List of volcanoes in the Hawaiian–Emperor seamount chain: Difference between revisions

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|-
|-
! Name
! Name
! Island
! Last Eruption
! Last eruption
! class="unsortable" |Coordinates
! class="unsortable" |Coordinates
! width="12%" | Age
! width="12%" | Age
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|-
|-
| [[Loihi Seamount|Lō{{okina}}hi Seamount]]
| [[Loihi Seamount|Lō{{okina}}hi Seamount]]
| {{center|—}}
| 1996 (Active)<ref name="Garcia, et. al.-2005" />
| 1996 (Active)<ref name="Garcia, et. al.-2005" />
| {{coord|18.92|N|155.27|W |type:mountain_region:US-HI |display=inline}}
| {{coord|18.92|N|155.27|W |type:mountain_region:US-HI |display=inline}}
| > 400,000<ref name="Garcia, et. al.-2005" />
| > 400,000<ref name="Garcia, et. al.-2005" />
| Submarine volcano approximately {{convert|35|km|mi|0|abbr=on|sp=us}} southeast of Hawaii. It will eventually breach sea level and become the newest Hawaiian island.<ref name="Garcia, et. al.-2005">{{cite paper| coauthors = Michael O. Garcia, Jackie Caplan-Auerbanch, Eric H. De Carlo, M.D. Kurz, N. Becker| title = Geology, geochemistry and earthquake history of Lō{{okina}}ihi Seamount, Hawai{{okina}}i| version = This is the pre-press version of a paper that was published on 2006-05-16 as "Geochemistry, and Earthquake History of Lō{{okina}}ihi Seamount, Hawai{{okina}}i's youngest volcano", in ''Chemie der Erde – Geochemistry'' (66) 2:81–108 | publisher = University of Hawaii – [[School of Ocean and Earth Science and Technology]] | date = 2005-09-20 | url =http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B7CW6-4HKD01M-1&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&_docanchor=&view=c&_searchStrId=1103763094&_rerunOrigin=google&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=d9108dc4131193bcb700b18c568a5783| format = PDF | accessdate = 2009-03-20}} [http://myweb.facstaff.wwu.edu/caplanj/pdf/pubs/loihi_chemie_der_erde.pdf Pre-press version]</ref>{{ref|haw1|[a]}}
| Submarine volcano approximately {{convert|35|km|mi|0|abbr=on|sp=us}} southeast of Hawaii. It will eventually breach sea level and become the newest Hawaiian island.<ref name="Garcia, et. al.-2005">{{cite paper| coauthors = Michael O. Garcia, Jackie Caplan-Auerbanch, Eric H. De Carlo, M.D. Kurz, N. Becker| title = Geology, geochemistry and earthquake history of Lō{{okina}}ihi Seamount, Hawai{{okina}}i| version = This is the pre-press version of a paper that was published on 2006-05-16 as "Geochemistry, and Earthquake History of Lō{{okina}}ihi Seamount, Hawai{{okina}}i's youngest volcano", in ''Chemie der Erde – Geochemistry'' (66) 2:81–108 | publisher = University of Hawaii – [[School of Ocean and Earth Science and Technology]] | date = 2005-09-20 | url =http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B7CW6-4HKD01M-1&_user=10&_rdoc=1&_fmt=&_orig=search&_sort=d&_docanchor=&view=c&_searchStrId=1103763094&_rerunOrigin=google&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=d9108dc4131193bcb700b18c568a5783| format = PDF | accessdate = 2009-03-20}} [http://myweb.facstaff.wwu.edu/caplanj/pdf/pubs/loihi_chemie_der_erde.pdf Pre-press version]</ref>{{ref|haw1|[a]}}
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Hawaii (island)|Big Island]]'''
|-
|-
| [[Kīlauea]]
| [[Kīlauea]]
| [[Hawaii (island)|Big Island]]
| Erupting<ref name="USGS-Kīlauea" />
| Erupting<ref name="USGS-Kīlauea" />
| {{coord|19|25|N|155|17|W|type:mountain_region:US|display=inline}}
| {{coord|19|25|N|155|17|W|type:mountain_region:US|display=inline}}
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|-
|-
| [[Mauna Loa]]
| [[Mauna Loa]]
| [[Hawaii (island)|Big Island]]
| 1984 (Active)<ref name=worldatlas>{{cite book|author=School Specialty Publishing |title=World Atlas |year=2006 |publisher=School Specialty Publishing |page=13 |isbn=0769642608 |edition=Illustrated |url=http://books.google.com/books?id=Gt1DFukw42YC&lpg=PA13 |accessdate=2009-12-13}}</ref>
