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  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Watching The Dog
  • Nature images of the North Georgia mountains in the autumn.
    Winter Seed Pods
  • Nature images of the North Georgia mountains in the autumn.
    Flowing Water II
  • Nature images of the North Georgia mountains in the autumn.
    Flowing Water I
  • Nature images of the North Georgia mountains in the autumn.
    ChattoogaForestTrail.jpg
  • Nature images of the North Georgia mountains in the autumn.
    Chattooga Fall Colors V
  • Nature images of the North Georgia mountains in the autumn.
    Chattooga Fall Colors IV
  • Nature images of the North Georgia mountains in the autumn.
    Chattooga Fall Colors I
  • Beach images of Coastal Georgia's Barrier Islands
    Wide Jekyll Beach
  • Beach images of Coastal Georgia's Barrier Islands
    Sunset Sand Pattern II
  • Beach images of Coastal Georgia's Barrier Islands
    Sunset Sand Pattern I
  • Beach images of Coastal Georgia's Barrier Islands
    GIRE_063.jpg
  • Beach images of Coastal Georgia's Barrier Islands
    Jekyll Tide
  • Beach images of Coastal Georgia's Barrier Islands
    GIRE_062
  • Beach images of Coastal Georgia's Barrier Islands
    Jekyll Beach Ramp
  • Beach images of Coastal Georgia's Barrier Islands
    Dune Grass
  • Beach images of Coastal Georgia's Barrier Islands
    Beach Access, Jekyll
  • Beach images of Coastal Georgia's Barrier Islands
    Beach Terns II
  • Beach images of Coastal Georgia's Barrier Islands
    Beach Terns I
  • Beach images of Coastal Georgia's Barrier Islands
    Oat Dunes2.jpg
  • Nature images of the North Georgia mountains in the autumn.
    Chattooga River Rapids
  • Nature images of the North Georgia mountains in the autumn.
    Chattooga Fall Colors II
  • Beach images of Coastal Georgia's Barrier Islands
    GIRE_061
  • Beach images of Coastal Georgia's Barrier Islands
    Twilight Dune
  • Beach images of Coastal Georgia's Barrier Islands
    GIRE_066
  • Beach images of Coastal Georgia's Barrier Islands
    Oat Dune
  • Beach images of Coastal Georgia's Barrier Islands
    Beach Terns III
  • Beach images of Coastal Georgia's Barrier Islands
    BoatandBirds.jpg
  • Nature images of the North Georgia mountains in the autumn.
    Chattooga River Road
  • Images of the Altamaha River, Georgia in Fall View of the Altamaha River in Southeast Georgia
    Through the Leaves
  • Images of the Altamaha River, Georgia in Fall View of the Altamaha River in Southeast Georgia
    Altamaha Kayaker
  • Images of Fall along the Altamaha River in Southeast Georgia
    Yellow Blaze
  • Beach images of Coastal Georgia's Barrier Islands
    Down To The Beach II
  • Images of the Altamaha River, Georgia in Fall View of the Altamaha River in Southeast Georgia
    Yellow Canopy Kayaker
  • Images of the Altamaha River, Georgia in Fall View of the Altamaha River in Southeast Georgia
    Little Sand Bar, Altamaha
  • Images of the Altamaha River, Georgia in Fall View of the Altamaha River in Southeast Georgia
    Gentle Shore, Altamaha
  • Images of the Altamaha River, Georgia in Fall View of the Altamaha River in Southeast Georgia
    Edge of the River
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Can I Help You?
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Hang'in Out
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Turtle Extruder
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    The Crew
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Misty Shrimpers
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    The Watcher
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Dilapidated Dock I
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Ropes n' Sterns
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Bird on a Wire
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    The Skipper II
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Boats In The Mist
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Sunset Shrimpers
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Cobia
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Messy Nets
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Peeling Paint
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    The Orange Door
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Fully Equiped.jpg
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Mesh Mender Net Shop
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Libert Ship Rail
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    The Assistant
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Dry Dock Shed
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Dilapidated Dock 2.jpg
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Sterns In The Mist
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Ropes
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Three in a Row
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Misty Trio
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Pelican Town II
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Dock Gossip
  • A Misty morning on the Shrimp Boat docks of Brunswick, Georgia.  A favorite Brown Pelican hangout.
    Bows and Anchors II
  • Train trestle over the Altamaha River in Southeast Georgia.
    Altamaha Regional Park Bridge I
  • Images of the Altamaha River, Georgia in Fall near Darien.
    Lower Altamaha
  • Images of the Altamaha River, Georgia in Fall.
