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Artist

  • ? 86 (nononononoway) 27

Copyright

  • ? original 1.3M

General

  • ? 1girl 6.6M
  • ? antennae 22k
  • ? bag 250k
  • ? black eyes 258k
  • ? black hair 1.7M
  • ? black suit 13k
  • ? building 67k
  • ? city 28k
  • ? cityscape 19k
  • ? coat 265k
  • ? dragon 30k
  • ? dress 1.5M
  • ? eiffel tower 391
  • ? english text 280k
  • ? european architecture 762
  • ? evening 9.3k
  • ? formal clothes 71k
  • ? france 512
  • ? full body 933k
  • ? hair bun 279k
  • ? handbag 28k
  • ? hands in pockets 27k
  • ? looking afar 17k
  • ? outdoors 600k
  • ? paris 157
  • ? rooftop 5.3k
  • ? satellite dish 677
  • ? scarf 231k
  • ? scenery 58k
  • ? shoes 630k
  • ? single hair bun 77k
  • ? skeleton 10k
  • ? skirt 1.7M
  • ? suit 82k
  • ? sun 23k
  • ? town 3.7k
  • ? white skirt 101k
  • ? wind 57k

Meta

  • ? highres 6.0M

Information

  • ID: 4392381
  • Uploader: RaisinBread »
  • Date: over 4 years ago
  • Approver: nonamethanks »
  • Size: 4.43 MB .jpg (2500x1215) »
  • Source: pixiv.net/artworks/85995802 »
  • Rating: General
  • Score: 13
  • Favorites: 15
  • Status: Active

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Resized to 34% of original (view original)
original drawn by 86_(nononononoway)

Artist's commentary

  • Original
  • BONES IN PARIS

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    RaisinBread
    over 4 years ago
    [hidden]

    the text at the bottom is from the fossil article on wikipedia

    A fossil (from Classical Latin: fossilis, literally "obtained by digging")[1] is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood, oil, coal, and DNA remnants. The totality of fossils is known as the fossil record.

    Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old.[2] The oldest fossils are around 3.48 billion years old[3][4][5] to 4.1 billion years old.[6][7] The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils.

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