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North Carolina Watersheds
and River Basins
By Kella Randolph
Copyright 2019
https://upload.wikimedia.org/wikipedia/commons/thumb/9/9b/Neuse_River-27527.jpg/1200px-Neuse_River-
27527.jpg
What is a River Basin?
• A river basin is the land that
water flows across or under on
its way to a river. It is the
drainage area of a river. As a
bathtub catches all the water
that falls within its sides, a
river basin sends all the water
falling on the surrounding land
into a central river and out to
an estuary or the sea.
• Image:
https://www.ncwildlife.org/Conserving/Habitats/North-
Carolina-River-Basins)
Watershed • Land that drains into a specific body of water is a watershed.
It is all the land drained by a river.
Image left: https://images.app.goo.gl/TNQuvZccGbaSkoi4A
Image above: https://images.app.goo.gl/fq67Ky6nEaWzRHoMA
What is groundwater?
Groundwater is the water
found in cracks and pores in
sand, gravel and rocks below
the earth’s surface.
https://upload.wikimedia.org/wikipedia/commons/b/b1/Groundwaterimage.jpg
Ecosystem
An ecosystem is a natural system linked by
living and non-living things. So an ecosystem
may include the soil, water, air and the
plants, animals, birds and insects of a specific
area.
Image left:
http://www.openlearningworld.com/World_Geography/imgs/figure
_7.6.1.jpg
Image above:
https://c2.staticflickr.com/6/5245/5366897663_b156729c10_b.jpg
Estuary
An estuary is a semi-enclosed area where fresh water from a river meets salty water from the sea
https://www.e-education.psu.edu/earth107/sites/www.e-
education.psu.edu.earth107/files/Unit1/Mod1/BayareaUSGS.jpg
https://upload.wikimedia.org/wikipedia/commons/thumb/f/ff/Mid_to_upper_reach_of_Ythan_Est
uary_looking_west%2C_Aberdeenshire.jpg/1200px-
Mid_to_upper_reach_of_Ythan_Estuary_looking_west%2C_Aberdeenshire.jpg
There are several river
basins in North Carolina
• The land near each river basin drains into
that river. We call the land that “sheds”
water into the river a “watershed”.
https://images.app.goo.gl/SNHC3CihLDaV5vvo8
https://www.carolana.com/NC/Transportation/nc_watersheds.html
Know your watersheds
https://images.app.goo.gl/6CQc5HfmWyAW8AJ49
This map shows the town of Chapel Hill, N.C.
Each named area is the body of water into
which the watershed drains.
Earth’s water budget
• The same amount of water on the planet today
was present 3 billion years ago. Water on Earth
circulates continuously. It falls as rain, filters into the
ground to recharge aquifers and runs along the
earth’s surfaces, creeks, rivers and streams. That
same water is absorbed by roots of plants and then
some of it transpires through the plants or
evaporates through the surface soil, That vapor then
re-enters the atmosphere and rises to form clouds,
then falls again as rain or snow.
Discover North Carolina’s River Basins: file:///C:/Users/Kella/AppData/Local/Temp/discover-nc-river-
basins-booklet.pdf
https://upload. _Management_with_trees.webm/437px--
wikimedia.org/wikipedia/commons/thumb/e/e2/StormwaterStorm
water_Management_with_trees.webm.jpg
https://62e528761d0685343e1c-
f3d1b99a743ffa4142d9d7f1978d9686.ssl.cf2.rackcdn.com/files/
81071/area14mp/image-20150508-22773-1bi6vh6.jpg
(17) major River Basins
within North Carolina
NORTH CAROLINA HAS 17 MAJOR RIVER BASINS.
Five of the state’s river basins—the Hiwassee, Little
Tennessee, French Broad, Watauga and New—are
part of the Mississippi River Basin, which drains to
the Gulf of Mexico. All the others flow to the
Atlantic Ocean. Of the 17 basins, 11 originate in
North Carolina, but only four are contained entirely
within the state’s borders—the Cape Fear , Neuse,
White Oak and Tar-Pamlico.
