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À l’horizon, une touche d’argent
On the horizon, a touch of silver
Comme après l’orage, s’en vont les nuages
Like after a storm, the clouds disappear
Les nuits d’été, sommeils oubliés
The summer nights, forgotten dreams
Grâce à ton parfum, je retrouve mon chemin
Thanks to your perfume, I find my way back
Il pleut de l’or, chaque fois que tu me parles d’amour
It’s raining gold, each time you talk to me about love
Il pleut de l’or, ensemble partons pour faire le grand tour
It’s raining gold, let’s leave together for the big journey
Sous la voûte étoilée, les destins sont dorés
Under the starry vault, destinies are golden
Il pleut de l’or It’s raining gold
Et au matin, secret commun
And in the morning, shared secret
Des regards échangés sont complices de l’été Exchanging glances
, accomplice of summer
Le jour chasse la magie, restent les yeux qui brillent
The day chases magic, the shimmering eyes remain
Il pleut de l’or, chaque fois que tu me parles d’amour (Il pleut de l’or)
It’s raining gold, each time you talk to me about love (It’s raining gold)
Il pleut de l’or, ensemble partons pour faire le grand tour
It’s raining gold, let’s leave together for the big journey
Sous la voûte étoilée, les destins sont dorés
Under the starry vault destinies are golden
Il pleut de l’or, toute la nuit et jusqu’à l’aurore It’s raining gold,
the whole night and until the dawn
Il pleut de l’or
It’s raining gold
Danse avec moi, vole avec moi Dance
with me, fly with me
Parle tout bas, parle moi
Speak quietly, speak with me
(Il pleut de l’or) Il pleut de l’or (Il pleut de l’or)
(It’s raining gold) It’s raining gold (It’s raining gold)
Il pleut de l’or, ensemble partons pour faire le grand tour
It’s raining gold, let’s leave together for the big journey
Sous la voûte étoilée, les destins sont dorés
Under the starry vault, destinies are golden
Il pleut de l’or, toute la nuit et jusqu’à l’aurore
It’s raining gold, the whole night and until the dawn
Il pleut de l’or
It’s raining gold
À l’horizon, une touche d’argent
On the horizon, a touch of silver
Comme après l’orage, s’en vont les nuages
Like after a storm, the clouds disappear
Les nuits d’été, sommeils oubliés
The summer nights, forgotten dreams
Grâce à ton parfum, je retrouve mon chemin
Thanks to your perfume, I find my way back
Il pleut de l’or, chaque fois que tu me parles d’amour
It’s raining gold, each time you talk to me about love
Il pleut de l’or, ensemble partons pour faire le grand tour
It’s raining gold, let’s leave together for the big journey
Sous la voûte étoilée, les destins sont dorés
Under the starry vault, destinies are golden
Il pleut de l’or
It’s raining gold
Et au matin, secret commun
And in the morning, shared secret
Des regards échangés sont complices de l’été
Exchanging glances, accomplice of summer
Le jour chasse la magie, restent les yeux qui brillent
The day chases magic, the shimmering eyes remain
Il pleut de l’or, chaque fois que tu me parles d’amour (Il pleut de l’or)
It’s raining gold, each time you talk to me about love (It’s raining gold)
Il pleut de l’or, ensemble partons pour faire le grand tour
It’s raining gold, let’s leave together for the big journey
Sous la voûte étoilée, les destins sont dorés
Under the starry vault, destinies are golden
Il pleut de l’or, toute la nuit et jusqu’à l’aurore
It’s raining gold, the whole night and until the dawn
Il pleut de l’or
It’s raining gold
Sun and I went trick or treating this morning. Our favorite pet shop gives free treats to any pup that comes to visit wearing a costume on Halloween day!
More swans I'm afraid but they make such brilliant subjects! From the expression I was given I guess he isn't sharing his lunch
Sorry my friends I've got behind with your uploads, had to take a break with my tendonitis again ...
© copyrighted image; all rights reserved.
Canon or Nikon? Macro or Micro? There's something for everyone. Either way, you can't go wrong.
This was the ending picture of a light & shoot play-day Cricce and I did.
Strobist information:
A Elinchrom D-Lite 2 it with a 66x66cm Portalite soft box above the cameras, pointing down, slightly angled to the camera to get more fall-off towards the back. A gelled (CTB) Canon 430EX bounced via a silver reflector just under the camera to shine a little bit light into the lenses and on the front of the cameras.
Contax S2b + Zeiss Distagon T* 2,8/35
CineStill 800t
Out on a 35mm-prime-only street photography walk.
This is a composite of two separate photos taken during the Scott Kelby Worldwide photowalk on Oct. 13, 2012. Both were shot from the patio at the base of the soaring steeple of the First United Methodist Church. You can see the neo-Gothic detail of the steeple, as well as the chain link fence that encloses the patio. The view of the top of the Jewelers Building is unmistakable.
or should i say sharp where it counts ,as you can probably see the more i use this new sigma 150-600 sport the better i get used to it .really feel that i'm moving forward now and getting the i/q i have long been after .
shot with the lens wide open and a slow shutter speed to ,bean bag support
Bantra Sanmelani Club, Howrah.
Kumari Puja :
Kumari, or Kumari Devi, is the tradition of worshiping young pre-pubescent girls as manifestations of the divine female energy or devi in Hindu religious traditions. The word Kumari, derived from Sanskrit Kaumarya meaning "virgin", means young unmarried girls in Nepali and some Indian languages and is a name of the goddess Durga as a child.
In Nepal a Kumari is a pre-pubescent girl selected from the Shakya or Bajracharya clan of the Nepalese Newari community. The Kumari is revered and worshiped by some of the country'sHindus as well as the Nepali Buddhists, though not the Tibetan Buddhists. While there are several Kumaris throughout Nepal, with some cities having several, the best known is the Royal Kumari of Kathmandu, and she lives in the Kumari Ghar, a palace in the center of the city. The selection process for her is especially rigorous. The current Royal Kumari, Matina Shakya, aged four, was installed in October 2008 by the Maoist government that replaced the monarchy. Samita Bajracharya, as the Kumari of Patan is the second most important living goddess.
