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The atoll is roughly crescent-shaped, measuring about 11 miles by 5.6 miles, and oriented in a north-south direction. The atoll reef is unbroken except for a 22 yard-wide channel in the west. Ten islets lie on the eastern and southeastern reef. The more important named islets, from north to south, are North Island, Kamwome, Bwdije, Sibylla, Bokak, and Bwokwla. Sibylla is the largest, measuring approximately 4.5 miles in length and up to 333 yards in width. Kamwome Islet to the north-east of Sibylla is the second largest, while Bokak (Taongi), after which the atoll is named, lies to the south of Sibylla<ref>{{cite web|url=http://sea.unep-wcmc.org/sites/pa/0374w.htm|publisher=United Nations Environment Programme (UNEP), World Conservation Monitoring Centre|title=2008 World Database on Protected Areas|date=2008-1-1}}</ref>.
The atoll is roughly crescent-shaped, measuring about 11 miles by 5.6 miles, and oriented in a north-south direction. The atoll reef is unbroken except for a 22 yard-wide channel in the west. Ten islets lie on the eastern and southeastern reef. The more important named islets, from north to south, are North Island, Kamwome, Bwdije, Sibylla, Bokak, and Bwokwla. Sibylla is the largest, measuring approximately 4.5 miles in length and up to 333 yards in width. Kamwome Islet to the north-east of Sibylla is the second largest, while Bokak (Taongi), after which the atoll is named, lies to the south of Sibylla<ref>{{cite web|url=http://sea.unep-wcmc.org/sites/pa/0374w.htm|publisher=United Nations Environment Programme (UNEP), World Conservation Monitoring Centre|title=2008 World Database on Protected Areas|date=2008-1-1}}</ref>.


[[Image:Taongi Beach & Lagoon.jpg|thumb|left|250px|Bokak's perched lagoon sits 3 feet above the mean tide level, resulting in a usually calm surface.]]Based on the results of drilling operations on [[Enewetak]] (Eniwetok) Atoll, in the nearby Ralik Chain of the Marshall Islands, Bokak may be include as much as 4600 feet of reef material atop a basalt rock base. As most local coral growth stops at about 150 feet below the ocean surface, such a massive stony coral base suggests the [[isostatic]] subsidence of the underlying extinct volcano<ref>{{cite web|url=http://www.grisda.org/origins/06088.htm|publisher=Geoscience Research Institute|title=Coral Reef Growth|date=1979-1-1}}</ref>, which itself rises 10000 feet from the surrounding ocean floor.
[[Image:Taongi Beach & Lagoon.jpg|thumb|left|250px|Bokak's perched lagoon sits 3 feet above the mean tide level, resulting in a usually calm surface.]]Based on the results of drilling operations on [[Enewetak]] (Eniwetok) Atoll, in the nearby Ralik Chain of the Marshall Islands, Bokak may be include as much as 4600 feet of reef material atop a basalt rock base. As most local coral growth stops at about 150 feet below the ocean surface, such a massive stony coral base suggests the [[isostatic]] subsidence of the underlying extinct volcano<ref>{{cite web|url=http://www.grisda.org/origins/06088.htm|publisher=Geoscience Research Institute|title=Coral Reef Growth|date=1979-1-1}}</ref>, which itself rises 10000 feet from the surrounding ocean floor. Shallow water fossils taken from just above the basalt base are about 55 [[mya|mya (unit)]]<ref>{{cite web|url=http://hdl.handle.net/10088/5039|publisher=|title=Atoll Research Bulletin No. 260|date=1983}}</ref>.


More Taongi papers to review:
More Taongi papers to review:

Revision as of 06:06, 15 March 2009

Bokak Atoll - NASA NLT Landsat 7 (Visible Color) Satellite Image

Bokak Atoll (also known as Taongi Atoll) is an uninhabited atoll in the Ratak Chain of the Marshall Islands, located in the North Pacific Ocean at 14°32′N 169°00′E / 14.533°N 169.000°E / 14.533; 169.000.

Geography

It is located 425 miles north of Majuro Atoll, the capital of the Marshall Islands, and 174 miles NE of Bikar Atoll, the closest atoll, making it the most northerly and most isolated atoll of the country. Wake Island is 348 miles NNW. The land area is 1.25 sq. miles, and the lagoon measures 30.12 sq. miles. It consists of 36 islets.The total area is 49.8 sq. miles (including reef flat)[1].

