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Yay my first french braid... I always thought they were pretty and have always wanted a long one on my back ...Yesterday my friend braided my hair into a single french braid...she is a pro at french braiding ..Hope someday I could braid my own hair :)
Alaska
flows east to Kennicott Glacier (see map)
my lichen photos by genus - www.flickr.com/photos/29750062@N06/collections/7215762439...
my photos arranged by subject, e.g. mountains - www.flickr.com/photos/29750062@N06/collections
Silky scalp Braids. Long as I could get them on this day. Deep wave ends is what she requested, cute n Flawless! www.jehaanstyles.com
Tanana river near Richardson highway.
A braided river consists of a network of river channels separated by small, and often temporary, islands called braid bars.
Alaska, 2011
Call Ashleigh for appts 408 762 9902
*prices vary depending on thickness/length of hair as well as size of the braids and how intricate the design. Conultation recommended.
These are hair designs by Katje Sabin, Chicago IL. Please contact mamagotcha at gee mail dot com if you are interested in hiring Katje to braid or teach.
www.youtube.com/watch?v=kwPZmcgUBJM
Braids - Lemonade Lyrics
I don't want to go out there*
I don't want to know what you're wearing.
There are black diamonds in your eyes,
And just so you know your skin is scaling.
Have you fucked all the stray kids yet?
They're their sleeping in my backyard
They're just looking out for no one.
Except to smoke and have some good fun
with their dogs and wives and new sons,
And they probably never will hug
'cause she's never really found love.
Just a woman who will always love.
Just a unhappy with a man
And what I, and what I found is that we
We're all just sleeping around.
His daughter used to come here
With her daughter and her husband
Now no one sees her husband
'Cause her ass has caught the harvest
And her pants have got a good fill
I know the suns beneath the window sill.
Well I was joking with my lemonade
I told him to get fucked and then get laid.
Now what do you say to a man who's got no taste,
Who's really got no potential
Except to procreate so inessential.
And what I, and what I found is that we
We're all just sleeping around.
All we really want to do is love.
File name: 10_03_002166b
Binder label: Thread
Title: Star braid [back]
Date issued: 1870 - 1900 (approximate)
Physical description: 1 print : chromolithograph ; 7 x 17 cm.
Genre: Advertising cards
Subject: Adults; Ribbons
Notes: Title from item. Retailer: Nelson C. Farr, Littleton, N. H.
Collection: 19th Century American Trade Cards
Location: Boston Public Library, Print Department
Rights: No known restrictions.
Wrangell - St. Elias National Park, Alaska
Geologic Guide to Wrangell–Saint Elias National Park and Preserve, Alaska by Gary R. Winkler
pubs.usgs.gov/pp/p1616/P1616-508.pdf -
The rugged mountain ridges surrounding Kennicott
and Root Glaciers and the canyons of the Chitistone and
Nizina Rivers expose in nearly continuous outcrops the most
characteristic rocks of Wrangellia (fig. 17). The distinctive
maroon-weathering slopes of the Nikolai Greenstone contrast
conspicuously with the light-gray-weathering cliffs and ledges
of the overlying Chitistone and Nizina Limestones. The color
contrast can be seen easily from a distance, and by the late
1800’s, the contact zone had gained the attention of prospec
tors and geologists, who discovered that copper lodes were
concentrated in its proximity. By 1900, the fabulous Bonanza
lode east of Kennicott Glacier had been located. By 1905,
probably every linear foot of the contact zone in the southern
Wrangell Mountains had been scrutinized, where it was acces
sible, and all major known copper deposits of the region had
been staked.
The Nikolai Greenstone (fig. 14) consists of Triassic
basalt flows whose aggregate thickness is nearly 10,000 ft.
The greenstone formed a vast volcanic field; today’s rem
nants cover large tracts on both north and south flanks of
the Wrangell Mountains and the south flank of the eastern
Alaska Range, as well as adjacent parts of Canada at least as
far as the Kluane Lake region. Correlative basalts are known
as far west as the Alaska Peninsula and at least as far east as
the Chilkat Peninsula near Haines, Alaska. Large areas of
Triassic basalt on the Queen Charlotte and Vancouver Islands
in British Columbia, known as the Karmutsen Formation,
probably are offset continuations of the same volcanic field,
although displaced by post-Triassic movement along the
Denali, Queen Charlotte, or other major transcurrent fault
systems. The Nikolai Greenstone was extruded during a 7–8
million year interval onto a mostly subaerial volcanic plateau;
near the perimeters of its outcrops, however, submarine flows
have been identified. Volumetric estimates for the Nikolai
Greenstone exceed a staggering 60,000 mi3, enough to bury
the entire State of Oregon with a quarter mile of basalt! The
Nikolai Greenstone is overlain by as much as 3,600 ft of
Upper Triassic limestone and dolomite in the area between
the Kennicott Glacier and the Chitistone River canyon, but
the carbonate rocks thin rapidly westward, eastward, and
northward. The lower part of the Chitistone Limestone in the
McCarthy area contains stromatolites, relicts of evaporites,
and algal-mat chips, which collectively indicate deposition
in a tidal-flat sabkha environment. Sabkhas are widespread
in the Middle East today. The upper part of the Chitistone
Limestone, and the overlying Nizina Limestone, were depos
ited in progressively deepening seawater, culminating, by
latest Triassic time, in deposition of spiculite, muddy lime-
stone, and shale of the McCarthy Formation. The McCarthy
Formation makes up the thin-bedded, dull-brown-weathering,
slope-forming units above the cliff- and ledge-forming Triassic
limestones throughout the region. Between Kennicott and
Nizina Glaciers, an overlying Jurassic sedimentary succession
more than 5,200 ft thick forms the higher ridges and consists
primarily of marine sandstone, shale, and conglomerate.
Locally, the succession includes spiculite and minor coquina;
some beds contain abundant ammonites and mollusks that
substantiate ages ranging from Early to Late Jurassic. Thin
lava flows and beds of volcanic ash in the Middle and Upper
Jurassic parts of the succession, as well as abundant primary
volcanic detritus in the clastic rocks, indicate arc magmatism
from about 170 to 150 m.y. ago in Wrangellia (the so-called
Chitina arc). Lenses of conglomerate and disconformities
within the upper part of the succession indicate episodic uplift
and subsidence—tectonism that probably is an early manifes
tation of the docking of Wrangellia.
Within the Wrangell–Saint Elias region, this complete
Jurassic sequence occurs only in the McCarthy area; its pres
ence indicates the deepest parts of a depositional basin whose
hydraulic regime may have influenced the genesis of Ken
necott-type copper deposits.
In a few widely scattered localities, remnants of fossilif
erous marine siltstone, shale, and limestone of Middle Triassic
age, as much as 300 ft thick, intervene between the Nikolai
Greenstone and underlying rocks. These strata contain the
distinctive age-diagnostic pelecypod, Daonella, and provide
biostratigraphic timing of the onset of basaltic volcanism rep
resented by the overlying Nikolai Greenstone.
my photos arranged by subject - www.flickr.com/photos/29750062@N06/collections