    Ground Leaves
  • Images of the Altamaha River, Georgia in Fall
    Cypress Roots.jpg
  • Images of the Altamaha River, Georgia in Fall
    Cypress Grove 2.jpg
  • Images of the Altamaha River, Georgia in Fall
    Cypress Grove.jpg
  • Images of the Altamaha River, Georgia in Fall
    Altamaha_RifleKnife2.jpg
  • Images of the Altamaha River in Southeast Georgia in Fall .
    Altamaha Morning Light II
  • Lily pad images of the Altamaha River in Southeast Georgia
    Altamaha Lily Pads
  • Images of the Altamaha River, Georgia in Fall
    Across the River.jpg
  • Kayaking along the Altamaha River in Southeast Georgia
    Quiet Morning Kayaking
  • Images of Fall along the Altamaha River in Southeast Georgia
    Frosty Kayaks
  • Images of Fall along the Altamaha River in Southeast Georgia
    Altamaha Morning Light
  • Images of Fall along the Altamaha River in Southeast Georgia
    Altamaha Still Morning
  • Images of Fall along the Altamaha River in Southeast Georgia
    Altamaha Fall Shore
  • Images of Fall along the Altamaha River in Southeast Georgia
    Altamaha Morning Shore
  • Images of the Altamaha River, Georgia in Fall
    Investigating.jpg
  • Images of the Altamaha River, Georgia in Fall
    IMG_6037.JPG
  • Images of the Altamaha River, Georgia in Fall
    AltamahaCyressShore_4.jpg
  • Images of Fall along the Altamaha River in Southeast Georgia
    Altamaha Misty Morning
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    Twilight Dunes-5.jpg
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    GIRE_067.jpg
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    Twilight Dunes-4.jpg
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    Twilight Dunes-10.jpg
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    Twilight Dunes-9.jpg
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    Twilight Dunes-8.jpg
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    GIRE_068.jpg
  • Coastal sand dunes are dynamic but fragile buffer zones of sand and vegetation that form where the following three characteristics can be found:<br />
large quantities of sand<br />
persistent wind capable of moving the sand<br />
suitable locations for sand to accumulate<br />
The process of dune formation begins with a steady on-shore wind capable of moving sand. The wind moves the sand into piles. Eventually the sand pile becomes so steep that the leeward side of the sand pile collapses under its own weight and spills down at an angle that serves to stabilize the dune. Over time, the dune migrates in the direction of the wind, as the wind moves sand up the dune's slope and over the edge.<br />
Sand dunes often form around obstructions such as rocks, drift wood, decaying plant matter, and detritus that is washed up during high-tide. This decaying plant matter forms a perfect substrate for plants to set root. Plants the first set root in sand dunes are referred to as pioneer plants and are often grasses that have special adaptations for the harsh environment of the dune (high salt tolerance, waxy leaves that retain water, rolled leaves to reduce surface area and exposure to evaporation). These pioneer plants stabilize the dune. Their roots bind the sand and their leaves decrease wind speed and reduce erosion.<br />
After pioneer plants stabilize the dune, it becomes more habitable for other plants to move in. A progression of vegetation types set hold onto the dune, each changing the substrate's characteristics and structure, gradually making the dune suitable for the next vegetation type.<br />
Sand dunes, though dynamic, are fragile habitats. The mat of vegetation covering a dune is vital to reducing dune erosion and if this vegetation is disturbed or uprooted, the dune is destroyed.
    Twilight Dunes-7.jpg
  • Wood Textures and pattern from driftwood found on Blackbeard Island, Georgia USA Weathered wood images from the driftwood beach on Blackbeard Island, Georgia
    Wood Texture LXII
  • Wood Textures and pattern from driftwood found on Blackbeard Island, Georgia USA Weathered wood images from the driftwood beach on Blackbeard Island, Georgia
    Wood Texture LV
  • Wood Textures and pattern from driftwood found on Blackbeard Island, Georgia USA Weathered wood images from the driftwood beach on Blackbeard Island, Georgia
    Wood Texture V
  • Wood Textures and pattern from driftwood found on Blackbeard Island, Georgia USA Weathered wood images from the driftwood beach on Blackbeard Island, Georgia
    Wood Texture XLV
  • Wood Textures and pattern from driftwood found on Blackbeard Island, Georgia USA Weathered wood images from the driftwood beach on Blackbeard Island, Georgia
    Wood Texture XLIV
  • Wood Textures and pattern from driftwood found on Blackbeard Island, Georgia USA Weathered wood images from the driftwood beach on Blackbeard Island, Georgia
    Wood Texture XL
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