Revision as of 14:49, 4 September 2017 editRenamed user 1000000008 (talk | contribs)8,215 editsm ce intro← Previous edit | Latest revision as of 22:56, 13 November 2024 edit undoAnomieBOT (talk | contribs)Bots6,589,493 editsm Dating maintenance tags: {{When}} | ||
(47 intermediate revisions by 30 users not shown) | |||
Line 1: | Line 1: | ||
{{Short description|Former island in the Pacific Ocean}} | |||
{{Citation style|date=July 2021}} | |||
] | ] | ||
] | ] | ||
'''Elugelab''' or '''Elugelap''' ({{ |
'''Elugelab''', or '''Elugelap''' ({{langx|mh|Āllokļap}}, {{IPAc-mh|yall&kwlhap}}<ref></ref>), was an ], part of the ] in the ]. It was destroyed in the world's first full-scale thermonuclear explosion, the '']'' shot of ], on November 1, 1952.{{NoteTag|Some sources date the event as October 31, based on their time zone. Locally, it was November 1 (GMT+12).|name=Note}} Prior to being destroyed, the island was described as "just another small naked island of the atoll".<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 24:00|year=1952 }}</ref> | ||
==Environment== | |||
⚫ | The fireball created by ] had a maximum ] of {{convert| |
||
The land had ] and the surrounding marine had '']'' coral growth which was home to '']'' and '']'', most of which are now{{when|date=November 2024}} dead or dying.<ref>{{Cite news |date=April 8, 1954 |title=Elugelab, the Island That Was |publisher=The Nanty-Glo Journal}}</ref><ref>{{Cite journal |last=Hartman |first=Olga |date=1954 |title=Marine Annelids From the Northern Marshall Islands |url=https://pubs.usgs.gov/pp/0260q/report.pdf |journal=Professional Paper 260-Q|doi=10.3133/pp260Q }}</ref> | |||
⚫ | </ref><ref>{{Cite web | last=Walker | first=John | |
||
==Explosion== | |||
⚫ | The detonation produced a crater {{convert| |
||
⚫ | The fireball created by ] had a maximum ] of {{convert|5.8|to|6.56|km|abbr=on}}.<ref>{{Cite web | last=Walker | first=John | author-link=John Walker (programmer) | title=Nuclear Bomb Effects Computer | publisher=Fourmilab | date=June 2005 | access-date=2009-11-22 | url=http://www.fourmilab.ch/cgi-bin/Bombcalc?yield=10400&yunit=1&range=5&runit=0.62137119&rotate=310&imsize=800 }} | ||
⚫ | </ref><ref>{{Cite web | last=Walker | first=John | author-link=John Walker (programmer) | title=Nuclear Bomb Effects Computer Revised Edition 1962, Based on Data from The Effects of Nuclear Weapons, Revised Edition 'he maximum fireball radius presented on the computer is an average between that for air and surface bursts. Thus, the fireball radius for a surface burst is 13 percent larger than that indicated and for an air burst, 13 percent smaller' | publisher=Fourmilab | date=June 2005 | access-date=2009-11-22 | url=http://www.fourmilab.ch/bombcalc/instructions.html}}</ref><ref>{{cite web |url=http://www.remm.nlm.gov/RemmMockup_files/radiationlethality.jpg |title=Mock up |publisher=Remm.nlm.gov |access-date=2013-11-30 |archive-date=2013-06-07 |archive-url=https://web.archive.org/web/20130607091341/http://www.remm.nlm.gov/RemmMockup_files/radiationlethality.jpg |url-status=dead }}</ref> This maximum is reached a number of seconds after the detonation and during this time the hot fireball invariably rises due to ]. While still relatively close to the ground, the fireball had yet to reach its maximum dimensions and was thus approximately {{convert|5.2|km|abbr=on}} wide.<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 56:50|year=1952 }}</ref> | ||
⚫ | The detonation produced a crater {{convert|1.9|km|ft|abbr=on}} in diameter and {{Convert|50|m|abbr=on}} deep where Elugelab had once been;<ref></ref> the blast and water waves from the explosion (some waves up to {{convert|6.1|m|abbr=on}} high) stripped the test islands clean of vegetation, as observed by a helicopter survey within 60 minutes after the test, by which time the mushroom cloud had blown away. The island "became dust and ash, pulled upward to form a ] that rose about twenty-seven miles into the sky." The outcome of the test was reported to incoming president ] by Atomic Energy Commission Chairman, ], as follows: “The island of Elugelab is missing!”.<ref></ref> | ||
