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  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop10.jpg
  • Black sand beach in Hana Bay on the northeast coast of Maui, in the town of Hana.<br />
.....<br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    HanaBlackSandBeach1.jpg
  • Red sand beach in Hana, Maui, Hawaii<br />
..... <br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Wailuku is the seat of Maui County and is the third-largest CDP as of 2010. Other significant places include Kīhei (including Wailea and Makena in the Kihei Town CDP, which is the second-most-populated CDP in Maui); Lahaina (including Kāʻanapali and Kapalua in the Lahaina Town CDP); Makawao; Pāʻia; Kula; Haʻikū; and Hāna. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    HanaRedSandBeach1.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles2.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles2.jpg
  • Death Valley is a desert valley located in Eastern California. Situated within the Mojave Desert, it is the lowest and driest area in North America. The Mesquite Flat Sand Dunes are at the northern end of the valley floor and are nearly surrounded by mountains on all sides. Due to their easy access from the road and the overall proximity of Death Valley to Hollywood, these dunes have been used to film sand dune scenes for several movies including films in the Star Wars series. The largest dune is called Star Dune and is relatively stable and stationary because it is at a point where the various winds that shape the dunes converge. The depth of the sand at its crest is 130–140 feet but this is small compared to other dunes in the area that have sand depths of up to 600–700 feet deep.<br />
<br />
The primary source of the dune sands is probably the Cottonwood Mountains which lie to the north and northwest. The tiny grains of quartz and feldspar that form the sinuous sculptures that make up this dune field began as much larger pieces of solid rock.<br />
<br />
In between many of the dunes are stands of creosote bush and some mesquite on the sand and on dried mud, which used to cover this part of the valley before the dunes intruded (mesquite was the dominant plant here before the sand dunes but creosote does much better in the sand dune conditions).<br />
<br />
Located near the border of California and Nevada, in the Great Basin, east of the Sierra Nevada mountains, Death Valley constitutes much of Death Valley National Park and is the principal feature of the Mojave and Colorado Deserts Biosphere Reserve. It is located mostly in Inyo County, California. It runs from north to south between the Amargosa Range on the east and the Panamint Range on the west; the Sylvania Mountains and the Owlshead Mountains form its northern and southern boundaries, respectively.
    DeathValleyDuneAndSky1-LAB.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei4.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop13.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop5.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop2.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei17.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop26.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei15.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei9.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei8.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei7.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei6.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei5.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei3.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei2.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei1.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop29.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop16.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop6.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop4.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop11.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop21.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop20.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop19.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop14.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop9.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop15.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop1.jpg
  • Sand dunes at Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles4.jpg
  • Sand dunes at Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles4.jpg
  • Sand dune in Guadalupe Mountains National Park in west Texas
    GuadalupeDune-Vertical.jpg
  • Black sand beach in Waianapanapa State Park, Maui, Hawaii<br />
.....<br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    Waianapanapa1.jpg
  • Black sand beach and palm trees in Hana Bay on the northeast coast of Maui, in the town of Hana.
    HanaPalmTrees2-2.jpg
  • Raabjerg Mile is a migrating coastal dune between Skagen and Frederikshavn, Denmark. It is the largest moving dune in Northern Europe with an area of around 1 km² (0.4 mi²) and a height of 40 m (130 ft). The dune contains a total of 4 million m³ of sand.
    SkagenRaabjergDunes2.jpg
  • Raabjerg Mile is a migrating coastal dune between Skagen and Frederikshavn, Denmark. It is the largest moving dune in Northern Europe with an area of around 1 km² (0.4 mi²) and a height of 40 m (130 ft). The dune contains a total of 4 million m³ of sand.