In India a Kumari is generally chosen for one day and worshipped accordingly on certain festivals like Navaratri or Durga Puja. In the Indian state of Bengal this is a particularly prevalent practice.
A Kumari is believed to be the incarnation of the goddess Taleju (the Nepalese name for Durga) until she menstruates, after which it is believed that the goddess vacates her body. Serious illness or a major loss of blood from an injury are also causes for her to revert to common status.
Philosophy and scriptures
The worship of the goddess in a young girl represents the worship of divine consciousness spread all over the creation. As the supreme goddess is thought to have manifested this entire cosmos out of her womb she exists equally in animate as well as inanimate objects. While worship of an idol represents the worship and recognition of supreme through inanimate materials, worship of a human represents veneration and recognition of the same supreme in conscious beings.
In the Shakta text Devi Mahatmyam or Chandi, the goddess is said to have declared that she resides in all female living beings in this universe. The entire ritual of Kumari is based on this verse. But while worshiping a goddess, only a young girl is chosen over a mature lady because of their inherent purity and chastity which are considered to be principal characteristics of Durga.
Hindu scriptures like the Jñanarnava Rudrayamala tantra assign different names to a Kumari depending on her age. A one year-old girl is called Sandhya, a two year-old girl is called Sarasvati, a child of three years of age is called Tridhamurti, on her fourth year she is Kalika, on fifth she is Subhaga, on sixth she is Uma, on her seventh year she is called Malini. an eight year girl is called Kubjika, on the ninth year she is Kaalasandarbha, on reaching tenth year she is Aparajita, on eleventh she is Rudrani, on twelfth year she is named Bhairavi, on thirteenth she is Mahalakshmi, on fourteenth she is Pithanayika, on fifteenth she is Kshetragya, and on sixteenth years of her age she is Ambika.
In India, Kumaris are worshiped only for a day and these names are assigned only while the ritual lasts, usually a few hours. Usually one cannot be a Kumari beyond sixteen years of age due to menarche.
The main target of a Kumari puja is to realize the potential divinity in every human being, mostly female. A Hindu spiritual aspirant sees the universal consciousness manifested in an innocent child.(en.wikipedia.org/wiki/Kumari_(children))
heute nacht oder nie 今宵限りは
The illuminated flower decoration is a farewell gift to the last train which leaves this world forever.
照らされた花の装飾は、永遠にこの世界を去る最後の電車への別れのプレゼントです。（逆直訳）
Google map 錦糸町 This shot has taken at Kinshi-cho, Tokyo 1971.
Small Skipper Butterfly (Thymelicus Sylvestris) with friend!
Many thanks to all who take the time to view, comment or fav my images
Yellowstone National Park (Arapaho: Henihco'oo or Héetíhco'oo) is a national park located primarily in the U.S. state of Wyoming, although it also extends into Montana and Idaho. It was established by the U.S. Congress and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone, widely held to be the first national park in the world, is known for its wildlife and its many geothermal features, especially Old Faithful Geyser, one of the most popular features in the park. It has many types of ecosystems, but the subalpine forest is most abundant. It is part of the South Central Rockies forests ecoregion.
Yellowstone National Park spans an area of 3,468.4 square miles (8,983 km2), comprising lakes, canyons, rivers and mountain ranges. Yellowstone Lake is one of the largest high-altitude lakes in North America and is centered over the Yellowstone Caldera, the largest supervolcano on the continent. The caldera is considered an active volcano. It has erupted with tremendous force several times in the last two million years. Half of the world's geothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly-intact ecosystem in the Earth's northern temperate zone.
Hundreds of species of mammals, birds, fish and reptiles have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the Continental United States. Grizzly bears, wolves, and free-ranging herds of bison and elk live in the park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.
The park is located at the headwaters of the Yellowstone River, from which it takes its historical name. Near the end of the 18th century, French trappers named the river "Roche Jaune", which is probably a translation of the Hidatsa name "Mi tsi a-da-zi" (Rock Yellow River). Later, American trappers rendered the French name in English as "Yellow Stone". Although it is commonly believed that the river was named for the yellow rocks seen in the Grand Canyon of the Yellowstone, the Native American name source is not clear.
The first detailed expedition to the Yellowstone area was the Cook–Folsom–Peterson Expedition of 1869, which consisted of three privately funded explorers. The Folsom party followed the Yellowstone River to Yellowstone Lake. The members of the Folsom party kept a journal and based on the information it reported, a party of Montana residents organized the Washburn-Langford-Doane Expedition in 1870. It was headed by the surveyor-general of Montana Henry Washburn, and included Nathaniel P. Langford (who later became known as "National Park" Langford) and a U.S. Army detachment commanded by Lt. Gustavus Doane.
The expedition spent about a month exploring the region, collecting specimens and naming sites of interest. A Montana writer and lawyer named Cornelius Hedges, who had been a member of the Washburn expedition, proposed that the region should be set aside and protected as a national park; he wrote a number of detailed articles about his observations for the Helena Herald newspaper between 1870 and 1871. Hedges essentially restated comments made in October 1865 by acting Montana Territorial Governor Thomas Francis Meagher, who had previously commented that the region should be protected. Others made similar suggestions. In an 1871 letter from Jay Cooke to Ferdinand V. Hayden, Cooke wrote that his friend, Congressman William D. Kelley had also suggested "Congress pass a bill reserving the Great Geyser Basin as a public park forever".
By 1915, 1,000 automobiles per year were entering the park, resulting in conflicts with horses and horse-drawn transportation. Horse travel on roads was eventually prohibited.
The Civilian Conservation Corps (CCC), a New Deal relief agency for young men, played a major role between 1933 and 1942 in developing Yellowstone facilities. CCC projects included reforestation, campground development of many of the park's trails and campgrounds, trail construction, fire hazard reduction, and fire-fighting work. The CCC built the majority of the early visitor centers, campgrounds and the current system of park roads.
