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The Highland Rim is a physiographic section of the larger Interior Low Plateaus province, which in turn is part of the larger Interior Plains physiographic division. [1] Most of the Highland Rim is located in U.S. EPA Ecoregion 71, Interior Plateau, which is a part of the Eastern Temperate Forest.
Tennessee is in the Southeastern United States.Most of the state is considered part of the Upland South, and the eastern third is part of Appalachia. [1] Tennessee covers roughly 42,143 square miles (109,150 km 2), of which 926 square miles (2,400 km 2), or 2.2%, is water.
The High Lava Plains ecoregion is a vast, nearly level to undulating sagebrush steppe containing scattered volcanic cones and buttes. Elevation varies from 4,200 to 6,800 feet (1,280 to 2,073 m). Elevation varies from 4,200 to 6,800 feet (1,280 to 2,073 m).
Great Plains: Missouri Plateau, Glaciated: Missouri Plateau, Unglaciated: Black Hills: High Plains: Plains Border: Arctic Coastal Plain: Colorado Piedmont: Raton section Pecos Valley: Edwards Plateau: Central Texas section Central Lowland Dissected Till Plains: Eastern Lake section Osage Plains: Till Plains Western Lake section Wisconsin ...
The region takes a U shape starting in western Tennessee, going south through eastern Mississippi, and forming most of Alabama. On the eastern side, the plains lie between the Appalachian Mountains and the coastal plains, forming central Georgia, South Carolina, and North Carolina. It forms part of eastern Virginia before terminating in Maryland.
The Brothers Fault Zone is also the locus of the High Lava Plains (HLP) volcanism of central and southeastern Oregon. HLP volcanism is notable for showing an age progression from 16 Ma at its eastern end (near the Oregon–Nevada–Idaho corner) to the active Newberry Volcano at its western end.
Short Mountain is a mountain-sized monadnock that is the highest point in Cannon County, Tennessee and the Nashville metropolitan area.It is surrounded by the Highland Rim to the north, east and south but is an outlier of the Cumberland Plateau, evidenced by its sandstone caprock reaching over 2,000 feet (610 meters) in elevation; [1] this makes it the westernmost part of Tennessee with an ...
In 1992, Coffin and Eldholm initially defined the term "large igneous province" as representing a variety of mafic igneous provinces with areal extent greater than 100,000 km 2 that represented "massive crustal emplacements of predominantly mafic (magnesium- and iron-rich) extrusive and intrusive rock, and originated via processes other than 'normal' seafloor spreading."