    SkagenRaabjergDunes1.jpg
  • Sand dune in Guadalupe Dune in western Texas
    GuadalupeDune-Horizontal-New2.jpg
  • Black sand beach in Hana Bay on the northeast coast of Maui, in the town of Hana.<br />
.....<br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    HanaPalmTrees3.jpg
  • Black sand beach in Hana Bay on the northeast coast of Maui, in the town of Hana.<br />
.....<br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    HanaPalmTrees2.jpg
  • Black sand beach in Hana Bay on the northeast coast of Maui, in the town of Hana.<br />
.....<br />
The island of Maui is the second-largest of the Hawaiian Islands and is the 17th largest island in the United States. Maui is part of the State of Hawaii and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. Native Hawaiian tradition gives the origin of the island's name in the legend of Hawaiʻiloa, the navigator credited with discovery of the Hawaiian Islands. According to that legend, Hawaiʻiloa named the island of Maui after his son, who in turn was named for the demigod Māui. The earlier name of Maui was ʻIhikapalaumaewa. The Island of Maui is also called the "Valley Isle" for the large isthmus between its northwestern and southeastern volcanoes and the numerous large valleys carved into both mountains.
    HanaPalmTrees4.jpg
  • Flamingos are a type of wading bird in the genus Phoenicopterus, the only genus in the family Phoenicopteridae. There are four flamingo species in the Americas and two species in the Old World. Flamingos often stand on one leg, the other leg tucked beneath the body. The reason for this behaviour is not fully understood. Recent research indicates that standing on one leg may allow the birds to conserve more body heat, given that they spend a significant amount of time wading in cold water. However, the behaviour also takes place in warm water. As well as standing in the water, flamingos may stamp their webbed feet in the mud to stir up food from the bottom.
    FlamingoPanorama-5.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei9.jpg
  • Flamingos are a type of wading bird in the genus Phoenicopterus, the only genus in the family Phoenicopteridae. There are four flamingo species in the Americas and two species in the Old World. Flamingos often stand on one leg, the other leg tucked beneath the body. The reason for this behaviour is not fully understood. Recent research indicates that standing on one leg may allow the birds to conserve more body heat, given that they spend a significant amount of time wading in cold water. However, the behaviour also takes place in warm water. As well as standing in the water, flamingos may stamp their webbed feet in the mud to stir up food from the bottom.
    FlamingoPanorama-3.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    SossusvleiFromAbove7.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei2.jpg
  • Flamingos are a type of wading bird in the genus Phoenicopterus, the only genus in the family Phoenicopteridae. There are four flamingo species in the Americas and two species in the Old World. Flamingos often stand on one leg, the other leg tucked beneath the body. The reason for this behaviour is not fully understood. Recent research indicates that standing on one leg may allow the birds to conserve more body heat, given that they spend a significant amount of time wading in cold water. However, the behaviour also takes place in warm water. As well as standing in the water, flamingos may stamp their webbed feet in the mud to stir up food from the bottom.
    FlyingFlamingos2.jpg
  • Flamingos are a type of wading bird in the genus Phoenicopterus, the only genus in the family Phoenicopteridae. There are four flamingo species in the Americas and two species in the Old World. Flamingos often stand on one leg, the other leg tucked beneath the body. The reason for this behaviour is not fully understood. Recent research indicates that standing on one leg may allow the birds to conserve more body heat, given that they spend a significant amount of time wading in cold water. However, the behaviour also takes place in warm water. As well as standing in the water, flamingos may stamp their webbed feet in the mud to stir up food from the bottom.