Physical Features

The atoll is roughly crescent-shaped, measuring about 11 miles by 5.6 miles, and oriented in a north-south direction. The atoll reef is unbroken except for a 22 yard-wide channel in the west. Ten islets lie on the eastern and southeastern reef. The more important named islets, from north to south, are North Island, Kamwome, Bwdije, Sibylla, Bokak, and Bwokwla. Sibylla is the largest, measuring approximately 4.5 miles in length and up to 333 yards in width. Kamwome Islet to the north-east of Sibylla is the second largest, while Bokak (Taongi), after which the atoll is named, lies to the south of Sibylla[2].

Bokak's perched lagoon sits 3 feet above the mean tide level, resulting in a usually calm surface.

Based on the results of drilling operations on Enewetak (Eniwetok) Atoll, in the nearby Ralik Chain of the Marshall Islands, Bokak may be include as much as 4600 feet of reef material atop a basalt rock base. As most local coral growth stops at about 150 feet below the ocean surface, such a massive stony coral base suggests the isostatic subsidence of the underlying extinct volcano[3], which itself rises 10000 feet from the surrounding ocean floor. Shallow water fossils taken from just above the basalt base are about 55 mya (unit)[4].

More Taongi papers to review: http://si-pddr.si.edu/dspace/handle/10088/4782/simple-search?query=taongi&start=10 http://si-pddr.si.edu/dspace/handle/10088/4782//simple-search?query=taongi More Marshall Island papers to review, including land ownership: http://si-pddr.si.edu/dspace/handle/10088/4782/simple-search?query=marshall+islands including rats, hydrology, etc.

High boulder ridges and sand ridges indicate a history of severe storms and are a feature of the islets. Inland on the wider islets are sand and rubble flats, while back from the lagoon sides are low sand and gravel ridges. Soils are mostly very immature, a mixture of coarser coral sand and gravel of various textures with very little humus accumulation. The lagoon is shallow, probably not exceeding 30m depth, and has many coral heads and patch reefs, some reaching the surface[5].

The lagoon water level is up to 3' higher than the surrounding ocean due to an influx of wind-driven waters over the windward ocean reef and the presence of only one narrow reef passage on the leeward side. Water cascades over the coral-covered rim and flats of the sloping leeward reef. A massive algal ridge lines the outer edge of the windward reef, while the south and west reefs are coral-covered narrow flats where landings can be made in quiet weather. A very small algal rim, 4-6" high, on lagoon shores of the westernmost islets, on east-facing lagoon reef-fronts and on the windward edges of coral patches in the lagoon, may be a feature unique to Taongi. This rim is maintained by the constant flow of water over the reef flat[6].

Climate

Bokak is the driest of the Marshall Islands atolls, having a semi-arid character. Mean annual temperature is approximately 82°F. Mean annual rainfall is less than 40", and falls primarily during the November through January rainy season. Prevailing winds are north to north-easterlies[7].

Vegetation

The shoreline of the perched lagoon at Sibylla Island. In the foreground: coral rubble beach and Naupaka shrubland.

Bokak supports just nine plant species. All are native to the Marshall Islands and entirely undisturbed by introduced species. A combination of insufficient rainfall, excellent drainage, and high temperatures lead to an arid environment in which coconut palm is unable to grow[8]. The most common formation is a low, sparse scrub forest of velvet soldierbush, 6-20' tall, with occasional taller trees. The understory typically comprises beach naupaka, or sparse endemic bunchgrass, 'Ihi, 'ilima, or alena, the latter being more abundant on broken coral gravel. A small stand of Pisonia grandis is found on Kamwome Islet and in another very small stand on Sibylla[9].

Pure stands of very dense beach naupaka shrubland, sometimes with velvet soldierbush trees, are predominant and cover 50-75% of southern, and nearly 100% of north-eastern Sibylla. Tournefortia, Scaevola, and Sida dominated shrublands and the sandy bunchgrass savanna (Lepturus spp.) represent the finest examples of such vegetation in the Marshalls and probably the entire Pacific region[10].

The aquatic vegetation of the shallow edges of the lagoon consists of sparse coralline algae, encrusting fragments of coral, shell etc., and patches of green sea weed[11].

Fauna

Female Frigatebird on Sibylla Island.

The atoll supports a large population of sea and shorebirds, with up to 26 species present. Species breeding during 1988 included the brown booby, red-footed booby, Great Frigatebird, Red-tailed Tropicbird, Sooty Tern, White Tern, Brown Noddy, and possibly the Reef Heron. Migratory birds present during included the bristle-thighed curlew, turnstone, wandering tattler, golden plover, and the sanderling. The densest bird populations are on three islets to the north of Sibylla: North (Kita), Kamwome and an unnamed islet. Bokak is the only known breeding ground of Christmas Shearwater and possibly Bulwer's petrel[12].

