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  • 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.
    Ground Leaves
  • Leaves and water reflection abstracts
    Floating Petals I
  • Leaves and water reflection abstracts
    Floating Petals II
  • Leaves and water reflection abstracts
    Autumn Pond Reflections II
  • Leaves and water reflection abstracts
    Autumn Pond Reflections I
  • Frosty Leaves
  • Leaf Fresco IV
  • Hint of Blue
  • Leaf Fresco III
  • Horsetail Ferns
  • leaf Fresco II
  • Green Roma Tomatos grow in an organic garden.
    Organic Gardening-77.tif
  • Lily pads stand above the water in a pond with it's raining.
    Winter_Swamp-1769.JPG
  • Yellow, grean and orange lily pads covered with raindrops float in dark water.
    Winter_Swamp-1834.JPG
  • Tomatos ripen on the vine in an organic garden.
    Organic Gardening-79.tif
  • Green Roma Tomatos grow in an organic garden.
    Organic Gardening-78.tif
  • A radish grow int eh dark soil of an organic garden.
    Organic Gardening-75.tif
  • Fava beans growing in an organic garden.
    Organic Gardening-23.tif
  • Fava beans growing in an organic garden.
    Organic Gardening-21.tif
  • Reaching Branches
  • Abstract lily pads
    X-ray Lily Pod Abstract VII
  • Abstract lily pads
    X-ray Lily Pod Abstract I
  • Images of Fall along the Altamaha River in Southeast Georgia
    Frosty Kayaks
  • 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 the Okefenokee Swamp in  south east Georgia
    Lily Pad Blossom I
  • Images of the Okefenokee Swamp in  south east Georgia
    Lilly Pond Reflections
  • Images of the Okefenokee Swamp in  south east Georgia
    Okefenokee Lily Pad Pond Pattern
  • Images of the Okefenokee Swamp in  south east Georgia
    Lily Pad Light Reflections
  • Colorful lily pads are highlighted by the blue reflection of the sky.
    Winter_Swamp-0290.JPG
  • Fava beans growing in an organic garden.
    Organic Gardening-22.tif
  • Fava beans growing in an organic garden.
    Organic Gardening-20.tif
  • Misty morning on the fairways of the Plantation Course of the Sea Island Golf Resort on St. Simons Island, Georgia
    Misty Golf Fairway II
  • The Avenue of Oaks, Retreat Plantation, St. Simons Island, Georgia
    Retreat Plantation Canal
  • The Avenue of Oaks, Retreat Plantation, St. Simons Island, Georgia
    Plantation Canal
  • The Avenue of Oaks, Retreat Plantation, St. Simons Island, Georgia
    Sweeping Branches
  • Abstract lily pads
    X-ray Lily Pod Abstract VI
  • Abstract lily pads
    X-ray Lily Pod Abstract IV
  • Abstract lily pads
    X-ray Lily Pod Abstract II
  • Abstract lily pads
    X-ray Lily Pod Abstract III
  • Kayaking along the Altamaha River in Southeast Georgia
    Quiet Morning Kayaking
  • Images of Fall along the Altamaha River in Southeast Georgia
    Altamaha Morning Light
  • Images of Fall along the Altamaha River in Southeast Georgia
    Altamaha Morning Shore
  • Images of the Okefenokee Swamp in  south east Georgia
    Lily Pad Blossom III
  • Images of the Okefenokee Swamp in  south east Georgia
    Little Lilly Pads
  • Images of the Okefenokee Swamp in  south east Georgia
    Lilly Pad I
  • Fava beans grow in an organic garden.
    Organic Gardening-37.tif
  • Fava beans growing in an organic garden.
    Organic Gardening-24.tif
  • The Avenue of Oaks, Retreat Plantation, St. Simons Island, Georgia
    Where the Wild Things Are
  • Abstract lily pads
    X-ray Lily Pod Abstract V
  • 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.
    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-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.
    Twilight Dunes-7.jpg
  • Leaves-1.jpg
  • Fall Chattooga Leaves
  • Turning Leaves