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02-Dec-2016 15:12

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Lö'ihi rises 10,100 feet above the ocean floor to within 3,100 feet of the water surface.

Recent detailed mapping shows Lö'ihi to be similar in form to Kïlauea and Mauna Loa. In fact, since 1959 the HVO seismic network has recorded large earthquake swarms at Lö'ihi during 1971-1972, 1975, 1984-1985, 1990-1991, and 1996, suggesting major submarine eruptions or magma intrusions into the upper part of Lö'ihi.

Based on INSIVUMEH special bulletins, CONRED reported increased activity at Fuego on 4 August, characterized by explosions ejecting incandescent material as high as 300 m above the crater rim and lava traveling 600 m down the Ceniza (SSW) ravine.

Explosions generated ash plumes that rose almost 1 km and drifted 12 km W and SW.

The volcano's Ultra Plinian eruption on June 15, 1991 produced the second-largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in the Alaska Peninsula.

Complicating the eruption was the arrival of Typhoon Yunya (Diding), bringing a lethal messy mix of ash and rain to towns and cities surrounding the volcano.

Some explosions generated shock waves that rattled nearby structures.

Predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives.

Surrounding areas were severely damaged by pyroclastic surges, ash falls, and subsequently, by the flooding lahars caused by rainwater re-mobilizing earlier volcanic deposits.

Incandescent material was ejected 100 m above the crater rim, and caused avalanches of material that traveled down the Ceniza, Taniluyá (SW), Santa Teresa (W), Las Lajas (SE), Honda (E), and Trinidad (S) drainages.

Ash fell in areas downwind, including Sangre de Cristo (8 km WSW) and Yepocapa (8 km WNW).

Some explosions generated shock waves that rattled nearby structures.Predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives.Surrounding areas were severely damaged by pyroclastic surges, ash falls, and subsequently, by the flooding lahars caused by rainwater re-mobilizing earlier volcanic deposits.Incandescent material was ejected 100 m above the crater rim, and caused avalanches of material that traveled down the Ceniza, Taniluyá (SW), Santa Teresa (W), Las Lajas (SE), Honda (E), and Trinidad (S) drainages.Ash fell in areas downwind, including Sangre de Cristo (8 km WSW) and Yepocapa (8 km WNW). Hoping to meet someone special for a hot, sexual relationship or even just a quick fling?