Inge Johnsson Photography

Show Navigation
  • Portfolio
  • Galleries
    • All Galleries
    • Search
    • Cart
    • Lightbox
    • Client Area
  • Buy artwork at Fine Art America
  • About
  • Contact

Search Results

Refine Search
Match all words
Match any word
Prints
Personal Use
Royalty-Free
Rights-Managed
(leave unchecked to
search all images)
{ 130 images found }

Loading ()...

  • 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
  • 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
  • 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
  • Sossus Dune Lodge is nestled against the low-lying mountains in the Namib-Naukluft National Park, providing guests with breath-taking views across the plains to the surrounding dunes. Built in a village style, the lodge blends in with its surroundings and was built with the utmost care paid to the environment. Falling under the Namibia Wildlife Resorts umbrella, Sossus Dune Lodge is the only lodge that is situated inside of the Namib-Naukluft National Park. This allows guests the benefit of being able to reach Sossusvlei before the sunrises and to leave after the sun sets. After an adventurous day of exploring the area you can sit back and relax in the utmost comfort under the large, expansive African Sky.
    SossusDuneLodge1.jpg
  • Sand dune in Guadalupe Mountains National Park in west Texas
    GuadalupeDune-Vertical.jpg
  • Sand dune in Guadalupe Mountains National Park in west Texas
    GuadalupeDune-Vertical-New2011.jpg
  • Sand dune in Guadalupe Mountains National Park in west Texas
    GuadalupeDune-Vertical-New.jpg
  • Sand dune in Guadalupe Mountains National Park in west Texas
    GuadalupeDune-Vertical-New2011.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.
    SossusvleiFromAbove4.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
  • 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.
    DeathValleyBush.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.
    DeathValleyBush.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.
    SkagenDuneFlowers-1.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
  • 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.
    Deadvlei12.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.
    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.
    Deadvlei4.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
  • 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
  • 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.
    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
  • Sand dune in Guadalupe Dune in western Texas
    GuadalupeDune-Horizontal-New2.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
  • 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
  • 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
  • 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.
    Sossusvlei10.jpg
  • Sand dune in Guadalupe Mountains National Park in west Texas
    GuadalupeDune-Horizontal-New.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.
    Kolmanskop25.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles1.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.
    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.
    SossusvleiFromAbove2.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
  • 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.
    Sossusvlei5.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-23.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.
    SossusvleiFromAbove-17.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.
    SossusvleiFromAbove11.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.
    SossusvleiFromAbove10.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.
    SossusvleiFromAbove5.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.
    Sossusvlei7.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-18.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.
    SossusvleiFromAbove9.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.
    Sossusvlei11.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.
    Sossusvlei6.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
  • 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.
    Sossusvlei7.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.
    SossusvleiFromAbove6.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.
    SossusvleiFromAbove1.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.
    Sossusvlei12.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.
    Sossusvlei3.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles2.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
  • 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
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleySunrise.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
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleyDuneAndSky2-LAB.jpg
  • Sand dunes near Yei-bi-Chai rocks in Monument Valley, AZ
    MonumentValleyTotemPoles2.jpg
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleyDuneAndSky2-LAB.jpg
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleySunrise.jpg
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleyDuneAndSky2-LAB.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.
    FlyingFlamingos1.jpg
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleySunrise.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.
    FlamingoReflections-6.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.
    MarchingFlamingoes1.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.
    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.
    Kolmanskop2.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-Edit.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.
    Kolmanskop22-Edit.jpg
  • Cracked earth and bushes in Valley of the Gods, Utah
    ValleyOfTheGods2.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
  • 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.
    Kolmanskop24.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.
    Kolmanskop3.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.
    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.
    Kolmanskop18.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.
    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.
    Kolmanskop12.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.
    Kolmanskop10.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.
    Kolmanskop7.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
  • Grass and Ripples
    MonumentValleyTotemPolesRipples.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.
    Kolmanskop29.jpg
Next
  • Facebook
  • Twitter
x