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'Alluvial' images and/or videos results

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Images of 'Alluvial' found, 77

 
China / Taiwan: Pepohoan woman and child (Paul Ibis, 1877).

PFH1167108

China / Taiwan: Pepohoan woman and child (Paul Ibis, 1877).

PFH1167108

 
China / Taiwan: A 'Pepohoan' woman of Taiwan with her child (John Thomson, 1871).

PFH1167106

China / Taiwan: A 'Pepohoan' woman of Taiwan with her child (John Thomson, 1871).

PFH1167106

 
China / Taiwan: Map of the distribution of indigenous peoples in Taiwan.

PFH1167109

China / Taiwan: Map of the distribution of indigenous peoples in Taiwan.

PFH1167109

 
China / Taiwan: A 'Pepohoan' mother and child, 1875.

PFH1167107

China / Taiwan: A 'Pepohoan' mother and child, 1875.

PFH1167107

 
Aerial View from Savute Elephant Camp, Chobe National Park and from Eagle Island Camp outside the Moremi Game Reserve, Botswana (photo)

Sergi Reboredo

SRB1202867

Aerial View from Savute Elephant Camp, Chobe National Park and from Eagle Island Camp outside the Moremi Game Reserve, Botswana (photo)

Sergi Reboredo

SRB1202867

 
Aerial View, Savute Elephant Camp and Eagle Island Camp outside the Moremi Game Reserve, Chobe National Park, Botswana (photo)

Sergi Reboredo

SRB1202612

Aerial View, Savute Elephant Camp and Eagle Island Camp outside the Moremi Game Reserve, Chobe National Park, Botswana (photo)

Sergi Reboredo

SRB1202612

 
Aerial Views from Savute Elephant Camp, Chobe National Park and from Eagle Island Camp outside the Moremi Game Reserve, Botswana (photo)

Sergi Reboredo

SRB1202866

Aerial Views from Savute Elephant Camp, Chobe National Park and from Eagle Island Camp outside the Moremi Game Reserve, Botswana (photo)

Sergi Reboredo

SRB1202866

 
A sunset. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arunchal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG798770

A sunset. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arunchal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG798770

 
Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG798771

Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers empty into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG798771

 
China - Yellow River Delta 1989 - China - Yellow River delta in 1989 - The Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. Image obtained by the Landsat 5 satellite in 1989. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat 5 satellite shows the Yellow River Delta at the river mouth in 1989. In 1989, the ri

PIX4659888

China - Yellow River Delta 1989 - China - Yellow River delta in 1989 - The Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. Image obtained by the Landsat 5 satellite in 1989. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development. This natural - color image from Nasa's Landsat 5 satellite shows the Yellow River Delta at the river mouth in 1989. In 1989, the ri

PIX4659888

 
China - Yellow River Delta 2009 - China - Yellow River delta in 2009 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 2009. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development.

PIX4659907

China - Yellow River Delta 2009 - China - Yellow River delta in 2009 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 2009. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal development.

PIX4659907

 
China - Yellow River Delta in 1999 - China - Yellow River delta in 1999 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 1999. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal developmen

PIX4659895

China - Yellow River Delta in 1999 - China - Yellow River delta in 1999 - Huang He is the second longest river in China and the most sediments-loaded river in the world. On his journey from Tibet, he erodes more than a million tons of sediments every year and takes on alluvial or his nickname the Yellow River. It flows into the Yellow Sea, via the Gulf of Bohai, where its delta extends over 36,000 km. In 1996, Chinese engineers derive the river causing a withdrawal of the delta and the formation of a new peninsula to the north. Image obtained by one of the Landsat satellites in 1999. China's Huang He (Yellow River) is the most sediment - filled river on Earth. In the lower reaches, where the current slows, the natural accumulation of sediment in the riverbed has caused the river to change course often in the past. Since the mid-nineteenth century, however, the lower reaches of the river and the delta have been extensively engineered to control flooding and to protect coastal developmen

PIX4659895

 
Fishing boats, on the Brahmaputra river, in Gauhati, Assam, Northeast India. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers fall into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG799741

Fishing boats, on the Brahmaputra river, in Gauhati, Assam, Northeast India. Brahmaputra the major river of Central and South Asia, flows some 1,800 miles, 2,900 kilometers, from its source in the Himalayas to its confluence with the Ganges River, after which the mingled waters of the two rivers fall into the Bay of Bengal. Along its course it passes through the Tibet - Autonomous Region of China, the Indian states of Arun?chal Pradesh and Assam, and Bangladesh. For most of its length, the river serves as an important inland waterway; it is not, however, navigable between the mountains of Tibet and the plains of India. In its lower course, the river is both a creator and a destroyer depositing huge quantities of fertile alluvial soil but also causing disastrous and frequent floods. Source: Britannica online encyclopedia. (photo)

UIG799741

 
Old town of Cuzco where tile roofs dominateMachu Picchu, Peru (photo)

Sergi Reboredo

SRB3584741

Old town of Cuzco where tile roofs dominateMachu Picchu, Peru (photo)

Sergi Reboredo

SRB3584741

 
Peru Machu Picchu (photo)

Sergi Reboredo

SRB3585205

Peru Machu Picchu (photo)

Sergi Reboredo

SRB3585205

 
Cuzco Cathedral in the Plaza de Armas, Machu Pichu, Peru (photo)

Sergi Reboredo

SRB3584740

Cuzco Cathedral in the Plaza de Armas, Machu Pichu, Peru (photo)

Sergi Reboredo

SRB3584740

 
Cuzco Cathedral in the Plaza de Armas, Machu Pichu, Peru (photo)

Sergi Reboredo

SRB3584742

Cuzco Cathedral in the Plaza de Armas, Machu Pichu, Peru (photo)

Sergi Reboredo

SRB3584742

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