Nice pictures
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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.
This little mouse was in and out from under the log and it picked up dry leaves in its mouth and scurried back under the log with the make do bedding
Wood mice are mainly active during the dark, probably having evolved so to avoid predation, employing several anti-predatory strategies, though breeding females may be more active in daylight in order to collect sufficient food.[9] While foraging, wood mice pick up and distribute visually conspicuous objects, such as leaves and twigs, which they then use as landmarks during exploration.[10][11] If a wood mouse is caught by its tail, it can quickly shed the end of it, which may never regrow.[12] Despite its name, it prefers hedgerows to woodland. During the colder months, wood mice do not hibernate; however, during severe winter seasons they can fall into a torpid state, a decrease in physiological activity.
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.
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.
Wegen Bauarbeiten im Grenzbahnhof Horka wurde der Güterverkehr 2014 auf verschiedene andere Strecken umgeleitet,
So rollt 232 658 der east-west Bahngesellschaft mit dem Kohlezug GM 49 412 Weglieniec – Salzgitter Beddingen VPS in den Bahnhof Klinge
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 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!
Een werktrein staat in Kallo op de nieuwe bedding van Lijn 10. Op de voorgrond het oude enkelsporige tracé dat een paar maanden later zal verdwijnen.
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.
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