Human Generated Data

Title

Badlands on the Wind River, Wyoming
Date

1860s
People

Artist: William Henry Jackson, American 1843 - 1942
Classification

Photographs
Credit Line

Harvard Art Museums/Fogg Museum, Transfer from the Carpenter Center for the Visual Arts, Transferred from Geology Department Library, 2.2002.604

Human Generated Data

Title

Badlands on the Wind River, Wyoming

People

Artist: William Henry Jackson, American 1843 - 1942

Date

1860s

Classification

Photographs

Credit Line

Harvard Art Museums/Fogg Museum, Transfer from the Carpenter Center for the Visual Arts, Transferred from Geology Department Library, 2.2002.604

Machine Generated Data

Tags

Amazon
created on 2022-01-08

Outdoors 94.9
Nature 94
Text 81.8
Page 70.1
Art 69.1
Poster 63.4
Advertisement 63.4
Building 59.3
Countryside 58.3
Ground 57.8
Soil 56.8

Clarifai
created on 2023-10-25

no person 97.8
paper 97.7
art 96.7
nature 95.5
retro 94.6
page 93.9
print 91.1
people 90.6
sepia 89.7
one 89.5
landscape 89.3
antique 89.1
wear 86.8
sepia pigment 85.5
vintage 82.9
dirty 82
sky 81.4
snow 81
outdoors 81
two 79.1

Imagga
created on 2022-01-08

book 32.7
paper 26.8
brass 24.1
page 23.2
texture 22.2
memorial 21.1
text 20.1
envelope 19.5
old 19.5
textured 18.4
vintage 18.2
sand 18
binding 17.3
blank 17.1
structure 16.2
grunge 16.2
frame 15.8
empty 15.5
document 14.8
design 14.6
aged 14.5
product 14.3
retro 13.9
note 13.8
bible 13.7
parchment 13.4
creation 12.8
border 12.7
religion 12.5
pattern 12.3
newspaper 12
rough 11.8
dirty 11.7
open 11.7
space 11.6
prayer 11.6
holy 11.6
religious 11.2
letter 11
desert 11
read 10.6
god 10.5
detail 10.5
landscape 10.4
sheet 10.3
art 10.1
message 10
container 10
travel 9.9
new 9.7
card 9.7
damaged 9.5
antique 9.5
cover 9.2
decorative 9.2
color 8.9
testament 8.9
information 8.9
surface 8.8
pray 8.7
ancient 8.6
worn 8.6
canvas 8.5
writing 8.5
wall 8
material 8
business 7.9
notebook 7.8
manuscript 7.8
rock 7.8
nobody 7.8
torn 7.7
spirituality 7.7
wallpaper 7.7
faith 7.7
communication 7.6
word 7.5
line 7.5
brown 7.4
board 7.3
object 7.3
yellow 7.3
drawing 7.2
shadow 7.2
scenic 7
sky 7

Google
created on 2022-01-08

Plant community 93.8
Mountain 85.5
Natural landscape 84.6
Slope 83.9
Font 82.9
Terrain 81.7
Grass 81.3
Landscape 77.6
Sky 74
Grassland 72.6
Bedrock 70.1
Paper 68.4
Paper product 67.2
Rock 66.3
Outcrop 65.5
History 65.5
Plateau 63
Plant 62
Soil 61.6
Rectangle 60.7

Microsoft
created on 2022-01-08

text 97.9
mountain 78.7
picture frame 13.1

Color Analysis

Categories

Imagga

paintings art 98.4%
streetview architecture 1.1%

Captions

Microsoft
created on 2022-01-08

text 88.7%

Text analysis

Amazon

level
that
the
cutting
which
LANDS
THE
The
PLATE
time
slowly
surface
this
by
occupied
deposited
has
away
done
times
probable
of
In
region.
and
SERIES
ON
well
WIND
were
river
of the
not
view
lake
horizontally
ancient
These
wore
in
no
have a
face of the
stratified
until
probably
cut
which once occupied this region. The soft beds which appear in the foreground
beds
was
soft
There
rose
worn
BAD
action.
" B probable that the level of the lake slowly rose until its surface was well
"
appear
in no river near by now and the cutting of the لاناء has been done in ancient times
BAD LANDS ON THE WIND RIVER. WYOMING
were deposited beneath the waters, which in that time wore away the face of the clid.
These cliffi were probably worn by the waves of a lake
foreground
once
beneath
been
rock.
waves of a
In this view we have a series of cliff cut 6 horizontally stratified rock. There
its
SERIES C PLATE .
near
waters,
by forces not GOW ي action.
ي
we
WYOMING
RIVER.
now
.
C
forces
series
B
clid.
GOW
6
cliffi
cliff
لاناء

Google

pration.of Then the rain, wearing SERIES C. PLATE 1 HAD LANDS ON THE WIND RIVER. WYOMING. In this view we have a series of cliffs cut in horizontally stratiied rock. There is no river near by now, and the cutting of the cliff has been done in ancient times by forces not now in action. These clitfs were probably worn by the waves of a lake which once occupied this region. The soft beds which appear in the foreground were deposited beneath the waters, which in that time wore away the face of the cliff. It is probalile that the level of the lake slowly rose until its surface was well up or the face of the clifs, or perhaps quite above their escarpment, and that the beds which were accumulated on its bottom hid the slope which the waves carved while at their lower level. Finally, owing to a diminstion of the surface of this lake, doc to a decrease of vainfall, or an increase of barrier which pasted it from the sea, the Lakec r owing to a removal of the away the soft beds deposited in the lake more rapidly than those which formed the old cliffs, gradually bared the face of the elifls again. As this went on, the rain furrowed the old cliff as is slhown in the plate. Notice the banded appearance of the beds which form the clifl. This is doe to the dillerence in color of the strata. Notice also the broad valley leading towards the distant snow-clad mountains. This probably was the valley of a river which, in the time of greater rainfall, fell into the lake. Observe the form of the distant mountains sce that their outlines are like those of the cliff summits. These are forms often shown when rocks of nearly even hardness have been gradually worn down by a , frost, and streams Formation of en D La Deslation of he rtor, L -13, 2
pration.of
Then
the
rain,
wearing
SERIES
C.
PLATE
1
HAD
LANDS
ON
THE
WIND
RIVER.
WYOMING.
In
this
view
we
have
a
series
of
cliffs
cut
in
horizontally
stratiied
rock.
There
is
no
river
near
by
now,
and
cutting
cliff
has
been
done
ancient
times
forces
not
now
action.
These
clitfs
were
probably
worn
waves
lake
which
once
occupied
region.
The
soft
beds
appear
foreground
deposited
beneath
waters,
that
time
wore
away
face
cliff.
It
probalile
level
slowly
rose
until
its
surface
was
well
up
or
clifs,
perhaps
quite
above
their
escarpment,
accumulated
on
bottom
hid
slope
carved
while
at
lower
level.
Finally,
owing
to
diminstion
lake,
doc
decrease
vainfall,
an
increase
barrier
pasted
it
from
sea,
Lakec
r
removal
more
rapidly
than
those
formed
old
cliffs,
gradually
bared
elifls
again.
As
went
on,
rain
furrowed
as
slhown
plate.
Notice
banded
appearance
form
clifl.
This
doe
dillerence
color
strata.
also
broad
valley
leading
towards
distant
snow-clad
mountains.
which,
greater
rainfall,
fell
into
lake.
Observe
mountains
sce
outlines
are
like
summits.
forms
often
shown
when
rocks
nearly
even
hardness
down
,
frost,
streams
Formation
en
D
La
Deslation
he
rtor,
L
-13,
2