| 1984 (Active)<ref name=worldatlas>{{cite book|author=School Specialty Publishing |title=World Atlas |year=2006 |publisher=School Specialty Publishing |page=13 |isbn=0769642608 |edition=Illustrated |url=http://books.google.com/books?id=Gt1DFukw42YC&lpg=PA13 |accessdate=2009-12-13}}</ref>
| {{coord|19|28|46.3|N|155|36|09.6|W |type:mountain_region:US-HI |display=inline}}
| {{coord|19|28|46.3|N|155|36|09.6|W |type:mountain_region:US-HI |display=inline}}
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|-
|-
| [[Hualālai]]
| [[Hualālai]]
| [[Hawaii (island)|Big Island]]
| 1801 (Dormant)<ref name="Macdonald" />
| 1801 (dormant)<ref name="Macdonald" />
| {{coord|19|41|32|N|155|52|02|W|type:mountain_region:US-HI}}
| {{coord|19|41|32|N|155|52|02|W|type:mountain_region:US-HI}}
| > 300,000 years<ref name="Macdonald">{{cite book|author=G. A. Macdonald|coauthors=A. T. Abbott|year=1970|title=Volcanoes in the Sea|publisher=University of Hawai{{okina}}i Press|pages=441}}</ref>
| > 300,000 years<ref name="Macdonald">{{cite book|author=G. A. Macdonald|coauthors=A. T. Abbott|year=1970|title=Volcanoes in the Sea|publisher=University of Hawai{{okina}}i Press|pages=441}}</ref>
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|-
|-
| [[Mauna Kea]]
| [[Mauna Kea]]
| [[Hawaii (island)|Big Island]]
| About 4460 [[Before Present|BP]] (Dormant)
| About 4460 [[Before Present|BP]] (dormant)
| {{coord|19|49|14.39|N|155|28|05.04|W|type:mountain_region:US-HI_source:ngs|display=inline}}
| {{coord|19|49|14.39|N|155|28|05.04|W|type:mountain_region:US-HI_source:ngs|display=inline}}
| ~ 375,000–1 million years<ref name=soestform>{{cite web |author=Rubin, Ken|url=http://www.soest.hawaii.edu/GG/HCV/haw_formation.html |title=The Formation of the Hawaiian Islands |accessdate=2009-05-18 |publisher=Hawaii Center for Vulcanology }}</ref><ref name="USGS-Mauna Kea">{{cite web|url=http://hvo.wr.usgs.gov/volcanoes/maunakea/ |title=Mauna Kea Hawai`i's Tallest Volcano|publisher=[[United States Geological Survey]]|accessdate=2009-05-14}}</ref>
| ~ 375,000–1 million years<ref name=soestform>{{cite web |author=Rubin, Ken|url=http://www.soest.hawaii.edu/GG/HCV/haw_formation.html |title=The Formation of the Hawaiian Islands |accessdate=2009-05-18 |publisher=Hawaii Center for Vulcanology }}</ref><ref name="USGS-Mauna Kea">{{cite web|url=http://hvo.wr.usgs.gov/volcanoes/maunakea/ |title=Mauna Kea Hawai`i's Tallest Volcano|publisher=[[United States Geological Survey]]|accessdate=2009-05-14}}</ref>
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|-
|-
| [[Kohala (mountain)|Kohala]]
| [[Kohala (mountain)|Kohala]]
| [[Hawaii (island)|Big Island]]
| About 120,000 [[Before Present|BP]] (Extinct)<ref name="USGS-2007" />
| About 120,000 [[Before Present|BP]] (extinct)<ref name="USGS-2007" />
| {{coord|20|05|10|N|155|43|02|W|type:mountain_region:US-HI_source:ngs|display=inline}}
| {{coord|20|05|10|N|155|43|02|W|type:mountain_region:US-HI_source:ngs|display=inline}}
| ~ 430,000–1 million years<ref name=soestform/><ref name="USGS-2007">{{cite web|url=http://pubs.usgs.gov/of/2007/1089/Hawaii_expl_pamphlet.pdf |title=Geological Map of the State of Hawaii|coauthors=David R. Sherrod, John M. Sinton, Sarah E. Watkins, Kelly M. Brunt|date=2007|work=USGS Hawaii geology pamphlet|publisher=[[United States Geological Survey]]|accessdate=2009-04-12|format=PDF}} pg. 41–43</ref>
| ~ 430,000–1 million years<ref name=soestform/><ref name="USGS-2007">{{cite web|url=http://pubs.usgs.gov/of/2007/1089/Hawaii_expl_pamphlet.pdf |title=Geological Map of the State of Hawaii|coauthors=David R. Sherrod, John M. Sinton, Sarah E. Watkins, Kelly M. Brunt|date=2007|work=USGS Hawaii geology pamphlet|publisher=[[United States Geological Survey]]|accessdate=2009-04-12|format=PDF}} pg. 41–43</ref>
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|-
|-
| [[Māhukona]]
| [[Māhukona]]
| [[Hawaii (island)|Big Island]]
