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  • 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 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 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 IV
  • 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 XXXIV
  • 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 III
  • 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 XXII
  • 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 XX
  • 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 XVI
  • 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 XIII
  • 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 XI
  • 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 VII
  • 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
  • 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 XXVIII
  • 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 XXV
  • 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 XIX
  • 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 XVII
  • 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 XII
  • 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 X
  • 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 L
  • 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 XLI
  • 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 XIV
  • Saguaro National Park, Tucson. lacey cholla wood
    Cholla Wood
  • Wood storks during nesting season.
    Harris Neck-11.jpg
  • Portrait of a Wood Stork
    Harris Neck-7.jpg
  • Wood_Stork_Landing.jpg
  • Indigenous_Details-24.jpg
  • Wood storks standing in a tree.
    WoodStork Mug 2.jpg
  • Indigenous_Details-17.jpg
  • Indigenous_Details-18.jpg
  • _MG_1438-Edit.jpg
  • Rookery-33.jpg
  • Rookery-30.jpg
  • Rookery-31.jpg
  • Rookery-32.jpg
  • A pair of egrets during nesting season.
    EgretLoversSQ.jpg
  • Egret with mating season plumage.
    Harris Neck-12.jpg
  • A panorama view of the Avenue of Oaks of Retreat Plantation, St. Simons Island, Georgia.  Desaturated.
    AvenuePanorama.jpg
  • Retreat Plantation Avenue of Oaks in the morning mist. St Simons Ialand, Georgia.
    Retreat Avenue
  • Egret bringing a twig for the nest.
    Harris Neck Rookery Egret-3.jpg
  • Hiker on Rough Ridge trail in the Cohutta Wilderness, Chattahoochee National Forest
    HIking&Camping-Lifestyle9.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-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.
    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.
    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-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-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-7.jpg
  • Wood Pond, Harris Neck
  • Cockle Wood Textures
  • Plants and scenes of British Columbia, Canada
    Shell on Wood