Terrestrial species includes the Polynesian rat on Sibylla. The more aggressive black rat appears to be absent, despite wrecked fishing vessels on the eastern and north eastern reefs. The Snake-eyed Skink and large hermit crabs are common[13].

In general, the aquatic fauna population is healthy, but of low diversity, possibly due to the atoll's isolation. Researchers have not seen any marine turtles, but Polynesian custom regarding harvesting assumed their presence[14]. Examples of the giant clam family Tridacnidae are very abundant, except for the largest giant clam T. gigas. Smaller bivalves were present, but few Mollusks. The reef fish are primarily emperor breams, parrotfish, and snappers. Also present are moray eel and grey reef shark. Approximately 100 stony coral species and two soft coral species are present[15].

History

Prehistory

Although humans migrated to the Marshall Islands about 2000 years ago[16], there appear to be no traditional Marshallese artifacts present that would indicate any long term settlement. The harsh, dessicated climate, lack of potable water, and poverty of the soils indicate that the atoll will probably remain uninhabited. The atoll has traditionally been used for hunting and gathering, particularly sea birds, by inhabitants of other atolls in the northern Ratak chain[17]. Along with the other uninhabited northern Radak atolls of Bikar and Toke, Bokak was traditionally the hereditary property of the Radak atoll chain Iroji Lablab (the title of the senior ranking member of the ruling clan). The exploitation of abundant sea turtles, birds, and eggs was regulated by custom, and overseen by the Iroji[18].

16th to 19th century

The first European to record discovering Bokak was Alonso de Salazar, a Spanish explorer, on August 21, 1526. A number of Western ships recorded landfall on or passage by Bokak over the following three hundred years, but no attempt at settlement or establishment of food animals was noted, likely due to the arid conditions, and more fertile atolls nearby[19].

The Marshall Islands were added to the protectorate of German New Guinea in 1906. Using the justification that uninhabited atolls were unclaimed, the Germans seized Bokak as government property, despite the protests of the Iroji. As Japan's economic vigor expanded under the Meiji Emperor, the German administration noted Marshallese complaints of Japanese bird poaching, more from the view of protecting German sovereignty, rather than the interests of the islanders[20].

20th century to Present

In 1914, Japan occupied the Marshall Islands, and transferred German government properties to their own, including Bokak. Like the Germans before them, the Japanese colonial administrations did not attempt to exploit the atoll, and the Northern Radak Marshallese continued to hunt and fish unmolested[21].

As a part of the 1930s Japanese militarization the Marshall Islands, a small seaplane and communication outpost was established on Sibylla Island. During the early stages of the United States war against Japan, USN submarines operating in the area would periodically note patrols by Japanese aircraft[22]. In March, 1943, the 20 man garrison was removed to Wake Island because of the lack of food and their general inability to sustain themselves on Bokak[23]. Air elements of the USAAF, USN, and USMC bombed the (abandoned) facility on April 23, 1944[24]. In September, 1945, as a part of the post-war repatriation of Japanese from their former Pacific possessions, a landing party was dispatched on LCI(L) 601 from Kwajalein to Bokak Atoll, and in conjunction with a PBM Mariner searched for potential survivors. Two days of search failed to turn up any survivors, human remains, or graves[25].

Corroded skeleton of IJN landing craft, Sibylla Island, 1953.

While en route from the US to Asia in April, 1953, LST 1138 dropped anchor at Bokak to search for rumored Japanese stragglers. The landing party noted the remains of the wartime outpost, but found no signs of occupation[26].

Nuclear test site master plan, from a declassified 1957 LASL document.

In 1954, the experience of large scale fallout from the Castle Bravo nuclear test on Bikini Atoll lead to a pre-planned aerial survey of atolls adjacent to the subsequent Castle Romeo test, timed at one and four hours after the shot. The aircraft were equipped with gamma radiation detectors designed to measure ground contamination from altitudes of 200 to 500 feet. An overflight of Sybilla Island measured 1.0 mrem/hr (10 μGy) an hour after the shot, dropping to 0.4 mrem/hr (4 μGy) three hours later[27]. In 1957, Bokak was surveyed as a site for nuclear weapons testing as a part of Operation Hardtack, but was passed over in favor of other atolls due to the significant dredging needed to provide adequate anchorage for development of a nuclear test site[28]. The atoll came under renewed consideration for use during Operation Dominic, but by that time the potential for political fallout from nuclear testing within a United Nations Trust Territory was deemed too great.[29]

Reference the proposed garage dump[30].

