Surface Water
1242 Photos
A pond near paddy field
by
S W G M
Quite flows a river.
by
S W G M
A small stream
by
S W G M
Quite flows a river.
by
S W G M
River
by
S W G M
Sunset on the beach
by
S W G M
Waterbody
by
S W G M
A forest stream
by
S W G M
Sunset in the sea.
Khazan lands
by
Anil Agarwal
by
Anil Agarwal
by
Anil Agarwal
The arid Ladakh region depends on glacier melt for it’s water …
by
Anil Agarwal
The arid Ladakh region depends on glacier melt for it’s water …
by
Anil Agarwal
The arid Ladakh region depends on glacier melt for it’s water …
by
Anil Agarwal
The arid Ladakh region depends on glacier melt for it’s water …
by
Anil Agarwal
The Zing : The entire cultivated area of Ladakh, which stands out …
by
Anil Agarwal
The smaller Zing : The entire cultivated area of Ladakh, which …
by
Anil Agarwal
by
Anil Agarwal
by
Anil Agarwal
by
Anil Agarwal
by
Anil Agarwal
by
Anil Agarwal
by
Anil Agarwal
The arid Ladakh region depends on glaciers melt for it’s water …
by
Anil Agarwal
The arid Ladakh region depends on glaciers melt for it’s water …
by
Anil Agarwal
The arid Ladakh region depends on glaciers melt for it’s water …
by
Anil Agarwal
Indus river
by
Anil Agarwal
Indus river
by
Anil Agarwal
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
The arid Ladakh region depends on glacier melt for it’s water supply. Water is available mainly late in the evening in the streams, and the flow of the streams is much greater late in the summer season. The people of Ladakh have built a system of water reservoirs to meet their water needs. Glaciers melt slowly through the day and fill the streams mainly in late evening. Water is diverted from streams with the help of guiding channels, and towards the evening, it is taken to a small tank, locally known as a Zing. picture shows a Zing.
Surface Water
1242 Photos
The arid Ladakh region depends on glacier melt for it’s water supply. Water is available mainly late in the evening in the streams, and the flow of the streams is much greater late in the summer season. The people of Ladakh have built a system of water reservoirs to meet their water needs. Glaciers melt slowly through the day and fill the streams mainly in late evening. Water is diverted from streams with the help of guiding channels, and towards the evening, it is taken to a small tank, locally known as a Zing. picture shows a Zing.
Surface Water
1242 Photos
The arid Ladakh region depends on glacier melt for it’s water supply. Water is available mainly late in the evening in the streams, and the flow of the streams is much greater late in the summer season. The people of Ladakh have built a system of water reservoirs to meet their water needs. Glaciers melt slowly through the day and fill the streams mainly in late evening. Water is diverted from streams with the help of guiding channels, and towards the evening, it is taken to a small tank, locally known as a Zing. picture shows a Zing.
Surface Water
1242 Photos
The arid Ladakh region depends on glacier melt for it’s water supply. Water is available mainly late in the evening in the streams, and the flow of the streams is much greater late in the summer season. The people of Ladakh have built a system of water reservoirs to meet their water needs. Glaciers melt slowly through the day and fill the streams mainly in late evening. Water is diverted from streams with the help of guiding channels, and towards the evening, it is taken to a small tank, locally known as a Zing. picture shows a Zing.
Surface Water
1242 Photos
The Zing : The entire cultivated area of Ladakh, which stands out like an oasis in a cold, rocky desert, depends on assured irrigation from the waters of melting snow through long, winding streams from the upper mountain reaches. Snow and glaciers melt slowly throughout the day and water is available for irrigation in the late evening. This water collected in tanks, locally called Zing, and used the next day.
Surface Water
1242 Photos
The smaller Zing : The entire cultivated area of Ladakh, which stands out like an oasis in a cold, rocky desert, depends on assured irrigation from the waters of melting snow through long, winding streams from the upper mountain reaches. Snow and glaciers melt slowly throughout the day and water is available for irrigation in the late evening. This water is collected in tanks, locally called Zings, and used the next day.
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
Surface Water
1242 Photos
The arid Ladakh region depends on glaciers melt for it’s water supply. Water is available mainly late in the evening in the streams, and the flow of the streams is much greater late in the summer season. The people of Ladakh have built a system of water reservoirs to meet their water needs . Glaciers melt slowly through the day and fill the streams mainly in late evening. Picture show same stream in morning.
Surface Water
1242 Photos
The arid Ladakh region depends on glaciers melt for it’s water supply. Water is available mainly late in the evening in the streams, and the flow of the streams is much greater late in the summer season. The people of Ladakh have built a system of water reservoirs to meet their water needs . Glaciers melt slowly through the day and fill the streams mainly in late evening. Picture show same stream in morning.
Surface Water
1242 Photos
The arid Ladakh region depends on glaciers melt for it’s water supply. Water is available mainly late in the evening in the streams, and the flow of the streams is much greater late in the summer season. The people of Ladakh have built a system of water reservoirs to meet their water needs . Glaciers melt slowly through the day and fill the streams mainly in late evening. Picture show same stream in morning.
Surface Water
1242 Photos
Indus river
Surface Water
1242 Photos
