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Lake Altus-Lugert, also known as Lake Altus, [3] Lake Lugert, [4] Lake Lugert-Altus, [5] and Lugert Lake, [3] is a reservoir located on the North Fork Red River, [1] about 17 miles (27 km) north of Altus, Oklahoma on the former site of the town of Lugert, Oklahoma.
In 1927, Lake Altus (now Lake Altus-Lugert) was created at the base of the Quartz Mountains. In 1935, a 148.3-acre (0.600 km 2 ) tract adjoining the lake was declared Quartz Mountain State Park. This tract was bought by citizens of Altus who donated it to the state for use as a park.
The City of Altus and private donors bought 3,000 acres (1,200 ha) of land for the park. [3] NPS spent about $500,000 building roads, trails, rest rooms and other amenities. Quartz Mountain became one of the first seven state parks in Oklahoma when the NPS turned the completed project over to the state in 1937.
It is near the cities of Mangum, Oklahoma and Altus, Oklahoma. The park is open to the public year-round for rock climbing, hiking, boating, camping, nature observation and photography, and environmental education and interpretation. The mountain overlooks scenic Lake Altus-Lugert. [3]
Aerial view of Fort Gibson Lake and Sequoyah State Park. Many large Oklahoma lakes have state parks and lodges. Shorelines of most lakes are publicly owned and accessible to everyone. Ranked by surface acres, Lake Eufaula is the 34th largest lake in the United States and Lake Texoma is the 38th largest. [2]
The nearly 8100 major dams in the United States in 2006. The National Inventory of Dams defines a major dam as being 50 feet (15 m) tall with a storage capacity of at least 5,000 acre-feet (6,200,000 m 3), or of any height with a storage capacity of 25,000 acre-feet (31,000,000 m 3).
In sharp contrast, the period between 14,300 and 11,100 years ago, which includes the Younger Dryas interval, was an interval of reduced sea level rise at about 6.0–9.9 mm/yr. Meltwater pulse 1C was centered at 8,000 years ago and produced a rise of 6.5 m in less than 140 years, such that sea levels 5000 years ago were around 3m lower than ...
Lake Stanley-Hough; 8,700 YBP, the water levels had risen to connect both Lake Stanley and Lake Hough into a single body of water. [1] Lake Stanley; 9,000 YBP [1] covered only the northern and eastern portion of the main Huron basin with channels into Lake Hough. [1] Lake Hough; 9,000 YBP [1] covered Georgian Bay, Ontario. [1]