clysmian:

sistema:

imaballoon:

manwaifu:

platyputopia:

Remember the photosets about abandoned mental asylums, abandoned theme parks and the ghost city of Prypiat? Today I bring you photos about the abandoned island city of Hashima, Japan.

HAAAAAAAAAAAAAAAAAAAASHIIIIIIIIIIIIIIIIIiiiiiiiiiiiiiiiiMAAAAAAAAAAAAAaaaaaaaaaaa

Whenever I see pictures of abandoned areas like this, my first thought isn’t “OH SCARY.”

It’s more, “Hm. What would cause people to abandon a place like this? Why did this happen?” and it makes me think.

Just thought I’d share.

see my first thought is “lets go get some masks so we dont breathe potential asbestos in, put on some protective clothing, and go explore”

I wanna go explore there

(Source: decadentopia)


Io, Jupiter’s most interesting moon.
It is not the Earth but Jupiter’s innermost moon, Io, which is the most volcanically active body in our Solar System. Between 1995 and 2003, the space probe Galileo was able to detect around 120 volcanoes that shoot gas and dust up to a height of 400 kilometres. On average, every one hundred years the material emitted forms an approximately one centimetre thick layer all over Io, so that the surface is continually changing. Lava flows up to 300 kilometres long and with temperatures of 1500 degrees Celsius, containing sulphurous material and melted silicates, run over the surface. Various sulphur compounds are responsible for the reddish-yellow colouration. Where does the energy required for volcanism come from? On its orbit, Io is subject to the influences of the gravitational fields of Jupiter and the neighbouring moons Europa and Ganymede. Together with Io they orbit the planet in resonance – during one Ganymede orbit, Europa orbits Jupiter twice and Io three times. Thus, the three moons are regularly positioned in a line and the two outer moons exert a combined force on Io, their innermost partner. At the same time, Jupiter pulls much more strongly in the opposite direction and this leads to a strong tidal force. One the one hand, this causes an approximately one hundred metre-high bulge in the crust to move across Io’s surface like a flood wave. On the other hand, the interior of the moon is kneaded like dough. In the process, the material heats up so much that it melts and becomes lava, powering explosive volcanoes. 

Io, Jupiter’s most interesting moon.

It is not the Earth but Jupiter’s innermost moon, Io, which is the most volcanically active body in our Solar System. Between 1995 and 2003, the space probe Galileo was able to detect around 120 volcanoes that shoot gas and dust up to a height of 400 kilometres. On average, every one hundred years the material emitted forms an approximately one centimetre thick layer all over Io, so that the surface is continually changing. Lava flows up to 300 kilometres long and with temperatures of 1500 degrees Celsius, containing sulphurous material and melted silicates, run over the surface. Various sulphur compounds are responsible for the reddish-yellow colouration. 

Where does the energy required for volcanism come from? On its orbit, Io is subject to the influences of the gravitational fields of Jupiter and the neighbouring moons Europa and Ganymede. Together with Io they orbit the planet in resonance – during one Ganymede orbit, Europa orbits Jupiter twice and Io three times. Thus, the three moons are regularly positioned in a line and the two outer moons exert a combined force on Io, their innermost partner. At the same time, Jupiter pulls much more strongly in the opposite direction and this leads to a strong tidal force. One the one hand, this causes an approximately one hundred metre-high bulge in the crust to move across Io’s surface like a flood wave. On the other hand, the interior of the moon is kneaded like dough. In the process, the material heats up so much that it melts and becomes lava, powering explosive volcanoes. 

(Source: crownedrose)



headlikeanorange:

A male Six-plumed Bird-of-Paradise tidies up his display area and tries to attract a female.



theparrotmage:

mimejuice:

heavyweaponskawaii:

catbountry:

thisismouseface:

donc-desole:

Part 2 of my dumping of wips ^^

The meatier wips <3

:>

These are lovely.

Medic: What shall we do with him, mein Kuschelbär?

Heavy: (~*Deep Thoughts*~)

Oh boy I love that first one

ggggodd ugh I love desole’s art so much

A theory for the story behind Jim.

Somehow after getting to know this strange earth monkey called Sheila, Dimitri ends up coming across this entity called Jim. However it is surprisingly similar to an experimental interface called J.I.M. (Joint Information Middleware) that helps transmission information between the conscious minds of people. However, the one he encounters is a bit more advanced than what he last saw, and now he’s worried that his presence in Sheila’s life is more intertwined than he thought…


Flafla: Ohoohohoho…. yes.



(Source: colorsoffauna)

11 Free Philip K. Dick Short Stories

technoccult:

beyond lies the wub

Open Culture rounded up 11 Philip K. Dick short stories that you can download for free - legally. It includes his first published story, “Beyond Lies the Wub,” which is also the source for the illustration above.

[[I make a new thread so as not to butt into the RP]]

gentlespy:

sheila—marie:

Nn- ow ow ow. *She can try all she wants to dig her heels into the ground, but she’s still yanked towards him.* 

Well, what the fuck do you want me to call you! Y’don’t like Lettuce, y’don’t like me usin’ your first name, what do you want me to fuckin’ call you!

[Intesifying his grib on her, getting closer to the woman’s face, in a slightly crouched posture, the male tugs her arm up slightly as one would do to a child. ]

You will call me ‘Mister’.

[[……At first I actually read it as “You will call me ‘Master’.”

And I was all:

D’ohohohohohohoh—aww false alarm ]]

¯ stupidsexysniper radioed, "Wot. Wot do yeh want Space man? B{"
--------------------

A hug. UuU

PSST SHEILA

LET ME COMFORT YO BUTT


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