The Atlantic Seaboard Fall Line or ”Fall Zone”, is a 1,400 kilometers escarpment where the “Piedmont” and “Atlantic coastal” plain meet in the eastern United States. Much of the Atlantic Seaboard fall line passes across the areas where no evidence of faulting is available now. Moreover, the fall line marks the geologic boundary of hard metamorphosed terrain “the product of the Taconic orogeny” and the sandy, relatively flat outwash plain of the upper continental shelf, created of unconsolidated Cretaceous and Cenozoic sediments. The main examples of the Fall Zone comprise the “Potomac River’s Great Falls” and the rapids in Richmond, Virginia, where the James River falls across a series of rapids down to its own tidal estuary.

Before navigation improvements such as locks, the fall line was normally the head of navigation on rivers due to their fast-moving water or waterfalls, and the essential portage around them. The Great Falls of the Potomac River is one example. Due to the commercial traffic, requisite labor and accessibility of water power to operate mills; several cities were founded at the intersection of rivers and the fall line. United States Route 1 connects several of the fall line cities. In 1808, Treasury Secretary “Albert Gallatin” noticed the importance of the fall line as a hindrance to improved national communication and commerce among the Atlantic seaboard and the western river systems. The most well-known, though not maybe the most challenging obstruction in the navigation of the Atlantic rivers, comprises in their lower falls, which are ascribed to a presumed incessant granite ridge, rising about 130 feet above tide water.

Although, the ridge from New York to James River inclusively arrests the ascent of the tide; the falls of every river within that space being specifically at the head of the tide; following thence southwardly a direction almost parallel to the mountains, it recedes from the sea, leaving in each southern river a coverage of good navigation between the tide and the falls. Other falls of less magnitude are found at the gaps of the Blue Ridge, from side to side which the rivers have forced their passage.Source: Virginiaplaces and Wikipedia

the Fall Line zone (black line) separates the Coastal Plain of eastern Virginia (yellow) from the hard bedrock of the Piedmont

the Fall Line zone (black line) separates the Coastal Plain of eastern Virginia (yellow) from the hard bedrock of the Piedmont

the Fall Line separates the Coastal Plain (darker green...) and the Piedmont

the Fall Line separates the Coastal Plain (darker green…) and the Piedmont

the Fall Line on the Rappahannock River led to the establishment of Fredericksburg Falmouth and the location of Route 1

the Fall Line on the Rappahannock River led to the establishment of Fredericksburg Falmouth and the location of Route 1

the Fall Line extends from New York to Georgia

the Fall Line extends from New York to Georgia

Teddy Roosevelt Island marks the geologic boundary between the hard crystalline bedrock of the Piedmont and the soft sediments of the Coastal Plain

Teddy Roosevelt Island marks the geologic boundary between the hard crystalline bedrock of the Piedmont and the soft sediments of the Coastal Plain

Captain Newport's exploration up the James River in April, 1607 ended with the discovery of rapids near what is now called Mayo's Island in downtown Richmond (direction of flow indicated by arrow)

Captain Newport’s exploration up the James River in April, 1607 ended with the discovery of rapids near what is now called Mayo’s Island in downtown Richmond (direction of flow indicated by arrow)

Great Falls, on the Potomac River, reveals the hard metamorphic rock of the Piedmont - and how rivers in flood stage carve channels

Great Falls, on the Potomac River, reveals the hard metamorphic rock of the Piedmont – and how rivers in flood stage carve channels

Map showing part of the Eastern Seaboard Fall Line where the pale colored coastal plain meets the brightly colored Piedmont.

Map showing part of the Eastern Seaboard Fall Line where the pale colored coastal plain meets the brightly colored Piedmont.

migration of Potomac River waterfall from geologic boundary at I-66 bridge upstream to Great Falls (blue), and on to Seneca Creek (red) in next million or so years

migration of Potomac River waterfall from geologic boundary at I-66 bridge upstream to Great Falls (blue), and on to Seneca Creek (red) in next million or so years

rapids at the Fall Line of the Rappahannock River in Fredericksburg (I-95 just to left)

rapids at the Fall Line of the Rappahannock River in Fredericksburg (I-95 just to left)

Africa and North America collided, the sediments in the Iapetus Ocean were compressed and metamorphosed to become part of the bedrock in the Piedmont physiographic province

Africa and North America collided, the sediments in the Iapetus Ocean were compressed and metamorphosed to become part of the bedrock in the Piedmont physiographic province

500-million-year-old (Cambrian Period) crystalline bedrock outcrops are buried beneath younger Coastal Plain sediments and artificial fill east of Teddy Roosevelt Island and Rock Creek Park

500-million-year-old (Cambrian Period) crystalline bedrock outcrops are buried beneath younger Coastal Plain sediments and artificial fill east of Teddy Roosevelt Island and Rock Creek Park

Originally posted 2015-08-15 10:22:56. Republished by Blog Post Promoter

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