During World War II, tourist travel fell sharply, staffing was cut, and many facilities fell into disrepair. By the 1950s, visitation increased tremendously in Yellowstone and other national parks. To accommodate the increased visitation, park officials implemented Mission 66, an effort to modernize and expand park service facilities. Planned to be completed by 1966, in honor of the 50th anniversary of the founding of the National Park Service, Mission 66 construction diverged from the traditional log cabin style with design features of a modern style. During the late 1980s, most construction styles in Yellowstone reverted to the more traditional designs. After the enormous forest fires of 1988 damaged much of Grant Village, structures there were rebuilt in the traditional style. The visitor center at Canyon Village, which opened in 2006, incorporates a more traditional design as well.
A large arch made of irregular-shaped natural stone over a road
The 1959 Hebgen Lake earthquake just west of Yellowstone at Hebgen Lake damaged roads and some structures in the park. In the northwest section of the park, new geysers were found, and many existing hot springs became turbid. It was the most powerful earthquake to hit the region in recorded history.
In 1963, after several years of public controversy regarding the forced reduction of the elk population in Yellowstone, United States Secretary of the Interior Stewart Udall appointed an advisory board to collect scientific data to inform future wildlife management of the national parks. In a paper known as the Leopold Report, the committee observed that culling programs at other national parks had been ineffective, and recommended management of Yellowstone's elk population.
The wildfires during the summer of 1988 were the largest in the history of the park. Approximately 793,880 acres (321,272 ha; 1,240 sq mi) or 36% of the parkland was impacted by the fires, leading to a systematic re-evaluation of fire management policies. The fire season of 1988 was considered normal until a combination of drought and heat by mid-July contributed to an extreme fire danger. On "Black Saturday", August 20, 1988, strong winds expanded the fires rapidly, and more than 150,000 acres (61,000 ha; 230 sq mi) burned.
The expansive cultural history of the park has been documented by the 1,000 archeological sites that have been discovered. The park has 1,106 historic structures and features, and of these Obsidian Cliff and five buildings have been designated National Historic Landmarks. Yellowstone was designated an International Biosphere Reserve on October 26, 1976, and a UN World Heritage Site on September 8, 1978. The park was placed on the List of World Heritage in Danger from 1995 to 2003 due to the effects of tourism, infection of wildlife, and issues with invasive species. In 2010, Yellowstone National Park was honored with its own quarter under the America the Beautiful Quarters Program.
Heritage and Research Center
The Heritage and Research Center is located at Gardiner, Montana, near the north entrance to the park. The center is home to the Yellowstone National Park's museum collection, archives, research library, historian, archeology lab, and herbarium. The Yellowstone National Park Archives maintain collections of historical records of Yellowstone and the National Park Service. The collection includes the administrative records of Yellowstone, as well as resource management records, records from major projects, and donated manuscripts and personal papers. The archives are affiliated with the National Archives and Records Administration.
Approximately 96 percent of the land area of Yellowstone National Park is located within the state of Wyoming. Another three percent is within Montana, with the remaining one percent in Idaho. The park is 63 miles (101 km) north to south, and 54 miles (87 km) west to east by air. Yellowstone is 2,219,789 acres (898,317 ha; 3,468.420 sq mi) in area, larger than the states of Rhode Island or Delaware. Rivers and lakes cover five percent of the land area, with the largest water body being Yellowstone Lake at 87,040 acres (35,220 ha; 136.00 sq mi). Yellowstone Lake is up to 400 feet (120 m) deep and has 110 miles (180 km) of shoreline. At an elevation of 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high altitude lake in North America. Forests comprise 80 percent of the land area of the park; most of the rest is grassland.
The Continental Divide of North America runs diagonally through the southwestern part of the park. The divide is a topographic feature that separates Pacific Ocean and Atlantic Ocean water drainages. About one third of the park lies on the west side of the divide. The origins of the Yellowstone and Snake Rivers are near each other but on opposite sides of the divide. As a result, the waters of the Snake River flow to the Pacific Ocean, while those of the Yellowstone find their way to the Atlantic Ocean via the Gulf of Mexico.
The park sits on the Yellowstone Plateau, at an average elevation of 8,000 feet (2,400 m) above sea level. The plateau is bounded on nearly all sides by mountain ranges of the Middle Rocky Mountains, which range from 9,000 to 11,000 feet (2,700 to 3,400 m) in elevation. The highest point in the park is atop Eagle Peak (11,358 feet or 3,462 metres) and the lowest is along Reese Creek (5,282 feet or 1,610 metres). Nearby mountain ranges include the Gallatin Range to the northwest, the Beartooth Mountains in the north, the Absaroka Range to the east, and the Teton Range and the Madison Range to the southwest and west. The most prominent summit on the Yellowstone Plateau is Mount Washburn at 10,243 feet (3,122 m).
Yellowstone National Park has one of the world's largest petrified forests, trees which were long ago buried by ash and soil and transformed from wood to mineral materials. This ash and other volcanic debris, are believed to have come from the park area itself. This is largely due to the fact that Yellowstone is actually a massive caldera of a supervolcano. There are 290 waterfalls of at least 15 feet (4.6 m) in the park, the highest being the Lower Falls of the Yellowstone River at 308 feet (94 m).
Three deep canyons are located in the park, cut through the volcanic tuff of the Yellowstone Plateau by rivers over the last 640,000 years. The Lewis River flows through Lewis Canyon in the south, and the Yellowstone River has carved two colorful canyons, the Grand Canyon of the Yellowstone and the Black Canyon of the Yellowstone in its journey north.
Yellowstone is at the northeastern end of the Snake River Plain, a great U-shaped arc through the mountains that extends from Boise, Idaho some 400 miles (640 km) to the west. This feature traces the route of the North American Plate over the last 17 million years as it was transported by plate tectonics across a stationary mantle hotspot. The landscape of present-day Yellowstone National Park is the most recent manifestation of this hotspot below the crust of the Earth.
