Nice pictures
View allAll Photos Tagged Bedding,
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 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.
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.
Just returned from one of our nearby lakes..
While a pelican pair were bedding down for the night onshore, two black swans were still enjoying their pristine water wonderland.
Was sunny and warm today, and quite a magical evening lakeside.
Besides a tiny straighten up, no edits. Seems I can't hold the camera level these days..
Ended up with a cool series tonight..
Was quite reluctant to go home !
BTW, the mountains are covered with gum tree forests, so it always looks a bit bumpy up there..
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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 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!
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 ;)
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.
One of the hardest things to do is get an accurate focus point locked on your subject when he is behind weeds. To do this I set my lens to manual/infinity then my camera to AF focus search off and selected center focal point.
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Copyright@louisruthphotography 2017
Brown or Grizzly Bear (ursus arctos) named "Scout" adusting a few items in the bedding materials to create a comfortable day bed for his nap. Grizzly bears in San Diego do not tuck in for long winter sleeps like their wild cousins. In our cooler months they eat a lot less and sleep most of the time, but can still often be seen foraging for favorite foods.
San Diego Zoo.
Conservation status: least concern