USGS
Hawaiian Volcano Observatory

Kilauea
Eruption
Summary

Hazards
History

Mauna Loa

Earthquakes

Other Volcanoes

Volcanic Hazards

About HVO

Kilauea

10 July 2001

E. Kupapa`u--just another day in the office
Ocean entry at dusk, Kilauea volcano, Hawai'i.
| med | large |
Ocean entry after dark, Kilauea volcano, Hawai'i.
| med | large |
Views from east of E. Kupapa`u ocean entry at dusk and after dark. The bench is rather large, reaching out about 120 m from the sea cliff. Most activity this evening was at the most seaward point of the bench. Note the new black sand beach formed by deposition of glass created when lava enters the sea.
Lava enters the sea at dusk, Kilauea volcano, Hawai'i.
| med | large |
Glow reflected in water, Kilauea volcano, Hawai'i.
| med | large |
Left. Dusk view of front of E. Kupapa`u bench, with lava behind flowing off the bench into the water. Two floating pieces of incandescent crust are visible at left, kept afloat by expanding gas within the crust and steam from heated sea water along the base of the crust. Right. Glow from the ocean entry reflected off rippled sea surface.

 

Map of flows from Pu`u `O`o: June 2001

Map of lava flows on south coastal part of Kilauea Volcano as of June 2001

Large map Map shows lava flows erupted during the 1983-present activity of Pu`u `O`o and Kupaianaha. The flows active from December 17, 2000 through June 30, 2001 are shown in red, above and on Pulama pali and on the coastal plain,. Most of the recent flows are fed from breakout points at 1920-1700 feet, above the pali in the northern part of the large red area. Lava re-entered the sea just west of Kamokuna on January 21, 2001, but soon stopped when activity shifted from the western to the eastern branch of the flow. Since then, activity has been divided between the eastern and western branches. Breakouts from the eastern tube system have destroyed hundreds of meters of the Royal Gardens access road. Lava fed through the eastern system has been entering the ocean since April 25, a few hundred meters northeast of Kupapa`u Point. Since then, a large bench has developed at the E. Kupapa`u entry site. On May 31, a tiny trickle of lava fed through the western tube system dripped into the water about 500 m west of the Kamokuna bench but stopped within a day. Since then, all lava entering the sea has gone through the E. Kupapa`u entry.

The shatter ring is a prominent tumulus near the western branch of the active flow that is a handy reference point for some of our observations.


HomeVolcano WatchProductsPhoto GalleryPress Releases
How Hawaiian Volcanoes Work

The URL of this page is http://hvo.wr.usgs.gov/multimedia/archive/2000/Aug/
Contact: hvowebmaster@usgs.gov
Updated: 6 August 2001 (DAS)