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The Arkansas Scenic Byways Program is a list of highways, mainly state highways, that have been designated by the Arkansas Department of Transportation (ArDOT) as scenic highways. The Arkansas General Assembly designates routes for scenic byway status upon successful nomination. For a highway to be declared scenic, a group interested in ...
There are four of these in Arkansas. The National Park Service lists these four together with the NHLs in the state, [6] The Arkansas Post National Memorial, the Fort Smith National Historic Site (shared with Oklahoma) and the Little Rock Central High School National Historic Site are also NHLs and are listed above. The remaining one is:
Pine forest near Lake Winona (Arkansas); part of Ouachita National Forest. Mammoth Spring: 1972: Fulton: State The largest first magnitude spring in Arkansas, it is connected underground to the Grand Gulf State Park in Missouri. Roaring Branch Research Natural Area
The Sylamore Scenic Byway is a scenic route in the Arkansas Scenic Byways program. The route runs through the Sylamore Ranger District of the Ozark National Forest in Arkansas for 26.5 miles (42.6 km) in Stone County. [1] It passes through undeveloped forest land as a scenic route to Blanchard Springs Caverns.
A Jan. 29 Facebook post (direct link, archive link) shows a montage of tornado and extreme weather footage. "Tornado in Roger Arkansas (sic)," reads text superimposed on the video. The post's ...
Crowley's Ridge Parkway is a 212.0-mile-long (341.2 km) National Scenic Byway in northeast Arkansas and the Missouri Bootheel along Crowley's Ridge in the United States. . Motorists can access the parkway from US Route 49 (US 49) at its southern terminus near the Helena Bridge over the Mississippi River outside Helena-West Helena, Arkansas, or from Missouri Route 25 (Route 25) near Kennett, Mi
View from scenic overlook in Carroll County in the heart of the Ozarks. Northwest Arkansas contains the southern half of the Ozarks, including the steeper Boston Mountains and the more gentle Springfield Plateau. These mountains are heavily forested by an oak-hickory ecosystem and less than 25% has been cleared for agriculture. [10]
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.