Bedding world wide
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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.
The species is native to Peru and, in the wild, spreads like a bedding beneath larger plants. However, it can also be grown in pots and kept indoors.
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.
A dusting of snow overnight highlights the bedding planes (the lines separating one layer of compressed rock from the next).
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Eternus ༶ Nyla Robe set
• Babydoll / Stockings / Roibe
•Full colour HUD with Lace/Bow HUD
Made for → Legacy/Perky/Bombshell // Reborn/Juicy Boobs/Waifu // LaraX+PetiteX
- Reborn+Juicy Boobs+Waifu
Available from → Cosmopolitan Event
There after available from → Eternus in world store.
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RBento:: Eris Bento static poses
with Tatt (not shown)
The Astrophe Event
Starts: 5th - 25th at 12AM SLT
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♥ CHEZ MOI ༶ Pristine Bed
• Bed withheadboard and side tables
• single // couple // sex animations
• Multi colour HUD with blanket cushions wood and bedding choices
Available from → CHEZ MOI in world store.
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
Nemesia is a genus of annuals, perennials and sub-shrubs which are native to sandy coasts or disturbed ground in South Africa. Numerous hybrids have been selected, and the annual cultivars are popular with gardeners as bedding plants.
Perennial: The Nesia series offer large-sized flowers in striking colors on strong, stable stems. Long bloom season.
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!
Am 9. Februar 2018 ist die 155 103 von CLR mit ihrem Brammenzug von Oberhausen West nach Beddingen (VPS) bei Evesen unterwegs.
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.
DB Cargo 185 160 met trein 51178 Beddingen - Mannheim Rbf.
Na de Lotos / Cargounit was het weer de beurt aan DB Cargo.
Met de DB Cargo 185 160 voorop met een sleep beladen Shimmns, passeert hier het geheel de omgeving van Peine en gaat zo verder richting Lehrte en Mannheim.
Upper Antelope Canyon - Navajo Reservation - Page, Arizona View On Black
The rocks that make up Antelope canyon are the petrified remains of prehistoric sand dunes laid down when a shallow ocean filled this portion of North America. Cross bedding is noticable in the soft sandy walls. Many large overhangs with spiraling grooves carved into the sandstone loom overhead. Millions of years of erosion created this awesome splender of Mother Nature. Over time, the water started cutting it's way into this sandstone with tremendous force creating eddies and whirlpools, this is what makes the spiraling walls referred to as the Corkscrew formation.
Happy Friday to all my friends....hope everyone has a wonderful weekend....53 days & counting to vacation :-) Thanks for stopping by to visit!!!