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P-47N Thunderbolt, U. S. Army Air Force (44-89320), Eglin Air Force Base, U. S. Air Force Armament Museum
Another one of my new dolls of 2015. This is the Maternity Licca - who is a "grown up" version of an alternative Licca rather than a Licca's mom doll as I learned. Coincidentally she was released when Japan's crown princess was pregnant in 2001. Pearl is still patiently waiting for her baby to arrive.
A walk down Cole Bank Road in Sarehole (Hall Green / Moseley border) near Sarehole Mill.
Before walking up Swanshurst Lane to Swanshurst Park.
Nobody expects the Spanish Inquisition! (Monty Python)
Graffiti / street art on the old council billboard space unused currently on Cole Bank Road near Sarehole Mill.
Not sure what it is supposed to represent.
في البايه وقبل كل شي
بليز قولوا ماشاااااااء الله على المودل اخوي
Say Mashallah please
( ربي يحفظه لي )
و اول تجربه لي بالتصوير والدمج لنفس الشخصيه
>> تم تصوير الفائز <<
بس ماراح انزلها الا بعد التصويت
<3
ارااااااائكم
:)
"Furious campaigners have accused senior officers of breaking the Remembrance Sunday tradition to honour Britain’s war dead but the police forces insist they have no choice because of Government cuts."
However, this one went ahead with combined efforts of a PC, 3 x PSCOs and volunteers.
This is a statue of the founder of International Society for Krishna Consciousness (ISKCON).
ISKCON has popularized Indian philosophy particularly related to Krishna, the Hindu god, amongst the people of the western society.
Em dezembro do ano passado eu fui fotografar este casal tão divertido que está à espera da Stella! =) O ensaio ficou uma graça e estou louca pra colocar mais umas por aqui.. e logo, logo elas também estarão no blog!
gisa.sauer@gmail.com
expected overlaps
Choreografie: Mario Heinemann Jaillet
Tänzerin: Gaëlle Morello
Darsteller: Nicolas Menze
Puppenspieler: Werner Ries
Licht: Norbert Mohr
Koordination: Sophie Jaillet Heinemann
© All rights reserved
Photos: Günter Krämmer
Model: Claire
Makeup: Iraigui Flores de Crété
© 2010 Jean Lemoine - Tous droits réservés.
Strobist info:
Multiblitz Profilux 600 with softbox.
Courtenay Solapro 300 with softbox.
Wire trigger.
2017 World Championship Group Stage at Wuhan Sports Center Gymnasium in Wuhan, Hubei, China on 5 October 2017.
These are my personal notes taken during a geology presentation. I give them here because they may be of some interest. Do not expect the notes to always be in complete sentences, etc.
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A Look at Biotic Events at High Southern Latitudes at the End of the Cretaceous
Presented by: William Zinsmeister (Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana, USA) (www.eaps.purdue.edu/people/faculty-pages/zinsmeister.html)
19 November 1998
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The Cretaceous-Tertiary (K-T) extinction is the smallest of the big 5 extinctions. 11% of all families go extinct at the K-T boundary. But, the K-T extinction is a favourite of many people, mainly because it included the extinction of the dinosaurs. There have been many theories proposed about why the dinosaurs went extinct, including mammals eating their eggs, the evolution of angiosperms interfering with their digestive systems, and other ideas.
But, all these dinosaurs extinction hypotheses are flawed because they only deal with dinosaurs. Many terrestrial and marine groups (plant and animal) went extinct at the same time.
Then, the impact hypothesis came along in the early 1980s, proposed by Alvarez. This idea explained the K-T extinction in both the terrestrial and marine realm - basically, the global food chain collapsed. Also, the impact theory caught people’s imaginations, and was immediately accepted as fact by the media and the general public. There is much debate among scientists, though.
Now, there is much compelling evidence for an impact. Lots of computer modelling has been done to see what an impact would do the the Earth. One idea is that debris would be thrown up high into the atmosphere and would fall back down as an enormous meteor shower, which would heat the atmosphere to 800˚ and everything on the surface was cooked. Other scary ideas: rainshowers of nitric acid and sulfuric acid, nuclear winter scenario, and global forest fires.
Problem: If things were so bad, how did anything survive? Where are the burned/charred dinosaur bones and trees if all this happened?
There are a few diehards who still say an impact didn’t happen.
Other than that, there are 2 hypothese: 1) Bad Day Hypothesis; 2) Impending Doom Hypothesis.
The Impending Doom Hypothesis says that the Earth’s biosphere had been under a long period of stress up to the time of the impact. The impact was the capstone to the extinction. This seems like a logical idea.