Broad River
Basin Cape Fear River Basin Catawba River Basin
Chowan River
Basin
French Broad River Basin Hiwassee River Basin
Litte Tennessee
River Basin
Lumber River Basin Neuse River Basin
New River
Basin
Pasquotank River Basin Roanoke River Basin
Savannah River
Basin
Tar-Pamlico River Basin Watauga River Basin
White Oak
River Basin
Yadkin River Basin
Groundwater in coastal areas
• Ground water is a vital resource for communities and
ecosystems of the Atlantic coastal zone. Ground-water
withdrawals for public supplies, agriculture, industry, and other
uses in coastal counties from Maine to Florida were about 7.7
billion gallons per day in 1995, and in many coastal communities,
ground water is the primary or sole source of drinking-water
supply. Ground water sustains the flow of coastal streams and
rivers and is a source of freshwater to coastal ponds, wetlands,
and other coastal ecosystems. The U.S. Geological Survey (USGS)
has a long history of conducting scientific studies of ground water
in the Atlantic coastal zone. This Circular draws heavily on the
body of scientific knowledge developed over several decades of
USGS monitoring and studies.
• Above text: https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608
• Right Image and text: https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608)
Population (A) and ground-water withdrawals (B) by county,
1995, in States along the Atlantic coast of the United States.
More than two-thirds of the population of these States live
in coastal counties, defined as having at least 15 percent of
their land area in a coastal watershed (National Oceanic and
Atmospheric Administration, 1998).
Groundwater in coastal areas (continued)
Because of a growing awareness of the critical role of
ground water in sustaining coastal populations,
economies, and ecosystems, the time is right to review
some of the important water-management issues and
scientific principles related to ground water in the
Atlantic coastal zone, and to identify some of the
scientific and management challenges that lie ahead.
This Circular describes the occurrence and flow of
freshwater and saltwater in ground-water systems of
the Atlantic coastal zone; reviews the causes, modes,
and management of saltwater intrusion along the
Atlantic coast; and illustrates some of the mechanisms
of ground-water discharge and contaminant loading to
coastal ecosystems. The Circular also illustrates
traditional approaches for monitoring and managing
saltwater intrusion, and highlights some of the
innovative approaches being used to enhance the
sustainability of coastal ground-water resources, such
as desalination and aquifer storage and recovery
systems. As coastal populations and ground-water use
increase, new monitoring and research efforts will be
needed to characterize the occurrence and movement
of saline ground water in different types of coastal
terrains and to better understand linkages between
ground-water discharge and quality and the health of
coastal ecosystems. The USGS looks forward to
continued service to the citizens of the Atlantic coastal
zone, providing science to help them manage their
water resources.
(Text:
https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608)
Ground-water flow paths in an idealized coastal
watershed along the Atlantic coast. Fresh ground water is
bounded by saline ground water beneath the bay and
ocean. Fresh ground water discharges to coastal streams,
ponds, salt marshes, and tidal creeks and directly to the
bay and ocean. Image and text:
https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608)
Depletion of Fossil
Water Resources
By their very definition fossil water resources
will eventually run out one they begin being
used. For over 50 years Libya has relied on fossil
water supplies that are now dwindling but the
prospect of fossil water reserves running out is
not limited to the Middle East or northern
Africa. Parts of the former USSR, India, China
and Mexico all depend on non-renewable water
taken from ancient aquifers. In the United States
a number of the Great Plains states take a
considerable amount of their water from a fossil
water aquifer. This water reservoir is the
Ogallala Aquifer or the high planes Aquifer.
Estimates forecast this aquifer being empty in
25 years. The disruption is likely to be immense
as the aquifer covers portions of eight states,
and supplies 82% of the drinking water for these
states and around 30% of the water used for
crop irrigation in the area.
(https://www.azocleantech.com/article.aspx?ArticleID=167 Written by
AZoCleantechJun 23 2009)
http://4.bp.blogspot.com/-
CwZ37uwlim8/U_gcAN1D0gI/AAAAAAABGUE/cnAHYYa7U-
0/s1600/waste%2Bfacility.jpg
https://s3-us-west-2.amazonaws.com/courses-images-archive-read-only/wp-
content/uploads/sites/667/2015/06/22204248/aquifersandwells.gif
Alternate Options to Fossil
Water
• For poor countries there are few options available
other than using fossil water supplies. For wealthier
nations options include desalination of saltwater
from oceans. The problem with this is that fossil
water supplies have no regard for international
boundaries. Neighboring countries may share an
aquifer and one country is unlikely to use the
expensive desalination option while its neighbor
continues to cheaply extract fossil water.
