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DeGray Lake Resort State Park is a 984-acre (398 ha) Arkansas state park in Clark and Hot Spring counties, Arkansas in the United States.Situated in the Ouachita Mountains, the park features the 13,800-acre (5,600 ha) DeGray Lake, the park features a championship rated 18 hole golf course and Arkansas's only state park resort. [2]
Opal's Steak House is a historic building located at 871 Park Avenue in Hot Springs, Arkansas.Opal's Steak House was constructed between 1946 and 1948 to serve tourists visiting the thermal springs in Hot Springs; its location on Park Avenue served travelers on nearby U.S. Route 70, the main highway between Little Rock and Hot Springs.
The commission surveyed and set aside 264.93 acres (1.0721 km 2) encompassing the hot springs and Hot Springs Mountain to be a permanent government reservation. Another 1,200 acres (4.9 km 2 ) became the Hot Springs townsite, with 700 acres (2.8 km 2 ) awarded to claimants.
The Arlington Resort Hotel & Spa is a resort in the Ouachita Mountains of Hot Springs National Park, Arkansas, home of Oaklawn Race Track and the Arkansas Derby. The Arlington's design inspired the Baker Hotel in Mineral Wells, Texas. [citation needed] The hotel is located at the north end of "Bathhouse Row".
The Central Avenue Historic District is the historic economic center of Hot Springs, Arkansas, United States, located directly across Central Avenue from Bathhouse Row. Built primarily between 1886 and 1930, the hotels, shops, restaurants and offices on Central Avenue have greatly benefited from the city's tourism related to the thermal waters ...
One of three mountain state parks in the Arkansas River Valley, includes historic cabins, 14 miles (23 km) of hiking trails, and popular hang-gliding launch points. Ozark Folk Center: Stone: 637 acres (258 ha) 1973: None: Located near Mountain View, Arkansas, it preserves the music, culture, and traditions of the Ozark Mountains. Hosts special ...
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The Arkansas Novaculite consists of lower, middle, and upper members. The lower member is a massive fractured novaculite, and is the dominant member on Hot Springs Mountain, with a thickness of about 275 ft (84 m) The middle member is a black clay shale interbedded with novaculite, about 10 ft (3.0 m) thick on Hot Springs Mountain.