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2. Hawaii Center for Volcanology - Wikipedia

   en.wikipedia.org/wiki/Hawaii_Center_for_Volcanology

   The Hawaii Center for Volcanology was a cooperative effort between the School of Ocean and Earth Science and Technology at the University of Hawaiʻi at Mānoa, the Hawaiian Volcano Observatory of the United States Geological Survey, and the Center for the Study of Active Volcanoes at the University of Hawaii at

3. Hawaiian Volcano Observatory - Wikipedia

   en.wikipedia.org/wiki/Hawaiian_Volcano_Observatory

   The Hawaiian Volcano Observatory (HVO) is an agency of the United States Geological Survey (USGS) and one of five volcano observatories operating under the USGS Volcano Hazards Program. Based in Hilo, Hawaii , the observatory monitors six Hawaiian volcanoes: Kīlauea , Mauna Loa , Kamaʻehuakanaloa (formerly Lōʻihi), Hualālai , Mauna Kea ...

4. Janet Babb - Wikipedia

   en.wikipedia.org/wiki/Janet_Babb

   Janet L. Babb is a geologist from the U.S. Geological Survey who is best known for her work at the Hawaiian Volcano Observatory. [1] [2] Babb is frequently quoted in the news media as an authority source on Hawaiian volcanology. [3] She was a member of the Hawaii Center for Volcanology during its operation. [4] She retired in 2020 and is now an ...

5. Hawaii’s Kilauea Volcano shows more vigorous eruption activity

   www.aol.com/hawaii-kilauea-volcano-shows-more...

   What had been low-level lava flows since Thursday morning became more vigorous fountaining Friday evening, according to the U.S. Geological Survey’s Hawaii Volcano Observatory.

6. Category:Research institutes in Hawaii - Wikipedia

   en.wikipedia.org/wiki/Category:Research...

   Pages in category "Research institutes in Hawaii" The following 16 pages are in this category, out of 16 total. ... Hawaii Center for Volcanology; Honolulu Zoo; I.

7. Honolulu Volcanics - Wikipedia

   en.wikipedia.org/wiki/Honolulu_Volcanics

   The Honolulu Volcanics are a series of volcanoes in the southeastern sector of Oʻahu [2] and includes dikes, lava flows, spatter cones, [3] tephra deposits, [4] tuff cones, [3] and mesas where the surrounding terrain has been eroded away. [5]