Continental shelf of the United States

Last updated

Diagram of the Extended Continental Shelf claim and the existing claims of continental shelves of the United States US ECS Regions 2023.png
Diagram of the Extended Continental Shelf claim and the existing claims of continental shelves of the United States

The continental shelf of the United States is the total of the continental shelves adjacent to the United States. In marine geology, it is the elevated seabed near US coasts; in the political sense, it is the area claimed by the United States as sovereign, according to the United Nations Convention on the Law of the Sea. [1]

Contents

Geopolitics

The continental shelf of the United States serves as the limit of United States sovereign power, when not demarcated by an actual land border. Due to the fact that "The coastal State exercises over the continental shelf sovereign rights," [1] the continental shelf serves as the territorial sea and the exclusive economic zone of the United States, and as such, is claimed by the United States. [1] [2] The United States also claims an extended continental shelf which follows a distinct category.

The seabed claimed by the United States is claimed as continental shelf due to a combination of qualifications offered by article 76 [1] in the UN convention. These qualifications most notably include paragraph 4(b), paragraph 5, and paragraph 7, all in article 76, according to a report published in 2023. [3] All new claims made by the United States follow these qualifications, along with all previously existing claims by the United States. [3] The United States claims that they have mapped these regions since 2003 to determine the worthiness of these claims. [3] The data collected from these surveys is publicly available on the US State Department website. [4]

Disputes and overlaps

While a some of the borders claimed by the United States are pursuant to existing treaties, most notably with Mexico [5] and Russia, [6] many new claims overlap with existing claims of other countries.

In the Arctic, Atlantic, and Mariana Islands regions, new American claims overlap with claims made by the Bahamas, Canada, and Japan. In the Arctic and Atlantic regions, both the Bahamas and Canada signaled willingness to negotiate boundary claims following the release of the 2023 report. [3] However, the US-Japanese maritime border near the Mariana Islands has been disputed since a 1993 report, [7] [ page needed ] and Japan has not signaled willingness to negotiate or accept US proposals over the shared border, according to the 2023 report. [3]

Marine geology

The continental shelf of the United States is one of the largest examples of marine geology in the world, with thousands of miles of submarine land making up the various shelves of the collective. Each different shelf features different extents of continental shelves, from the long, elevated shelves of Alaska, to the short shelf of the Pacific Coast. [3] Bathymetric data collected by the United States [4] reveals the peculiarities of the different shelves.

Alaska

Detailed relief map of the United States continental shelf in north Alaska, including US extended continental shelf claims North Alaskan Summary 01.png
Detailed relief map of the United States continental shelf in north Alaska, including US extended continental shelf claims

Alaska features some of the most prominent continental shelves in the world, extending over 400 nautical miles from the tip of Alaska, near Utqiagvik. At a depth of less than 200 meters, the Chukchi Shelf is the preeminent shelf in the arctic, barely engulfed by the Arctic Ocean. This shelf has been intensively studied for its mineral resources, most notably crude oil. As of January 2004, more than 10 billion barrels of oil had been produced from the shelf, all from the Prudhoe Bay Oil Field, according to a British Petroleum report from 2006. [8] The rest of the northern shelf is made up of the Chukchi Plateau, or the Chukchi Borderlands, as referred to in the 2023 Extended Continental Shelf document. [3] These borderlands, while more broken up and slightly deeper, are claimed to be in accordance to all six qualification measured by the United States in the survey. [3] This area is strategically important due to is purported rich natural resources, especially oil and manganese, [9] [ full citation needed ] although no resources have been proven.

Detailed relief map of the United States continental shelf in south Alaska, including US extended continental shelf claims South Alaskan Summary.png
Detailed relief map of the United States continental shelf in south Alaska, including US extended continental shelf claims

In the Bering Sea, the large Bering Shelf dominates the area, stretching over 300 nautical miles from southwest mainland Alaska, at a depth of around 500 metres. [3] The shelf features the large and sparsely populated Nunivak Island, the eight largest island in the United States. [10] The Alaskan Peninsula and Aleutian Islands extend from the south edge of the Bering Shelf, and the submarine Aleutian Ridge extends all the way to Attu Island, [3] over 1000 miles from mainland Alaska. [11] Bowers Ridge, located along the Aleutian Ridge and jutting northwest 200 nautical miles from Semisopochnoi Island, forms the last major feature of the Bering Sea continental shelf. [3] Both the Aleutian Ridge and Bowers Ridge were formed by volcanic activity drifting due to the movement of the Pacific tectonic plate. [12]

