The extended continental shelf, [1] [2] scientific continental shelf, [1] [2] or outer continental shelf, [3] refers to a type of maritime area, established as a geo-legal paradigm by the United Nations Convention on the Law of the Sea (UNCLOS). Through the process known as the extension of the outer limit of the continental shelf or establishment of the outer edge of the continental margin , every coastal state has the privilege, granted by the international community of nations, to acquire exclusive and perpetual rights to exploit the biotic and abiotic resources found on the seabed and subsoil of these maritime areas. These areas are located beyond the 200 nautical miles that make up the state's exclusive economic zone (EEZ) and would otherwise be considered international waters. [4] [5]
In these deep-water areas, resource exploitation was either technically impossible with available methods or economically unfeasible. Thanks to sustained scientific and industrial progress, these oceanic waters have become increasingly accessible through new technologies, which gives these areas extraordinary geopolitical and geoeconomic importance. [4]
In the case of the scientific or extended continental shelf, the coastal state to which it has been granted is the only one entitled to exploit the natural resources found in the seabed and subsoil, whether mineral resources or other non-living resources, as well as living organisms. This includes those organisms that penetrate the seabed or have sedentary habits, defined as those that remain immobile on the seabed during exploitation or move in permanent physical contact with it. [1] [2]
This type of maritime space differs significantly from the geomorphological concept of a continental shelf, which is similar to an epicontinental sea. This concept identifies the submerged extensions of the landmass of the coastal state up to depths of 200 meters.
It also differs from the concept of the legal continental shelf, [6] which refers to the right of states to exploit their maritime projections up to the limit of 200 nautical miles (regardless of the characteristics of the seabed or its depths, and whether or not there is an extension of the coast under the sea) measured from their baselines (exclusive economic zone or EEZ). In this concept, the rights to exploit the seabed and subsoil are combined with rights over the water column and surface. [1] [2]
Scientific or extended shelves are always located in maritime areas more than 200 nautical miles (370.4 km) from the straight baselines from which the width of the territorial sea is measured, and they do not extend beyond 350 nautical miles at the maximum. [6]
The creation and implementation of this legal concept, which allows coastal states to enjoy exclusive rights over vast oceanic territories, stems from the United Nations Convention on the Law of the Sea (UNCLOS), specifically in Part VI. [7] This multilateral treaty was approved in April 1982 and came into force on November 16, 1994, a year after its ratification by Guyana, which fulfilled the requirement that at least 60 signatory states ratify it.
The regulations developed and issued by UNCLOS have global application. The meeting of the states that are part of the convention established the Commission on the Limits of the Continental Shelf (CLCS), and the validation of the commission gives political and legal legitimacy. This commission is based at the United Nations headquarters in New York. [4]
For a coastal state to acquire rights over scientific continental shelves, it must rigorously follow specific steps. First, it must submit a detailed report to the CLCS, in which the state must demonstrate its rights over a specific area, outlined in a cartographic presentation. This process must consider the scientific-technical guidelines established by UNCLOS, and the report must be based on extensive data collection, including surveys and various scientific analyses, such as gravimetric, bathymetric, magnetometric, geological, geophysical, morphological, seismic, sedimentological studies, etc. Specialists in multiple disciplines, including oceanography, hydrography, geography, cartography, law, and international law, participate in this effort. [5] [3]
The CLCS, through a subcommission of seven members from a total of 21 technical experts in hydrography, geophysics, and geology, reviews the claim. They carefully examine the state's arguments, the technical data, and the accompanying maps. The commission can request clarifying meetings, make recommendations for modifications, or provide scientific-technical advice, potentially reprocessing the submitted data. [5] [8] [9] After completing the analysis, the subcommission issues draft recommendations, which are then approved by the full commission. If the state follows these recommendations, the new limits are validated. If the commission finds excessive extensions, it may recommend adjustments, leaving disputed sections in suspense. [10] The state may accept or revise its claim, and after further review, the commission may finally validate the submission. [4] [5]
Under UNCLOS Article 76.8, once the CLCS validates a state's outer limit, it is definitive and binding, enforceable against third-party states, and internationally mandatory. [4] [5]
Legally, the boundary is drawn by the state itself, with the CLCS only providing recommendations to ensure compliance with UNCLOS requirements. This ensures that the extension aligns with the rights developed under the convention. [11]
The coastal state will submit to the secretary-general of the United Nations cartography, geodetic data, and additional information describing the new outer limit, permanently established, who upon receiving them will give them appropriate dissemination so that such limits are respected by the community of nations. [12] [13]
UNCLOS, in Article 76, established complex scientific-technical guidelines that all coastal states must follow when estimating the extent of their continental shelf. These guidelines are synthesized into a combination of 4 rules—2 formulas and 2 restrictions. These standards were debated and agreed upon over several years, finally being approved in New York City on May 13, 1999, during the fifth session.