The atoll played a part in the disappearance of several men from Maui, Hawaii. On February 11, 1979, Scott Moorman and four companions set sail from Hana harbor in a 17' Boston Whaler, and went missing in subsequent high seas. The boat and buried remains of Mr. Moorman were discovered on Bokak in 1988[31].

Reference the ham expedition, on Sibylla Island at N 14 36.574, E 168 59.977.[32].

The Dominion of Melchizedek, an unrecognized micronation, claims sovereignty over Bokak, based on a 45 year lease allegedly granted by the Iroji Lablab[33].

Currently, historic remains include an abandoned camp/homestead, several wrecked ships and the remnant of the former World War Two Japanese communication outpost[34].

Footnotes

  1. ^ "Marshall Islands Atoll Information, Bokak (Taongi) Atoll". Institute of Land, Water and Society, Charles Sturt University. 1998-5-1. {{cite web}}: Check date values in: |date= (help)
  2. ^ "2008 World Database on Protected Areas". United Nations Environment Programme (UNEP), World Conservation Monitoring Centre. 2008-1-1. {{cite web}}: Check date values in: |date= (help)
  3. ^ "Coral Reef Growth". Geoscience Research Institute. 1979-1-1. {{cite web}}: Check date values in: |date= (help)
  4. ^ "Atoll Research Bulletin No. 260". 1983.
  5. ^ "UNEP".
  6. ^ "ibid".
  7. ^ "ibid".
  8. ^ "Atoll Research Bulletin No. 113, Terrestrial Sediments and Soils of the Northern Marshall Islands, pg. 47". Smithsonian National Museum of Natural History. 1965-12-31.
  9. ^ "UNEP".
  10. ^ "ibid".
  11. ^ "ibid".
  12. ^ "ibid".
  13. ^ "ibid".
  14. ^ "Atoll Research Bulletin No. 419, Description of Reefs and Corals for the 1988 Protected Area Survey of the Northern Marshall Islands, p. 33". Smithsonian National Museum of Natural History. 1994-8-1. {{cite web}}: Check date values in: |date= (help)
  15. ^ "Smithsonian".
  16. ^ "Early Human Settlement And Adaptation In The Marshall Islands". Pacific Studies Program, PIAS-DG, University of the South Pacific, Suva, Fiji. 2007-10-09.
  17. ^ "UNEP".
  18. ^ "Atoll Research Bulletin No. 11, Land Tenure in the Marshall Islands". Smithsonian National Museum of Natural History. 1952-9-1. {{cite web}}: Check date values in: |date= (help)
  19. ^ "Ships visiting the Marshall Islands (until 1885): Bokak (Taongi) Atoll". Digital Micronesia. Retrieved 2009-03-13. {{cite web}}: Check date values in: |date= (help)
  20. ^ "Smithsonian".
  21. ^ "Smithsonian".
  22. ^ "U.S.S. WAHOO - Report Of First War Patrol". Bryan MacKinnon. retrieved 2009-03-14. {{cite web}}: Check date values in: |date= (help)
  23. ^ "Report of Surrender and Occupation of Japan, Part V, Surrender and Development of Outlying Japanese-held Islands in the Pacific Ocean Areas, Search of Taongi Atoll, p. 205". Office of the CNO, Navy Department. 1946-5-9. {{cite web}}: Check date values in: |date= (help)
  24. ^ "CINCPAC Press Release No. 374, APRIL 25, 1944". CINCPAC, Navy Department. 1944-4-25. {{cite web}}: Check date values in: |date= (help)
  25. ^ "CNO". 1946-5-9. {{cite web}}: Check date values in: |date= (help)
  26. ^ "LST 1138 aka USS STEUBEN COUNTY, Years 1952-1955". C.D. Pardee. 2007-07-11.
  27. ^ "Reports On Evacuation Of Natives And Surveys Of Several Marshall Island Atolls" (PDF). Department of Health, Safety, and Security , DOE. 1954-5-24. {{cite web}}: Check date values in: |date= (help)
  28. ^ cite something
  29. ^ cite something
  30. ^ cite something
  31. ^ "Anniversary of Hana's Sarah Joe remembered". Maui News. 2009-2-11. {{cite web}}: Check date values in: |date= (help)
  32. ^ cite something
  33. ^ "Cyberfraud: The fictitious "Dominion of Melchizedek"". Asia Pacific Media Services Limited. retrieved 2009-3-13. {{cite web}}: Check date values in: |date= (help)
  34. ^ "UNEP".

References