Congaree national park South Carolina

South Carolina

South Carolina stands as one of the 13 original colonies, along the southeastern edge of the United States, immersed in history and flexibility. The specific size – one upside down the triangle – from about 459 km east to west, with a vertical access of 360 km. The state shares its northern border with North Carolina, the huge Atlantic in the south -East and neighbors in the south -west of Georgia. Columbia in the heart is the capital and the largest metropolis, a center of culture and governance.

The English settlement first arrived in 1670, where the plantation was a prosperous elite society run by agriculture. However, this prosperity was forced into forced labor by slave Africans, which until 1730 formed about two-thirds of the colonia. As the 19th century expanded the plantation economy beyond the coast -Tera regions, took themselves to the rolling interior, adjusting South Carolina with a cotton belt that dominated the southern landscape. The explosion of the American Civil War (1861–65) destroyed the state, which destroyed economically and politically. The difficulty of a century characterized by the upheaval and the fight was followed. Nevertheless, intensive change in the middle of the 20th century growth began and intended to grow, flourished in cities, and the civil rights movement built up the social material. Today, South Carolina was turned into Carolina, a will for flexibility and reinforcement. Area: 32,020 square kilometers. Population: (2020) 5.118,425; (2023 Location.) 5.373,555.

Congaree national park South Carolina
Congaree national park South Carolina 4

South Carolina: A landscape with separate provinces

The area of ​​South Carolina appears in three separate geological provinces, except its own character throughout the state. In the western corner, the Blue Ridge Mountain Province claims the appearance, even though it only claims 2 percent of the total land area in the state. Here, the Sasfas mountain reaches the sky up to 1,085 m), and marks the most spectacular peak of the state. Time has not yet softened, with rapid rolling expansion of the old slopes in the region that is as follows.

READ ALSO  The ODOS 'One DAE One Subscription' Program

Southeast, the Pidmont province spread, its indigenous hills are at height between 90 to 365 m. In its southeast edge, Sandhills – an old coastline sausages – diagonally in the chopped state, their sand lines are whispered into a prehistoric coastline that has long been later.

Beyond the sand hills, the coastal plain provides to empty the southern and east -third of the province of the province. Up to a height of 90 meters from the sea level from the sea level, gradual infections from the middle role area near Midlands to the almost uninterrupted flatness. Grand Strand, an ancient 100 kilometers (160 km) ancient stretch of beach, labirintin tides and freshwater islands dominate the beach before the yield of the Astrueri on the islands of the sea, which continues south in Georgia.

Two defining geological thresholds delineate these regions. The fall line, where rivers cascade over abrupt rapids, marks the division between the Coastal Plain’s sedimentary deposits and the Piedmont’s ancient metamorphic bedrock. Further inland, the Piedmont meets the Blue Ridge province along a dramatic fault line known as the Brevard Zone, a silent but enduring boundary in South Carolina’s complex geological tapestry.

Drainage and soils

South Carolina’s waterways carve a path from the northwest to the southeast, shaping the land as they flow. Three dominant river systems command nearly 80% of the state’s expanse: the Pee Dee, which drains the northeast; the Santee and its network of tributaries, coursing through the Piedmont as part of the greater Santee-Wateree-Catawba system; and the Savannah, which marks the western boundary, siphoning waters from both the Coastal and Piedmont regions. The Ashley-Combahee-Edisto system, by contrast, consists of shorter rivers born near the Sandhills, meandering through the Coastal Plain. Their waters, darkened by tannic acid from the surrounding swamps, carry little sediment, giving them an inky, almost mystical hue. Natural lakes are absent from the state’s topography those now dotting the Savannah River and Santee tributaries are products of 20th-century hydroelectric ventures.

READ ALSO  Asian Surfing Championship 2024

Scattered in the coastal field, takes a deep event form: hundreds of oval depression, their perimeter with marshy flora thick, their centers still cried, melted water. These esoteric structures known as Carolina Bez are long -lasting geography. Some people assume that they are brands that are released from an old astronomical collision, the remains of a comet or meteor effects, forever changing the calm, timeless flow of the country.

Congaree national park South Carolina
Congaree national park South Carolina 5

Climate

South Carolina is based in a subtropical climate, where summer boils with heat and moisture, while winters generally remain temperate. In July, the robust 70s climbed Fahrenheit (less 20 -year -old Celsius) the robust north -western, and climbed the 80s Fahrenheit (Upper 20 Celsius) throughout the Middleland and the coast. Vintors shout a milder rock climbing close to 3 ° F (7 ° C), the Midland average is about 7 ° C, and the coastal areas benefit from the medium touch of the Gulf stream which is about 50 ° F (10 ° C)

The growing weather in the state varies dramatically, which spreads in the Sagar Islands for about 290 days in the northwest for less than 200 days. The annual rainfall is close to an average of 1 270 mm, although the ground drinks a heavy drink from 70 to 80 inches (1 780 to 2,030 mm). The summer storms, often in the afternoon, dominate the pattern of rainfall. Each spring, about 10 tornado bends through the state, while the storm – although sporadic – threatening whips the beach, leaving imprints.

South Carolina’s Diverse Flora and Fauna

The natural landscape of South Carolina appears in separate organic regions, each of which claims its unique vegetation. In the blurry forests of Blue Ridge, the northern species that white pine and hemlock will stand, the remains of a cooler era. Pidmont, once a patchwork of land crews, saw the cultivated land in the mid -1900s, giving the way for the slow revival of the forests. Nevertheless, Vishal Oak and Hikari, once dominated the 1700s canopy, have not recovered their reign; Instead, the pine is grown in pine, huge, regimical groves, the province has become a defined tree. On the south side, the coastal plain is celebrating with an almost-interconnection juicy-coal collosel and luxurious live oak-hinges, with Saru and Mangolias, branches with ether’s veil of Spanish moss. The C Islands and the Terai parties resonate with an old peace, protected by state and federal conservatives, which adapt to these important houses from intervention.

READ ALSO  Bodies of a woman and two children were discovered floating in the Barak River

In the original south Carolina organisms, no more symbol than a white deer has no more symbol. Although the number decreased in Pidamont in the 1940s, the expansion of the coastal area has carefully and the expansion of forest deck recovered its presence across the state. The resurrection of American Beaver and Wild Türkiye outlines further flexibility in nature. However, history has not been kind to other species – Basan, Elk, Kaugar and Wolves, when the past of the past of the region disappeared in the 1800s. Today, Black Bears is a rare view, while both red foxes and wild pigs – both have been introduced by early European settlers – Rome independently. The Blue Ridge shelters woodchucks and red squirrels, while the sweltering Coastal Plain harbors alligators and all four venomous snake species native to the United States. With more than 300 avian species documented, the skies of South Carolina teem with life, though the Sandhills form a natural divide, restricting the movement of reptiles and amphibians between the Piedmont and the Coastal Plain.Make you

Related Articles

Dry Desert

Why are deserts dry? Deserts remain due to a convergence of atmospheric and geographical effects that prevent rain. These regions are within constant high pressure areas and feel that they cover wind streams that suppress the shooting and effectively prevent rain. Some deserts appear in the shade of impressing mountain ranges, where moisture filled with moisture loses the moisture to the air and crosses the extension of Lewards. Others, especially the coastal dryer, take the form of streams of the temptation sea that reduce atmospheric temperature, and reduce the air capacity to maintain moisture and cause rain.

Responses