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 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.
This changing of the seasons brings out the earthy aromas of the forest preparing for the big sleep. Leaves start bedding down to provide a warm blanket for insects for the winter. Fungi are evident on aging logs. Orange and browns seem to be the dominant colours of this month. Happy Macro Monday.
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.
This slice of Navajo sandstone in Grand Staircase Escalante National Monument shows well at least six layers of cross bedding, where the layers are angled relative to the horizontal plane. These cross beds occur where sand has been blown by the wind across a sloped dune formation, resulting in a layer that is deposited at an angle different than the flat surface.
Navajo sandstone was deposited 200 million years ago when this area was a massive sand dune formation, larger than the current Sahara desert, with depoists as thick as 2400'/ 730 m.
A dusting of snow overnight highlights the bedding planes (the lines separating one layer of compressed rock from the next).
“Winter bedding plants such as Primroses bring cheer to a garden during the coldest months. The plants can be spaced more closely together as they won't grow much during winter. They may not flower during very cold weather but will pick up again during milder spells.”
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 ;)
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