|
| {{center|—}}
| {{coord|20|01|0|N|156|1|0|W|type:mountain_region:US|display=inline}}
| {{coord|20|01|0|N|156|1|0|W|type:mountain_region:US|display=inline}}
|
|
| Submerged, having long since disappeared into the sea.<ref>{{cite book|coauthors=Clague, D.A., and Moore, J.G.|title=Geology and Petrology of Mahukona Volcano, Hawaii|publisher=[[Bulletin of Volcanology]]|date=1991|volume=53|pages=159–172|accessdate=10-24-09}}</ref>{{ref|haw2|[b]}}
| Submerged, having long since disappeared into the sea.<ref>{{cite book|coauthors=Clague, D.A., and Moore, J.G.|title=Geology and Petrology of Mahukona Volcano, Hawaii|publisher=[[Bulletin of Volcanology]]|date=1991|volume=53|pages=159–172|accessdate=10-24-09}}</ref>{{ref|haw2|[b]}}
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Maui]]'''
|-
|-
| [[Haleakalā]]
| [[Haleakalā]]
| [[Maui]]
| 18th Century<ref name="USGS-East Maui" />
| 18th Century<ref name="USGS-East Maui" />
| {{coord|display=inline|20|42|35|N|156|15|12|W|type:mountain_region:US-HI}}
| {{coord|display=inline|20|42|35|N|156|15|12|W|type:mountain_region:US-HI}}
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|-
|-
| [[West Maui Mountains|West Maui]]
| [[West Maui Mountains|West Maui]]
| [[Maui]]
|
| {{center|—}}
| {{coord|20|54|N|156|37|W|type:mountain_region:US-HI|display=inline}}
| {{coord|20|54|N|156|37|W|type:mountain_region:US-HI|display=inline}}
| ~ 1.32 million years<ref name=soestform/>
| ~ 1.32 million years<ref name=soestform/>
| Much eroded shield volcano which makes up the western quarter of Maui.
| Much eroded shield volcano which makes up the western quarter of Maui.
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Kahoolawe|Kaho{{okina}}olawe]]'''
|-
|-
| [[Kahoolawe|Kaho{{okina}}olawe]]
| [[Kahoolawe|Kaho{{okina}}olawe]]
| [[Kahoolawe|Kaho{{okina}}olawe]]
|
| {{center|—}}
| {{coord|20|33|N|156|36|W|display=inline}}
| {{coord|20|33|N|156|36|W|display=inline}}
| > 1.03 million years<ref name=soestform/><ref name="Kahoolawe Photo Gallery">{{cite web|url=http://volcano.oregonstate.edu/vwdocs/volc_images/north_america/hawaii/kahoolawe.html |title=Kaho{{okina}}olawe, Hawaii|work=Photo Gallery of Kaho{{okina}}olawe island|publisher=[[Oregon State University]]|accessdate=2009-04-04}}</ref>
| > 1.03 million years<ref name=soestform/><ref name="Kahoolawe Photo Gallery">{{cite web|url=http://volcano.oregonstate.edu/vwdocs/volc_images/north_america/hawaii/kahoolawe.html |title=Kaho{{okina}}olawe, Hawaii|work=Photo Gallery of Kaho{{okina}}olawe island|publisher=[[Oregon State University]]|accessdate=2009-04-04}}</ref>
| Smallest of the 8 principal Hawaiian islands.<ref name="USGS-2007"/> Uninhabited.<ref>{{cite web |url=http://factfinder.census.gov/servlet/DTTable?_bm=y&-show_geoid=Y&-tree_id=4001&-_caller=geoselect&-context=dt&-errMsg=&-all_geo_types=N&-mt_name=DEC_2000_SF1_U_P001&-redoLog=true&-transpose=N&-search_map_config=|b=50|l=en|t=4001|zf=0.0|ms=sel_00dec|dw=0.3235256323641746|dh=0.22787245954044197|dt=gov.census.aff.domain.map.EnglishMapExtent|if=gif|cx=-156.5954874499071|cy=20.568734378783724|zl=5|pz=5|bo=318:317:316:314:313:323:319|bl=362:393:358:357:356:355:354|ft=350:349:335:389:388:332:331|fl=381:403:204:380:369:379:368|g=14000US15009031600&-PANEL_ID=p_dt_geo_map&-_lang=en&-geo_id=15000US150090303029&-CONTEXT=dt&-format=&-search_results=14000US15009030302&-ds_name=DEC_2000_SF1_U |title=Block Group 9, Census Tract 303.02, Maui County, Hawaii |accessdate=2009-05-17 |date=2000 |publisher=[[U.S. Census Bureau]] }}</ref>