    MarchingFlamingoes2.jpg
  • San Francisco's Golden Gate Bridge from Baker Beach
    SanFranciscoBakerBeach1.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach12.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach4.jpg
  • The Manhattan Beach Pier is a pier located in Manhattan Beach, California, on the coast of the Pacific Ocean. The pier is 928 feet long and located at the end of Manhattan Beach Boulevard. An octagonal Mediterranean-style building sits at the end of the pier and houses the Roundhouse Marine Studies Lab & Aquarium. Surfers can be seen below the pier and sometimes weave in and out of the mussel-covered pilings. The pier is popular with locals, tourists, photographers, and artists and for fishing. It offers sunsets and vantage points from the shore and hillside. In 1897, the Potencia Company was incorporated to develop land in the area and proposed a seaside resort with wharves and piers. The area was named Potencia, but the city of Manhattan was incorporated in 1912 with the word "Beach" being added in 1927. The name was chosen by land developer John Merrill[disambiguation needed], a native of New York. A pier is believed to have been one of the first features built when the Manhattan Beach community was developed. Two wooden piers were built in 1901, one at Center Street (later renamed Manhattan Beach Boulevard) and one at Marine Avenue called Peck's Pier and Pavilion.
    ManhattanPierUnder1.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach7.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach13.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach6.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach3.jpg
  • The Manhattan Beach Pier is a pier located in Manhattan Beach, California, on the coast of the Pacific Ocean. The pier is 928 feet long and located at the end of Manhattan Beach Boulevard. An octagonal Mediterranean-style building sits at the end of the pier and houses the Roundhouse Marine Studies Lab & Aquarium. Surfers can be seen below the pier and sometimes weave in and out of the mussel-covered pilings. The pier is popular with locals, tourists, photographers, and artists and for fishing. It offers sunsets and vantage points from the shore and hillside. In 1897, the Potencia Company was incorporated to develop land in the area and proposed a seaside resort with wharves and piers. The area was named Potencia, but the city of Manhattan was incorporated in 1912 with the word "Beach" being added in 1927. The name was chosen by land developer John Merrill[disambiguation needed], a native of New York. A pier is believed to have been one of the first features built when the Manhattan Beach community was developed. Two wooden piers were built in 1901, one at Center Street (later renamed Manhattan Beach Boulevard) and one at Marine Avenue called Peck's Pier and Pavilion.
    ManhattanPierUnder2.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach15.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach14.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach1.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach6.jpg
  • The Manhattan Beach Pier is a pier located in Manhattan Beach, California, on the coast of the Pacific Ocean. The pier is 928 feet long and located at the end of Manhattan Beach Boulevard. An octagonal Mediterranean-style building sits at the end of the pier and houses the Roundhouse Marine Studies Lab & Aquarium. Surfers can be seen below the pier and sometimes weave in and out of the mussel-covered pilings. The pier is popular with locals, tourists, photographers, and artists and for fishing. It offers sunsets and vantage points from the shore and hillside. In 1897, the Potencia Company was incorporated to develop land in the area and proposed a seaside resort with wharves and piers. The area was named Potencia, but the city of Manhattan was incorporated in 1912 with the word "Beach" being added in 1927. The name was chosen by land developer John Merrill[disambiguation needed], a native of New York. A pier is believed to have been one of the first features built when the Manhattan Beach community was developed. Two wooden piers were built in 1901, one at Center Street (later renamed Manhattan Beach Boulevard) and one at Marine Avenue called Peck's Pier and Pavilion.
    BeachKids1.jpg
  • Folly Beach is a city located on Folly Island in Charleston County, South Carolina, United States. Folly Beach is within the Charleston-North Charleston-Summerville metropolitan area and the Charleston-North Charleston Urbanized Areas. <br />
Folly Beach is located 11 miles south of downtown Charleston along the Atlantic Ocean. <br />
<br />
Known to Charleston locals as "the Edge of America", Folly Beach is home to numerous surf spots, the most popular being the Washout, 10th Street and the Folly Beach Pier. Despite its usually calm conditions, Folly Beach has gained prominence as one of the more popular surf spots along the East Coast. Folly Beach is an eclectic beach community with surf shops, restaurants, gift shops, offices, and bars along Center Street; the main road and gateway to the community.<br />
<br />
Endangered North Atlantic right whales, the state animal of Georgia and South Carolina migrate along the coast during the migration seasons. Folly Island was named after its coastline which was once densely packed with trees and undergrowth, as the Old English name for such an area was “Folly.” The first official document that mentions the island is a land grant from King William III to William Rivers that dates to September 9, 1696.
