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Natural arch developed in chalk & impure chalk in the Cretaceous of Kansas, USA.
This western Kansas landscape consists of chalk badlands and chalk pillars and a natural arch. The rocks are chalks and impure chalks (e.g., argillaceous chalk and chalky shale) that range in color from whitish to light gray to yellowish. Chalk is a biogenic, calcitic, marine sedimentary rock composed of numerous coccolith microfossils (see: www.soes.soton.ac.uk/staff/tt/eh/pics/lith2.gif). Coccoliths are individual calcareous plates that covered a single-celled photosynthetic marine organism called a coccolithophorid (a.k.a. coccolithophore) (see: upload.wikimedia.org/wikipedia/commons/d/d9/Emiliania_hux...). These beds were deposited in the ancient Western Interior Seaway, a section of ocean that existed during parts of the Mesozoic Era in what is now the American and Canadian Great Plains.
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Rock arches are rare erosional features - those developed in chalk beds are even rarer. If a stream goes under an arch, it is known as a natural bridge. If no stream is present, the feature is a natural arch. Along lakeshores, they are called lake arches. Along oceanic coastlines, they are called sea arches. The highest concentration of natural arches on Earth is Arches National Park in eastern Utah.
Stratigraphy: Smoky Hill Chalk Member (a.k.a. Smoky Hills Member), Niobrara Formation, mid-Upper Cretaceous
Locality: Monument Rocks (also known as the Chalk Pyramids), along Gove County Road 16, north of the Smoky Hill River, Gove County, western Kansas, USA (38° 47' 43.24" North latitude, 100° 45' 52.06" West longitude)
ANTALYA, TURKEY - MAY 26: A general view from a session within Midterm Review of the Istanbul Programme of Action at the Titanic Hotel in Antalya, Turkey on May 26, 2016. The Midterm Review conference for the Istanbul Programme of Action for the Least Developed Countries will take place in Antalya, Turkey from 27-29 May 2016. The conference will undertake a comprehensive review of the implementation of the Istanbul Programme of Action by the least developed countries (LDCs) and their development partners and likewise reaffirm the global commitment to address the special needs of the LDCs. Gokhan Balci / Anadolu Agency
Developed with Microdol-X for 9.30 minutes, 1 minute stop and 3 minutes fix. The fixing went wrong, so I had to fix it twice.
Also, a lot of dustspecks gathered on the negatives.
--
This was the last frame of the roll and due to some miswind it got cut. Frame 12.
F/14 at 1/250s
The early morning prayer was followed by various activities to develop fine motor skills among kids. The activities involved tracing in semolina, sticking cotton in the worksheet, crayon doodling, and a lot more. Have a look at how the tiny tots enjoyed doing different activities with their parents and teachers!
Check out below link to get more information about activities in the best preschool in Ahmedabad
www.satelliteschool.in/ Activity
#ECC #ECCActivity #DevelopingFineMotorSkills #SatelliteSchoolForChildren
Natural arch developed in chalk & impure chalk in the Cretaceous of Kansas, USA.
This western Kansas landscape consists of chalk badlands and chalk pillars and a natural arch. The rocks are chalks and impure chalks (e.g., argillaceous chalk and chalky shale) that range in color from whitish to light gray to yellowish. Chalk is a biogenic, calcitic, marine sedimentary rock composed of numerous coccolith microfossils (see: www.soes.soton.ac.uk/staff/tt/eh/pics/lith2.gif). Coccoliths are individual calcareous plates that covered a single-celled photosynthetic marine organism called a coccolithophorid (a.k.a. coccolithophore) (see: upload.wikimedia.org/wikipedia/commons/d/d9/Emiliania_hux...). These beds were deposited in the ancient Western Interior Seaway, a section of ocean that existed during parts of the Mesozoic Era in what is now the American and Canadian Great Plains.
Rock arches are rare erosional features - those developed in chalk beds are even rarer. If a stream goes under an arch, it is known as a natural bridge. If no stream is present, the feature is a natural arch. Along lakeshores, they are called lake arches. Along oceanic coastlines, they are called sea arches. The highest concentration of natural arches on Earth is Arches National Park in eastern Utah.