| Smallest of the 8 principal Hawaiian islands.<ref name="USGS-2007"/> Uninhabited.<ref>{{cite web |url=http://factfinder.census.gov/servlet/DTTable?_bm=y&-show_geoid=Y&-tree_id=4001&-_caller=geoselect&-context=dt&-errMsg=&-all_geo_types=N&-mt_name=DEC_2000_SF1_U_P001&-redoLog=true&-transpose=N&-search_map_config=|b=50|l=en|t=4001|zf=0.0|ms=sel_00dec|dw=0.3235256323641746|dh=0.22787245954044197|dt=gov.census.aff.domain.map.EnglishMapExtent|if=gif|cx=-156.5954874499071|cy=20.568734378783724|zl=5|pz=5|bo=318:317:316:314:313:323:319|bl=362:393:358:357:356:355:354|ft=350:349:335:389:388:332:331|fl=381:403:204:380:369:379:368|g=14000US15009031600&-PANEL_ID=p_dt_geo_map&-_lang=en&-geo_id=15000US150090303029&-CONTEXT=dt&-format=&-search_results=14000US15009030302&-ds_name=DEC_2000_SF1_U |title=Block Group 9, Census Tract 303.02, Maui County, Hawaii |accessdate=2009-05-17 |date=2000 |publisher=[[U.S. Census Bureau]] }}</ref>
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Lanai|Lāna{{okina}}i]]'''
|-
|-
| [[Lanai|Lāna{{okina}}i]]
| [[Lanai|Lāna{{okina}}i]]
| [[Lanai|Lāna{{okina}}i]]
|
| {{center|—}}
| {{coord|20|50|N|156|56|W|type:isle|display=inline}}
| {{coord|20|50|N|156|56|W|type:isle|display=inline}}
| ~ 1.28 million years<ref name=soestform/>
| ~ 1.28 million years<ref name=soestform/>
| Sixth-largest island.<ref>{{cite web |url=http://hawaii.gov/dbedt/info/economic/databook/db2004/section05.pdf |title=The State of Hawaii Data Book 2004 |accessdate=2009-05-17 |date=2004 |publisher=Hawaii.gov |format=PDF}}</ref> The only town is [[Lānaʻi City]], a small settlement.
| Sixth-largest island.<ref>{{cite web |url=http://hawaii.gov/dbedt/info/economic/databook/db2004/section05.pdf |title=The State of Hawaii Data Book 2004 |accessdate=2009-05-17 |date=2004 |publisher=Hawaii.gov |format=PDF}}</ref> The only town is [[Lānaʻi City]], a small settlement.
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Molokai|Moloka{{okina}}i]]'''
|-
|-
| [[East Molokai|East Moloka{{okina}}i]]
| [[East Molokai|East Moloka{{okina}}i]]
| [[Molokai|Moloka{{okina}}i]]
|
| {{center|—}}
| {{coord|21|7|N|156|51|W|type:mountain_region:US-HI|display=inline}}
| {{coord|21|7|N|156|51|W|type:mountain_region:US-HI|display=inline}}
| ~ 1.76 million years<ref name=soestform/>
| ~ 1.76 million years<ref name=soestform/>
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|-
|-
| [[West Molokai|West Moloka{{okina}}i]]
| [[West Molokai|West Moloka{{okina}}i]]
| [[Molokai|Moloka{{okina}}i]]
|
| {{center|—}}
| {{coord|21|9|N|157|14|W|type:mountain_region:US-HI|display=inline}}
| {{coord|21|9|N|157|14|W|type:mountain_region:US-HI|display=inline}}
| ~ 1.9 million years<ref name=soestform/>
| ~ 1.9 million years<ref name=soestform/>
| Northern half suffered a large collapse 1.5 million years ago.<ref name=MBARI9>{{cite web |url=http://www.mbari.org/volcanism/Hawaii/HR-Landslides.htm |title=Hawaiian Landslides |accessdate=2009-06-13 |date=2009-02-05 |publisher=Monterey Bay Aquarium Research Institute }}</ref>
| Northern half suffered a large collapse 1.5 million years ago.<ref name=MBARI9>{{cite web |url=http://www.mbari.org/volcanism/Hawaii/HR-Landslides.htm |title=Hawaiian Landslides |accessdate=2009-06-13 |date=2009-02-05 |publisher=Monterey Bay Aquarium Research Institute }}</ref>
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Oahu]]'''
|-
|-
| [[Koolau Range]]
| [[Koolau Range]]
| [[Molokai|Moloka{{okina}}i]]
|
| {{center|—}}
| {{coord|21|19|N|157|46|W|type:mountain_region:US-HI|display=inline}}
| {{coord|21|19|N|157|46|W|type:mountain_region:US-HI|display=inline}}
| 2.7 million<ref name=soest>{{cite web |url=http://www.soest.hawaii.edu/coasts/publications/hawaiiCoastline/oahu.html |title=Hawaii's Coastline – Oahu |accessdate=2009-05-18 |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref>
| 2.7 million<ref name=soest>{{cite web |url=http://www.soest.hawaii.edu/coasts/publications/hawaiiCoastline/oahu.html |title=Hawaii's Coastline – Oahu |accessdate=2009-05-18 |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref>
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|-
|-
| [[Waianae Range|Wai{{okina}}anae Range]]
| [[Waianae Range|Wai{{okina}}anae Range]]
| [[Molokai|Moloka{{okina}}i]]