⚫ | Aerial footage of Elugelab and adjacent islands well before ''Mike'' shot at a time prior to the connecting ] being created is available,<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 23:00}}</ref> as is footage after the causeway was finished that supported the diagnostic ] light pipe system,<ref>{{cite web |url=http://www.nuclearweaponarchive.org/Usa/Tests/Ivy.html |title=Operation Ivy 1952 - Enewetak Atoll, Marshall Islands "The 9000 foot long causeway linking the islands together is the "Krause-Ogle box", a 9 foot square aluminum-sheathed plywood tunnel filled with helium ballonets. This box allowed gamma and neutron radiation from the blast to travel with little absorption to test instruments on Bogon."}}</ref> with numerous trees removed in preparation of the shot also plainly evident,<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 30:00}}</ref> along with footage of the aforementioned helicopter survey of the Mike crater soon after the detonation,<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 47:00}}</ref> and finally, high |
||
⚫ | According to ], all that remained of Elugelab was a circular crater filled with seawater, more than a mile in diameter and "fifteen stories deep".<ref>{{cite book |title=Command and Control: Nuclear Weapons, the Damascus Accident, and the Illusion of Safety |first=Eric |last=Schlosser |author-link=Eric Schlosser |publisher=Penguin Press |isbn=978-1-59420-227-8 |year=2013 |url-access=registration |url=https://archive.org/details/commandcontrol00eric }}</ref> ] yielded 10.4 megatons of explosive energy, 700 times the energy that leveled central ].<ref>{{cite news |url=https://www.nytimes.com/2008/12/30/science/30bomb.html?_r=1&8dpc |title=Soviets Stole Bomb Idea From U.S., Book Says |access-date=2008-12-29 | work=] | date=30 December 2008}}</ref> Aerial footage of Elugelab and adjacent islands well before ''Mike'' shot at a time prior to the connecting ] being created is available,<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 23:00|year=1952 }}</ref> as is footage after the causeway was finished that supported the diagnostic ] light pipe system,<ref>{{cite web |url=http://www.nuclearweaponarchive.org/Usa/Tests/Ivy.html |title=Operation Ivy 1952 - Enewetak Atoll, Marshall Islands "The 9000 foot long causeway linking the islands together is the "Krause-Ogle box", a 9 foot square aluminum-sheathed plywood tunnel filled with helium ballonets. This box allowed gamma and neutron radiation from the blast to travel with little absorption to test instruments on Bogon."}}</ref> with numerous trees removed in preparation of the shot also plainly evident,<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 30:00|year=1952 }}</ref> along with footage of the aforementioned helicopter survey of the Mike crater soon after the detonation,<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 47:00|year=1952 }}</ref> and finally, high-altitude footage of the crater accompanied with details of its depth{{snd}}"175 feet deep"{{snd}}equivalent to the height of a "17-story building" and with an area large enough to accommodate about "14 ]".<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 58:30|year=1952 }}</ref> | ||
The detonation also collapsed some natural crevices in the ], some distance away from the rim of the crater.<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 58:50 note the black lines drawn on the picture that appear momentarily at 58:55}}</ref> | |||
Full ] recovery surveys were documented before and after each test series. |