Seymour Island - located near the northeastern tip of the Antarctic Peninsula. The geology on Seymour Island is mostly a homoclinal succession of rocks - Cretaceous to upper Paleocene. (www.geologicallocations.com/antarctica/seymour-island.htm)
Post-impact scenarios - it has been difficult to assess post-impact scenarios because there are few areas in the world with Danian-age rocks (= earliest Tertiary). Danian rocks occur in northwestern Europe, a few other places, and on Seymour Island. The north part of Seymour Island is Tertiary in age.
There are about 70 square kilometers of outcrop to look at on Seymour Island (upper Cretaceous and lower Tertiary). The island has a desert-like topography similar to southwestern USA. These are good exposures, and they are packed with fossils with a high diversity and good preservation. About 800 species of fossils have been described from Seymour Island. Lots of ammonites are just lying on the surface. The ammonites are aragonitic. There are also good gastropods and bivalves (all fresh looking). There are also fossil echinoids (including 1 form with 5 brood pouches - the juveniles live in the parent up to a certain point). There are also plesiosaurs and mosasaurs. Ammonites are common.
A spectacular specimen of Diplomoceras was found last year - a specimen that was 1.5 meters long (but curved; uncurved, it would be 14 feet long). The animal itself was ~6 feet long (a 6 feet long living chamber). Smaller pieces of this fossil are relatively common, but this specimen was unusually preserved. It is the nicest, most remarkable specimen known. (www.geologicallocations.com/assets/photos/antarctica/Seym...)
Seymour Island is very muddy to work on - it is always above freezing during the field seasons.
An iridium anomaly does occur here on Seymour Island. It occurs in a unit referred to as the K-T glauconite, which is a greenish, glauconitic sandstone that occurs at the boundary. The glauconitic sandstone is easily correlatable across the island. (www.geologicallocations.com/assets/photos/antarctica/Seym...)
There are no stratigraphic or sedimentological signatures at the K-T boundary within the glauconitic sandstone interval. There is no boundary clay, as classically seen at Gubbio, Italy.
Antarctica is ~8000 miles away from the Chicxulub Crater in Yucatan, Mexico, which is a significant point as far as considering the after-effects expected to be seen in Antarctica. (www.theyucatantimes.com/wp-content/uploads/2014/06/Chicxu...)
Rudist record - there is a gradual increase in the diversity of rudist bivalves in the Cretaceous. (www.paleotax.de/rudists/intro-Dateien/image002.jpg) Most rudists went extinct at 67.5 to 68 million years ago (~early-late Maastrichtian boundary). This pattern mirrors other groups’ diversity patterns as well - all mostly go extinct before the K-T boundary.
Seymour Island ammonites crash at the end of the Campanian. Seymour Island inoceramid bivalves are gone near the end of the Campanian. (www.flickr.com/photos/jsjgeology/19921135882) Seymour Island belemnites virtually disappear at the end of the Campanian. Seymour Island ammonites are quite diverse in the Campanian (35-36 species), but their diversity crashes to 10 species in the Maastrichtian (= latest Cretaceous), and they are gone at the K-T boundary. Several Campanian cosmopolitan ammonite families disappear in the Campanian in the Seymour Island area, but they extend to the K-T boundary in lower latitudes. So, their disappearance in the Seymour Island area indicates a general temperature decline (cooling).
A regression occurred at the mid-Maastrichtian.
Superimposed on the Maastrichtian temperature decline are several rapid warming spikes. 50,000 years before the K-T boundary event was a warming event, documented from some ODP sites.
Note the restricted occurrence to 1 horizon on Seymour Island of the ammonite Zealandites varuna in the Maastrichtian Lopez de Bertodano Formation. Its presence probably represents a warming spike.
The faunal transition across the K-T boundary on Seymour Island - no single extinction event seen - a gradual decline is seen instead. There is no marked extinction horizon.
Then, someone suggested that this pattern is due to the Signor/Lipps Effect, a phenomenon produced by collection/preservation biases. One can get a gradual extinction pattern purely due to collecting and preservation biases. So, Zinsmeister and others recollected the fossils on Seymour Island, and collected fossils spatially, doing detailed mapping.
The K-T glauconite (~5 meters thick) is actually 3 units - a lower glauconite, a middle fish bed/horizon, and an upper glauconite. The fish debris bed could represent a victim bed from the K-T impact.
Renewed fossil collecting has resulted in a new diversity record - the extinction is less gradual now - it is more abrupt, but all groups are dying out just before the iridium anomaly. The K-T extinction is now more abrupt is high southern latitudes than previously thought.
Fish horizon - interpreted to be the effect of extreme ocean disruption; fish kills are not due to ocean poisoning (strangelove ocean), but by pulses of nutrients into the oceans. This is the only fish horizon in 1600 meters of section. It could be an interval of slow deposition, but this is not likely because fish degrade relatively quickly, and one needs special conditions to preserve fish. The fish debris bed represents conditions after the K-T event - lots of fish kills occurred.