| 2.5 million [[Before Present|BP]]<ref name=usgs1995>{{cite web |url=http://hvo.wr.usgs.gov/volcanowatch/1995/95_09_29.html |title=O'ahu, Ni'ihau, and Kaua'i |accessdate=2009-06-13 |date=1995-09-29 |publisher=[[United States Geological Survey]] }}</ref>
| 2.5 million [[Before Present|BP]]<ref name=usgs1995>{{cite web |url=http://hvo.wr.usgs.gov/volcanowatch/1995/95_09_29.html |title=O'ahu, Ni'ihau, and Kaua'i |accessdate=2009-06-13 |date=1995-09-29 |publisher=[[United States Geological Survey]] }}</ref>
| {{coord|21|30|N|158|9|W|type:mountain_region:US-HI|display=inline}}
| {{coord|21|30|N|158|9|W|type:mountain_region:US-HI|display=inline}}
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| The eroded remains of a shield volcano that comprised the western half of the island.<ref name=usgs1995/>
| The eroded remains of a shield volcano that comprised the western half of the island.<ref name=usgs1995/>
|-
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Kaʻula]]'''
|-
| [[Kaʻula]]
| [[Kaʻula]]
| [[Kaʻula]]
|
| {{center|—}}
| {{coord|21|39|N|160|32|W|source:eswiki|display=inline}}
| {{coord|21|39|N|160|32|W|source:eswiki|display=inline}}
| ~ 4 million years<ref name=soestform/>
| ~ 4 million years<ref name=soestform/>
| Tiny crescent-shaped barren island. Uninhabited but for divers & fishermen.<ref>{{cite web |url=http://www.hawaiioirc.org/OIRC-ISLETS-Niihau/OIRC-ISLETS-Niihau-Kaula.htm |title=Offshore Island Restoration Committee – Kaula |accessdate=2009-06-11 |publisher=Offshore Island Restoration Committee }}</ref>
| Tiny crescent-shaped barren island. Uninhabited but for divers & fishermen.<ref>{{cite web |url=http://www.hawaiioirc.org/OIRC-ISLETS-Niihau/OIRC-ISLETS-Niihau-Kaula.htm |title=Offshore Island Restoration Committee – Kaula |accessdate=2009-06-11 |publisher=Offshore Island Restoration Committee }}</ref>
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Niihau|Ni{{okina}}ihau]]'''
|-
|-
| [[Niihau|Ni{{okina}}ihau]]
| [[Niihau|Ni{{okina}}ihau]]
| [[Niihau|Ni{{okina}}ihau]]
|
| {{center|—}}
| {{coord|21|54|N|160|10|W|type:isle|display=inline}}
| {{coord|21|54|N|160|10|W|type:isle|display=inline}}
| ~4.9 million<ref name=soestform/><ref>{{cite web |url=http://www.soest.hawaii.edu/coasts/publications/hawaiiCoastline/niihau.html |title=Hawaii's Coastline – Niihau |accessdate=2009-05-18 |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref>
| ~4.9 million<ref name=soestform/><ref>{{cite web |url=http://www.soest.hawaii.edu/coasts/publications/hawaiiCoastline/niihau.html |title=Hawaii's Coastline – Niihau |accessdate=2009-05-18 |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref>
| Smallest inhabited island.<ref>{{cite web |url=http://www.soest.hawaii.edu/pibhmc/pibhmc_mhi_nii.htm |title=Main Hawaiian Islands: Ni‘ihau |accessdate=2009-06-13 |date= |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref> Formed from a side vent of Kaua{{okina}}i.
| Smallest inhabited island.<ref>{{cite web |url=http://www.soest.hawaii.edu/pibhmc/pibhmc_mhi_nii.htm |title=Main Hawaiian Islands: Ni‘ihau |accessdate=2009-06-13 |date= |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref> Formed from a side vent of Kaua{{okina}}i.
|-
| colspan="5" style="text-align:center; background:lightblue" | '''[[Kauai|Kaua{{okina}}i]]'''
|-
|-
| [[Kauai|Kaua{{okina}}i]]
| [[Kauai|Kaua{{okina}}i]]
| [[Kauai|Kaua{{okina}}i]]
|
| {{center|—}}
| {{coord|22|05|N|159|30|W|type:isle|display=inline}}
| {{coord|22|05|N|159|30|W|type:isle|display=inline}}
| >5 million<ref name=soestform/><ref>{{cite web |url=http://www.soest.hawaii.edu/coasts/publications/hawaiiCoastline/kauai.html |title=Hawaii's Coastline – Kauai |accessdate=2009-05-18 |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref>
| >5 million<ref name=soestform/><ref>{{cite web |url=http://www.soest.hawaii.edu/coasts/publications/hawaiiCoastline/kauai.html |title=Hawaii's Coastline – Kauai |accessdate=2009-05-18 |publisher=University of Hawaii – [[School of Ocean and Earth Science and Technology]] }}</ref>