See also

Related Research Articles

<span class="mw-page-title-main">Bering Sea</span> Sea of the northern Pacific Ocean off the coast of Alaska and Russia

The Bering Sea is a marginal sea of the Northern Pacific Ocean. It forms, along with the Bering Strait, the divide between the two largest landmasses on Earth: Eurasia and the Americas. It comprises a deep water basin, which then rises through a narrow slope into the shallower water above the continental shelves. The Bering Sea is named after Vitus Bering, a Danish-born Russian navigator, who, in 1728, was the first European to systematically explore it, sailing from the Pacific Ocean northward to the Arctic Ocean.

USCGC <i>Healy</i> Icebreaker of the US Coast Guard

USCGC Healy (WAGB-20) is the United States' largest and most technologically advanced icebreaker as well as the US Coast Guard's largest vessel. She is classified as a medium icebreaker by the Coast Guard. She is homeported in Seattle, Washington, and was commissioned in 1999. On 6 September 2001 Healy visited the North Pole for the first time. The second visit occurred on 12 September 2005. On 5 September 2015, Healy became the first unaccompanied United States surface vessel to reach the North Pole, and Healy's fourth Pole visit happened on 30 September 2022.

<span class="mw-page-title-main">Territorial waters</span> Coastal waters that are part of a sovereign states sovereign territory

Territorial waters are informally an area of water where a sovereign state has jurisdiction, including internal waters, the territorial sea, the contiguous zone, the exclusive economic zone, and potentially the extended continental shelf. In a narrower sense, the term is often used as a synonym for the territorial sea.

<span class="mw-page-title-main">Chukchi Sea</span> Marginal sea of the Arctic Ocean north of the Bering Strait

The Chukchi Sea, sometimes referred to as the Chuuk Sea, Chukotsk Sea or the Sea of Chukotsk, is a marginal sea of the Arctic Ocean. It is bounded on the west by the Long Strait, off Wrangel Island, and in the east by Point Barrow, Alaska, beyond which lies the Beaufort Sea. The Bering Strait forms its southernmost limit and connects it to the Bering Sea and the Pacific Ocean. The principal port on the Chukchi Sea is Uelen in Russia. The International Date Line crosses the Chukchi Sea from northwest to southeast. It is displaced eastwards to avoid Wrangel Island as well as the Chukotka Autonomous Okrug on the Russian mainland.

<span class="mw-page-title-main">Lomonosov Ridge</span> Underwater ridge of continental crust in the Arctic Ocean

The Lomonosov Ridge is an unusual underwater ridge of continental crust in the Arctic Ocean. It spans 1,800 kilometres (1,100 mi) between the New Siberian Islands over the central part of the ocean to Ellesmere Island of the Canadian Arctic Archipelago. The ridge divides the Arctic Basin into the Eurasian Basin and the Amerasian Basin. The width of the Lomonosov Ridge varies from 60 to 200 kilometres. It rises 3,300 to 3,700 metres above the 4,200-metre (13,800 ft) deep seabed. The minimum depth of the ocean above the ridge is less than 400 metres (1,300 ft). Slopes of the ridge are relatively steep, broken up by canyons, and covered with layers of silt. It is an aseismic ridge.

<span class="mw-page-title-main">History of Alaska</span>

The history of Alaska dates back to the Upper Paleolithic period, when foraging groups crossed the Bering land bridge into what is now western Alaska. At the time of European contact by the Russian explorers, the area was populated by Alaska Native groups. The name "Alaska" derives from the Aleut word Alaxsxaq, meaning "mainland".

USCGC <i>Spar</i> (WLB-206)

USCGC Spar (WLB-206) is a United States Coast Guard Juniper-class seagoing buoy tender home-ported in Duluth, Minnesota. The ship maintains aids to navigation in the Twin Ports and Great Lakes.

<span class="mw-page-title-main">Petroleum exploration in the Arctic</span> Industry in the Arctic

Exploration for petroleum in the Arctic is expensive and challenging both technically and logistically. In the offshore, sea ice can be a major factor. There have been many discoveries of oil and gas in the several Arctic basins that have seen extensive exploration over past decades but distance from existing infrastructure has often deterred development. Development and production operations in the Arctic offshore as a result of exploration have been limited, with the exception of the Barents and Norwegian seas. In Alaska, exploration subsequent to the discovery of the Prudhoe Bay oilfield has focussed on the onshore and shallow coastal waters.

