Vorlage:Short description Vorlage:Infobox Seamount Bowie Seamount, or SG̱aan Ḵinghlas ("Supernatural One Looking Outward") in the Haida language,[1][2] is a large submarine volcano in the northeastern Pacific Ocean, located Vorlage:Convert west of Haida Gwaii, British Columbia, Canada. The seamount is also known as Bowie Bank. The English name for the feature is after William Bowie of the United States Coast and Geodetic Survey.[3]
The volcano has a flat-topped summit rising about Vorlage:Convert above the seabed, to Vorlage:Convert below sea level.[4] The seamount lies at the southern end of a long underwater volcanic mountain range called the Pratt-Welker or Kodiak-Bowie Seamount chain, stretching from the Aleutian Trench in the north almost to Haida Gwaii in the south.[4]
Bowie Seamount lies on the Pacific Plate, a large segment of the Earth's surface which moves in a northwestern direction under the Pacific Ocean. It is adjacent to two other submarine volcanoes; Hodgkins Seamount on its northern flank and Graham Seamount on its eastern flank.
Geology
BearbeitenStructure
BearbeitenSeamounts are volcanic mountains which rise from the seafloor. The unlimited supply of water surrounding these volcanoes can cause them to behave differently from volcanoes on land. The lava emitted in eruptions at Bowie Seamount is made of basalt, a common gray to black or dark brown volcanic rock low in silica content (the lava is mafic). When basaltic lava makes contact with the cold sea water, it may cool very rapidly to form pillow lava, through which the hot lava breaks to form another pillow. Pillow lava is typically fine-grained, due to rapid cooling, with a glassy crust, and has radial jointing.[5]
With a height of at least Vorlage:Convert and rising to within only Vorlage:Convert of the sea surface, Bowie Seamount is the shallowest submarine volcano on the British Columbia Coast, as well as in Canadian waters, and one of the shallowest submarine volcanoes in the northeast Pacific Ocean.[4][6] Most seamounts are found hundreds to thousands of metres below sea level, and are therefore considered to be within the deep sea. If Bowie Seamount were on land it would be about Vorlage:Convert higher than Whistler Mountain in southwestern British Columbia and Vorlage:Convert lower than Mount Robson, the highest mountain in the Canadian portion of the Rocky Mountains.[6]
Bowie Seamount is about Vorlage:Convert long and Vorlage:Convert wide.[6] Its flat-topped summit is made of weakly consolidated tephra and consists of two terraces.[6][7] The lowest terrace is about Vorlage:Convert below sea level while the highest is about Vorlage:Convert below sea level, but contains steep-sided secondary summits that rise to within Vorlage:Convert below sea level. From a physical perspective, the effective size of the submarine volcano is considerably large. The effects of other submarine volcanoes along the Pacific Northwest, including Cobb Seamount off the coast of Washington, affect the composition and abundance of plankton up to Vorlage:Convert away from the seamount summit due to the upwelling of nutrients from deeper waters. Because of its similar size, Bowie Seamount most likely has a similar effect on its adjacent waters.[6]
Eruptive history
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Bowie Seamount was formed by submarine eruptions along fissures in the seabed throughout the last glacial, or "Wisconsinian", period, which began about 110,000 years ago and ended between 15,000 and 10,000 years ago. While most submarine volcanoes in the Pacific Ocean are more than one million years old, Bowie Seamount is relatively young. Its base was formed less than one million years ago, but its summit shows evidence of volcanic activity as recently as 18,000 years ago.[6] This is recent in geological terms, suggesting the volcano may yet have some ongoing volcanic activity.[4]
Close to Bowie's submerged summit, former coastlines cut by wave actions and beach deposits show that the submarine volcano would once have stood above sea level, as either a single volcanic island or as a small cluster of shoals that would have been volcanically active. Sea levels during the last glacial period, when Bowie Seamount was formed, were at least Vorlage:Convert lower than they are today.[4][6] It would have had a land area similar to, if not larger than, Midway Atoll in the central Pacific Ocean.
