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Another one from the wonderful Ballintoy, for this one I climbed up a very steep sea stack it was pretty dam windy up there so I had the tripod flat on the ground so this shot was taken lying down.
EXIF: 24mm | ISO:100 | 37s @ ƒ/16 | Lee 0.9s GND + Lee 10 Stop
I'd been wanting to check out these stacks for a long exposure and finally went over there with my friend Chris and broke out the star machine.
Chris was featured this month on yahoo!'s Weekly flickr. Check it out here, you'll have to endure some ads first but it's well worth it. screen.yahoo.com/weekly-flickr-many-wonders-light-2224183...
..and check out the stellar work he does: www.flickr.com/photos/christopherrenfrophotography/678724...
My new facebook:
South Stack is a tiny island off the north-western tip of Holy Island - itself an island off the north-western tip of Anglesey. It is joined to Holy island by a small suspension bridge for pedestrians, at the foot of a steep flight of 350 steps down the cliffs, and is crowned by a 90ft lighthouse, now automatically operated.
A westbound NS stack train makes it way over the Ohio Connecting Bridge on the Mon Line in Pittsburgh.
Nikon AF Micro Nikkor 60mm f/2.8D on 60 mm extension tube
focus stack of 4 images combined with Zerene Stacker (DMap)
Marchin - Condroz - Belgique
I was happy to catch these 2 sun dogs (the bits of rainbows on either side of the sun) and a little later, the sun pillar that appeared as the sun got close to the horizon, which you can see in the timelapse video one my instagram page www.instagram.com/mattmolloyphoto/
I made this time stack by combining 251 photos into one image. Here's a quick and easy Photoshop tutorial of the process I use to make time stacks. youtu.be/oTfp47jTzWc
This circular brick wall is the same size as the top of the Anaconda Stack. The walkway I'm on is the size of the base of the stack.
NS 3674 leads intermodal train NS 259 westbound through Mexico, Pennsylvania, along the Middle Division of the NS Pittsburgh Line.
An unique building on the corner of Stewart St. and 1st Avenue in Seattle, where the upper floors do not quite line up. Interesting design choice.
A cairn of rocks on a rainy day. Found along side a forest service road near Icicle Creek, Leavenworth, Washington
Nikon D7000
Among the most impressive sights along the Jurassic Coast are the sea stacks at Ladram Bay. The sandstones contain numerous vertical fractures and joints that were formed deep in the Earths crust during past mountain building periods. The sea picked out these planes of weakness to form caves and natural arches that have since collapsed to produce sea stacks. The “Otter Sandstone” that forms the cliffs and sea stacks were deposited in a hot dry climates in the Triassic Period about 220 Million years ago. The stacks are composed of the same rock, which is relatively soft, but they have a harder band of sandstone at their base which prevents their rapid erosion by the sea. The striking red colour of the rock is caused by iron oxide, which tells us that the layers were formed in a desert. The presence of ripple marks and channels in the sandstones, together with the remains of the long-extinct plants, insects, fish, amphibians and reptiles, show that the desert was crossed by fertile river valleys.
The “Otter Sandstone” is the richest source of Triassic reptile remains in Britain and one of the most important in the world. At the south-west end of the bay, the most common fossils in the sandstone are networks of vertical, tube-like carbonate petrifactions (rhizocretions): these represent the roots of plants that were able to survive in the harsh dry climate of the Triassic Period.[2]
The bay is sited on the same band of Sandstone that forms the oil reservoir at the Wytch Farm oilfield on the Isle of Purbeck.