The Yellowstone Caldera is the largest volcanic system in North America. It has been termed a "supervolcano" because the caldera was formed by exceptionally large explosive eruptions. The magma chamber that lies under Yellowstone is estimated to be a single connected chamber, about 37 miles (60 km) long, 18 miles (29 km) wide, and 3 to 7 miles (5 to 12 km) deep. The current caldera was created by a cataclysmic eruption that occurred 640,000 years ago, which released more than 240 cubic miles (1,000 km³) of ash, rock and pyroclastic materials. This eruption was more than 1,000 times larger than the 1980 eruption of Mount St. Helens. It produced a caldera nearly five eighths of a mile (1 km) deep and 45 by 28 miles (72 by 45 km) in area and deposited the Lava Creek Tuff, a welded tuff geologic formation. The most violent known eruption, which occurred 2.1 million years ago, ejected 588 cubic miles (2,450 km³) of volcanic material and created the rock formation known as the Huckleberry Ridge Tuff and created the Island Park Caldera. A smaller eruption ejected 67 cubic miles (280 km³) of material 1.3 million years ago, forming the Henry's Fork Caldera and depositing the Mesa Falls Tuff.
Each of the three climactic eruptions released vast amounts of ash that blanketed much of central North America, falling many hundreds of miles away. The amount of ash and gases released into the atmosphere probably caused significant impacts to world weather patterns and led to the extinction of some species, primarily in North America.
Wooden walkways allow visitors to closely approach the Grand Prismatic Spring.
A subsequent caldera-forming eruption occurred about 160,000 years ago. It formed the relatively small caldera that contains the West Thumb of Yellowstone Lake. Since the last supereruption, a series of smaller eruptive cycles between 640,000 and 70,000 years ago, has nearly filled in the Yellowstone Caldera with >80 different eruptions of rhyolitic lavas such as those that can be seen at Obsidian Cliffs and basaltic lavas which can be viewed at Sheepeater Cliff. Lava strata are most easily seen at the Grand Canyon of the Yellowstone, where the Yellowstone River continues to carve into the ancient lava flows. The canyon is a classic V-shaped valley, indicative of river-type erosion rather than erosion caused by glaciation.
Each eruption is part of an eruptive cycle that climaxes with the partial collapse of the roof of the volcano's partially emptied magma chamber. This creates a collapsed depression, called a caldera, and releases vast amounts of volcanic material, usually through fissures that ring the caldera. The time between the last three cataclysmic eruptions in the Yellowstone area has ranged from 600,000 to 800,000 years, but the small number of such climactic eruptions cannot be used to make an accurate prediction for future volcanic events.
The most famous geyser in the park, and perhaps the world, is Old Faithful Geyser, located in Upper Geyser Basin. Castle Geyser, Lion Geyser and Beehive Geyser are in the same basin. The park contains the largest active geyser in the world—Steamboat Geyser in the Norris Geyser Basin. A study that was completed in 2011 found that at least 1283 geysers have erupted in Yellowstone. Of these, an average of 465 are active in a given year. Yellowstone contains at least 10,000 geothermal features altogether. Half the geothermal features and two-thirds of the world's geysers are concentrated in Yellowstone.
In May 2001, the U.S. Geological Survey, Yellowstone National Park, and the University of Utah created the Yellowstone Volcano Observatory (YVO), a partnership for long-term monitoring of the geological processes of the Yellowstone Plateau volcanic field, for disseminating information concerning the potential hazards of this geologically active region.
In 2003, changes at the Norris Geyser Basin resulted in the temporary closure of some trails in the basin. New fumaroles were observed, and several geysers showed enhanced activity and increasing water temperatures. Several geysers became so hot that they were transformed into purely steaming features; the water had become superheated and they could no longer erupt normally. This coincided with the release of reports of a multiple year United States Geological Survey research project which mapped the bottom of Yellowstone Lake and identified a structural dome that had uplifted at some time in the past. Research indicated that these uplifts posed no immediate threat of a volcanic eruption, since they may have developed long ago, and there had been no temperature increase found near the uplifts. On March 10, 2004, a biologist discovered 5 dead bison which apparently had inhaled toxic geothermal gases trapped in the Norris Geyser Basin by a seasonal atmospheric inversion. This was closely followed by an upsurge of earthquake activity in April 2004. In 2006, it was reported that the Mallard Lake Dome and the Sour Creek Dome— areas that have long been known to show significant changes in their ground movement— had risen at a rate of 1.5 to 2.4 inches (3.8 to 6.1 cm) per year from mid–2004 through 2006. As of late 2007, the uplift has continued at a reduced rate. These events inspired a great deal of media attention and speculation about the geologic future of the region. Experts responded to the conjecture by informing the public that there was no increased risk of a volcanic eruption in the near future. However, these changes demonstrate the dynamic nature of the Yellowstone hydrothermal system.
Yellowstone experiences thousands of small earthquakes every year, virtually all of which are undetectable to people. There have been six earthquakes with at least magnitude 6 or greater in historical times, including a 7.5‑magnitude quake that struck just outside the northwest boundary of the park in 1959. This quake triggered a huge landslide, which caused a partial dam collapse on Hebgen Lake; immediately downstream, the sediment from the landslide dammed the river and created a new lake, known as Earthquake Lake. Twenty-eight people were killed, and property damage was extensive in the immediate region. The earthquake caused some geysers in the northwestern section of the park to erupt, large cracks in the ground formed and emitted steam, and some hot springs that normally have clear water turned muddy. A 6.1‑magnitude earthquake struck inside the park on June 30, 1975, but damage was minimal.
For three months in 1985, 3,000 minor earthquakes were detected in the northwestern section of the park, during what has been referred to as an earthquake swarm, and has been attributed to minor subsidence of the Yellowstone caldera. Beginning on April 30, 2007, 16 small earthquakes with magnitudes up to 2.7 occurred in the Yellowstone Caldera for several days. These swarms of earthquakes are common, and there have been 70 such swarms between 1983 and 2008. In December 2008, over 250 earthquakes were measured over a four-day span under Yellowstone Lake, the largest measuring a magnitude of 3.9. In January 2010, more than 250 earthquakes were detected over a two-day period. Seismic activity in Yellowstone National Park continues and is reported hourly by the Earthquake Hazards Program of the U.S. Geological Survey.