Origins
BearbeitenThere is some disagreement about the origin of Bowie seamount: Geological studies indicate that the Kodiak-Bowie Seamount chain may have formed above a center of upwelling magma called a mantle plume. The seamounts comprising the Kodiak-Bowie Seamount chain would be formed above the mantle plume and carried away from the mantle plume's magmatic source as the Pacific Plate moves in a northwesterly direction towards the Aleutian Trench, along the southern coastline of Alaska.[8]
The volcanic rocks which make up some of the seamounts in the Kodiak-Bowie Seamount chain are unusual in that they have an acid-neutralizing chemical substance like typical ocean-island basalts but a low percentage of strontium as found at mid-ocean ridge basalts. However, the strontium-bearing volcanic rocks comprising Bowie Seamount also contain lead. Therefore, the magma mixtures that formed Bowie Seamount seem to have originated from varying degrees of partial melting of a depleted source in the Earth's mantle and basalts which had distinctly high lead isotopic ratios. Estimates during geological studies indicate that the abundance of the depleted-source component ranges from 60 to 80 percent of the erupted material.[8]
Some aspects of the origin of the Kodiak-Bowie Seamount chain remain uncertain. The volcanic rocks found at the Tuzo Wilson Seamounts south of Bowie are fresh glassy pillow basalts of recent age, as would be expected if these seamounts are located above or close to a mantle plume south of Haida Gwaii. However, the origin of Bowie Seamount is less certain because even though the seafloor which Bowie lies on formed 16 million years ago during the late Miocene period, Bowie's summit shows evidence of recent volcanic activity. If Bowie Seamount formed above a mantle plume at the site presently occupied by the Tuzo Wilson Seamounts, it has been displaced from its magma source by about Vorlage:Convert at a rate of about Vorlage:Convert per year. The geologic history of Bowie Seamount is consistent with its flat-topped eroded summit, but the source for Bowie's recent volcanic activity remains uncertain.[8] Still others, such as Dickens Seamount and Pratt Seamount further north of Bowie Seamount, fall a little to the side of the chain's expected trend.[9] Another hypothesized origin of some or all seamounts in the Kodiak-Bowie Seamount chain is that they formed on top of the Explorer Ridge, a divergent tectonic plate boundary west of Vancouver Island, and have been displaced from it by seafloor spreading.[8]
Although some of the seamounts in the Kodiak-Bowie Seamount chain appear to follow the expected age progression for a mantle plume trail, others, such as Denson Seamount, are older than that hypothesis would suggest.[9] As a result, the Kodiak-Bowie Seamount chain has also been proposed by geoscientists to be a mix of ridge and mantle plume volcanism.
Biology
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Bowie Seamount supports a biologically rich area with a vigorous ecosystem. Studies have recorded high densities of crab, sea stars, sea anemones, sponges, squid, octopus, rockfish, halibut and sablefish. Eight species of marine mammal have been found in the Bowie Seamount area, including Steller sea lions, orca, humpback and sperm whales, along with 16 varieties of seabirds.[10] This has made Bowie Seamount a rare habitat in the northeast Pacific Ocean and one of the most biologically rich submarine volcanoes on Earth.[4][11] The rich marine life is due to the intense food supply of microscopic animals and plants, including phytoplankton and zooplankton.[12]
SGaan Kinghlas-Bowie Seamount Marine Protected Area
BearbeitenBecause of its biological richness, Bowie Seamount was designated as Canada's seventh Marine Protected Area on April 19, 2008 under the provisions of the Oceans Act.[10] The announcement was made by federal Fisheries Minister Loyola Hearn and Gidansda Guujaaw, President of the Council of the Haida Nation, in Skidegate on Haida Gwaii (formerly called the Queen Charlotte Islands). During the announcement, Natural Resources Minister Gary Lunn said: "Bowie Seamount is an oceanic oasis in the deep sea, a rare and ecologically rich marine area, and our government is proud to take action to ensure it is protected. By working in partnership with the Council of the Haida Nation and groups like the World Wildlife Fund-Canada, we are ensuring this unique treasure is preserved for future generations."[11]
The Marine Protected Area measures about Vorlage:Convert long and Vorlage:Convert wide, totaling an area of Vorlage:Convert.[12] The Bowie Seamount Marine Protected Area also includes Peirce Seamount (also called Davidson Seamount) and Hodgkins Seamount.[11] Previous to this designation, beginning in 1997, Bowie Seamount was a Haida marine protected area.[13]
