You’d by no means confuse them for the rapid-filled rivers snaking by way of our Mountains, however the flat, straight rivers of the North Carolina Coastal Plain even have a tumultuous historical past and an occasional indignant streak, turning into raging and flooding torrents throughout our worst storms.
Alongside these rivers, and subsequent to our turbulent ocean, are delicate wetlands that give beginning to new life, from uncommon venus fly traps and seabeach amaranth to numerous fish species that go on to populate the rivers and the ocean.
The stability between these hydrological havens and the wild waters surrounding them is a cautious one, and in jap North Carolina, it’s now being thrown off by broader environmental modifications because of human impacts on the local weather and land floor.
In right now’s put up about our curious coast, we enterprise down the rivers and into the wetlands of the Coastal Plain to discover what makes them particular – and what’s altering at and beneath the floor.
Our Main Rivers
In comparison with components of the central and western United States, the place a single river and its tributaries can span complete states, the Coastal Plain of North Carolina stands out for its orderly collection of rivers, every flowing from their inland headwaters all the way down to our sounds and ocean.
Amongst them is the Cape Worry, which runs by way of Fayetteville and Wilmington earlier than emptying into the Atlantic at its namesake landform – so known as due to the worry of a shipwreck that it imbued within the crew of Sir Richard Grenville’s 1585 expedition up the coast.
There are additionally the Neuse and Tar-Pamlico river basins, every contained totally inside North Carolina. On the banks of those rivers emerged a few of our earliest cities and buying and selling hubs, together with New Bern, Tarboro, and Raleigh.
Our smaller rivers are not any much less culturally essential. The Lumbee River has been the house of Indigenous individuals for greater than 1,000 years, whereas the Chowan River and its numerous fish shares traditionally sustained a pair of Indigenous Tribes: the Weapemeoc on its west shore and the Chowanoke to the east.
In fact, the historical past of our rivers goes far past even our oldest human civilizations. As we’ve already highlighted, our shoreline as soon as reached all the best way to the present-day fall line close to Interstate 95 when sea ranges have been highest nearly three million years in the past.
As our Coastal Plain emerged from the ocean, rivers started forming shortly thereafter. Geologists have discovered proof of 5 separate terraces – the flat remnants of historical floodplains – of the Cape Worry River relationship again so far as 2.75 million years in the past.
These researchers discovered that the Cape Worry has shifted southward, primarily because of tectonic uplift throughout southeastern North Carolina.
Local weather has additionally performed an essential function within the evolution of our rivers, in accordance with Dr. Mike Benedetti, a professor of geography at UNC Wilmington, and Dr. Shannon Klotsko, assistant professor of geology at UNC Wilmington.
They famous that our rivers are at present labeled as meandering, or characterised by regular streamflow charges and vast floodplains. However within the prehistoric previous, our rivers have been braided, or flashier and able to carrying a better amount and velocity of water and sediment downstream, and thus topic to better erosion and extra fast shifts of their channels.

These braided river processes of North Carolina’s historical previous positioned rivers in dramatically totally different positions in comparison with the place we discover them right now.
“The place we dwell in Wilmington, we’d have had rivers reducing by way of there,” stated Klotsko.
Primarily based on carbon relationship and luminescence relationship of sediments, Benedetti stated we all know the transition from braided to meandering rivers occurred close to the top of the Final Glacial Most round 14,000 years in the past, as we settled into our present humid local weather with roughly evenly distributed seasonal precipitation.
These well-behaved trendy rivers have helped help human civilization and replenish the plentiful freshwater options throughout the Coastal Plain.
Coastal Water Provides
After we take into consideration water provides, particularly within the Piedmont of North Carolina, our massive reservoirs – together with Lake Norman, which provides Charlotte, and Falls Lake, which provides Raleigh – could come to thoughts.
Nevertheless, these human-made lakes have been round for lower than a century. Previous to that, consuming water got here from rivers, streams, and groundwater wells. And throughout the Coastal Plain, that’s nonetheless largely the case.
Because of its flat terrain, damming a river to create a reservoir nearly anyplace in jap North Carolina can be an train in futility – and nearly actually fatality, given the extent of land it could flood. Coastal communities subsequently have few choices however to make use of the handful of pure freshwater sources accessible to them.
In some locations, meaning pulling water immediately from the rivers. Since 1974, when its present water therapy plant was accomplished, Goldsboro has gotten its consuming water from the Neuse River. Likewise, Rocky Mount has its water provide within the Tar River, together with the Tar River Reservoir – one of many few human-made reservoirs within the area, constructed by the US Military Corps of Engineers in 1971.

