The ‘a‘ā flow continued toward the ocean and reached it at 1:05 a.m. The Ka‘apuna flow, shown here, traveled from the Southwest Rift Zone vent (7,800 ft elevation) to the coast in just 17 hours, creating a huge steam plume as lava flowed into the sea. The offshoot traveled farther south and reached within 500 m (1,640 ft) of the highway but never crossed it.Late in the evening of June 1, the fissurecontinued to propagate farther downrift. Observatory personnel estimated Late in the evening of June 2 or early on June 3, a new lobe broke out from the 2,530-m (8,300-ft) elevation. At 12:30 p.m. a National Guard plane making an overflight recommended that the ground observers evacuate their current location for positions farther south, as the flow was headed in their direction.The Ka‘apuna flow crossed the highway at 2:00 p.m., 400 m south of the ‘Ōhi‘a Lodge and 6.4 km (4 mi) south of the Ka‘ohe (middle) lobe. Observers reported that a 4.0-km-long (2.5-mi-long) fissure opened near the pit crater, Lua Hou (3,840 m, 12,600 ft), and propagated downrift to near Sulphur Cone (3,350 m, 10,990 ft). Observatory personnel estimated Late in the evening of June 2 or early on June 3, a new lobe broke out from the 2,530-m (8,300-ft) elevation. Originating from the volcano's southwestern rift zone, the eruption remains the largest rift event in the volcano's modern history, lasting 23 days, emitting 376 million cubic meters of lava, and reaching 24 km (15 mi) out to the ocean within 3 hours. Scientists estimate that over the past 3,000 years Mauna Loa has erupted flows on average, every six years.Scientists further note that in the past 100 years, as much as 35 to 40 percent of the volcano’s surface has been covered by new lava—that’s an area equal to or greater than the islands of Oʻahu and Maui.HVO scientists detailed the 1950 event as they study the event to better interpret current activity. Detailed Description The glow of an erupting fissure of lava fountains is seen in a fume cloud high on Mauna Loa's southwest rift zone at the start of the June 1 1950 eruptio…
The upper system extended from 3,200 to 2,590 m (10,500 to 8,500 ft) along 9.6 km (6 mi) of the rift zone. By daybreak on June 2 it crossed Kahuku Ranch's upper pasture road. Yes and no. For example, the Honokua flow covered the 24-km (15-mile) journey, from vent to the ocean, in less than 3 hours.Was this eruption unusually large and rapid? (Public domain.)
The ‘a‘ā flow continued toward the ocean and reached it at 1:05 a.m. Observers reported that a 4.0-km-long (2.5-mi-long) By 10:23 p.m., a bright glow appeared in a fume cloud 13 km (8 mi) downrift from the previous At 12:20 a.m. on June 2, the Honokua flow was approximately 1.5 km above Highway 11. of Massachussetts, Amherst, who has studied the details of this and other Mauna Loa Eruptions) The 1950 eruption of Mauna Loa began on June 1 and continued until June 23. (Public domain. Damage from Earthquakes. This flow moved southward toward Kahuku Ranch. The lava flowed directly into the sea, unimpeded by the cooling effects of the water. On May 29 at 3:17 p.m., two days before the eruption, a magnitude-6.4 earthquake occurred beneath the volcano's west flank. During the Mauna Loa 1950 eruption, three large, fast-moving lava flows advanced down the west flank of the volcano, each crossing the main highway before reaching the ocean. It lasted 23 … By 12:30 a.m., ‘a‘ā flows it crossed Highway 11 at the town of Pāhoehoe, taking out a gas station, the post office, and several homes.
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