Revision as of 23:34, 19 December 2009

The Hawaiian – Emperor seamount chain. The two sects, the Emperor and Hawaiian strands, are separated by a large L-shaped bend.

This is a list of volcanoes in the Hawaiian – Emperor seamount chain. It documents all of the most notable volcanoes in the chain, however there are many others that have yet to be properly studied.

The Hawaiian-Emperor seamount chain is a chain of volcanoes and seamounts extending across the Pacific Ocean. The chain has been produced by the movement of the ocean crust over the Hawaii hotspot, a "bump" of heat responsible for the creation and volcanic activity of the volcanoes in the chain. As the oceanic crust moves the volcanoes further away from their source of energy, they slowly lose power and erupt less powerfully and less frequently, eventually ceasing to erupt at all. At that point erosion takes over, and slowly grinds the volcano down into the ocean, creating first atolls and atoll islands, and then submerging into the sea altogether, becoming seamounts and/or guyots.[1]

Following this pattern, the seamounts to the back of the chain are far older then those at the forefront; the oldest known seamount in the chain, Meiji Seamount, is estimated to be between 81 and 86 million years,[2] whereas Lōʻhi Seamount, the newest volcano in the chain, is of under 400,000 years of age.[3] There may be even older seamounts, as the end of the chain dangles near the Kuril–Kamchatka Trench, which could have since destroyed them.[4]

The chain can be divided into three subsections. The first, the Hawaiian archipelago (also known as the Windward isles), is made up of the islands comprising Hawaii state (not to be confused with Hawaii island). Being closest to the hotspot, it is both the youngest part of the chain, and also the part that is still volcanically active. Hawaii island is comprised of five volcanoes, of which two (Kilauea and Mauna Loa) are still active. Lōʻhi Seamount continues to grow offshore, and is the only known volcano in the chain that is in the submarine pre-shield stage.[1]

The second part of the chain are the Northwestern Hawaiian Islands, collectively referred to as the Leeward isles. Erosion has long since overtaken activity at these islands, and most of them are atolls, atoll islands, or at the least extinct islands. They contain many of the most northerly atolls in the world; one of them, Kure Atoll, is the northern-most atoll in the world.[5] On June 15, 2006, President George W. Bush issued a proclamation creating Papahānaumokuākea Marine National Monument under the Antiquities Act of 1906. The national monument, meant to protect the biodiversity of the isles, encompasses all of the northern isles, and is one of the biggest such protected areas in the world. It limits tourism to the area, and calls for a phase-out of fishing by 2011.[6]

The oldest and most heavily eroded part of the chain are the Emperor seamounts. The Emperor and Hawaiian chains are separated by a large L-shaped bend in the chain, differing in orientation by about 60°. It was long attributed to a sudden plate movement, but recent research, conducted in 2003, suggests that it was the movement of the hotspot itself that caused the bend.[7] All of the volcanoes in this part of the chain have long since subsided below the sea, becoming seamounts and guyots. Many of the volcanoes are named after former Emperors of Japan. The seamount chain extends across the Pacific, all the way to the West Pacific, terminating at the Kuril–Kamchatka Trench, at the border of Russia.[4]

Hawaiian archipelago

Name Island Last eruption Coordinates Age Notes
Lōʻhi Seamount
1996 (Active)[3] 18°55′N 155°16′W / 18.92°N 155.27°W / 18.92; -155.27 > 400,000[3] Submarine volcano approximately 35 km (22 mi) southeast of Hawaii. It will eventually breach sea level and become the newest Hawaiian island.[3][a]
Kīlauea Big Island Erupting[8] 19°25′N 155°17′W / 19.417°N 155.283°W / 19.417; -155.283 300,000–600,000 years[8] Kīlauea is currently the most active volcano on Earth.[8]

Puʻu ʻŌʻō, a cinder cone of Kīlauea, has been erupting continuously since January 3, 1983, making it the longest-lived rift-zone eruption of the last six centuries.[9]

