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My attempt at painting a Llama, using Photoshop!
"Click here" Oil Painting! ............. Your turn to have a go; if you have Photoshop CS3, or later!
To view more of my images of Alpaca & Llama, please click "here" !
The Llama is a domesticated South American camelid, widely used as a meat and pack animal by Andean cultures since the Pre-Columbian era. The height of a full-grown, full-size llama is 1.7 to 1.8 m (5.6 to 5.9 ft) tall at the top of the head, and can weigh between 130 and 200 kg (290 and 440 lb). At birth, a baby llama (called a cria) can weigh between 9 and 14 kg (20 and 31 lb). Llamas typically live for 15 to 25 years, with some individuals surviving 30 years or more. They are very social animals and live with other llamas as a herd. The wool produced by a llama is very soft and lanolin-free. Llamas are intelligent and can learn simple tasks after a few repetitions. When using a pack, they can carry about 25 to 30% of their body weight for 8 to 13 km (5–8 miles). The name llama (in the past also spelled 'lama' or 'glama') was adopted by European settlers from native Peruvians. Llamas appear to have originated from the central plains of North America about 40 million years ago. They migrated to South America about three million years ago. By the end of the last ice age (10,000–12,000 years ago), camelids were extinct in North America. As of 2007, there were over seven million llamas and alpacas in South America, and due to importation from South America in the late 20th century, there are now over 158,000 llamas and 100,000 alpacas in the United States and Canada. Lamoids, or llamas (as they are more generally known as a group), consist of the vicuña (Vicugna vicugna, prev. Lama vicugna), guanaco (Lama guanicoe), Suri alpaca, and Huacaya alpaca (Vicugna pacos, prev. Lama guanicoe pacos), and the domestic llama (Lama guanicoe glama). Guanacos and vicuñas live in the wild, while alpacas – as well as llamas – exist only as domesticated animals. Although early writers compared llamas to sheep, their similarity to the camel was soon recognized. They were included in the genus Camelus along with alpaca in the Systema Naturae (1758) of Linnaeus. They were, however, separated by Cuvier in 1800 under the name of lama along with the guanaco. Alpacas and vicuñas are in genus Vicugna. The genera Lama and Vicugna are, with the two species of true camels, the sole existing representatives of a very distinct section of the Artiodactyla or even-toed ungulates, called Tylopoda, or "bump-footed", from the peculiar bumps on the soles of their feet. The Tylopoda consist of a single family, the Camelidae, and shares the order Artiodactyla with the Suina (pigs), the Tragulina (chevrotains), the Pecora (ruminants), and the Whippomorpha (hippos and cetaceans, which belong to Artiodactyla from a cladistic, if not traditional, standpoint). The Tylopoda have more or less affinity to each of the sister taxa, standing in some respects in a middle position between them, sharing some characteristics from each, but in others showing special modifications not found in any of the other taxa. The 19th-century discoveries of a vast and previously unexpected extinct Paleogene fauna of North America, as interpreted by paleontologists Leidy, Cope, and Marsh, aided understanding of the early history of this family. Llamas were not always confined to South America; abundant llama-like remains were found in Pleistocene deposits in the Rocky Mountains and in Central America. Some of the fossil llamas were much larger than current forms. Some species remained in North America during the last ice ages. North American llamas are categorized as a single extinct genus, Hemiauchenia. Llama-like animals would have been a common sight 25,000 years ago, in modern-day California, Texas, New Mexico, Utah, Missouri, and Florida. The camelid lineage has a good fossil record. Camel-like animals have been traced from the thoroughly differentiated, modern species back through early Miocene forms. Their characteristics became more general, and they lost those that distinguished them as camelids; hence, they were classified as ancestral artiodactyls. No fossils of these earlier forms have been found in the Old World, indicating that North America was the original home of camelids, and that Old World camels crossed over via the Bering Land Bridge. The formation of the Isthmus of Panama three million years ago allowed camelids to spread to South America as part of the Great American Interchange, where they evolved further. Meanwhile, North American camelids died out at the end of the Pleistocene.
