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  • Salt marsh grass is lush and green after a storm.
    Morning_Marsh-2363.JPG
  • Salt marsh grass is lush and green after a storm.
    Morning_Marsh-2400.JPG
  • Vibrant green marsh grass lines the edge of a creek in a coastal salt marsh.
    Morning_Marsh-2349.JPG
  • Vibrant green marsh grass lines the edge of a creek in a coastal salt marsh.
    Morning_Marsh-2338.JPG
  • vibrant green marsh grass lines the edge of a creek in a coastal salt marsh.
    Morning_Marsh-2221.JPG
  • High tide covers marsh grass in a coastal salt water marsh along the Atlantic
    Morning_Marsh-2243.JPG
  • Salt marsh grass is lush and green after a storm.
    Morning_Marsh-2245.JPG
  • Vibrant green marsh grass lines the edge of a creek in a coastal salt marsh.
    Morning_Marsh-2265.JPG
  • Vibrant green marsh grass lines the edge of a creek in a coastal salt marsh.
    Morning_Marsh-2381.JPG
  • A great Egret stands in the marsh grass
    Morning_Marsh-2534.JPG
  • Vibrant green marsh grass lines the edge of a creek in a coastal salt marsh.
    Morning_Marsh-2320.JPG
  • Vibrant green marsh grass lines the edge of a creek in a coastal salt marsh.
    Morning_Marsh-2378.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.
    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
  • Beach images of Coastal Georgia's Barrier Islands
    Dune Grass
  • St.Simons Island Bloody Marsh-5.jpg
  • Printed on archival metallic paper.  Print size:  11x14  Framed: 17x21<br />
$380.00
    Critter Prints II.JPG
  • Printed on archival metallic paper.  Print size:  6x9  Framed: 10x13<br />
$180.00
    Critter Prints III.JPG
  • Printed on archival metallic paper.  Print size:  11x14  Framed: 17x21<br />
$380.00
    Critter Prints I.JPG
  • Printed on archival metallic paper.  Print size:  6x9  Framed: 10x13<br />
$180.00
    Critter Prints V.JPG
  • Printed on archival metallic paper.  Print size:  6x9  Framed: 10x13<br />
$180.00
    Critter Prints IV.JPG
  • Beach Grazers
  • Cumberland_Horses_TheGreeting.jpg
  • Beach Trio
  • Printed on archival metallic paper.  Print size:  6x9  Framed: 10x13<br />
$180.00
    Critter Prints VI.JPG
  • The Conversation.jpg
  • Cumberland_Horses_Grazing.jpg
  • Retreat_Avenue.jpg
  • Where_the_Wild_Things_Are.jpg
  • Reaches_Branches.jpg
  • Retreat_Plantation_Canal.jpg
  • A panorama view of the Avenue of Oaks of Retreat Plantation, St. Simons Island, Georgia.  Desaturated.
    AvenuePanorama.jpg
  • Avenue_of_Oaks_Morning.jpg
  • Dead trees stand watch over the edge of a creek in a coastal Salt Marsh on the Southern Atlantic coast.
    Morning_Marsh-2402.JPG
  • A view of the salt marsh from Village Creek Landing on St. Simons Island.
    Winter_Marsh_BW-2566.JPG
  • Palmetto plants line the edge of a coastal salt marsh hammock
    Morning_Marsh-2340.JPG
  • Palmetto plants line the edge of a coastal salt marsh hammock
    Morning_Marsh-2341.JPG
  • Freshwater marsh at the Savannah National Wildlife Refuge.
    SC_Marsh-6956.JPG
  • Palmetto plants line the edge of a coastal salt marsh hammock
    Morning_Marsh-2345.JPG
  • Palmetto plants line the edge of a coastal salt marsh hammock
    Morning_Marsh-2346.JPG
  • Freshwater marsh at the Savannah National Wildlife Refuge.
    SC_Marsh-2.JPG
  • Storm clouds gather over a coastal salt marsh in Georgia.
    Morning_Marsh-2354.JPG
  • Light streams through the couds over a coastal salt marsh on the Atlantic coast.
    Morning_Marsh-2365.JPG
  • A stand of trees on an island or hammock in a salt marsh along the Southern Atlantic Coast.
    Morning_Marsh-2393.JPG
  • Trees stand on a coastal salt marsh hammock.
    Morning_Marsh-2398.JPG
  • Storm clouds gather over a coastal salt marsh in Georgia.
    Morning_Marsh-2411.JPG
  • Retreat Plantation Avenue of Oaks in the morning mist. St Simons Ialand, Georgia.
    Retreat Avenue
  • A misty morning on the fairways of the Plantation Golf Course of the Sea Island Golf Resort.  St. Simons Island, Georgia
    Misty Golf Fairway 1
  • Images of the Altamaha River, Georgia in Fall near Darien.
    Lower Altamaha
  • Beach images of Coastal Georgia's Barrier Islands
    GIRE_061
  • Beach images of Coastal Georgia's Barrier Islands
    Wide Jekyll Beach
  • 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
    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
    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
  • Storm clouds gather over a coastal salt marsh in Georgia.
    Morning_Marsh-2258.JPG
  • Dead trees and great Egret sit at the edge of a coastal salt marsh.
    Morning_Marsh-2302.JPG
  • A treen hangs over the edge a hammock in a coastal salt marsh.
    Morning_Marsh-2322.JPG
  • Storm clouds gather over a coastal salt marsh in Georgia.
    Morning_Marsh-2327.JPG
  • Palmetto plants line the edge of a coastal salt marsh hammock
    Morning_Marsh-2331.JPG
  • The light shines through stormy clouds over a coastal salt marsh.
    Morning_Marsh-2336.JPG
  • A stormy sky threatens a coastal Atlantic Salt marsh
    Morning_Marsh-2339.JPG
  • Freshwater marsh at the Savannah National Wildlife Refuge.
    SC_Marsh-6958.JPG
  • Dead trees stand watch over the edge of a creek in a coastal Salt Marsh on the Southern Atlantic coast.
    Morning_Marsh-2405.JPG
  • A view of the salt marsh from Village Creek Landing on St. Simons Island.
    Morning_Marsh-2566.JPG
  • Misty morning on the fairways of the Plantation Course of the Sea Island Golf Resort on St. Simons Island, Georgia
    Misty Golf Fairway II
  • 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
  • Images of the Okefenokee Swamp in  south east Georgia
    Pine Reflections
  • A small palmetto covered hammock with trees sits in the middle of a salt marsh.
    Morning_Marsh-2342.JPG
  • a view of the salt marsh from Village Creek Landing on St. Simons Island. Looking towards Hampton Marina.
    Morning_Marsh-2553.JPG
  • Beach images of Coastal Georgia's Barrier Islands
    Down To The Beach II
  • Leaf Fresco III
  • Frosty Leaves
  • Leaf Fresco IV
  • Hint of Blue
  • Horsetail Ferns
  • leaf Fresco II
  • Sand and Grass IV
  • Sand and Grass II
  • Sand and Grass I
  • Blades of Grass
  • Grass Texture
  • Sand and Grass V
  • Sand and Grass III