On March 30, 2014, a magnitude 4.8 earthquake struck almost the very middle of Yellowstone near the Norris Basin at 6.34am; reports indicated no damage. This was the biggest earthquake to hit the park since February 22, 1980.
Over 1,700 species of trees and other vascular plants are native to the park. Another 170 species are considered to be exotic species and are non-native. Of the eight conifer tree species documented, Lodgepole Pine forests cover 80% of the total forested areas. Other conifers, such as Subalpine Fir, Engelmann Spruce, Rocky Mountain Douglas-fir and Whitebark Pine, are found in scattered groves throughout the park. As of 2007, the whitebark pine is threatened by a fungus known as white pine blister rust; however, this is mostly confined to forests well to the north and west. In Yellowstone, about seven percent of the whitebark pine species have been impacted with the fungus, compared to nearly complete infestations in northwestern Montana. Quaking Aspen and willows are the most common species of deciduous trees. The aspen forests have declined significantly since the early 20th century, but scientists at Oregon State University attribute recent recovery of the aspen to the reintroduction of wolves which has changed the grazing habits of local elk.
There are dozens of species of flowering plants that have been identified, most of which bloom between the months of May and September. The Yellowstone Sand Verbena is a rare flowering plant found only in Yellowstone. It is closely related to species usually found in much warmer climates, making the sand verbena an enigma. The estimated 8,000 examples of this rare flowering plant all make their home in the sandy soils on the shores of Yellowstone Lake, well above the waterline.
In Yellowstone's hot waters, bacteria form mats of bizarre shapes consisting of trillions of individuals. These bacteria are some of the most primitive life forms on earth. Flies and other arthropods live on the mats, even in the middle of the bitterly cold winters. Initially, scientists thought that microbes there gained sustenance only from sulfur. In 2005 researchers from the University of Colorado at Boulder discovered that the sustenance for at least some of the diverse hyperthermophilic species is molecular hydrogen.
Thermus aquaticus is a bacterium found in the Yellowstone hot springs that produces an important enzyme (Taq polymerase) that is easily replicated in the lab and is useful in replicating DNA as part of the polymerase chain reaction (PCR) process. The retrieval of these bacteria can be achieved with no impact to the ecosystem. Other bacteria in the Yellowstone hot springs may also prove useful to scientists who are searching for cures for various diseases.
Non-native plants sometimes threaten native species by using up nutrient resources. Though exotic species are most commonly found in areas with the greatest human visitation, such as near roads and at major tourist areas, they have also spread into the backcountry. Generally, most exotic species are controlled by pulling the plants out of the soil or by spraying, both of which are time consuming and expensive.
Yellowstone is widely considered to be the finest megafauna wildlife habitat in the lower 48 states. There are almost 60 species of mammals in the park, including the gray wolf, the threatened lynx, and grizzly bears. Other large mammals include the bison (often referred to as buffalo), black bear, elk, moose, mule deer, white-tailed deer, mountain goat, pronghorn, bighorn sheep, and mountain lion.
Bison graze near a hot spring
The Yellowstone Park bison herd is the largest public herd of American bison in the United States. The relatively large bison populations are a concern for ranchers, who fear that the species can transmit bovine diseases to their domesticated cousins. In fact, about half of Yellowstone's bison have been exposed to brucellosis, a bacterial disease that came to North America with European cattle that may cause cattle to miscarry. The disease has little effect on park bison, and no reported case of transmission from wild bison to domestic livestock has been filed. However, the Animal and Plant Health Inspection Service (APHIS) has stated that bison are the "likely source" of the spread of the disease in cattle in Wyoming and North Dakota. Elk also carry the disease and are believed to have transmitted the infection to horses and cattle. Bison once numbered between 30 and 60 million individuals throughout North America, and Yellowstone remains one of their last strongholds. Their populations had increased from less than 50 in the park in 1902 to 4,000 by 2003. The Yellowstone Park bison herd reached a peak in 2005 with 4,900 animals. Despite a summer estimated population of 4,700 in 2007, the number dropped to 3,000 in 2008 after a harsh winter and controversial brucellosis management sending hundreds to slaughter. The Yellowstone Park bison herd is believed to be one of only four free roaming and genetically pure herds on public lands in North America. The other three herds are the Henry Mountains bison herd of Utah, at Wind Cave National Park in South Dakota and on Elk Island in Alberta.
Elk Mother Nursing Her Calf
To combat the perceived threat of brucellosis transmission to cattle, national park personnel regularly harass bison herds back into the park when they venture outside of the area's borders. During the winter of 1996–97, the bison herd was so large that 1,079 bison that had exited the park were shot or sent to slaughter. Animal rights activists argue that this is a cruel practice and that the possibility for disease transmission is not as great as some ranchers maintain. Ecologists point out that the bison are merely traveling to seasonal grazing areas that lie within the Greater Yellowstone Ecosystem that have been converted to cattle grazing, some of which are within National Forests and are leased to private ranchers. APHIS has stated that with vaccinations and other means, brucellosis can be eliminated from the bison and elk herds throughout Yellowstone.
A reintroduced northwestern wolf in Yellowstone National Park
Starting in 1914, in an effort to protect elk populations, the U.S. Congress appropriated funds to be used for the purposes of "destroying wolves, prairie dogs, and other animals injurious to agriculture and animal husbandry" on public lands. Park Service hunters carried out these orders, and by 1926 they had killed 136 wolves, and wolves were virtually eliminated from Yellowstone. Further exterminations continued until the National Park Service ended the practice in 1935. With the passing of the Endangered Species Act in 1973, the wolf was one of the first mammal species listed. After the wolves were extirpated from Yellowstone, the coyote then became the park's top canine predator. However, the coyote is not able to bring down large animals, and the result of this lack of a top predator on these populations was a marked increase in lame and sick megafauna.