Mauna Loa Big Island 1984 (Active)[10] 19°28′46.3″N 155°36′09.6″W / 19.479528°N 155.602667°W / 19.479528; -155.602667 ~1 million years[11] Largest volcano on Earth.[10]
Hualālai Big Island 1801 (dormant)[12] 19°41′32″N 155°52′02″W / 19.69222°N 155.86722°W / 19.69222; -155.86722 > 300,000 years[12] Lies more or less due west of the much taller Mauna Kea and Mauna Loa mountains.[12]
Mauna Kea Big Island About 4460 BP (dormant) 19°49′14.39″N 155°28′05.04″W / 19.8206639°N 155.4680667°W / 19.8206639; -155.4680667 ~ 375,000–1 million years[13][14] World's tallest mountain if below-sea elevation is counted.[15]
Kohala Big Island About 120,000 BP (extinct)[16] 20°05′10″N 155°43′02″W / 20.08611°N 155.71722°W / 20.08611; -155.71722 ~ 430,000–1 million years[13][16] Believed to be the oldest volcano that makes up Hawaii Island.[16]
Māhukona Big Island
20°01′0″N 156°1′0″W / 20.01667°N 156.01667°W / 20.01667; -156.01667 Submerged, having long since disappeared into the sea.[17][b]
Haleakalā Maui 18th Century[18] 20°42′35″N 156°15′12″W / 20.70972°N 156.25333°W / 20.70972; -156.25333 ~ 0.75–2 million years[13][18] forms more than 75% of Maui.[18]
West Maui Maui
20°54′N 156°37′W / 20.900°N 156.617°W / 20.900; -156.617 ~ 1.32 million years[13] Much eroded shield volcano which makes up the western quarter of Maui.
Kahoʻolawe Kahoʻolawe
20°33′N 156°36′W / 20.550°N 156.600°W / 20.550; -156.600 > 1.03 million years[13][19] Smallest of the 8 principal Hawaiian islands.[16] Uninhabited.[20]
Lānaʻi Lānaʻi
20°50′N 156°56′W / 20.833°N 156.933°W / 20.833; -156.933 ~ 1.28 million years[13] Sixth-largest island.[21] The only town is Lānaʻi City, a small settlement.
East Molokaʻi Molokaʻi
21°7′N 156°51′W / 21.117°N 156.850°W / 21.117; -156.850 ~ 1.76 million years[13] Volcano is today only what remains of the southern half.[16]
West Molokaʻi Molokaʻi
21°9′N 157°14′W / 21.150°N 157.233°W / 21.150; -157.233 ~ 1.9 million years[13] Northern half suffered a large collapse 1.5 million years ago.[22]
Koolau Range Molokaʻi
21°19′N 157°46′W / 21.317°N 157.767°W / 21.317; -157.767 2.7 million[23] A fragmented remnant of the eastern or windward shield volcano which also suffered a large collapse sometime before the Molokaʻi collapse.[22]
Waiʻanae Range Molokaʻi 2.5 million BP[24] 21°30′N 158°9′W / 21.500°N 158.150°W / 21.500; -158.150 3.7–3.9 million years[13][23] The eroded remains of a shield volcano that comprised the western half of the island.[24]
Kaʻula Kaʻula
21°39′N 160°32′W / 21.650°N 160.533°W / 21.650; -160.533 ~ 4 million years[13] Tiny crescent-shaped barren island. Uninhabited but for divers & fishermen.[25]
Niʻihau Niʻihau
21°54′N 160°10′W / 21.900°N 160.167°W / 21.900; -160.167 ~4.9 million[13][26] Smallest inhabited island.[27] Formed from a side vent of Kauaʻi.
Kauaʻi Kauaʻi
22°05′N 159°30′W / 22.083°N 159.500°W / 22.083; -159.500 >5 million[13][28] Oldest and fourth largest of the main islands, and home to Mount Waialeale, one of the wettest areas on Earth in terms of precipitation.[29]

Northwestern Hawaiian islands

Name Type Coordinates Age[30] Notes
Nihoa Extinct Island 23°03′38″N 161°55′19″W / 23.06056°N 161.92194°W / 23.06056; -161.92194 7.2 million ± 0.3[13] Small rocky island which supported a small population about 1000 CE; features over 80 cultural sites, including religious places, agricultural terraces, and burial caves.[31]
Necker Island Extinct Island 23°03′N 161°55′W / 23.050°N 161.917°W / 23.050; -161.917 10.3 million ± 0.4[13] Small deserted island with Hawaiian religious shrines and artifacts.[32]
French Frigate Shoals Atoll 23°52′08″N 166°17′10″W / 23.8689°N 166.2860°W / 23.8689; -166.2860 12 million[33] Largest atoll in the northwestern Hawaiian islands.[34]
Gardner Pinnacles Atoll Island 25°01′N 167°59′W / 25.017°N 167.983°W / 25.017; -167.983 12.3 million ± 1.0[13] Two barren rock outcrops surrounded by a reef.[35]
Maro Reef Atoll 25°25′N 170°35′W / 25.417°N 170.583°W / 25.417; -170.583 Largest coral reef of the northwestern Hawaiian islands.[36]
Laysan Atoll Island 25°46′03″N 171°44′00″W / 25.7675°N 171.7334°W / 25.7675; -171.7334 19.9 million ± 0.3[13] Originally named "Kauō" meaning egg, referring to its shape, and home to one of only five natural lakes in all of Hawaii.[37]
Lisianski Island Atoll Island 26°3′48.6564″N 173°57′57.346″W / 26.063515667°N 173.96592944°W / 26.063515667; -173.96592944 A small island surrounded by a huge coral reef nearly the size of Oahu.[38] Named after a Russian navy captain whose ship ran aground there in 1805.[39]
Pearl and Hermes Atoll Atoll Island 27°48′N 175°51′W / 27.800°N 175.850°W / 27.800; -175.850 20.6 million ± 2.7[13] A collection of small, sandy islands, with a lagoon and coral reef. Named after two whaling ships which wrecked on the reef in 1822.[40]
Midway Atoll Atoll Island 28°12′N 177°21′W / 28.200°N 177.350°W / 28.200; -177.350 27.7 million ± 0.6[13] Consists of a ring-shaped barrier reef and two large islets. Named "midway" because of its strategic location in the center of the Pacific Ocean, and was the site of a key battle during World War II.[41]
Kure Atoll Atoll 28°25′N 178°20′W / 28.417°N 178.333°W / 28.417; -178.333 Northern-most coral atoll in the world.[5]