The detonation also collapsed some natural crevices in the ], some distance away from the rim of the crater.<ref>{{cite web |url=https://archive.org/details/OperationIVY1952 |title=Operation Ivy (1952), see 58:50 note the black lines drawn on the picture that appear momentarily at 58:55|year=1952 }}</ref> Full ] recovery surveys were documented before and after each test series.<ref>For a brief online introduction into some of these studies{{snd}}with specific reference to the ecological effects of the 1.69-megaton ] ''Nectar'' shot, detonated in 1954 on a barge just north east of the crater of the 10.4-megaton ] thermonuclear test see a report by the University of Washington's Laboratory of Radiation Biology and .</ref> | ||
=== Impact on the nuclear arms race === | |||
This test marked a pivotal moment in escalating the nuclear weapons development arms race. The ] conducted its ] three years later. It was believed that Soviet scientists were able to sustain the development of the hydrogen bomb partly because they received U.S. research details from atomic spy ]. However, the '']'' indicated in the 1990s that most of the information Fuchs provided may have been useless.<ref>{{Cite journal |last=Norman |first=Colin |date=January 12, 1990 |title=How the Soviets Got the H-Bomb |journal=American Association for the Advancement of Science |volume=247 |issue=4939 |pages=151 |doi=10.1126/science.247.4939.151|pmid=17813267 |bibcode=1990Sci...247..151N }}</ref><ref>{{Cite journal |last1=Moss |first1=Norman |last2=Franklin |first2=H. Bruce |last3=Leitenberg |first3=Milton |last4=Bonheim |first4=Ralph |last5=Leventhal |first5=Paul |last6=Smith |first6=Lucius |last7=Robinowitz |first7=Mark |date=May 1990 |title=Letters |url=https://www.tandfonline.com/doi/full/10.1080/00963402.1990.11459832 |journal=Bulletin of the Atomic Scientists |language=en |volume=46 |issue=4 |pages=51–54 |doi=10.1080/00963402.1990.11459832 |bibcode=1990BuAtS..46d..51M |issn=0096-3402}}</ref> | |||
==Gallery== | ==Gallery== | ||
<gallery> | <gallery> | ||
File:Ivy Mike test.ogg|] test of 1952, this video contains a misleading ] explosion sound ] on |
File:Ivy Mike test.ogg|] test of 1952, this video contains a misleading ] explosion sound ] on what was a completely silent detonation from the vantage point of the camera, with the sound of the blast wave only arriving a number of seconds later, akin to ], with the exact time depending on its distance. | ||
File:Operation Castle - Nectar - Detonation.ogv|The 1954 test shot ''Nectar'' of ] produced a yield of 1.69 ] and was detonated just North East of Ivy Mike's Elugelab crater, off the coast of Teiter (Gene) Island. The Island of Bogon/Bokon (Irene), is the spearhead-shaped object at the bottom right of the screen. The maximum average ] radius is approximately {{convert|1.4|to|1.6|km|abbr=on}}.<ref>{{Cite web | last=Walker | first=John | author-link=John Walker (programmer) | title=Nuclear Bomb Effects Computer | publisher=Fourmilab | date=June 2005 | access-date=2009-11-22 | url=http://www.fourmilab.ch/cgi-bin/Bombcalc?yield=1690&yunit=1&range=5&runit=0.62137119&rotate=310&imsize=800 }}</ref><ref>{{Cite web | last=Walker | first=John | author-link=John Walker (programmer) | title=Nuclear Bomb Effects Computer Revised Edition 1962, Based on Data from The Effects of Nuclear Weapons, Revised Edition "The maximum fireball radius presented on the computer is an average between that for air and surface bursts. Thus, the fireball radius for a surface burst is 13 percent larger than that indicated and for an air burst, 13 percent smaller. " | publisher=Fourmilab | date=June 2005 | access-date=2009-11-22 | url=http://www.fourmilab.ch/bombcalc/instructions.html}}</ref> | |||
File:Redwing Seminole Detonation 320x240.ogv|Test shot Seminole of ], yield 13.7 |
File:Redwing Seminole Detonation 320x240.ogv|Test shot Seminole of ], yield 13.7 kilotons, conducted on the coast of the island of Bogon/Bokon (Irene) on June 6, 1956. | ||
File:Redwing Seminole 005.jpg|Redwing Seminole crater on Bogon/Bokon (Irene) island |