<span class="mw-page-title-main">Geography of Alaska</span>

Alaska occupies the northwestern portion of the North American continent and is bordered only by Canada on the east. It is one of two U.S. states not bordered by another state; Hawaii is the other. Alaska has more ocean coastline than all of the other U.S. states combined. About 500 miles (800 km) of Canadian territory consisting of British Columbia separate Alaska from Washington U.S. state. Alaska is thus an exclave of the United States that is part of the continental U.S. and the U.S. West Coast, but is not part of the contiguous U.S.

<span class="mw-page-title-main">Territorial claims in the Arctic</span>

The Arctic consists of land, internal waters, territorial seas, exclusive economic zones (EEZs) and international waters above the Arctic Circle. All land, internal waters, territorial seas and EEZs in the Arctic are under the jurisdiction of one of the eight Arctic coastal states: Canada, Denmark, Finland, Iceland, Norway, Russia, Sweden and the United States. International law regulates this area as with other portions of Earth.

<span class="mw-page-title-main">Continental shelf of Russia</span> Continental shelf adjacent to the Russian Federation

The continental shelf of Russia or the Russian continental shelf is the continental shelf adjacent to the Russian Federation. Geologically, the extent of the shelf is defined as the entirety of the continental shelves adjacent to Russia's coasts. In international law, however, the United Nations Convention on the Law of the Sea more narrowly defines the extent of the shelf as the seabed and subsoil of the submarine areas over which a state exercises sovereign rights.

<span class="mw-page-title-main">USSR–USA Maritime Boundary Agreement</span> Agreement between the United States and the Soviet Union

The Russia–United States maritime boundary was established by the June 1, 1990 USA/USSR Maritime Boundary Agreement. The United States Senate gave its advice and consent to ratification as early as on September 16, 1991, but it has yet to be approved by the Russian State Duma. This delimitation line is also known as the Baker-Shevardnadze line or Baker-Shevardnadze agreement, after the officials who signed the deal, Minister of Foreign Affairs of the Soviet Union Eduard Shevardnadze and US Secretary of State James Baker. The 1990 Agreement has been provisionally applied by the two countries since its date of signature.

<span class="mw-page-title-main">Outer Continental Shelf</span> Maritime U.S. federal zone of jurisdiction beyond the jurisdiction of the individual states

The Outer Continental Shelf (OCS) is a legally defined geographic feature of the United States. The OCS is the part of the internationally recognized continental shelf of the United States which does not fall under the jurisdictions of the individual U.S. states.

<span class="mw-page-title-main">Chukchi Shelf</span> Continental shelf

The Chukchi Shelf or Chukchi Sea Shelf is the westernmost part of the continental shelf of the United States and the easternmost part of the continental shelf of Russia. In the west it merges with the Russian Siberian Shelf. Within this shelf, the 50-mile Chukchi Corridor acts as a passageway for one of the largest marine mammal migrations in the world.

<span class="mw-page-title-main">Arctic Ocean</span> Ocean in the north polar region

The Arctic Ocean is the smallest and shallowest of the world's five oceanic divisions. It spans an area of approximately 14,060,000 km2 (5,430,000 sq mi) and is the coldest of the world's oceans. The International Hydrographic Organization (IHO) recognizes it as an ocean, although some oceanographers call it the Arctic Mediterranean Sea. It has also been described as an estuary of the Atlantic Ocean. It is also seen as the northernmost part of the all-encompassing world ocean.

USC&GS <i>Yukon</i> (1873)

USC&GS Yukon was a schooner that served as a survey ship from 1878 to 1894 in the United States Coast Survey, which was renamed the United States Coast and Geodetic Survey in 1878. She was the pioneering Coast Survey or Coast and Geodetic Survey ship in many of the waters of the Territory of Alaska, including the Bering Sea and the western Aleutian Islands, and she also operated extensively in California and Washington. She later entered commercial service as Elwood and was wrecked in 1895.