Stratigraphy: Smoky Hill Chalk Member (a.k.a. Smoky Hills Member), Niobrara Formation, mid-Upper Cretaceous
Locality: Monument Rocks (also known as the Chalk Pyramids), along Gove County Road 16, north of the Smoky Hill River, Gove County, western Kansas, USA (38° 47' 43.24" North latitude, 100° 45' 52.06" West longitude)
cgi.ebay.co.uk/ws/eBayISAPI.dll?ViewItem&item=2508861...
The 16mm cine film Developing Tank appears unused
or if used has been cleaned meticulously.
The ORIGINAL box shows some signs of wear.
The Developing Tank is from Leningrad, Russian / USSR. It has a certificate.
It dates 18 VIII 1964. (That's 18th of August 1964)
The rubber pipes are in really good condition and not porous or brittle at all.
Quite amazing for this age. The Tank itself is almost scratch free, shining
and just looks fantastic. I do not know how to use it. And I am only selling
as I have course fees to pay, so it is a reluctant sale of an object I adore.
If you are interested in the Developing Tank then please see the
collection of youtube videos I made showing it from all angles
www.youtube.com/playlist?list=PL000C1C02C698EBC3
(at the moment I have 8 or so individual short clips of the developing tank,
arranged in a playlist, please check through them on you tube)
You should be able to see how good it looks. I can re-film any aspect of it
if you are interested, so please just get in touch, with questions and suggestions.
I am uploading the youtube videos at the moment, so they may take an hour or
so before they link up correctly.
I hope you will love this item as I did.
check this page it lists lots of tanks for sale in the US and UK, mine is the cheapest: www.super8camera.com/netsearch.php?zoekterm=developing+ta...
21.11.19. Dublin, Ireland. The Irish Penal Reform Trust and the Irish Criminal Bar Association co-host a seminar on Developing Youth Justice: 18-24s in the Criminal Justice System. Main speakers included; David Stanton TD, Minister of State at the Department of Justice and Equality, Senator Lynn Ruane, Dr Laura Janes, Legal Director with the Howard League for Penal Reform, Ian Power, CEO of Community Creations (SpunOut.ie and Crisis Text Line Ireland), Sarah-Jane Judge BL, Barrister and Lecturer and Eddie D’Arcy, CEO of Solas Project. ©Photo by Derek Speirs
First roll developing film at home. Diafine. Results are mixed, a bit dodgy, but promising. Can't wait to try the next roll.
However, I think I have bromide drag. Is that what those lines are on the left side in the sky?
Natural arch developed in chalk & impure chalk in the Cretaceous of Kansas, USA.
This western Kansas landscape consists of chalk badlands and chalk pillars and a natural arch. The rocks are chalks and impure chalks (e.g., argillaceous chalk and chalky shale) that range in color from whitish to light gray to yellowish. Chalk is a biogenic, calcitic, marine sedimentary rock composed of numerous coccolith microfossils (see: www.soes.soton.ac.uk/staff/tt/eh/pics/lith2.gif). Coccoliths are individual calcareous plates that covered a single-celled photosynthetic marine organism called a coccolithophorid (a.k.a. coccolithophore) (see: upload.wikimedia.org/wikipedia/commons/d/d9/Emiliania_hux...). These beds were deposited in the ancient Western Interior Seaway, a section of ocean that existed during parts of the Mesozoic Era in what is now the American and Canadian Great Plains.
Rock arches are rare erosional features - those developed in chalk beds are even rarer. If a stream goes under an arch, it is known as a natural bridge. If no stream is present, the feature is a natural arch. Along lakeshores, they are called lake arches. Along oceanic coastlines, they are called sea arches. The highest concentration of natural arches on Earth is Arches National Park in eastern Utah.
Stratigraphy: Smoky Hill Chalk Member (a.k.a. Smoky Hills Member), Niobrara Formation, mid-Upper Cretaceous
Locality: Monument Rocks (also known as the Chalk Pyramids), along Gove County Road 16, north of the Smoky Hill River, Gove County, western Kansas, USA (38° 47' 43.24" North latitude, 100° 45' 52.06" West longitude)