View allAll Photos Tagged wrb
A representative soil profile of the Ditton series in England. (Cranfield University 2022. The Soils Guide. Available: www.landis.org.uk. Cranfield University, UK.)
These soils are loamy or clayey with an ordinary clay-enriched subsoil. They have dominantly brownish or reddish subsoils and no prominent mottling or greyish colours (gleying) above 40 cm depth. Most are in agricultural use.
For more information on the World Reference Base soil classification system, visit:
www.fao.org/3/i3794en/I3794en.pdf
For more information about this soil, visit:
:D
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This is about as spectacular (far from it) as it's gonna get today. Super muggy outside.. blah colors, no blue sky.. crappy pictures!
*View LARGE* It's so sharp =)
Malibu beach.
Resubmitted for the 2nd time --> Fixed that pesky pole. Hope everyone is finally happy with this version haha :)
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Prints for sale! Anything on flickr is up for grabs. Please message me if you're interested! :-))
e t s y | | | f a c e b o o k
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I have so many pictures from this day... :]
Put on my mudflaps that morning + went for a photo shoot.
Only had one pocket wizard so I couldn't move my lights around as much as I needed to. First time playing with my strobes outside.
A representative soil profile and landscape of the Tedburn soil series from England. (Photos and information provided by LandIS, Land Information System: Cranfield University 2022. The Soils Guide. Available: www.landis.org.uk. Cranfield University, UK. Last accessed 14/01/2022). (Photos revised.)
These and associated soils are seasonally waterlogged slowly permeable soils, formed above 3 m.0.D. and prominently mottled above 40 cm depth. They have no relatively permeable material starting within and extending below 1 m of the surface.
They have a distinct topsoil and are found mainly in lowland Britain. They formed in clayey material over lithoskeletal mudstone, shale or slate.
They are classified as Clayic Eutric Stagnosols by the WRB soil classification system. (www.fao.org/3/i3794en/I3794en.pdf)
For more information about this soil, visit:
X607 WRB
ERF ECX
Morris Amusements, 'Power Shot' Reverse Bungee
Everard Meadow, Bedford, 16 July 2014
Morris's Bungee attended the last River Festival in 2012 and has returned this year but now has a new tractor unit, the old G-reg ERF having been pensioned off.
Watco Australia's WRA001 and WRB 2183 are stranded on the grain loading loop in Miles with a loaded grain train, due to the floods and land slides.
www.canibeat.com/2013/08/law-of-motion-kirk-currans-05-su...
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A representative soil profile and landscape of the Sutton soil series from England. (Photos and information provided by LandIS, Land Information System: Cranfield University 2022. The Soils Guide. Available: www.landis.org.uk. Cranfield University, UK. Last accessed 14/01/2022). (Photos revised.)
These and associated soils are dominantly brownish or reddish subsoils and no prominent mottling or greyish colours (gleying) above 40 cm depth. They are developed mainly on permeable materials at elevations below about 300 m.0.D. Most are in agricultural use.
They are loamy or clayey with an ordinary clay-enriched subsoil. They formed in medium loamy material over calcareous gravel.
They are classified as Endoskeletic Luvisols by the WRB soil classification system. (www.fao.org/3/i3794en/I3794en.pdf)
For more information about this soil, visit:
Westbound at Birdlip, almost certainly heading for a car auction site, is Conod's ECX Olympic 6x2 TU. The name of its previous operator, Bowman, is picked out by the sunshine.
A representative soil profile and landscape of the Southhampton soil series from England. (Photos and information provided by LandIS, Land Information System: Cranfield University 2022. The Soils Guide. Available: www.landis.org.uk. Cranfield University, UK. Last accessed 14/01/2022). (Photos revised.)
These and associated soils are black, dark brown or ochreous humus and iron-enriched subsoils formed as a result of acid weathering conditions. Under natural or semi-natural vegetation, they have an unincorporated acid organic layer at the surface.
They are well drained, with a bleached subsurface horizon and no thin ironpan. They formed in sandy gravelly very hard siliceous stones.
They are classified as Episkeletic Ruptic Umbric Albic Podzols by the WRB soil classification system. (www.fao.org/3/i3794en/I3794en.pdf)
For more information about this soil, visit:
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My baby. We just came back from a trip to Akron to pick up a used turbo back exhaust. Super cheap deal. Thought I might as well stop by Cleveland on my way back to Michigan while the sun's still out. Just recently put on those canards as well! :D