Bison in Yellowstone National Park
By the 1990s, the Federal government had reversed its views on wolves. In a controversial decision by the U.S. Fish and Wildlife Service (which oversees threatened and endangered species), northwestern wolves, imported from Canada, were reintroduced into the park. Reintroduction efforts have been successful with populations remaining relatively stable. A survey conducted in 2005 reported that there were 13 wolf packs, totaling 118 individuals in Yellowstone and 326 in the entire ecosystem. These park figures were lower than those reported in 2004 but may be attributable to wolf migration to other nearby areas as suggested by the substantial increase in the Montana population during that interval. Almost all the wolves documented were descended from the 66 wolves reintroduced in 1995–96. The recovery of populations throughout the states of Wyoming, Montana and Idaho has been so successful that on February 27, 2008, the U.S. Fish and Wildlife Service removed the Northern Rocky Mountain wolf population from the endangered species list.
An estimated 600 grizzly bears live in the Greater Yellowstone Ecosystem, with more than half of the population living within Yellowstone. The grizzly is currently listed as a threatened species, however the U.S. Fish and Wildlife Service has announced that they intend to take it off the endangered species list for the Yellowstone region but will likely keep it listed in areas where it has not yet recovered fully. Opponents of delisting the grizzly are concerned that states might once again allow hunting and that better conservation measures need to be implemented to ensure a sustainable population. Black bears are common in the park and were a park symbol due to visitor interaction with the bears starting in 1910. Feeding and close contact with bears has not been permitted since the 1960s to reduce their desire for human foods. Yellowstone is one of the few places in the United States where black bears can be seen coexisting with grizzly bears. Black bear observations occur most often in the park's northern ranges and in the Bechler area which is in the park's southwestern corner.
Population figures for elk are in excess of 30,000—the largest population of any large mammal species in Yellowstone. The northern herd has decreased enormously since the mid‑1990s; this has been attributed to wolf predation and causal effects such as elk using more forested regions to evade predation, consequently making it harder for researchers to accurately count them. The northern herd migrates west into southwestern Montana in the winter. The southern herd migrates southward, and the majority of these elk winter on the National Elk Refuge, immediately southeast of Grand Teton National Park. The southern herd migration is the largest mammalian migration remaining in the U.S. outside of Alaska.
In 2003 the tracks of one female lynx and her cub were spotted and followed for over 2 miles (3.2 km). Fecal material and other evidence obtained were tested and confirmed to be those of a lynx. No visual confirmation was made, however. Lynx have not been seen in Yellowstone since 1998, though DNA taken from hair samples obtained in 2001 confirmed that lynx were at least transient to the park. Other less commonly seen mammals include the mountain lion and wolverine. The mountain lion has an estimated population of only 25 individuals parkwide. The wolverine is another rare park mammal, and accurate population figures for this species are not known. These uncommon and rare mammals provide insight into the health of protected lands such as Yellowstone and help managers make determinations as to how best to preserve habitats.
Eighteen species of fish live in Yellowstone, including the core range of the Yellowstone cutthroat trout—a fish highly sought by anglers. The Yellowstone cutthroat trout has faced several threats since the 1980s, including the suspected illegal introduction into Yellowstone Lake of lake trout, an invasive species which consume the smaller cutthroat trout. Although lake trout were established in Shoshone and Lewis lakes in the Snake River drainage from U.S. Government stocking operations in 1890, it was never officially introduced into the Yellowstone River drainage. The cutthroat trout has also faced an ongoing drought, as well as the accidental introduction of a parasite—whirling disease—which causes a terminal nervous system disease in younger fish. Since 2001, all native sport fish species caught in Yellowstone waterways are subject to a catch and release law. Yellowstone is also home to six species of reptiles, such as the painted turtle and Prairie rattlesnake, and four species of amphibians, including the Boreal Chorus Frog.
311 species of birds have been reported, almost half of which nest in Yellowstone. As of 1999, twenty-six pairs of nesting bald eagles have been documented. Extremely rare sightings of whooping cranes have been recorded, however only three examples of this species are known to live in the Rocky Mountains, out of 385 known worldwide. Other birds, considered to be species of special concern because of their rarity in Yellowstone, include the common loon, harlequin duck, osprey, peregrine falcon and the trumpeter swan.
As wildfire is a natural part of most ecosystems, plants that are indigenous to Yellowstone have adapted in a variety of ways. Douglas-fir have a thick bark which protects the inner section of the tree from most fires. Lodgepole Pines —the most common tree species in the park— generally have cones that are only opened by the heat of fire. Their seeds are held in place by a tough resin, and fire assists in melting the resin, allowing the seeds to disperse. Fire clears out dead and downed wood, providing fewer obstacles for lodgepole pines to flourish. Subalpine Fir, Engelmann Spruce, Whitebark Pine, and other species tend to grow in colder and moister areas, where fire is less likely to occur. Aspen trees sprout new growth from their roots, and even if a severe fire kills the tree above ground, the roots often survive unharmed because they are insulated from the heat by soil. The National Park Service estimates that in natural conditions, grasslands in Yellowstone burned an average of every 20 to 25 years, while forests in the park would experience fire about every 300 years.
About thirty-five natural forest fires are ignited each year by lightning, while another six to ten are started by people— in most cases by accident. Yellowstone National Park has three fire lookout towers, each staffed by trained fire fighters. The easiest one to reach is atop Mount Washburn, though it is closed to the public. The park also monitors fire from the air and relies on visitor reports of smoke and/or flames. Fire towers are staffed almost continuously from late June to mid-September— the primary fire season. Fires burn with the greatest intensity in the late afternoon and evening. Few fires burn more than 100 acres (40 ha), and the vast majority of fires reach only a little over an acre (0.5 ha) before they burn themselves out. Fire management focuses on monitoring dead and down wood quantities, soil and tree moisture, and the weather, to determine those areas most vulnerable to fire should one ignite. Current policy is to suppress all human caused fires and to evaluate natural fires, examining the benefit or detriment they may pose on the ecosystem. If a fire is considered to be an immediate threat to people and structures, or will burn out of control, then fire suppression is performed.
