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Syllabus
son Sound—where some offshore islands are more than six miles apart or more than six miles from the mainland—because it gives the United States "enclaves" of submerged lands, wholly or partly surrounded by state-owned submerged lands, beneath waters more than three miles from the mainland but not within three miles of an island. United States v. Louisiana, 470 U. S. 93, does not foreclose the conclusion that the Convention's normal baseline principles apply here. Alaska has not identified a firm and continuing United States rule treating waters between the mainland and fringing islands as "inland waters" when the openings between the off-lying islands are no more than 10 miles wide. The sources before the Master showed that, in its foreign relations, particularly in the period 1930 to 1949, the United States had advocated a rule under which objectionable pockets of high seas between the mainland and fringing islands would be assimilated to a coastal nation's territorial sea. Such a rule would have been inconsistent with Alaska's 10-mile rule, under which no objectionable pockets of high seas would have existed. The United States also advocated a rule for treating the waters of a strait leading to an inland sea as inland waters, but it is not equivalent to Alaska's rule. Pp. 7-22. 2. Alaska's exception to the recommended ruling that a gravel and ice formation known as Dinkum Sands is not an island constituting part of Alaska's coastline under the Submerged Lands Act is overruled. The Master did not err in concluding that Dinkum Sands does not meet the standard for an island because it is frequently below mean high water. The Convention's drafting history suggests that, to qualify as an island, a feature must be above high water except in abnormal circumstances. It does not support the broader conclusion that a feature with a seasonal loss in elevation that brings it below mean high water, such as Dinkum Sands, qualifies. Nor is there any precedent for deeming Dinkum Sands an island during the periods when it is above mean high water. Pp. 22-32. 3. Alaska's exception to the recommended ruling that submerged lands beneath tidally influenced waters within the Reserve's boundary did not pass to Alaska at statehood is overruled. The United States can reserve submerged lands under federal control for an appropriate public purpose. Under the strict standards of Utah Div. of State Lands v. United States, 482 U. S. 193, the 1923 Executive Order creating the Reserve reflected a clear intent to include submerged lands within the Reserve. In addition to the fact that the Order refers to coastal features and necessarily covers the tidelands, excluding submerged lands beneath the coastal features would have been inconsistent with the Reserve's purpose—to secure an oil supply that would necessarily exist
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