Emperor seamounts

Name Type Coordinates[42] Age Notes
Hancock Seamount 30°15′N 178°50′E / 30.250°N 178.833°E / 30.250; 178.833 Unknown
Colahan Seamount 31°15′N 176°0′E / 31.250°N 176.000°E / 31.250; 176.000 38.6 million ± 0.3[43]
Abbott Seamount 31°48′N 174°18′E / 31.800°N 174.300°E / 31.800; 174.300 38.7 million ± 0.9[43]
Daikakuji Guyot 32°5.00′N 172°18′E / 32.08333°N 172.300°E / 32.08333; 172.300 42.4 million ± 2.3[13] Also the name of a Japanese temple.
Kammu Guyot 32°10′N 173°0′E / 32.167°N 173.000°E / 32.167; 173.000 Unknown Named for former emperor of Japan Emperor Kammu.
Yuryaku Guyot 32°40.20′N 172°16.20′E / 32.67000°N 172.27000°E / 32.67000; 172.27000 43.4 million ± 1.6[13] Named after former emperor of Japan Emperor Yūryaku.
Kimmei Seamount 33°40.84′N 171°38.07′E / 33.68067°N 171.63450°E / 33.68067; 171.63450 ~ 39.9–50 million years[44][13] Named after former emperor of Japan Emperor Kimmei.
Koko Guyot 35°15.00′N 171°35.00′E / 35.25000°N 171.58333°E / 35.25000; 171.58333 48.1 million ± 0.8[13] Named after former emperor of Japan Emperor Kōkō.
Ojin Guyot 37°58.20′N 170°22.80′E / 37.97000°N 170.38000°E / 37.97000; 170.38000 55.2 million ± 0.7[13] Named after former emperor of Japan Emperor Ōjin.
Jingu Guyot 38°50′N 171°15′E / 38.833°N 171.250°E / 38.833; 171.250 55.4 million ± 0.9[45] Named after former empress of Japan Empress Jingū.
Nintoku Guyot 41°4.80′N 170°34.20′E / 41.08000°N 170.57000°E / 41.08000; 170.57000 56.2 million ± 0.6[13] Named after former emperor of Japan Emperor Nintoku.
Yomei Guyot 42°18′N 170°24′E / 42.300°N 170.400°E / 42.300; 170.400 Unknown Named for former emperor of Japan Emperor Yomei.
Suiko Guyot 44°35′N 170°20′E / 44.583°N 170.333°E / 44.583; 170.333 59.6 million ± 0.6 –64.7 million ± 1.1[46] Named after former empress of Japan Empress Suiko.
Detroit Seamount 51°28.80′N 167°36′E / 51.48000°N 167.600°E / 51.48000; 167.600 76–81 million years[2][47] Well documented seamount, second oldest.
Meiji Seamount 53°12′N 164°30′E / 53.200°N 164.500°E / 53.200; 164.500 81–86 million years[2][47] Named after former emperor of Japan Emperor Meiji. Oldest known seamount.

References

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  40. ^ "Midway Atoll". Public Broadcasting System – KQED. 2006-03-22. Retrieved 2009-06-13.
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  43. ^ Hugh Rance (1999). Historical Geology: The Present is the Key to the Past (PDF). QCC Press. pp. 405–407. Retrieved 2009-06-29.
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  45. ^ Clague, D. A. and Dalrymple, G. B. (1989) Tectonics, geochronology, and origin of the Hawaiian-Emperor Chain in Winterer, E. L. et al. (editors) (1989) The Eastern Pacific Ocean and Hawaii, Boulder, Geological Society of America, page 199.
  46. ^ a b "Drilling Strategy". Ocean Drilling Program. Retrieved 2009-04-04.

Notes

  • [a] ^ As Lōʻhi Seamount has not risen above the ocean, nor connected with mainland Hawaii, it is not usually included among the five volcanoes of Big Island.
  • [b] ^ Similar to Lōʻhi, Māhukona is not included in the regular five either, however this is because erosion has since sunk it far below the waves.