In an effort to minimize the chances of out of control fires and threats to people and structures, park employees do more than just monitor the potential for fire. Controlled burns are prescribed fires which are deliberately started to remove dead timber under conditions which allow fire fighters an opportunity to carefully control where and how much wood is consumed. Natural fires are sometimes considered prescribed fires if they are left to burn. In Yellowstone, unlike some other parks, there have been very few fires deliberately started by employees as prescribed burns. However, over the last 30 years, over 300 natural fires have been allowed to burn naturally. In addition, fire fighters remove dead and down wood and other hazards from areas where they will be a potential fire threat to lives and property, reducing the chances of fire danger in these areas. Fire monitors also regulate fire through educational services to the public and have been known to temporarily ban campfires from campgrounds during periods of high fire danger. The common notion in early United States land management policies was that all forest fires were bad. Fire was seen as a purely destructive force and there was little understanding that it was an integral part of the ecosystem. Consequently, until the 1970s, when a better understanding of wildfire was developed, all fires were suppressed. This led to an increase in dead and dying forests, which would later provide the fuel load for fires that would be much harder, and in some cases, impossible to control. Fire Management Plans were implemented, detailing that natural fires should be allowed to burn if they posed no immediate threat to lives and property.
1988 started with a wet spring season although by summer, drought began moving in throughout the northern Rockies, creating the driest year on record to that point. Grasses and plants which grew well in the early summer from the abundant spring moisture produced plenty of grass, which soon turned to dry tinder. The National Park Service began firefighting efforts to keep the fires under control, but the extreme drought made suppression difficult. Between July 15 and 21, 1988, fires quickly spread from 8,500 acres (3,400 ha; 13.3 sq mi) throughout the entire Yellowstone region, which included areas outside the park, to 99,000 acres (40,000 ha; 155 sq mi) on the park land alone. By the end of the month, the fires were out of control. Large fires burned together, and on August 20, 1988, the single worst day of the fires, more than 150,000 acres (61,000 ha; 230 sq mi) were consumed. Seven large fires were responsible for 95% of the 793,000 acres (321,000 ha; 1,239 sq mi) that were burned over the next couple of months. A total of 25,000 firefighters and U.S. military forces participated in the suppression efforts, at a cost of 120 million dollars. By the time winter brought snow that helped extinguish the last flames, the fires had destroyed 67 structures and caused several million dollars in damage. Though no civilian lives were lost, two personnel associated with the firefighting efforts were killed.
Contrary to media reports and speculation at the time, the fires killed very few park animals— surveys indicated that only about 345 elk (of an estimated 40,000–50,000), 36 deer, 12 moose, 6 black bears, and 9 bison had perished. Changes in fire management policies were implemented by land management agencies throughout the United States, based on knowledge gained from the 1988 fires and the evaluation of scientists and experts from various fields. By 1992, Yellowstone had adopted a new fire management plan which observed stricter guidelines for the management of natural fires.
from Wikipedia
I have been chatting with the delightful Jacqueline Landau about Lacie Satine & BadLacie. Other than giving myself large boobs, this is I think a lovely portrait, albeit poorly framed. A sign of my growing confidence, that I am starting to enjoy Satine.
Mushrooms or fungi on a piece wood fallen of a tree in , Arrowhead Provincial Park , Martin’s photographs , Huntsville , Ontario , Canada , August 23. 2016
Canada Gees swimming through the morning mist
Mist
Canada Gees swimming
Morning mist
Canada Gees
Canada Gees swimming through the morning mist in Arrowhead lake
Algonquin Park
Big East River which has its headwaters in Algonquin Park
Big Bend part of the Big East River in Arrowhead Provincial Park
Huntsville
Big Bend
Big East River
Snail
Large snail
Deer fly
Ontario parks
photograph converted to black and white
Fungus
Deer fly sitting on mushroom
Large snail crawling on a mushroom
fungus on a tree
converted to black and white
cropped photograph
Deer fly sitting on mushroom and a Large snail crawling on this tasty mushroom or fungus on a tree
Arrowhead
Provincial Park
black and white
Deer fly sitting on mushroom and a Large snail crawling on this tasty mushroom or fungus on a tree in
Arrowhead Provincial Park
photograph converted to black and white
cropped photograph
Martin’s photographs
Huntsville
Ontario
Canada
August 2016
Favourites
IPhone 6
Mushroom
Jawel
ⓒRebecca Bugge, All Rights Reserved
Do not use without permission.
Piccadilly Circus is perhaps the most famous road junction in the whole of London, built in 1819 to connect Regent Street and Piccadilly (the street that is). Already in the 19th century it was famous for there being a lot of traffic there due to it being the middle of the so called Theatreland.
The fountain is the Shaftesbury Memorial, erected in 1892-1893, was originally in the middle of the circus, but was moved to its current position after the second world war. The fountain was to commemorate the philanthropical work of Anthony Ashley-Cooper, 7th Earl of Shaftesbury. The winged figure on the top is sometimes called The Angel of Christian Charity (which is not what it's actually named) or Eros (which also is wrong). It is actually supposed to be Anteros - the god of requited love - symbolizing the the selfless work of the Earl for the poor. The nudity of the fountain was somewhat debated at the time of the unveiling - but generally the fountain got a good reception. It is the first statue in the world to be cast in aluminium - but the fountain itself is made of bronze. Now it is a popular meeting-place.
The name Piccadilly is first mentioned in 1626 and comes from a house belonging to the tailor Robert Baker famous for his piccadillies (a term for various terms for collars).
Last weekend a bunch of us gals went up to Whistler for a stagette. We all got decked out (well, minus me) and hit the town. Some of these girls were wearing some killer high heels. I don't know how they do it, but they definitely look like they could do some damage!
In 1894 a competition was held for the 1900 Exhibition area. The Palais de l'Industrie from the 1855 World’s Fair was considered unfitting and was to be replaced by something new for the 1900 Exhibition. Architects had the option to do what they pleased (alter, destroy, or keep) with the Palais de l’Industrie. In the end, Charles Girault won the competition and built the Petit Palais as one of the buildings that replaced the Palais de l’Industrie.
The construction of the Petit Palais began on October 10, 1897 and was completed in April 1900. The total cost of the Petit Palais at the time of the construction was 400,000 pounds.
