01/31 2012

(via cosmic-dust)

01/31 2012

(Source: yourmomfanclub)

01/31 2012

(Source: yourmomfanclub)

11/22 2011

(Source: 6thwonder)

11/21 2011
That’s Cool!

That’s Cool!

(Source: rrevolver, via smokinacey)

11/09 2011
electronicthroat:

HAPPY BIRTHDAY CARL!
I fucking miss you.

electronicthroat:

HAPPY BIRTHDAY CARL!

I fucking miss you.

(via magalomania)

11/08 2011
theswingingsixties:

Nancy Sinatra

Bang Bang

theswingingsixties:

Nancy Sinatra

Bang Bang

11/08 2011
suicideblonde:

Edward Scissorhands

Awkward Scissorhandz

suicideblonde:

Edward Scissorhands

Awkward Scissorhandz

07/10 2011
06/20 2011

(Source: youngmaslo, via lovegifs)

06/18 2011
lickypickysticky:

Midnight Rhythm Leonid Afremov
If you’ve been around here long enough you know that from time to time I HAVE to post an Afremov.
Art connaisseurs may not find his art high brow, but just like good ol’ Bob Ross I openly admire what he does.
His paintings have a huge feelgood effect on me.

lickypickysticky:

Midnight Rhythm
Leonid Afremov

If you’ve been around here long enough you know that from time to time I HAVE to post an Afremov.

Art connaisseurs may not find his art high brow, but just like good ol’ Bob Ross I openly admire what he does.

His paintings have a huge feelgood effect on me.

(Source: lickypickystickyfree)

06/17 2011
whoarei:

damu

whoarei:

damu

06/15 2011
theswingingsixties:

Twiggy, Twiggy, everywhere.. 

theswingingsixties:

Twiggy, Twiggy, everywhere.. 

06/15 2011
erosart:

Wind by ~y-u-k-i-k-o

erosart:

Wind by ~y-u-k-i-k-o

(via deadgirls)

06/15 2011
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 lickypickystickyfree)

1 of 46