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Interesting how the Badgers on Winter Watch were moving old bedding out of the set and collecting new possibly for new arrival’s. Could this rabbit be doing the same is Spring on its way!
Looking down on the eastern edge of the lovely fishing village of Pittenweem from the Fife Coastal Path. The low tide allows a good view of the parallel rock beds which are a feature of this stretch of coast.
Over Zion National Park - Utah.
Ancient cross bedding of Navajo Sandstone in the foreground.
Best viewed large.
Texture thank you IrisB
Absolutely Extraordinary High End.
This bedding was bought for Vasэka, but it seemed cramped to him, so now Yashka sleeps in it. But more often Yashka sleeps on the floor, he is hot!
Thank you all for visits, favs and comments. It's greatly appreciated!
The kitties always love when we change the bedding each weekend, immediately laying on it when it’s done. Today it was especially nice with the sun coming in. They really know how to enjoy the simple things in life (which are often the best things)!
Valley of Fire, Nevada, USA
In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original depositional layering is tilted, such tilting not being the result of post-depositional deformation. Cross-beds or "sets" are the groups of inclined layers, which are known as cross-strata.
Cross-bedding forms during deposition on the inclined surfaces of bedforms such as ripples and dunes; it indicates that the depositional environment contained a flowing medium (typically water or wind). Examples of these bedforms are ripples, dunes, anti-dunes, sand waves, hummocks, bars, and delta slopes. Environments in which water movement is fast enough and deep enough to develop large-scale bed forms fall into three natural groupings: rivers, tide-dominated coastal and marine settings.
Valley of Fire, Nevada, USA
In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original depositional layering is tilted, such tilting not being the result of post-depositional deformation. Cross-beds or "sets" are the groups of inclined layers, which are known as cross-strata.
Cross-bedding forms during deposition on the inclined surfaces of bedforms such as ripples and dunes; it indicates that the depositional environment contained a flowing medium (typically water or wind). Examples of these bedforms are ripples, dunes, anti-dunes, sand waves, hummocks, bars, and delta slopes. Environments in which water movement is fast enough and deep enough to develop large-scale bed forms fall into three natural groupings: rivers, tide-dominated coastal and marine settings.
Farn Islands puffin shots manages to get a few in flight shots either with sand eels or of one with some fresh bedding :)
A dusting of snow overnight highlights the bedding planes (the lines separating one layer of compressed rock from the next).
Took all our tulips and daffodils out of the containers and now replaced with summer bedding plants.
Valley of Fire, Nevada, USA
In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original depositional layering is tilted, such tilting not being the result of post-depositional deformation. Cross-beds or "sets" are the groups of inclined layers, which are known as cross-strata.
Cross-bedding forms during deposition on the inclined surfaces of bedforms such as ripples and dunes; it indicates that the depositional environment contained a flowing medium (typically water or wind). Examples of these bedforms are ripples, dunes, anti-dunes, sand waves, hummocks, bars, and delta slopes. Environments in which water movement is fast enough and deep enough to develop large-scale bed forms fall into three natural groupings: rivers, tide-dominated coastal and marine settings.
Obviously Paddy realsies that he should be going with the 'flow' of the strata. Behind looking back at the ridgeline we'd just traversed
I spent a happy half hour in the garden, in sunshine, with camera and coffee, watching the blue tits lining their chosen nesting box.
I took a whole bunch of shots of the 6988 this weekend, but my favorite, by far is this shot of it laying over on the west side of downtown DSM on Sunday night. I had just finished up dinner at Fong's, and ran down here to get something a bit different, before retiring to the hotel for the evening.
Shoutout to the IAIS, and all of the volunteers who helped make this weekend's trips possible!
2 VPS Lokomotiven der Baureihe 186 mit einem Kohlezug auf dem Weg vom Hamburger Hansaport in Altenwerder nach Salzgitter Beddingen auf der KBS 110 zwischen Winsen und Lüneburg in Radbruch
2 VPS locomotives of the class 186 with a coal train on the way from the Hamburg Hansaport in Altenwerder to Salzgitter Beddingen on the KBS 110 between Winsen and Lüneburg in Radbruch
Torridonian sandstone outcrop on the NE spur of Farrmheall, with Beinn Spionnaidh and Cranstackie in the background.
The bedding plane is interestingly varied in this outcrop, as is the texture - some layers contain pebbles, which have been buried in the rock since the these deposits - from a river delta - were laid down approximately 1 billion years ago.
I made some bedding...
More pics here:
www.emmr.co.uk/2013/05/21/new-bed-and-bedding/
Including a rather adorable PukiFee for size ref ;)
Bad Unicorn Work in progress for FaMESHed (opens the 1st)
maps.secondlife.com/secondlife/Cravone/111/204/23
marketplace.secondlife.com/p/Backwoods-Lounger-PG-Version...
Eider - Somateria Mollissima
Dunollie Oban - Scotland
Many thanks as always to those who view and in particular take time to comment on, or fave my photos.
DSC_0085
Im Harzvorland begeistern täglich die VPS-Werkspendel zwischen Beddingen und Ilsenburg. Hier verlässt Tiger Nr. 1 mit einem Brammenzug den Werksbahnhof auf seiner Reise Richtung Ilsenburg.