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.
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.
We were at our local Garden Centre the other day, there was a glorious colourful display of bedding plants..... For this image I used my phone to photograph them.....
A dusting of snow overnight highlights the bedding planes (the lines separating one layer of compressed rock from the next).
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!
See my story about this journey!
youtu.be/bHKeKGdRxOo
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Taking pictures a tool (camera), not a photographer.
The choice of tool limits the possibilities.
Experience allows him (instrument) less and less to limit their capabilities.
The ability to see is given only when the observer allows ...
The moment of observation is the real find ...
Training and mastering it defies. Training leads to poor imitations of the original.
Often the result should ripen, like wine. Although time is the understanding of the mind, therefore it is very speculative.
The meaning of all this is the process!
Find someone who inspires shooting the camera!
www.instagram.com/listenwave_photography/
Often we are visited by thoughts that may reveal something unknown ... Our mind many times tries to solve a problem with known methods ... This is its main mistake! The path of the heart opens the doors that appear in our path. It is a pity that not everyone has the courage to insert the keys that are always with us ...
(Listenwave- 圣彼得堡)
Lakhta. This small village on the northern shore of the Gulf of Finland, about 15 km north-west of the city, is the birthplace of human settlements on the banks of the Neva. It was in the territory of Lakhta that the remains of a man’s camp of three thousand years ago were found.
In official documents, the settlement named Lakhta has been dating since 1500. The name is derived from the Finnish-language word lahti - "bay". It is one of the few settlements that has not changed its name throughout its 500-year history. It is also known as Lahes, Lahes-by, Lahes and was originally inhabited by Izhora. In the last decades of the 15th century, Lakhta was a village (which indicates a significant number of its population) and was the center of the same name of the Grand-Ducal volost, which was part of the Spassko-Gorodensky pogost of Orekhovsky district of Vodskaya Pyatina. In the village there were 10 yards with 20 people (married men). In Lakhta, on average, there were 2 families each, and the total population of the village probably reached 75 people.
From the marks on the fields of the Swedish scribal book of the Spassky Pogost of 1640, it follows that the lands along the lower reaches of the Neva River and part of the coast of the Gulf of Finland, including Lakhta Karelia, Perekulyu (from the Finnish "back village", probably because of its position relative to Lakhta) and Konduya Lakhtinsky, was granted royal charter on January 15, 1638, to the possession of the Stockholm dignitary, General Rickshulz Bernhard Sten von Stenhausen, of Dutch origin. On October 31, 1648, the Swedish government granted these lands to the city of Nuena (Nyenskansu). With the arrival of the Swedes in the Neva region, Lakhta was settled by the Finns, who until the middle of the 20th century constituted the absolute majority of the villagers.
On December 22, 1766, Catherine 2 granted the Lakhta manor, which at that time belonged to the Office of the Chancellery from the buildings of palaces and gardens, "in which and in her villages with yard people 208 souls" to her favorite, Count Orlov. Not later than 1768 Count J.A. Bruce took possession of the estate. In 1788, the Lakhta manor with its wooden services on dry land (high place) and the villages of Lakhta, Dubki, Lisiy Nos and Konnaya, also on dry land, were listed there, in those villages of male peasants 238 souls. On May 1, 1813, Lakhta was taken over by the landlords of the Yakovlevs. On October 5, 1844, Count A. I. Stenbok-Fermor took possession of the Lakhta estate, in which there were then 255 male souls. This genus was the owner of the estate until 1912, when his last representative got into debt and the nobility was established over the estate. On October 4, 1913, the count, in order to pay off his debts, was forced to go into incorporation, and the Lakhta estate became the property of the Lakht Joint-Stock Company of Stenbock-Fermor and Co.
After the revolution, Lakhta was left to itself for some time; on May 19, 1919, in the former estate of the Stenbock-Fermor estate, the Lakhta sightseeing station was opened, which lasted until 1932. In the early 1920s, sand mining began on the Lakhta beaches, and the abandoned and dilapidated peat-bedding plant of the Lakhta estate in 1922 took the Oblzmotdel department under its jurisdiction and launched it after major repairs. In 1963, the village of Lakhta was included in the Zhdanovsky (Primorsky) district of Leningrad (St. Petersburg).
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.