File:Redwing Seminole 005.jpg|Redwing Seminole crater on Bogon/Bokon (Irene) island | ||
File:Redwing Apache.jpg| |
File:Redwing Apache.jpg|Test shot Apache of Operation Redwing, yield 1.85 megatons,<ref>{{cite web |url=http://www.dtra.mil/documents/ntpr/factsheets/Redwing.pdf |title=DTRA Operation REDWING Fact Sheet |access-date=2014-02-27 |archive-url=https://web.archive.org/web/20130218012602/http://www.dtra.mil/documents/ntpr/factsheets/Redwing.pdf |archive-date=2013-02-18 |url-status=dead }}</ref> detonated in a barge on July 8, 1956, at "Elugelab (Flora)" {{coord|11.66451|162.19446|display=inline|name=Apache}}{{citation needed|date=February 2014}} or off the coast of what remained of Teiter Island after the detonation of test shot Nectar of Operation Castle. | ||
File:Enewetak Atoll - 2002-02-07 - Landsat 7 ETM+ SLC - b3218 - 15m.png|A 2002 |
File:Enewetak Atoll - 2002-02-07 - Landsat 7 ETM+ SLC - b3218 - 15m.png|A 2002 true-color photograph of ]. The relatively large Ivy Mike crater can be seen at the top of the atoll in this image with the smaller, adjoining Castle Nectar crater, in close proximity. The much smaller Redwing Seminole crater can faintly be seen on Bogon Island. | ||
File:Atombombentest Redwing-Seminole 01.jpg|A single high-quality frame from test shot Seminole of ] | |||
</gallery> | </gallery> | ||
Line 32: | Line 39: | ||
* ] | * ] | ||
* ] | * ] | ||
* ] a deeper crater that formed in a natural ] with the release of about the same amount of energy |
* ], or Barringer crater – a deeper crater that formed in a natural ] with the release of about the same amount of energy: 10 megatons. | ||
* ] |
* ] – a larger island that was destroyed by a much more powerful natural volcanic explosion. | ||
*] | *] | ||
Line 42: | Line 49: | ||
==External links== | ==External links== | ||
* from ] | * from ] | ||
{{authority control}} | |||
{{Portal bar|Islands}} | |||
{{Marshall Islands}} | |||
== Footnotes == | |||
<references group="note" /> | |||
] | ] | ||
Line 49: | Line 64: | ||
] | ] | ||
] | ] | ||
] |
Latest revision as of 22:56, 13 November 2024
Former island in the Pacific OceanThis article has an unclear citation style. The references used may be made clearer with a different or consistent style of citation and footnoting. (July 2021) (Learn how and when to remove this message) |
Elugelab, or Elugelap (Marshallese: Āllokļap, ), was an island, part of the Enewetak Atoll in the Marshall Islands. It was destroyed in the world's first full-scale thermonuclear explosion, the Mike shot of Operation Ivy, on November 1, 1952. Prior to being destroyed, the island was described as "just another small naked island of the atoll".
Environment
The land had palm trees and the surrounding marine had Heliopora coral growth which was home to Eurythoe complanata and Haplosyllis spongicola, most of which are now dead or dying.
Explosion
The fireball created by Ivy Mike had a maximum diameter of 5.8 to 6.56 km (3.60 to 4.08 mi). This maximum is reached a number of seconds after the detonation and during this time the hot fireball invariably rises due to buoyancy. While still relatively close to the ground, the fireball had yet to reach its maximum dimensions and was thus approximately 5.2 km (3.2 mi) wide.
The detonation produced a crater 1.9 km (6,200 ft) in diameter and 50 m (160 ft) deep where Elugelab had once been; the blast and water waves from the explosion (some waves up to 6.1 m (20 ft) high) stripped the test islands clean of vegetation, as observed by a helicopter survey within 60 minutes after the test, by which time the mushroom cloud had blown away. The island "became dust and ash, pulled upward to form a mushroom cloud that rose about twenty-seven miles into the sky." The outcome of the test was reported to incoming president Eisenhower by Atomic Energy Commission Chairman, Gordon Dean, as follows: “The island of Elugelab is missing!”.