Wilmington will get its consuming water partially from the Cape Worry River, but additionally from a pair of aquifers, or pockets of water trapped amid underground rocks and soils. And in Elizabeth Metropolis, with out entry to any sizable close by rivers, the water provide is drawn from the Yorktown Aquifer, a part of the low-lying wetland atmosphere within the northeastern nook of the state.
Relying solely on these sources to produce your entire area might be difficult, particularly with extra individuals dwelling there than ever earlier than. The 41 counties in North Carolina’s Coastal Plain have almost doubled in inhabitants since 1970, from 1.6 million to 2.8 million individuals as of the 2020 census.
Throughout instances of drought, our often-ephemeral Coastal Plain freshwater sources can run low. Within the fall of 2007, Wilmington imposed necessary water use restrictions because the Cape Worry River fell to only 4 or 5 inches above the consumption in Bladen County. If it fell under that stage, town would have solely had round a 30-day provide remaining from that supply.
For areas that rely solely on groundwater, they don’t need to dig too deep to entry it. Benedetti stated the water desk is often solely 6 to 10 toes beneath the floor throughout many of the Coastal Plain. Nevertheless, that stage additionally varies significantly all year long and through instances of drought.
“It’s notable for having large fluctuations in depth from season to season because of the heat local weather, seasonal modifications in temperature, water use by vegetation, and the sandy soil texture that permits evaporation and infiltration to occur quickly,” he stated.
The water desk tends to be deepest on the southern coast and shallowest within the north, the place it additionally incorporates extra natural matter and should seem yellow or brown in shade, even after therapy that makes it protected to drink.
It’s in these organic-rich wetland areas near the coast, together with within the Albemarle-Pamlico estuarine system, the place freshwater and saltwater combine. Because of their totally different densities, the freshwater floats on high, forming what geologists name a freshwater lens. In unincorporated rural areas, non-public wells typically faucet into this lens as a water provide.
Nevertheless, this freshwater is fleeting because of the infiltration of saltwater pushed by rising sea ranges. This saltwater intrusion is pushing the freshwater lens farther inland and overtaking coastal wetland environments – a few of that are distinctive to North Carolina.
A Number of Useful Wetlands
Dr. Marcelo Ardón is an affiliate professor within the Division of Forestry and Environmental Sources at NC State College and an professional on our state’s wetlands, that are primarily concentrated within the Coastal Plain.
Whenever you consider wetlands, you may image bogs or swamps – soggy, shadowy areas the place timber draped in moss emerge from the nonetheless water and tower overhead. However our wetlands are rather more various than these scenes straight out of Creature from the Black Lagoon.
Ardón speaks with intrigue about Carolina bays, the mysterious spherical depressions which have shaped lakes throughout components of the Coastal Plain.
“When you see them on a North Carolina map, you’ll be able to’t not see them,” he stated. “They’re in every single place.”

Then there are the pocosins, or shrubby lavatory wetlands usually positioned at larger elevations close to the headwaters of coastal streams. Pocosins are fed by rainfall and topped with a number of toes of peat soil that has collected over hundreds of years.
Due to the decomposing natural matter within the soil, pocosins are likely to retailer a variety of carbon, though in circumstances akin to drought occasions, they’ll oxidize and launch this carbon again into the environment as carbon dioxide, one of many main greenhouse gasses accountable for local weather change.
“When there’s drought, there may be extra prone to be hearth in these ecosystems, and with hearth in these peat soils, you find yourself dropping a variety of carbon and emitting a variety of carbon,” stated Ardón.
Fires burning in these natural soils may also be troublesome to include, and so they generally smolder for weeks or months. That’s why they’re the sources of North Carolina’s largest and longest-lived historic wildfires.
There are additionally wetlands in areas you won’t count on – akin to cities. Riparian wetlands alongside rivers and streams have been encroached on by city growth, however they provide essential advantages akin to being a buffer for flood waters and enhancing water high quality. That’s why some cities in North Carolina like Jacksonville have prioritized restoring them.
Ardón stated that’s simply one in every of many causes to understand our wetlands.
“Typically, these coastal wetlands are typically essential and distinctive as a result of they supply a habitat for plenty of totally different species, they offer us flood safety, they sequester a variety of carbon,” he stated.
Nevertheless, a few of our wetlands are disappearing, and their names and the scenes going down inside them actually do evoke recollections of a horror film.
They’re known as ghost forests, and so they’re turning into more and more widespread throughout the Coastal Plain as estuaries and different forested wetlands at the moment are being overtaken by water, killing the timber inside them.

