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February 6th, 2016
A 3-light-year-long pillar, bathed in the glow of light from hot, massive stars to the top of the image. Scorching radiation and fast winds (streams of charged particles) from these stars are sculpting the pillar and causing new stars to form within it. Streamers of gas and dust can be seen flowing off the top of the structure.
Nestled inside this dense structure are fledgling stars. They cannot be seen in this image because they are hidden by a wall of gas and dust. Although the stars themselves are invisible, one of them is providing evidence of its existence. Thin puffs of material can be seen traveling to the left and to the right of a dark notch in the center of the pillar. The matter is part of a jet produced by a young star. Farther away, on the left, the jet is visible as a grouping of small, wispy clouds. A few small clouds are visible at a similar distance on the right side of the jet. Astronomers estimate that the jet is moving at speeds of up to 850,000 miles an hour. The jet's total length is about 10 light-years.
Composed of gas and dust, the pillar resides in a tempestuous stellar nursery called the Carina Nebula, located 7,500 light-years away in the southern constellation Carina.
By Dominic Kamp
November 29th, 2016
It is said that Tolkien travelled through the landscape of Switzerland to the Lauterbrunnen Valley, a deep valley that many people now believe was the direct inspiration for the valley of Rivendell, a place instrumental to events both in The Hobbit and The Lord of the Rings.
The name Rivendell itself means "Deeply Cloven Valley" and the Lauterbrunnen, with its steep sides and many waterfalls (72 to be exact), certainly fits this description, with the mountains of the Eiger, Monch, and Jungfrau lying beyond.
Adobe Photoshop and Adobe Lightroom, Color Efex, Turkey Bacon Avocado Sandwich.
Map: 46.6000, 7.9089
July 23rd, 2016
The form of the coastline around Durdle Door is controlled by its geology--both by the contrasting hardnesses of the rocks, and by the local patterns of faults and folds.The arch has formed on a concordant coastline where bands of rock run parallel to the shoreline. The rock strata are almost vertical, and the bands of rock are quite narrow. Originally a band of resistant Portland limestone ran along the shore, the same band that appears one mile along the coast forming the narrow entrance to Lulworth Cove. Behind this is a 120-metre (390 ft) band of weaker, easily eroded rocks, and behind this is a stronger and much thicker band of chalk, which forms the Purbeck Hills. These steeply dipping rocks are part of the geological structure known as the Lulworth crumple, itself part of a broader monocline (a kinked type of geological fold) produced by the building of the Alps during the mid-Cenozoic.
Nikon D800E, Samyang 14mm F2.8 IF ED MC Aspherical.
Photo Settings: 14mm, f/9, 1/200 second, ISO 125.
Map: 50.6225, -2.2725