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Loloru

Photo of this volcano
  • Country
  • Primary Volcano Type
  • Last Known Eruption
  •  
  • 6.52°S
  • 155.62°E

  • 1887 m
    6191 ft

  • 255030
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

Most Recent Bulletin Report: August 1995 (BGVN 20:08) Citation IconCite this Report

Weak to moderate steaming, but sublimate deposits in possible decline

An aerial inspection took place after the 16 August, M 7.8 earthquake 200 km to the NW. Weak-to-moderate, white vapor emissions were observed from the main fumarole field in a valley on the N flank of the summit lava dome. Sublimate deposits in the valley appeared to be less extensive than when last inspected in 1989. The lake at Loloru's summit appeared normal. There was no discoloration of lake water and the level of water appeared to be unchanged.

Information Contacts: Patrice de Saint-Ours and Ben Talai, RVO.

The Global Volcanism Program has no Weekly Reports available for Loloru.

Bulletin Reports - Index

Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.

10/1984 (SEAN 09:10) Solfataras active on dome and flank

04/1988 (SEAN 13:04) Higher fumarole temperature; sulfur ejected

08/1995 (BGVN 20:08) Weak to moderate steaming, but sublimate deposits in possible decline




Information is preliminary and subject to change. All times are local (unless otherwise noted)


October 1984 (SEAN 09:10) Citation IconCite this Report

Solfataras active on dome and flank

"Aerial inspection showed that dome and flank solfataras were active as normal. Water temperature most recently recorded in a pool by the stream draining the caldera lake was 80°C."

Information Contacts: K. McCue, Bougainville Copper Ltd.


April 1988 (SEAN 13:04) Citation IconCite this Report

Higher fumarole temperature; sulfur ejected

"The main thermal area on the middle NE flank of the dome was visited on 25 April. A temperature of 108°C was measured at the main fumarole, which was surrounded by a mound of sulphur ~1 m high. Measurements since 1964 had obtained maximum temperatures of 93-97°C. Emissions from this fumarole formed a column up to 20 m high, and were accompanied by a low roaring sound. Both H2S and SO2 were detected, and occasional droplets of molten sulphur were ejected."

Information Contacts: D. Lolok, C. McKee, and B. Talai, RVO.


August 1995 (BGVN 20:08) Citation IconCite this Report

Weak to moderate steaming, but sublimate deposits in possible decline

An aerial inspection took place after the 16 August, M 7.8 earthquake 200 km to the NW. Weak-to-moderate, white vapor emissions were observed from the main fumarole field in a valley on the N flank of the summit lava dome. Sublimate deposits in the valley appeared to be less extensive than when last inspected in 1989. The lake at Loloru's summit appeared normal. There was no discoloration of lake water and the level of water appeared to be unchanged.

Information Contacts: Patrice de Saint-Ours and Ben Talai, RVO.

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.

Eruptive History

There is data available for 6 confirmed Holocene eruptive periods.

1050 BCE (?) Confirmed Eruption  

Episode 1 | Eruption Episode
1050 BCE (?) - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 1 Events for Episode 1

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion

1260 BCE ± 300 years Confirmed Eruption  

Episode 1 | Eruption Episode
1260 BCE ± 300 years - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 2 Events for Episode 1

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Pyroclastic flow

2150 BCE (?) Confirmed Eruption  

Episode 1 | Eruption Episode
2150 BCE (?) - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 2 Events for Episode 1

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Pyroclastic flow

3150 BCE (?) Confirmed Eruption  

Episode 1 | Eruption Episode
3150 BCE (?) - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 2 Events for Episode 1

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Pyroclastic flow

4150 BCE (?) Confirmed Eruption  

Episode 1 | Eruption Episode
4150 BCE (?) - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 2 Events for Episode 1

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Pyroclastic flow

6950 BCE (?) Confirmed Eruption  

Episode 1 | Eruption Episode
6950 BCE (?) - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 1 Events for Episode 1

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
Deformation History

There is no Deformation History data available for Loloru.

Emission History

There is no Emissions History data available for Loloru.

GVP Map Holdings

The maps shown below have been scanned from the GVP map archives and include the volcano on this page. Clicking on the small images will load the full 300 dpi map. Very small-scale maps (such as world maps) are not included. The maps database originated over 30 years ago, but was only recently updated and connected to our main database. We welcome users to tell us if they see incorrect information or other problems with the maps; please use the Contact GVP link at the bottom of the page to send us email.

Smithsonian Sample Collections Database

There are no samples for Loloru in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.

External Sites