Happyteeth

Happyteeth flashes it's chompers only to the most worthy of creatures. This is not that domain. How dare you seek the elusive beast! Here you will find the trail, the essence, probing bits and bobs of interest approved by our beloved Happyteeth, that may or may not hit close to our respected homes.
cervus-venatio:

Pig trunk (by krelle)

cervus-venatio:

Pig trunk (by krelle)

(via tripudios)

heoro:

Dominican Republic (by skinnie minnie)

heoro:

Dominican Republic (by skinnie minnie)

(via heoro-deactivated20120121)

tokyofantasy:

Naha Harbor DinerThis life-sized rendition of a banyan tree is located in Okinawa, Japan and sits about six meters up, overlooking the ocean. “Accessible by a spiral staircase around back and an in-trunk elevator, the restaurant specializes in locally grown and organic harvested foods fresh from the farm.”

tokyofantasy:

Naha Harbor Diner

This life-sized rendition of a banyan tree is located in Okinawa, Japan and sits about six meters up, overlooking the ocean. “Accessible by a spiral staircase around back and an in-trunk elevator, the restaurant specializes in locally grown and organic harvested foods fresh from the farm.”

(via tokyofantasy-deactivated2011062)

cabbagerose:

Mehmet Ali Uysal: Artist
via: blueverticalstudio

cabbagerose:

Mehmet Ali Uysal: Artist

via: blueverticalstudio

wakannai:

Interesting

wakannai:

Interesting

lickypickysticky:

This up to 1000 years old snow has metamorphosed into highly pressurized glacier ice that contains almost no air bubbles. Thus it absorbs the visible light despite the scattered shortest blue fraction, giving it its distinct deep blue waved appearance. This cavity in the glacier ice formed as a result of a glacial mill, or moulin.
Rain and meltwater on the glacier surface is channelled into streams that enter the glacier at crevices. The waterfall melts a hole into the glacier while the ponded water drains towards lower elevations by forming long ice caves with an outlet at the terminus of the glacier. The fine grained sediments in the water along with wind blown sediments cause the frozen meltwater stream to appear in a muddy colour while the top of the cave exhibits the deep blue colour.
Due to the fast movement of the glacier of about 1 m per day over uneven terrain this ice cave cracked up at its end into a deep vertical crevice, called cerrac. This causes the indirect daylight to enter the ice cave from both ends resulting in homogeneous lighting of the ice tunnel.

lickypickysticky:

This up to 1000 years old snow has metamorphosed into highly pressurized glacier ice that contains almost no air bubbles. Thus it absorbs the visible light despite the scattered shortest blue fraction, giving it its distinct deep blue waved appearance. This cavity in the glacier ice formed as a result of a glacial mill, or moulin.

Rain and meltwater on the glacier surface is channelled into streams that enter the glacier at crevices. The waterfall melts a hole into the glacier while the ponded water drains towards lower elevations by forming long ice caves with an outlet at the terminus of the glacier. The fine grained sediments in the water along with wind blown sediments cause the frozen meltwater stream to appear in a muddy colour while the top of the cave exhibits the deep blue colour.

Due to the fast movement of the glacier of about 1 m per day over uneven terrain this ice cave cracked up at its end into a deep vertical crevice, called cerrac. This causes the indirect daylight to enter the ice cave from both ends resulting in homogeneous lighting of the ice tunnel.

(via lickystickypickywe)