From Wikipedia, the free encyclopedia
New portrait. Model: Guillaume. View all the edits I made on this photo in this video: youtu.be/N75KreP3u30
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Nouveau Portrait. Modèle: Guillaume. Vous pouvez voir toutes les différentes retouches que j'ai faites sur cette photo dans cette video: youtu.be/N75KreP3u30
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Photography: © Yaiza AB Photography
Cosplay: Illisia Cosplay and Photography
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To view more of my images, of Malham, Gardale Scar & Malham Cove, please click "here" !
Malham Cove is a natural limestone formation 1 km north of the village of Malham, North Yorkshire, England. A well-known beauty spot, it is a large, curved limestone cliff at the head of a valley, with a fine area of limestone pavement at the top. Describing the cove in 1779, Thomas West said, "This beautiful rock is like the age-tinted wall of a prodigious castle; the stone is very white, and from the ledges hang various shrubs and vegetables, which with the tints given it by the bog water. & c. gives it a variety that I never before saw so pleasing in a plain rock." On the west side of the 80 metre (260 foot) high cliff face are about 400 irregular stone steps: these form part of the route of the Pennine Way and lead to an uneven limestone pavement at the top. Originally, a large waterfall flowed over the cove as a glacier melted above it. The remnant of a stream which once fell over the cliff now flows out of the lake of Malham Tarn, on the moors 2 km north of the cove. That stream now disappears underground at the aptly named 'Water Sinks', 1.5 kilometres (one mile) before its valley reaches the top of the cove. A stream of a similar size (Malham Beck) emerges from a cave at the bottom of the cove. It used to be assumed that the two streams were one and the same. However, experiments with dyes have now shown that two separate streams go underground at different locations, cross paths without mixing behind the cliff, and re-emerge a couple of kilometres apart. This shows the complexity of the system of caves behind the cliff, which is thought to be around 50,000 years old. Divers have so far explored over 1.6 km of cave passage entered from the base of the cove. The lip of the cove has been more heavily eroded than the sides, creating a curved shape. A colossal amount of water used to flow over this waterfall, which measures 80 m (260 ft) high and over 300 m (1000 ft) wide. Nowadays the underlying cave systems have a large enough capacity to swallow any flood waters before it reaches the fall. The last record of water flowing over the fall in any kind of volume dates back to a period of heavy rain in the early 19th century. The valley was formed at the end of the last ice age when the ground was frozen. The frozen ground meant that meltwater from the melting ice sheet formed a large river flowing over the surface, eroding the valley that we see today. The water from this river flowed over Malham Cove to form a huge waterfall. When the climate warmed around 12,000 years ago the ground thawed and the river in the valley disappeared underground leaving the valley dry as we see it today.
The cove, along with nearby Gordale Scar, was featured in an episode of the BBC TV series Seven Natural Wonders as one of the natural wonders of Yorkshire. Gordale Scar is a limestone ravine 1 mile (1.6 km) northeast of Malham, North Yorkshire, England. It contains two waterfalls and has overhanging limestone cliffs over 100 metres high. The gorge could have been formed by water from melting glaciers or a cavern collapse. The stream flowing through the scar is Gordale Beck, which on leaving the gorge flows over Janet's Foss before joining Malham Beck two miles downstream to form the River Aire. A right of way leads up the gorge, but requires climbing approximately 10 feet of tufa at the lower waterfall. William Wordsworth wrote in the sonnet Gordale, "let thy feet repair to Gordale chasm, terrific as the lair where the young lions couch". James Ward created a large and imaginative painting of it that can be seen in Tate Britain. J. M. W. Turner also painted a picture of it in 1816, also to be seen in Tate Britain.
The Cove was also featured in the film Harry Potter and the Deathly Hallows (Part 1) as one of the places Hermione and Harry travel to. The scenes were filmed in November 2009.
From Wikipedia, the free encyclopedia
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Danbo Vader vs. Danbo Skywalker.. we probably know how that ends :D I know it's not high quality photo editing but I had fun doing this :)
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Photo: kodak.t-max.35.mm.print.film
Camera: Nikon FE2 with a 20mm Nikon Lens
Personalized Christmas Card
Photographer: Daniel Arauz
Creative Director: Alex Calder www.flickr.com/photos/44446587@N05/
Model: Alex Calder
Vehicle: 1970 Black Cadillac M&M Hearse Olympia End Loader
Location: Holy Cross Cemetery, Culver City, CA, L.A. County
www.youtube.com/watch?v=CRED67S57gg&feature=related
02/10