(https://www.azocleantech.com/article.aspx?ArticleID=167 Written by AZoCleantechJun 23 2009)
https://upload.wikimedia.org/wikipedia/commons/thu
mb/0/01/Faryab-_village_dug_well.JPG/1200px-Faryab-
_village_dug_well.JPG
https://c2.staticflickr.com/4/3501/3801125543_54f92b0e1e_z.jpg?zz=1
Brackish Water
• Brackish water is water having more salinity
than freshwater, but not as much as seawater. It
may result from mixing seawater with fresh
water together, as in estuaries, or it may occur in
brackish fossil aquifers.
https://wikiislam.net/wiki/images/thumb/a/a1/Estuary.jpg/400px-
Estuary.jpg
https://lh3.googleusercontent.com/FwiQcXNV7-JcDQikxtqQbZCd7K1-
3mYMjstHksI7PWUccJ4uaC5rI-D1jE1FIrmssEz55pk=s128
Desalinization
is an expensive process
that poorer countries
cannot afford.
• Desalination is a process that takes away mineral
components from saline water. More generally, desalination
refers to the removal of salts and minerals from a target
substance, as in soil desalination, which is an issue for
agriculture. ( https://en.wikipedia.org/wiki/Desalination)
https://www.e-education.psu.edu/earth111/sites/www.e-
education.psu.edu.earth111/files/Module10/TampaBayDesalinationPlantProce
ss_HR.jpeg
https://i0.wp.com/www.middleeastmonitor.com/wp-content/uploads/2018/01/Desalination-Plant2-
e1516544826721.jpg?resize=1200%2C800&quality=75&strip=all&ssl=1
Desalinization
• Desalination is a process that takes away mineral components from saline water. More generally, desalination refers to
the removal of salts and minerals from a target substance, as in soil desalination, which is an issue for agriculture.
• Saltwater is desalinated to produce water suitable for human consumption or irrigation. The by-product of the
desalination process is brine. Desalination is used on many seagoing ships and submarines. Most of the modern
interest in desalination is focused on cost-effective provision of fresh water for human use. Along with recycled
wastewater, it is one of the few rainfall-independent water sources.
• Due to its energy consumption, desalinating sea water is generally more costly than fresh water from rivers or
groundwater, water recycling and water conservation. However, these alternatives are not always available and
depletion of reserves is a critical problem worldwide. Desalination processes are usually driven by either thermal (in
the case of distillation) or electrical (e.g., photovoltaic or wind power) as the primary energy types.
• Currently, approximately 1% of the world's population is dependent on desalinated water to meet daily needs, but the
UN expects that 14% of the world's population will encounter water scarcity by 2025. Desalination is particularly
relevant in dry countries such as Australia, which traditionally have relied on collecting rainfall behind dams for water.
• Kuwait produces a higher proportion of its water than any other country, totaling 100% of its water use.
(Story from Wikipedia: https://en.wikipedia.org/wiki/Desalination)

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North Carolina watersheds and river basins

  • 1. North Carolina Watersheds and River Basins By Kella Randolph Copyright 2019 https://upload.wikimedia.org/wikipedia/commons/thumb/9/9b/Neuse_River-27527.jpg/1200px-Neuse_River- 27527.jpg
  • 2. What is a River Basin? • A river basin is the land that water flows across or under on its way to a river. It is the drainage area of a river. As a bathtub catches all the water that falls within its sides, a river basin sends all the water falling on the surrounding land into a central river and out to an estuary or the sea. • Image: https://www.ncwildlife.org/Conserving/Habitats/North- Carolina-River-Basins)
  • 3. Watershed • Land that drains into a specific body of water is a watershed. It is all the land drained by a river. Image left: https://images.app.goo.gl/TNQuvZccGbaSkoi4A Image above: https://images.app.goo.gl/fq67Ky6nEaWzRHoMA
  • 4. What is groundwater? Groundwater is the water found in cracks and pores in sand, gravel and rocks below the earth’s surface. https://upload.wikimedia.org/wikipedia/commons/b/b1/Groundwaterimage.jpg
  • 5. Ecosystem An ecosystem is a natural system linked by living and non-living things. So an ecosystem may include the soil, water, air and the plants, animals, birds and insects of a specific area. Image left: http://www.openlearningworld.com/World_Geography/imgs/figure _7.6.1.jpg Image above: https://c2.staticflickr.com/6/5245/5366897663_b156729c10_b.jpg
  • 6. Estuary An estuary is a semi-enclosed area where fresh water from a river meets salty water from the sea https://www.e-education.psu.edu/earth107/sites/www.e- education.psu.edu.earth107/files/Unit1/Mod1/BayareaUSGS.jpg https://upload.wikimedia.org/wikipedia/commons/thumb/f/ff/Mid_to_upper_reach_of_Ythan_Est uary_looking_west%2C_Aberdeenshire.jpg/1200px- Mid_to_upper_reach_of_Ythan_Estuary_looking_west%2C_Aberdeenshire.jpg
  • 7. There are several river basins in North Carolina • The land near each river basin drains into that river. We call the land that “sheds” water into the river a “watershed”. https://images.app.goo.gl/SNHC3CihLDaV5vvo8
  • 9. Know your watersheds https://images.app.goo.gl/6CQc5HfmWyAW8AJ49 This map shows the town of Chapel Hill, N.C. Each named area is the body of water into which the watershed drains.