“It appears to be a mixture of elevated saltwater intrusion in some areas, and elevated groundwater ranges,” defined Ardón, noting that elevated salinity makes it onerous for timber to take up water, making them die of thirst. However, rising groundwater ranges starve the roots of oxygen.
As they die, they lose their branches, the cover opens up, and new vegetation develops inside them, so it transitions from a forested wetland to a marsh wetland.
Whereas additionally they present ecological advantages, akin to habitats for birds and spawning grounds for fish, the marshes aren’t all the time sticking round.
“In some circumstances, the change appears to be occurring so quick that the marshes by no means get established, so the forested wetlands get swallowed by the sound or the ocean,” stated Ardón.
That underscores the vulnerability of North Carolina’s wetlands inside our current and future local weather.
New Threats to Wetlands
The kind of “climate whiplash” we noticed in 2021 – sudden swings between moist and dry intervals – doesn’t bode nicely for our wetlands.
Ardón famous that research utilizing remotely sensed observations confirmed that ghost forests are likely to kind when drought intervals are adopted by hurricanes, like we noticed within the mid-Nineteen Nineties, 2007-08, and 2011-12. We count on to see extra of these back-to-back dry-to-wet occasions sooner or later.
“The double-whammy of those two forms of occasions occurring collectively is an effective indication of once we can have a rise in ghost forests,” he stated.
Hurricanes can wipe out wetlands with their flooding rain and excessive winds, and that’s additionally unlikely to enhance.
“Storms are growing in magnitude, so when we’ve these stronger storms, we will lose a few of these ecosystems,” Ardón added.
That’s particularly essential as a result of these wetlands supply a stage of storm safety. Whether or not they’re alongside the shoreline or subsequent to a river in a significant metropolis, they’ll retailer extra water and cut back downstream discharge charges throughout flood occasions.

Due to that, and following the current floods from Floyd, Matthew, and Florence, Ardón hopes that curiosity will enhance in restoring wetlands and different pure working lands so their advantages aren’t misplaced for future generations.
The decrease Cape Worry Valley together with Wilmington is already surrounded by low-lying swampland, akin to Inexperienced Swamp to the east and Holly Shelter to the west. Because of sea stage rise and saltwater intrusion, extra of that land is prone to befalling an analogous destiny.
“If all of that will get transformed into salt marsh or open water, Wilmington will start to look much more like a peninsula than a coastal cape,” stated Benedetti.
Local weather modifications are additionally affecting the performance of our rivers – and will finally revert them to their prehistoric nature.
As our precipitation turns into extra excessive, with heavier rain falling in fewer occasions and longer dry spells in between, our rivers are seeing better water and sediment loading, which generates extra erosion and will trigger them to shift from their steady, meandering selection again to a extra risky braided habits.
“Because the system turns into extra flashy and also you see extra flood occasions and intervals of maximum drought, the river techniques can be much less steady and fewer hospitable for aquatic species,” stated Benedetti.

Our geological historical past suggests our rivers are hardly ever everlasting, even throughout steady intervals. Klotsko’s analysis makes use of seismic surveys to detect options akin to historical riverbeds, and it exhibits that heavy rain from a single storm could possibly be sufficient to open a brand new channel and finally drive a river to alter its location.
That will not occur in our lifetime, she stated, nevertheless it ought to make individuals who dwell alongside our coastal rivers contemplate their danger stage when these flooding storms transfer by way of.
“I doubt we’ll see a significant river avulsion within the subsequent 50 years, however meandering rivers naturally migrate and transfer in several instructions,” stated Klotsko. “Dwelling in a floodplain or near a floodplain isn’t a good suggestion, and we’ve constructed a variety of synthetic constructions in them.”
These potential modifications to rivers and wetlands are one other reminder of some extent this weblog collection has repeatedly realized: the very water working all through our Coastal Plain that has made this area liveable now threatens to overhaul all we’ve constructed and all we love concerning the area.
As tomorrow’s last put up on this collection will element, with some considerate planning and life like actions to mitigate in opposition to and put together for the modifications we’re seeing, we and our communities can nonetheless hope to keep away from the ghostly destiny of a few of our coastal wetlands.