    FollyBeach1.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach8.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach2.jpg
  • The Manhattan Beach Pier is a pier located in Manhattan Beach, California, on the coast of the Pacific Ocean. The pier is 928 feet long and located at the end of Manhattan Beach Boulevard. An octagonal Mediterranean-style building sits at the end of the pier and houses the Roundhouse Marine Studies Lab & Aquarium. Surfers can be seen below the pier and sometimes weave in and out of the mussel-covered pilings. The pier is popular with locals, tourists, photographers, and artists and for fishing. It offers sunsets and vantage points from the shore and hillside. In 1897, the Potencia Company was incorporated to develop land in the area and proposed a seaside resort with wharves and piers. The area was named Potencia, but the city of Manhattan was incorporated in 1912 with the word "Beach" being added in 1927. The name was chosen by land developer John Merrill[disambiguation needed], a native of New York. A pier is believed to have been one of the first features built when the Manhattan Beach community was developed. Two wooden piers were built in 1901, one at Center Street (later renamed Manhattan Beach Boulevard) and one at Marine Avenue called Peck's Pier and Pavilion.
    ManhattanPier1.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach11.jpg
  • Edisto Island is one of South Carolina's Sea Islands, the larger part of which lies in Charleston County, with its southern tip in Colleton County. The town of Edisto Beach is in Colleton County, while the Charleston County part of the island is unincorporated.<br />
<br />
The island, town, and Edisto River are named after the historic Edistow people, a Native American sub-tribe of the Cusabo Indians, who inhabited the island as well as nearby mainland areas.
    EdistoIslandBeach5.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach4.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    _Y6A4829.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    _Y6A4825.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach9.jpg
  • Charleston is the oldest and largest city in the U.S. state of South Carolina, known for its large role in the American slave trade. The city is the county seat of Charleston County, and the principal city in the Charleston–North Charleston–Summerville Metropolitan Statistical Area. The city lies just south of the geographical midpoint of South Carolina's coastline and is located on Charleston Harbor, an inlet of the Atlantic Ocean formed by the confluence of the Ashley, Cooper, and Wando rivers. <br />
<br />
Charleston was founded in 1670 as Charles Town, honoring King Charles II of England. Its initial location at Albemarle Point on the west bank of the Ashley River (now Charles Towne Landing) was abandoned in 1680 for its present site, which became the fifth-largest city in North America within ten years. One of the key cities in the British colonization of the Americas, Charles Town played a major role in the slave trade, which laid the foundation for the city's size and wealth, and was dominated by a slavocracy of plantation owners and slave traders. Independent Charleston slave traders like Joseph Wragg were the first to break through the monopoly of the Royal African Company, pioneering the large-scale slave trade of the 18th century. Historians estimate that "nearly half of all Africans brought to America arrived in Charleston", most at Gadsden's Wharf. Despite its size, it remained unincorporated throughout the colonial period; its government was handled directly by a colonial legislature and a governor sent by London, UK. Election districts were organized according to Anglican parishes, and some social services were managed by Anglican wardens and vestries. Charleston adopted its present spelling with its incorporation as a city in 1783 at the close of the Revolutionary War. Population growth in the interior of South Carolina influenced the removal of the state government to Columbia in 1788, but the port city remained among the ten largest cities in the United S
    FollyBeach5.jpg
  • First light at Yei-bi-Chai rocks in Monument Valley
    MonumentValleyYeibicheiSunrise2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo2.jpg
  • _A1A6268.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei13.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei8.jpg
  • Starfish on a rock in Olympic national park at low tide, near Point of the Arches
    PointOfArchesSeastars2.jpg
  • Sunset at Second Beach in Washington state's Olympic National Park<br />
.....<br />
Olympic National Park is a United States national park located in the state of Washington, on the Olympic Peninsula. The park has four basic regions: the Pacific coastline, alpine areas, the west side temperate rainforest and the forests of the drier east side. Within the park there are three distinct ecosystemswhich are sub-alpine forest and wildflower meadow, temperate forest, and the rugged Pacific Shore. These three different ecosystems are in pristine condition and have outstanding scenery. U.S. President Theodore Roosevelt originally created Mount Olympus National Monument on 2 March 1909. It was designated a national park by President Franklin Roosevelt on June 29, 1938. In 1976, Olympic National Park became an International Biosphere Reserve, and in 1981 it was designated a World Heritage Site. In 1988, Congress designated 95 percent of the park as the Olympic Wilderness.