  • 10. Earth’s water budget • The same amount of water on the planet today was present 3 billion years ago. Water on Earth circulates continuously. It falls as rain, filters into the ground to recharge aquifers and runs along the earth’s surfaces, creeks, rivers and streams. That same water is absorbed by roots of plants and then some of it transpires through the plants or evaporates through the surface soil, That vapor then re-enters the atmosphere and rises to form clouds, then falls again as rain or snow. Discover North Carolina’s River Basins: file:///C:/Users/Kella/AppData/Local/Temp/discover-nc-river- basins-booklet.pdf https://upload. _Management_with_trees.webm/437px-- wikimedia.org/wikipedia/commons/thumb/e/e2/StormwaterStorm water_Management_with_trees.webm.jpg https://62e528761d0685343e1c- f3d1b99a743ffa4142d9d7f1978d9686.ssl.cf2.rackcdn.com/files/ 81071/area14mp/image-20150508-22773-1bi6vh6.jpg
  • 11. (17) major River Basins within North Carolina NORTH CAROLINA HAS 17 MAJOR RIVER BASINS. Five of the state’s river basins—the Hiwassee, Little Tennessee, French Broad, Watauga and New—are part of the Mississippi River Basin, which drains to the Gulf of Mexico. All the others flow to the Atlantic Ocean. Of the 17 basins, 11 originate in North Carolina, but only four are contained entirely within the state’s borders—the Cape Fear , Neuse, White Oak and Tar-Pamlico. Broad River Basin Cape Fear River Basin Catawba River Basin Chowan River Basin French Broad River Basin Hiwassee River Basin Litte Tennessee River Basin Lumber River Basin Neuse River Basin New River Basin Pasquotank River Basin Roanoke River Basin Savannah River Basin Tar-Pamlico River Basin Watauga River Basin White Oak River Basin Yadkin River Basin
  • 12. Groundwater in coastal areas • Ground water is a vital resource for communities and ecosystems of the Atlantic coastal zone. Ground-water withdrawals for public supplies, agriculture, industry, and other uses in coastal counties from Maine to Florida were about 7.7 billion gallons per day in 1995, and in many coastal communities, ground water is the primary or sole source of drinking-water supply. Ground water sustains the flow of coastal streams and rivers and is a source of freshwater to coastal ponds, wetlands, and other coastal ecosystems. The U.S. Geological Survey (USGS) has a long history of conducting scientific studies of ground water in the Atlantic coastal zone. This Circular draws heavily on the body of scientific knowledge developed over several decades of USGS monitoring and studies. • Above text: https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608 • Right Image and text: https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608) Population (A) and ground-water withdrawals (B) by county, 1995, in States along the Atlantic coast of the United States. More than two-thirds of the population of these States live in coastal counties, defined as having at least 15 percent of their land area in a coastal watershed (National Oceanic and Atmospheric Administration, 1998).