According to Eric Schlosser, all that remained of Elugelab was a circular crater filled with seawater, more than a mile in diameter and "fifteen stories deep". The blast yielded 10.4 megatons of explosive energy, 700 times the energy that leveled central Hiroshima. Aerial footage of Elugelab and adjacent islands well before Mike shot at a time prior to the connecting causeway being created is available, as is footage after the causeway was finished that supported the diagnostic Krause-Ogle box light pipe system, with numerous trees removed in preparation of the shot also plainly evident, along with footage of the aforementioned helicopter survey of the Mike crater soon after the detonation, and finally, high-altitude footage of the crater accompanied with details of its depth – "175 feet deep" – equivalent to the height of a "17-story building" and with an area large enough to accommodate about "14 Pentagon buildings".
The detonation also collapsed some natural crevices in the reef, some distance away from the rim of the crater. Full radioecology recovery surveys were documented before and after each test series.
Impact on the nuclear arms race
This test marked a pivotal moment in escalating the nuclear weapons development arms race. The Soviet Union conducted its own thermonuclear test three years later. It was believed that Soviet scientists were able to sustain the development of the hydrogen bomb partly because they received U.S. research details from atomic spy Klaus Fuchs. However, the Bulletin of the Atomic Scientists indicated in the 1990s that most of the information Fuchs provided may have been useless.
Gallery
- Ivy Mike test of 1952, this video contains a misleading post-production explosion sound overdubbed on what was a completely silent detonation from the vantage point of the camera, with the sound of the blast wave only arriving a number of seconds later, akin to thunder, with the exact time depending on its distance.
- The 1954 test shot Nectar of Operation Castle produced a yield of 1.69 megatons and was detonated just North East of Ivy Mike's Elugelab crater, off the coast of Teiter (Gene) Island. The Island of Bogon/Bokon (Irene), is the spearhead-shaped object at the bottom right of the screen. The maximum average nuclear fireball radius is approximately 1.4 to 1.6 km (0.87 to 0.99 mi).
- Test shot Seminole of Operation Redwing, yield 13.7 kilotons, conducted on the coast of the island of Bogon/Bokon (Irene) on June 6, 1956.
- Redwing Seminole crater on Bogon/Bokon (Irene) island
- Test shot Apache of Operation Redwing, yield 1.85 megatons, detonated in a barge on July 8, 1956, at "Elugelab (Flora)" 11°39′52″N 162°11′40″E / 11.66451°N 162.19446°E / 11.66451; 162.19446 (Apache) or off the coast of what remained of Teiter Island after the detonation of test shot Nectar of Operation Castle.
- A 2002 true-color photograph of Enewetak Atoll. The relatively large Ivy Mike crater can be seen at the top of the atoll in this image with the smaller, adjoining Castle Nectar crater, in close proximity. The much smaller Redwing Seminole crater can faintly be seen on Bogon Island.
- A single high-quality frame from test shot Seminole of Operation Redwing
See also
- Nuclear fusion
- Ivy Mike
- Operation Ivy
- Operation Castle
- Operation Redwing
- Nuclear fission
- Meteor Crater, or Barringer crater – a deeper crater that formed in a natural impact event with the release of about the same amount of energy: 10 megatons.
- Krakatoa – a larger island that was destroyed by a much more powerful natural volcanic explosion.
- Explosion crater
References
11°40′0″N 162°11′13″E / 11.66667°N 162.18694°E / 11.66667; 162.18694
- Marshallese-English Dictionary – Place Name Index
- "Operation Ivy (1952), see 24:00". 1952.
- "Elugelab, the Island That Was". The Nanty-Glo Journal. April 8, 1954.
