BCE (±850 yrs)VEI 0Geological estimateBCE 700 – Ongoing
- 2000 BCEVEI 2Geological estimateBCE 2000 – Ongoing
- 2050 BCEVEI 2Geological estimateBCE 2050 – Ongoing
- 2200 BCEVEI 2Geological estimateBCE 2200 – Ongoing
- 2250 BCEVEI 2Geological estimateBCE 2250 – Ongoing
- 2450 BCEVEI 3Geological estimateBCE 2450 – Ongoing
- 2750 BCEVEI 2Geological estimateBCE 2750 – Ongoing
- 3450 BCEVEI 3Geological estimateBCE 3450 – Ongoing
- 3550 BCEVEI 0Geological estimateBCE 3550 – Ongoing
- 3580 BCE (±100 yrs)VEI 2Geological estimateBCE 3580 – Ongoing
- 3900 BCEVEI 2Geological estimateBCE 3900 – Ongoing
- 3950 BCEVEI 2Geological estimateBCE 3950 – Ongoing
- 4150 BCEVEI 2Geological estimateBCE 4150 – Ongoing
- 4300 BCE (±150 yrs)VEI 0Geological estimateBCE 4300 – Ongoing
- 4350 BCEVEI 3Geological estimateBCE 4350 – Ongoing
- 4450 BCEVEI 2Geological estimateBCE 4450 – Ongoing
- 4500 BCEVEI 2Geological estimateBCE 4500 – Ongoing
- 4600 BCEVEI 2Geological estimateBCE 4600 – Ongoing
- 4650 BCEVEI 3Geological estimateBCE 4650 – Ongoing
- 4700 BCEVEI 2Geological estimateBCE 4700 – Ongoing
- 4750 BCEVEI 3Geological estimateBCE 4750 – Ongoing
- 4950 BCEVEI 2Geological estimateBCE 4950 – Ongoing
- 5150 BCEVEI 3Geological estimateBCE 5150 – Ongoing
- 5300 BCEVEI 2Geological estimateBCE 5300 – Ongoing
- 5450 BCEVEI 3Geological estimateBCE 5450 – Ongoing
- 5500 BCEVEI 3Geological estimateBCE 5500 – Ongoing
- 5650 BCEVEI 3Geological estimateBCE 5650 – Ongoing
- 5950 BCEVEI 3Geological estimateBCE 5950 – Ongoing
- 6050 BCEVEI 0Geological estimateBCE 6050 – Ongoing
- 7250 BCEVEI 2Geological estimateBCE 7250 – Ongoing
- 7400 BCE (±150 yrs)VEI 0Geological estimateBCE 7400 – Ongoing
External links
⚠ For reference only. Not for emergency response.