Inspiration:
Charles Girault largely draws on the late seventeenth and early eighteenth century French style for the Petit Palais. Additionally his work, such as the domed central porch and the triple arcade, has many references to the stables at Chantilly.
Plan of the Building:
View from the Eiffel Tower
Girault’s plan for the Petit Palais had minimal alterations from the design to the execution. The plan was original and fit perfectly in its given location. The Petit Palais is a trapezoid shape with its larger side as the main façade facing the Grand Palais. The building’s shape makes a semi-circular courtyard at the center.
HERE
THE GARDEN
The trapezoid shape of the Petit Palace forms an open area at the center of the building. This enclosed area creates a semicircular, peristyle courtyard. The architecture of the courtyard incorporated many different architectural elements.
The elegant courtyard is considered Beaux Arts style because of the “symmetrical composition” and “rich decoration in high relief”. Coupled columns made of pink Vosges granite and gilt-bronze encircle the courtyard and bordering covered gallery.
Although the courtyard is in the central part of the Petit Palais, one of the main structures of the Exhibition, its purpose was to provide visitors with a relaxing space apart from the busy Exposition.
For more informations:
en.wikipedia.org/wiki/Petit_Palais
for the place:
wikimapia.org/#lang=en&lat=48.866207&lon=2.313749...
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“It is an illusion that photos are made with the camera…
they are made with the eye, heart and head.”
[Henry Cartier Bresson]
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Please don't use any of my images on websites, blogs or other media without my explicit written permission.
© All rights reserved
The term kathoey or katoey (Thai: กะเทย, IPA: [kaʔtʰɤːj]) generally refers to a male-to-female trans gender person or an effeminate gay male in Thailand. They are sometimes referred to as ladyboys, ladymen or as sao (or phuying) praphet song ("a second kind of woman"), or phet thee sam (third sex). The word kathoey is thought to be of Khmer origin.The term "kathoey" is not an exact equivalent of the modern western transwoman — it suggests that the person is a type of male, unlike the term sao praphet song, which suggests a female sex identity, or phet thee sam, which suggests a third gender.
An unusual ladyboy stories is that of Muay Thai boxer Parinya Kiatbusaba, better known by her nickname of Nong Toom. He would enter the weigh-in wearing full make up, and sometimes a wig, and goad his opponents by blowing kisses and generally acting effeminately. One of the reasons he entered the sport was to pay for a sex change operation. In 1999, at the age of 19, he underwent sex-change surgery in Bangkok, and reappeared as a statuesque and pretty female. She was now forbidden to fight, and took up a career in entertainment. A film called Beautiful Boxer was made about her life.
Two women of style in Newtown - one rocking a bouffant and one rocking a sword (and some barely-there shorts!)
The CORP Roseburg Hauler waits at a crossing just north of Wilbur Oregon for another CORP crew working the yard at Winchester. Once clear the hauler will run the last few miles south to Winchester where they wil tie up their train. The UP SD70M's used for this job are currently leased from Union Pacific, though in years past UP provided the power in exchange for CORP pre-blocking the train to keep UP's work needed at Eugene to a minimum.
Part of my 'Vacationers' series.
Taken with a Leica M6 + Voigtlander 35mm lens with Ilford XP2 super 400 film.
Honolulu, HI.
Passiflora, known also as the passion flowers or passion vines, is a genus of about 550 species of flowering plants, the type genus of the family Passifloraceae.
They are mostly tendril-bearing vines, with some being shrubs or trees. They can be woody or herbaceous. Passion flowers produce regular and usually showy flowers with a distinctive corona. The flower is pentamerous and ripens into an indehiscent fruit with numerous seeds. For more information about the fruit of the Passiflora plant, see passionfruit.
Have you been Naughty or Nice? You can see that Mandy has been naughty and Clem has been nice. I hope Santa brings you want you ask for if you've been nice. Merry Christmas.
(p.s. after I finished this, my Mister saw Clem in the tree, so he's been naughty too, but don't tell Santa!)
"We need to save those Elders who cannot speak for themselves -- the trees." ~ Haida Gwaii, Traditional Circle of Elders
The trees are the Elders of the Earth. Go to the forest or to the mountains and find a young tree. Then find an old tree. Spend time with each. Sit by the young tree and listen to your thoughts. Then move to an old tree and listen to your thoughts again. Just being in the presence of an old tree, you will feel more calm. Your thoughts will contain wisdom and your answers will be deeper. Why is this so? These old trees know more, have heard more, and are the Elders of the Earth. We must ensure these trees live so we can learn from them. My Creator, help me to protect the trees and listen to them.
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
all alone in a empty room
nothing left but the memory's
of whennn
i had my best friend
and i don't know how we ended up here
i don't know but it's never been so clear
we made a mistake dear
and i see the broken glass infront of me
i see your shadow hanging over me
and your face i can see
through the tree's
i will find you
i will heal
the ruins left inside you
cause im still here breathing now
im still here breathing now
im still here breathing now
im still here breathing now
until im set free
go quiet through the tree's
and i remember how we used to talk
about the places we will go when we were off
and all that we were gonna find
and i remember watching our seeds grow
and how you cried when you saw the first leaf show
the love was pouring for your eyes
so can you see
the branches hanging over me
can you see
the love you left inside of me
and my face
can you see
through the tree's
i will find you
i will heal
the ruins left inside you
cause im still here breathing now
im still here breathing now
im still here breathing now
im still here breathing now
until im set free
go quiet through the tree's
cause your not coming back
and your not coming back
noooooooooooooooooooooo
noooooooooooooooooooooo
nooo your not coming back
your not coming back
and take my breath
as your own
and take my eye's to guide you home
cause im still here breathing now
im still here breathing now
im still here breathing now
and im still here
cause im still here breathing now
im still here breathing now
im still here breathing now
and im still here
cuz im still here breathing now
im still here breathing now
im still here breathing now
and im still here
and your not coming back
im still here breathing now
and your not coming back
im still here breathing now
cause your not coming back
im still here breathing now
until im set free
go quiet through the tree's
* through the trees *- low shoulder (ryan levine)