Diving explorations and studies
BearbeitenThe shallow depth of Bowie Seamount makes it the only underwater mountain off the British Columbia Coast easily reached using scuba diving equipment. In March 1969, dives were made at the submarine volcano by Canadian Forces Maritime Command divers from the CSS Parizeau. Two dives were made to the summit where monochrome photographs were taken to record the environment and some biological samples were gathered to detect possible harmful plants, animals, or bacteria. These specimens were identified at the Pacific Biological Station in Nanaimo, creating a list of eleven varieties of sea bottom invertebrates.[7]
In August 1969, Canadian Forces Maritime Command divers made more dives during scientific studies by the Fisheries Research Board of Canada. They found very dense shoals of rockfish floating over Bowie's flat-topped summit and a variety of bottom life. A number of monochrome photographs were taken and a few seaweeds were collected, but no species record was created for other types of oceanic life around Bowie Seamount.[7]
In November 1996, an issue of National Geographic magazine included an article titled "Realm of the Seamount", describing dives made at Bowie Seamount by two explorers named Bill Curtsinger and Eric Hiner. They explored the slopes of Bowie Seamount using scuba diving equipment down to Vorlage:Convert. Their photographs featured one of Bowie's rugged peaks thickly covered with seaweeds and colourful sea bottom invertebrates. Shoals of young rockfish were seen on Bowie's steep flanks.[7]
Scientist Bill Austin of Khoyatan Marine Lab in the Northeast Pacific examined a video made during the National Geographic dives to identify the benthic flora and fauna of Bowie Seamount. From the video, Austin recognized some of the most noticeable invertebrates and noted that a few species generally occurring in the intertidal zone and in shallow subtidal environments were found deeper than might normally be expected, and were bigger than normal.[7]
A team of five divers, led by photographer/videographer Neil McDaniel, visited the seamount August 3–5, 2003 and conducted a biological and photographic survey of the summit down to depths of about Vorlage:Convert. A total of 18 taxa of algae, 83 taxa of conspicuous invertebrates and 12 taxa of fishes were documented, approximately 180 underwater still photographs were taken and approximately 90 minutes of digital video were recorded. Of particular note were the dense schools of rockfish hovering over the summit and numerous curious prowfish.[7]
Indigenous people
BearbeitenTo the Haida, the indigenous people who played a key role in establishing the Bowie Seamount Marine Protected Area, the submarine volcano is called SGaan Kinghlas. In Haida language it means "Supernatural Being Looking Outward".[11]
Haida have long recognized seamount as a special place. Gidansda Guujaaw, former President of the Council of the Haida Nation, has said: "SGaan Kinghlas represents a shift in recognizing the need for respect and care for the Earth. This is a very significant turning point in reversing the trends that have been leading to the depletion of life in the sea."[11]
Marine hazard
BearbeitenGiven its shallow depth, Bowie Bank is a potential marine hazard. Waves up to Vorlage:Convert high have been recorded along the British Columbia Coast during heavy weather, enough to expose the bank by wave troughs and cause devastation to any vessel transiting the seamount. For this reason, Environment Canada has recognized Bowie Seamount as a hazard to navigation, and it is avoided by shipping vessels.[14][15]
See also
BearbeitenReferences
BearbeitenExternal links
BearbeitenVorlage:Good article Vorlage:British Columbia parks Vorlage:Underwater diving
[[Category:Volcanoes of British Columbia]] [[Category:Submarine volcanoes]] [[Category:Seamounts of the Pacific Ocean]] [[Category:Hotspot volcanoes]] [[Category:Ridge volcanoes]] [[Category:Pleistocene volcanoes]] [[Category:Haida]] [[Category:Former islands of Canada]] [[Category:Underwater diving sites in Canada]] [[Category:Marine Protected Areas of Canada]] [[Category:Protected areas of British Columbia]] [[Category:Natural hazards in British Columbia]] [[Category:Polygenetic volcanoes]] [[Category:Undersea banks of the Pacific Ocean]] [[Category:Former islands from the last glacial maximum]] [[Category:Seamounts of Canada]]
- ↑ DFO SGaan Kinghlas-Bowie Seamount Marine Protected Area. In: www.dfo-mpo.gc.ca/. Department of Fisheries and Oceans Canada, abgerufen am 16. Januar 2018.