The procedure for states wishing to expand their maritime area begins with locating the foot of the continental slope, defined as the point of greatest change in gradient at its base. Once this point is identified, formula lines are drawn to find the farthest outer envelope, which will correspond to the outer edge of the continental shelf that the state intends to defend. Each state will choose the formula to use in each section, applying the most convenient based on seabed features and distances, to achieve the greatest possible extension of exclusive continental shelf. [4] [5]
Each formula was proposed by a geologist, and its technical name bears the scientist's last name:
Gardiner formula or sediment thickness formula
Its application results in a line drawn through fixed points where the sedimentary rock thickness is at least 1% of the shortest distance between that point and the foot of the slope.
Hedberg formula or distance formula
When applied, a line is drawn through fixed points located no more than 60 nautical miles from the foot of the continental slope.
Subsequently, the proposal obtained is evaluated through the belonging test, in which it must be demonstrated that the continental shelf extends beyond 200 nautical miles measured from the baselines.
In the next step, restriction rules are applied, which are two:
By combining the selected formula in the segment with the restrictions applied, the outer limits of the extended continental shelf are traced, with all segments ultimately joining in a continuous line. [14]
It was established that May 2009 would be the deadline for each state party to UNCLOS to submit a report to the CLCS, arguing their claim for expansion, which could be complete or only for a section. States that submitted on time were allowed to include new supplementary information on other claimed areas in later submissions. A state that did not submit its report by the deadline was disqualified from doing so. In the case of a state that has not yet ratified UNCLOS, any self-initiated maritime boundary expansion has no legal value. It will only acquire rights if it first adheres to the convention, after which it must submit its studies to the CLCS. A 10-year period is granted for this, starting from the date of ratification; if the state fails to submit within this decade, it will lose its right to expansion permanently. [1] [2]
The procedures established by UNCLOS are based on the principle that "land dominates the sea," meaning the status of maritime spaces legitimated by its bodies derives from the status of the coastal landmasses. If the CLCS encounters overlapping jurisdiction claims or pending conflicts during the extension process—i.e., ocean areas claimed by two or more countries, including those projected from disputed islands—any submission concerning those areas will not be examined or evaluated, as the commission cannot intervene on the substantive issue. Instead, the tracing or definitive allocation will be postponed, subject to the outcome of other legal bodies or negotiation mechanisms appropriate to the nature of these disputes, such as treaties, settlements, negotiations between the parties, mediation, rulings from international courts, etc. [15] [16] [17] Only if the claimants submit a joint presentation to the CLCS [18] [19] —a suggestion that has even been encouraged by the commission itself [20] —or express their consent, will the delimitation not prejudice the final legal settlement.
In July 2023, the International Court of Justice ruled on the priority of a Continental Shelf over an Extended Continental Shelf in the case of the territorial and maritime dispute between Colombia and Nicaragua. [21] Under the terms of the United Nations Convention on the Law of the Sea Article 59 disputed and overlapping claims have no legal force until the dispute is resolved between the opposing parties.
The United Nations Convention on the Law of the Sea (UNCLOS), also called the Law of the Sea Convention or the Law of the Sea Treaty, is an international treaty that establishes a legal framework for all marine and maritime activities. As of October 2024, 169 states and the European Union are parties.
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.
Law of the sea is a body of international law governing the rights and duties of states in maritime environments. It concerns matters such as navigational rights, sea mineral claims, and coastal waters jurisdiction. The connotation of ocean law is somewhat broader, but the law of the sea is so comprehensive that it covers all areas of ocean law as well.
An exclusive economic zone (EEZ), as prescribed by the 1982 United Nations Convention on the Law of the Sea, is an area of the sea in which a sovereign state has exclusive rights regarding the exploration and use of marine resources, including energy production from water and wind.
The Chilean Sea is the portion of the Pacific Ocean lying west of the Chilean mainland. The official Chilean usage for Chilean Sea was defined on 30 May 1974 when the Diario oficial de la Republica de Chile published Supreme Decree #346, which declared that "the waters surrounding or touching the shores of the national territory shall be known as Mar Chileno."