The biosphere is far more robust than we give it credit for. Organisms have been able to survive truly catastrophic events in geologic history.
Example: the Millbrig Bentonite (Middle Ordovician, eastern USA and Scandinavia). This large volcanic eruption resulted in no extinctions. Therefore, Earth’s biosphere is very robust. But, if the biosphere is already stressed, then a big event can push the biosphere into a mass extinction.
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The most adorable girl mimicking her pregnant mom. Update: when I took the photo I didn't know the tile 'Expecting a brother' would be the right one. The little girl did get the brother she expected. :)
No train will stop to pick up the folk on the platform of Lake Placid railroad depot. Passenger service at the former Atlantic Coast Line depot ceased in the 1960s. The 1926-built depot now houses a museum and is maintained by the Lake Placid Historical Society. But a vestigial train service does use the tracks in the foreground: the grandly-named South Central Florida Express is a short line that conveys the cane harvested by US Sugar around Lake Okeechobee to the south.
This picture I made it in the garden of a friend of Böblingen.
Tree is cherry.
The word cherry refers to a fleshy fruit (drupe) that contains a single stony seed. The cherry belongs to the family Rosaceae, genus Prunus, along with almonds, peaches, plums, apricots and bird cherries. The subgenus, Cerasus, is distinguished by having the flowers in small corymbs of several together (not singly, nor in racemes), and by having a smooth fruit with only a weak groove or none along one side. The subgenus is native to the temperate regions of the Northern Hemisphere, with two species in America, three in Europe, and the remainder in Asia. The word "cherry" comes from the French word "cerise", which comes in turn from the Latin words cerasum and Cerasus.
The cherry is generally understood to have been brought to Rome from northeastern Anatolia, historically known as the Pontus region, in 72 BC. The city of Giresun in present-day Turkey was known to the ancient Greeks as Choerades or Pharnacia, and later as Kerasous or Cerasus, < Kerason < Kerasounta < Kerasus "horn" (for peninsula) in Greek + ounta (Greek toponomical suffix). The name later mutated into Kerasunt (sometimes written Kérasounde or Kerassunde).
The English word cherry, French cerise, Spanish cereza, and Southern Italian dialect cerasa (standard Italian ciliegia) all come from the Classical Greek κέρασος "cherry," which has been identified with Cerasus. The cherry was first exported to Europe from Cerasus in Roman times. By the Middle Ages, cherries had disappeared in England. They were reestablished at Tyneham, near Sittingbourne in Kent by order of Henry VIII, who had tasted them in Flanders.
Besides the fruit, cherries also have attractive flowers, and they are commonly planted for their flower display in spring; several of the Asian cherries are particularly noted for their flower displays. The Japanese sakura in particular are a national symbol celebrated in the yearly Hanami festival. Many flowering cherry cultivars (known as 'ornamental cherries') have the stamens and pistils replaced by additional petals ("double" flowers), so are sterile and do not bear fruit. They are grown purely for their flowers and decorative value. The most common of these sterile cherries is the cultivar 'Kanzan'.
The photo I had to laugh. Can not smile without looking at it as a huge dog finds the members of his flock of children. Balian accompanies them everywhere:)
Oy Vey! - a Victoria institution.
Expect the unusual at the Roxy, "where movies are a religion!" The Roxy features second-run films and double bills at bargain prices. Tuesdays here are a real bargain -- two movies for $2.50. A regular double bill is $5.00.
Note from the owner (1986-2007) Howie Siegel, found here :
"I'll give you some specific info on the history of what was founded as the Fox, became the Quadra and is not the Roxy Cinegog in Victoria.
"Founded in 1949 by Walkey (the druggist who owned the land) and Nixon (the projectionist who ran the cinema) as the Fox with 424 seats.
"Bought by Barney Simmons, who was Nat Taylor's nephew and Arthur Hiller's cousin, in 1966. He changed the name because he played porno there while it was still the Fox. He needed a name change when he got away from porno and chose the Quadra. ...
" I bought the theatre in 1986 and made a mistake. I called it the Roxy Cinegog. I should have reverted to its original name and called it the Fox Cinegog. I redid the seating and it is now around 324."
My 2nd maternity shoot. Tried a few without the backdrop this time as the colours looked pretty good. Also, there wasn't loads of room to set up the backdrop due to the shape of the room.
For the shots without the backdrop I used both my Sony F42 flashguns with white shoot-through umbrellas.
For the backdrop shots I had a bare flash behind the backdrop and one camera right with a reflector on the floor aiming back up into Matt & Kiley.
The clip is not very steady which I apologise for but seeing the test train in motion gives it a little more interest. I was not expecting to see this as I was on my way to Stevenage. You have to grab your chances when you can.
Family baby shower. I don't remember which relative was the photographer. This is me with my younger sister and my mom.