    SecondBeachSunsetRockPool1.jpg
  • Sunset at Second Beach in Washington state's Olympic National Park<br />
.....<br />
Olympic National Park is a United States national park located in the state of Washington, on the Olympic Peninsula. The park has four basic regions: the Pacific coastline, alpine areas, the west side temperate rainforest and the forests of the drier east side. Within the park there are three distinct ecosystemswhich are sub-alpine forest and wildflower meadow, temperate forest, and the rugged Pacific Shore. These three different ecosystems are in pristine condition and have outstanding scenery. U.S. President Theodore Roosevelt originally created Mount Olympus National Monument on 2 March 1909. It was designated a national park by President Franklin Roosevelt on June 29, 1938. In 1976, Olympic National Park became an International Biosphere Reserve, and in 1981 it was designated a World Heritage Site. In 1988, Congress designated 95 percent of the park as the Olympic Wilderness.
    SecondBeachSunsetReflection1.jpg
  • Canyon wall in Buckskin Gulch, Paria Canyon Wilderness. The Buckskin Gulch, a canyon in southern Utah, is one of the main tributaries of the Paria River, which is itself a minor tributary of the Colorado River. It is the longest and deepest slot canyon in the southwest United States and may very well be the longest in the world. As such it is one of the premier destinations for slot canyon hikers, and receives a high amount of foot traffic.<br />
At over 13 miles (21 km) in length it is often visited in conjunction with the longer Paria Canyon, although some prefer to make a long day trip out of the hike. With a distance of 20 miles (32 km), hiking this canyon in one day is possible. Wire Pass, a short tributary to the Buckskin, is an ideal alternative for a short day hike that still takes hikers through the narrow, curving features that are the hallmark of slot canyons
    BuckskinRoughSea.jpg
  • Cracked earth and bushes in Valley of the Gods, Utah
    ValleyOfTheGods2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapHoodoos2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSky3.jpg
  • _A1A6265.jpg
  • _A1A6250.jpg
  • Jökulsárlón is a large glacial lake in southeast Iceland, on the edge of Vatnajökull National Park. Situated at the head of the Breiðamerkurjökull glacier, it developed into a lake after the glacier started receding from the edge of the Atlantic Ocean. The lake has grown since then at varying rates because of melting of the glaciers. It is now 1.5 kilometres (0.93 mi) away from the ocean's edge and covers an area of about 18 km2 (6.9 sq mi). It recently became the deepest lake in Iceland, at over 248 metres, as glacial retreat extended its boundaries. The size of the lake has increased fourfold since the 1970s. It is considered as one of the natural wonders of Iceland.
    JokulsarlonIceBeach1.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesSunrise1.jpg
  • Sightseeing helicopter in the Namib-Naukluft National Park in Namibia.<br />
<br />
Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    SossusvleiHelicopter1.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei4.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    SossusvleiFromAbove-22.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    SossusvleiFromAbove-19.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    Sossusvlei1-Edit.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    SossusvleiFromAbove8.jpg
  • Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring vleis such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia.<br />
<br />
The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River.
    SossusvleiFromAbove3.jpg
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