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Esoterica

rainbowbuttcake

iseultafire:

Sooooo, there might be snow when I get to France.

(via deliciouskaek)

flickr.com
splitminded:

01_TylerStableford (by Telluride Photo Festival)

splitminded:

01_TylerStableford (by Telluride Photo Festival)

cornersoftheworld
cornersoftheworld:

Moon Mountain, Yangshuo, Guangxi, China

cornersoftheworld:

Moon Mountain, Yangshuo, Guangxi, China

(via notime4yourshit)

behance.net

kilele:

“Using Your Head”

Photos by Jennifer Emick, taken in Ghana

Top: Accra,Ghana

Bottom: Takadori, Ghana

(via )

Flickr / adam_gibbon
fyeahafrica:

Tea farms in Rwanda (Photo by Adam Gibbon)

Tea growing in Rwanda started in 1952. Since its introduction, tea production has increased steadily, from 60 tons of black tea in 1958, to 1,900 tons in 1990, to 14,500 tons in 2000, reaching a peak of 17,800 tons in 2001.Over 90% of the production is exported, but represents only a small share of the total volume traded in the international market, which is about 1.4 million tons.
Rwanda tea is planted on hillsides at high altitude (between 1,900 and 2,500 m), and on well drained marshes at an altitude of between 1,550 and 1,800 m. Tea is grown on 11 estates. A total area of approximately 12,500 ha is planted in the Northern,western and Southern province. Tea plantations must be located near a tea factory because the harvest must be processed within a few hours of picking.

[source]

via kilele

fyeahafrica:

Tea farms in Rwanda (Photo by Adam Gibbon)

Tea growing in Rwanda started in 1952. Since its introduction, tea production has increased steadily, from 60 tons of black tea in 1958, to 1,900 tons in 1990, to 14,500 tons in 2000, reaching a peak of 17,800 tons in 2001.Over 90% of the production is exported, but represents only a small share of the total volume traded in the international market, which is about 1.4 million tons.

Rwanda tea is planted on hillsides at high altitude (between 1,900 and 2,500 m), and on well drained marshes at an altitude of between 1,550 and 1,800 m. Tea is grown on 11 estates. A total area of approximately 12,500 ha is planted in the Northern,western and Southern province. Tea plantations must be located near a tea factory because the harvest must be processed within a few hours of picking.

[source]

via kilele

(via )

Flickr / rasone
jorrty:

Frozen Abiqua (by Jesse Estes)

jorrty:

Frozen Abiqua (by Jesse Estes)

Flickr / svetlaaa
thenakedbrowneye:

**—****-***-*-*-*-*-*-*-*-*-*-********—-*** (by shtremulator)

thenakedbrowneye:

**—****-***-*-*-*-*-*-*-*-*-*-********—-*** (by shtremulator)

fantasyscapes

Evanescent sunrise by `AquaSixio

Evanescent sunrise by `AquaSixio

Flickr / franzj
sav3mys0ul:

fire ladder (by franzj)

sav3mys0ul:

fire ladder (by franzj)

Flickr / lichtjahre
theworldwelivein:

The Spirit of Iceland | Svínafellsjökull glacier, Skaftafell, Southern Iceland, Europe©  www.lichtjahre.eu
Photographer notes:Dramatic cloud sceneries with stray sun light are typical for Iceland. Such unique moods of the light arise from low elevation sunlight not reaching the ground that falls through broken multi-layered cloud decks. This indirect light is causing different hues and light intensities at the surface. The black hills in the background belong to the 330 ft (100 m) high terminal moraine of Svínafellsjökull glacier in Skaftafell, southern Iceland. The moraine is composed out of volcanic breccia eroded by the glacier from the surrounding mountains. The steep ice fall of Svínafellsjökull follows gravity at a speed of 3.3 ft (1 m) per day. Hence, the ice of the bordering glacial lake, that is up to 1.3 ft (40 cm) thick, is steeply piled up at the terminal moraine. This glacial drift of 0.4 inch (1 cm) within 15 minutes causes the ice of the glacier and the ice on the lake to crack constantly under this immense pressure. A multitude of tension cracks form within the ice. This produces a stunning network of parallel aligning white lines. The cracking sounds produced by the drifting ice, the harsh winter conditions at 17°F (-8°C) and chilly winds together with the impressive light situation made this experience on the ice unforgettable. 

theworldwelivein:

The Spirit of Iceland | Svínafellsjökull glacier, Skaftafell, Southern Iceland, Europe
©  www.lichtjahre.eu

Photographer notes:
Dramatic cloud sceneries with stray sun light are typical for Iceland. Such unique moods of the light arise from low elevation sunlight not reaching the ground that falls through broken multi-layered cloud decks. This indirect light is causing different hues and light intensities at the surface. The black hills in the background belong to the 330 ft (100 m) high terminal moraine of Svínafellsjökull glacier in Skaftafell, southern Iceland. The moraine is composed out of volcanic breccia eroded by the glacier from the surrounding mountains. The steep ice fall of Svínafellsjökull follows gravity at a speed of 3.3 ft (1 m) per day. Hence, the ice of the bordering glacial lake, that is up to 1.3 ft (40 cm) thick, is steeply piled up at the terminal moraine. This glacial drift of 0.4 inch (1 cm) within 15 minutes causes the ice of the glacier and the ice on the lake to crack constantly under this immense pressure. A multitude of tension cracks form within the ice. This produces a stunning network of parallel aligning white lines. The cracking sounds produced by the drifting ice, the harsh winter conditions at 17°F (-8°C) and chilly winds together with the impressive light situation made this experience on the ice unforgettable.