- ↑ SGAAN KINGHLAS BOWIE SEAMOUNT MARINE PROTECTED AREA MONITORING INDICATORS, PROTOCOLS AND STRATEGIES. In: www.dfo-mpo.gc.ca/. Department of Fisheries and Oceans Canada, abgerufen am 16. Januar 2018.
- ↑ Undersea Features History. GEOnet Names Server, archiviert vom am 11. Februar 2012; abgerufen am 7. März 2012.
- ↑ a b c d e f Bowie Seamount Marine Protected Area Management Plan. Fisheries and Oceans Canada, August 2001, archiviert vom am 24. März 2009; abgerufen am 27. Oktober 2008.
- ↑ Submarine Volcanoes, Vents, Ridges, and Eruptions. USGS, 13. März 2005, abgerufen am 27. Oktober 2008.
- ↑ a b c d e f g The Bowie Seamount Area. John F. Dower and Frances J. Fee, Februar 1999, archiviert vom am 24. März 2009; abgerufen am 27. Oktober 2008.
- ↑ a b c d e f Biological Observations at Bowie Seamount: August 3-5, 2003. N. McDaniel, D. Swanston, R. Haight, D. Reid and G. Grant, 22. Oktober 2003, archiviert vom am 24. März 2009; abgerufen am 6. November 2008.
- ↑ a b c d Gunter Faure: Origin of Igneous Rocks: The Isotopic Evidence. Springer, 2001, ISBN 978-3-540-67772-7, S. 66, 67 (google.com).
- ↑ a b Seamounts in the Eastern Gulf of Alaska: A Volcanic Hotspot with a Twist? National Oceanic and Atmospheric Administration, 12. Juli 2005, abgerufen am 27. Oktober 2008.
- ↑ a b Bowie Seamount Marine Protected Area. Fisheries and Oceans Canada, 25. Mai 2006, archiviert vom am 1. März 2009; abgerufen am 27. Oktober 2008.
- ↑ a b c d e Bowie Seamount Designated as Canada's Seventh Marine Protected Area. Fisheries and Oceans Canada, 19. April 2008, archiviert vom am 11. September 2009; abgerufen am 27. Oktober 2008.
- ↑ a b Designation of Bowie Seamount as a Marine Protected Area. Fisheries and Oceans Canada, 11. Oktober 2008, archiviert vom am 20. Mai 2011; abgerufen am 30. Oktober 2008.
- ↑ SGaan Kinghlas–Bowie Seamount Gin siigee tl'a damaan kinggangs gin k'aalaagangs Marine Protected Area Management Plan 2019. Council of the Haida Nation / Fisheries and Oceans Canada, 2019, abgerufen am 2. Juni 2023.
- ↑ Prostar Sailing Directions 2005 North Pacific British Columbia Enroute. ProStar Publications, 2005, ISBN 1-57785-658-9, S. 259.
- ↑ R. R. Canessa, K. W. Conley, B. D. Smiley: Bowie Seamount Pilot Marine Protected Area: An Ecosystem Overview Report. In: Canadian Technical Report of Fisheries and Aquatic Sciences. Fisheries and Oceans Canada, 2003, ISSN 0706-6457, S. 16.