  • 13. Groundwater in coastal areas (continued) Because of a growing awareness of the critical role of ground water in sustaining coastal populations, economies, and ecosystems, the time is right to review some of the important water-management issues and scientific principles related to ground water in the Atlantic coastal zone, and to identify some of the scientific and management challenges that lie ahead. This Circular describes the occurrence and flow of freshwater and saltwater in ground-water systems of the Atlantic coastal zone; reviews the causes, modes, and management of saltwater intrusion along the Atlantic coast; and illustrates some of the mechanisms of ground-water discharge and contaminant loading to coastal ecosystems. The Circular also illustrates traditional approaches for monitoring and managing saltwater intrusion, and highlights some of the innovative approaches being used to enhance the sustainability of coastal ground-water resources, such as desalination and aquifer storage and recovery systems. As coastal populations and ground-water use increase, new monitoring and research efforts will be needed to characterize the occurrence and movement of saline ground water in different types of coastal terrains and to better understand linkages between ground-water discharge and quality and the health of coastal ecosystems. The USGS looks forward to continued service to the citizens of the Atlantic coastal zone, providing science to help them manage their water resources. (Text: https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608) Ground-water flow paths in an idealized coastal watershed along the Atlantic coast. Fresh ground water is bounded by saline ground water beneath the bay and ocean. Fresh ground water discharges to coastal streams, ponds, salt marshes, and tidal creeks and directly to the bay and ocean. Image and text: https://pubs.usgs.gov/circ/2003/circ1262/#heading152526608)
  • 14. Depletion of Fossil Water Resources By their very definition fossil water resources will eventually run out one they begin being used. For over 50 years Libya has relied on fossil water supplies that are now dwindling but the prospect of fossil water reserves running out is not limited to the Middle East or northern Africa. Parts of the former USSR, India, China and Mexico all depend on non-renewable water taken from ancient aquifers. In the United States a number of the Great Plains states take a considerable amount of their water from a fossil water aquifer. This water reservoir is the Ogallala Aquifer or the high planes Aquifer. Estimates forecast this aquifer being empty in 25 years. The disruption is likely to be immense as the aquifer covers portions of eight states, and supplies 82% of the drinking water for these states and around 30% of the water used for crop irrigation in the area. (https://www.azocleantech.com/article.aspx?ArticleID=167 Written by AZoCleantechJun 23 2009) http://4.bp.blogspot.com/- CwZ37uwlim8/U_gcAN1D0gI/AAAAAAABGUE/cnAHYYa7U- 0/s1600/waste%2Bfacility.jpg https://s3-us-west-2.amazonaws.com/courses-images-archive-read-only/wp- content/uploads/sites/667/2015/06/22204248/aquifersandwells.gif
  • 15. Alternate Options to Fossil Water • For poor countries there are few options available other than using fossil water supplies. For wealthier nations options include desalination of saltwater from oceans. The problem with this is that fossil water supplies have no regard for international boundaries. Neighboring countries may share an aquifer and one country is unlikely to use the expensive desalination option while its neighbor continues to cheaply extract fossil water. (https://www.azocleantech.com/article.aspx?ArticleID=167 Written by AZoCleantechJun 23 2009) https://upload.wikimedia.org/wikipedia/commons/thu mb/0/01/Faryab-_village_dug_well.JPG/1200px-Faryab- _village_dug_well.JPG https://c2.staticflickr.com/4/3501/3801125543_54f92b0e1e_z.jpg?zz=1
  • 16. Brackish Water • Brackish water is water having more salinity than freshwater, but not as much as seawater. It may result from mixing seawater with fresh water together, as in estuaries, or it may occur in brackish fossil aquifers. https://wikiislam.net/wiki/images/thumb/a/a1/Estuary.jpg/400px- Estuary.jpg https://lh3.googleusercontent.com/FwiQcXNV7-JcDQikxtqQbZCd7K1- 3mYMjstHksI7PWUccJ4uaC5rI-D1jE1FIrmssEz55pk=s128
  • 17. Desalinization is an expensive process that poorer countries cannot afford. • Desalination is a process that takes away mineral components from saline water. More generally, desalination refers to the removal of salts and minerals from a target substance, as in soil desalination, which is an issue for agriculture. ( https://en.wikipedia.org/wiki/Desalination) https://www.e-education.psu.edu/earth111/sites/www.e- education.psu.edu.earth111/files/Module10/TampaBayDesalinationPlantProce ss_HR.jpeg https://i0.wp.com/www.middleeastmonitor.com/wp-content/uploads/2018/01/Desalination-Plant2- e1516544826721.jpg?resize=1200%2C800&quality=75&strip=all&ssl=1
  • 18. Desalinization • Desalination is a process that takes away mineral components from saline water. More generally, desalination refers to the removal of salts and minerals from a target substance, as in soil desalination, which is an issue for agriculture. • Saltwater is desalinated to produce water suitable for human consumption or irrigation. The by-product of the desalination process is brine. Desalination is used on many seagoing ships and submarines. Most of the modern interest in desalination is focused on cost-effective provision of fresh water for human use. Along with recycled wastewater, it is one of the few rainfall-independent water sources. • Due to its energy consumption, desalinating sea water is generally more costly than fresh water from rivers or groundwater, water recycling and water conservation. However, these alternatives are not always available and depletion of reserves is a critical problem worldwide. Desalination processes are usually driven by either thermal (in the case of distillation) or electrical (e.g., photovoltaic or wind power) as the primary energy types. • Currently, approximately 1% of the world's population is dependent on desalinated water to meet daily needs, but the UN expects that 14% of the world's population will encounter water scarcity by 2025. Desalination is particularly relevant in dry countries such as Australia, which traditionally have relied on collecting rainfall behind dams for water. • Kuwait produces a higher proportion of its water than any other country, totaling 100% of its water use. (Story from Wikipedia: https://en.wikipedia.org/wiki/Desalination)