<span class="mw-page-title-main">Aleutian Islands</span> Chain of islands in the Pacific Ocean

The Aleutian Islands —also called the Aleut Islands, Aleutic Islands, or, before 1867, the Catherine Archipelago—are a chain of 14 main, larger volcanic islands and 55 smaller ones. Most of the Aleutian Islands belong to the U.S. state of Alaska, with the archipelago encompassing the Aleutians West Census Area and the Aleutians East Borough. The Commander Islands, located further to the west, belong to the Russian federal subject of Kamchatka Krai, of the Russian Far East. The islands form part of the Aleutian Arc of the Northern Pacific Ocean, and occupy a land area of 6,821 sq mi (17,666 km2) that extends westward roughly 1,200 mi (1,900 km) from the Alaskan Peninsula mainland, in the direction of the Kamchatka Peninsula; the archipelago acts as a border between the Bering Sea to the north and the Pacific Ocean to the south. Crossing longitude 180°, at which point east and west longitude end, the archipelago contains both the westernmost and easternmost parts of the United States, by longitude. The westernmost U.S. island, in real terms, however, is Attu Island, west of which runs the International Date Line.

<span class="mw-page-title-main">Arctic cooperation and politics</span> Between the eight Arctic nations

Arctic cooperation and politics are partially coordinated via the Arctic Council, composed of the eight Arctic states: the United States, Canada, Iceland, Norway, Sweden, Finland, Russia, and Denmark with Greenland and the Faroe Islands. The dominant governmental power in Arctic policy resides within the executive offices, legislative bodies, and implementing agencies of the eight Arctic countries, and to a lesser extent other countries, such as United Kingdom, Germany, European Union and China. NGOs and academia play a large part in Arctic policy. Also important are intergovernmental bodies such as the United Nations and NATO.

<span class="mw-page-title-main">Chukchi Plateau</span> A large subsea formation extending north from the Alaskan margin into the Arctic Ocean

The Chukchi Plateau or Chukchi Cap is a large subsea formation extending north from the Alaskan margin into the Arctic Ocean. The ridge is normally covered by ice year-round, and reaches an approximate bathymetric prominence of 3,400 m with its highest point at 246 m below sea level. As a subsea ridge extending from the continental shelf of the United States north of Alaska, the Chukchi Plateau is an important feature in maritime law of the Arctic Ocean and has been the subject of significant geographic research. The ridge has been extensively mapped by the USCGC Healy, and by the Canadian icebreaker CCGS Louis S. St-Laurent in 2011 and RV Marcus Langseth, a National Science Foundation vessel operated by the Lamont–Doherty Earth Observatory of Columbia University.

<span class="mw-page-title-main">Smith Bay</span> Estuary in the Beaufort Sea

Smith Bay is an estuary in the Beaufort Sea that supports a wide range of fish, birds, and marine mammals. It is located northeast of Point Barrow, Alaska. The Bureau of Ocean Energy Management recognizes the southeastern portion of Barrow Canyon, which covers some, but not all, of Smith Bay, as an Environmentally Important Area.

References

  1. 1 2 3 4 United Nations Convention on the Law of the Sea. United Nations. December 10, 1982. pp. 53–56. Retrieved June 19, 2024 via WikiSource.
  2. "Limits in the Seas". United States Department of State. Retrieved June 19, 2024.
  3. 1 2 3 4 5 6 7 8 9 10 11 "U.S. ECS Executive Summary (PDF)" (PDF). United States Department of State. 2023. Retrieved June 19, 2024.
  4. 1 2 "Data Collection". United States Department of State. Retrieved June 21, 2024.
  5. "Treaty with Mexico on Delamination of Continental Shelf" (PDF). United States Government Printing Office. July 27, 2000. Retrieved June 21, 2024.
  6. "1990 USSR/USA Maritime Boundary Agreement" (PDF). United Nations Division for Ocean Affairs and the Law of the Sea. June 1, 1990. Retrieved June 21, 2024.
  7. Lapine, Lewis A. (August 1993). NOAA Technical Memorandum NOS NGS 62: United States–Japan Maritime Boundary Determination Survey (Technical report). U.S. National Geodetic Survey . Retrieved June 21, 2024.
  8. "Prudhoe Bay Fact Sheet" (PDF). BP. August 2006. Archived from the original (PDF) on March 26, 2009. Retrieved June 22, 2024.
  9. Lunchtime Talk: Law of the Sea and Extending U.S. Resource Rights in the Arctic. ISER UAA. November 14, 2013. Retrieved June 22, 2024 via YouTube.
  10. "Nunivak Island". Encyclopedia Britannica . Retrieved June 22, 2024.
  11. "Attu Island, Alaska". NASA Earth Observatory . NASA. July 5, 2006. Retrieved June 22, 2024.
  12. Keren_F (December 19, 2020). "An Introduction to the Aleutian Arc". An Armchair Volcanologist. Retrieved June 22, 2024.