Ambalat is a sea block in the Celebes sea located off the east coast of Borneo. It lies to the east of the Indonesian province of North Kalimantan and to the south-east of the Malaysian state of Sabah, and it is the subject of a territorial dispute between the two nations. Malaysia refers to part of the Ambalat block as Block ND6 (formerly Block Y) and part of East Ambalat Block as Block ND7 (formerly Block Z). The deep sea blocks contain an estimated 62,000,000 barrels (9,900,000 m3) of oil and 348 million cubic meters of natural gas. Other estimates place it substantially higher: 764,000,000 barrels (121,500,000 m3) of oil and 3.96 × 1010 cubic meters (1.4 trillion cubic feet) of gas, in only one of nine points in Ambalat.
The Argentine Sea is a marginal sea of the Atlantic Ocean adjacent to the southern tip of South America. It ranges from the mouth of the estuary of the Río de la Plata in the north to the Isla de los Estados in the south, and from the Argentine coast to the 200 meters isobath. Its width varies between 210 km in front of Mar del Plata and 850 km at the latitude of the Falkland Islands. The coastline extends for 4,725 km. To the east of the Argentine Sea extends much deeper and more extensive Argentine Basin.
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.
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.
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.
The Convention on the Continental Shelf was an international treaty created to codify the rules of international law relating to continental shelves. The treaty, after entering into force 10 June 1964, established the rights of a sovereign state over the continental shelf surrounding it, if there be any. The treaty was one of three agreed upon at the first United Nations Convention on the Law of the Sea. It has since been superseded by a new agreement reached in 1982 at UNCLOS III.
The Okinawa Trough is a seabed feature of the East China Sea. It is an active, initial back-arc rifting basin which has formed behind the Ryukyu arc-trench system in the West Pacific. It developed where the Philippine Sea Plate is subducting under the Eurasia Plate.
There are disputes between China, Japan, Taiwan and South Korea over the extent of their respective exclusive economic zones (EEZs) in the East China Sea.
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.
Several states have claimed interests over the sea bed adjoining Rockall, an uninhabitable granite islet which is located within the exclusive economic zone (EEZ) of the United Kingdom. Ireland, Denmark, Iceland, and the United Kingdom have all made submissions to the commission set up under the United Nations Convention on the Law of the Sea (UNCLOS).
The Argentina–Chile border is the longest international border of South America and the third longest in the world after the Canada–United States border and the Kazakhstan–Russia border. With a length of 5,308 kilometres (3,298 mi), it separates Argentina from Chile along the Andes and on the islands of Tierra del Fuego. However, there are some border disputes, particularly around the Southern Patagonian Ice Field. It is the largest border of the two countries, beating the Argentina–Paraguay and Chile–Bolivia, Argentina's and Chile's second largest borders, respectively.
India has the 18th-largest exclusive economic zone (EEZ) with a total size of 2,305,143 km2 (890,021 sq mi). It includes the Lakshadweep island group in the Laccadive Sea off the southwestern coast of India and the Andaman and Nicobar Islands in the Bay of Bengal and the Andaman Sea. India's EEZ is bordered to the west by Pakistan, to the south by the Maldives and Sri Lanka and to the east by Bangladesh, Myanmar, Thailand, Malaysia and Indonesia. Based on new scientific data, India has petitioned United Nations to extend its EEZ from 200 Nautical miles to 500 miles.
The dispute over the extended continental shelf in the Southern Zone Sea between Argentina and Chile is a disagreement between the two countries over a maritime area of 5,302 km² that began after Argentina attempted to extend its maritime space based on the theory of the extended continental shelf over the Southern Zone Sea, south of Point F as agreed in the 1984 treaty, in an area claimed by Chile as part of its "presential sea", and now as part of its continental shelf projected from the Diego Ramírez Islands.
The Sea of the Southern Zone or Southern Zone Sea is the name given by Argentina and Chile to the maritime area whose boundaries were undefined, located south of the Isla Grande de Tierra del Fuego. This maritime space was subject to delimitation in the Treaty of Peace and Friendship of 1984 between Chile and Argentina, which ended the Beagle conflict or "Southern Zone conflict."
The continental shelf of Chile refers to the underwater extension adjacent to the Chilean coasts that stretches from the shoreline to the edge of the continental shelf in the Pacific Ocean and the Southern Ocean.
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