- Hartman, Olga (1954). "Marine Annelids From the Northern Marshall Islands" (PDF). Professional Paper 260-Q. doi:10.3133/pp260Q.
- Walker, John (June 2005). "Nuclear Bomb Effects Computer". Fourmilab. Retrieved 2009-11-22.
- Walker, John (June 2005). "Nuclear Bomb Effects Computer Revised Edition 1962, Based on Data from The Effects of Nuclear Weapons, Revised Edition 'he maximum fireball radius presented on the computer is an average between that for air and surface bursts. Thus, the fireball radius for a surface burst is 13 percent larger than that indicated and for an air burst, 13 percent smaller'". Fourmilab. Retrieved 2009-11-22.
- "Mock up". Remm.nlm.gov. Archived from the original on 2013-06-07. Retrieved 2013-11-30.
- "Operation Ivy (1952), see 56:50". 1952.
- Nuclear Weapon Archive
- The Island is Missing!, article from the U.S. Army Heritage and Education Center
- Schlosser, Eric (2013). Command and Control: Nuclear Weapons, the Damascus Accident, and the Illusion of Safety. Penguin Press. ISBN 978-1-59420-227-8.
- "Soviets Stole Bomb Idea From U.S., Book Says". The New York Times. 30 December 2008. Retrieved 2008-12-29.
- "Operation Ivy (1952), see 23:00". 1952.
- "Operation Ivy 1952 - Enewetak Atoll, Marshall Islands "The 9000 foot long causeway linking the islands together is the "Krause-Ogle box", a 9 foot square aluminum-sheathed plywood tunnel filled with helium ballonets. This box allowed gamma and neutron radiation from the blast to travel with little absorption to test instruments on Bogon."".
- "Operation Ivy (1952), see 30:00". 1952.
- "Operation Ivy (1952), see 47:00". 1952.
- "Operation Ivy (1952), see 58:30". 1952.
- "Operation Ivy (1952), see 58:50 note the black lines drawn on the picture that appear momentarily at 58:55". 1952.
- For a brief online introduction into some of these studies – with specific reference to the ecological effects of the 1.69-megaton Operation Castle Nectar shot, detonated in 1954 on a barge just north east of the crater of the 10.4-megaton Ivy Mike thermonuclear test see a report by the University of Washington's Laboratory of Radiation Biology and .
- Norman, Colin (January 12, 1990). "How the Soviets Got the H-Bomb". American Association for the Advancement of Science. 247 (4939): 151. Bibcode:1990Sci...247..151N. doi:10.1126/science.247.4939.151. PMID 17813267.
- Moss, Norman; Franklin, H. Bruce; Leitenberg, Milton; Bonheim, Ralph; Leventhal, Paul; Smith, Lucius; Robinowitz, Mark (May 1990). "Letters". Bulletin of the Atomic Scientists. 46 (4): 51–54. Bibcode:1990BuAtS..46d..51M. doi:10.1080/00963402.1990.11459832. ISSN 0096-3402.
- Walker, John (June 2005). "Nuclear Bomb Effects Computer". Fourmilab. Retrieved 2009-11-22.
- Walker, John (June 2005). "Nuclear Bomb Effects Computer Revised Edition 1962, Based on Data from The Effects of Nuclear Weapons, Revised Edition "The maximum fireball radius presented on the computer is an average between that for air and surface bursts. Thus, the fireball radius for a surface burst is 13 percent larger than that indicated and for an air burst, 13 percent smaller. "". Fourmilab. Retrieved 2009-11-22.
- "DTRA Operation REDWING Fact Sheet" (PDF). Archived from the original (PDF) on 2013-02-18. Retrieved 2014-02-27.
External links
- "Mike" Test from PBS
Marshall Islands articles | |||||||
---|---|---|---|---|---|---|---|
History | |||||||
Geography |
| ||||||
Politics |
| ||||||
Economy | |||||||
Culture |
| ||||||
|
Footnotes
- Some sources date the event as October 31, based on their time zone. Locally, it was November 1 (GMT+12).