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The Ian Potter Centre - National Gallery of Victoria.
I love the building. It's beautifully designed.
Somehow it reminds of one of M.C. Escher's Drawings.
One more interpretation of cool installation in front of downtown art gallery (nighttime), Fort Myers, Florida
The clean lines and geometric curves of the Da Lat opera house create an abstract composition. I focused on the play of light and shadow across the structure, simplifying the scene into a study of form and symmetry.
Shot with a Minox 35 GT-E
Minox Color-Minotar 35mm f/2.8 lens
Ilford HP5+ 400 film
Shot at EI 400
Developed in the Ego Lab using XTOL (1:1, 6:23min at 82F, agitated first and each minute)
Scanned on a Super Coolscan 9000ED
Shot with a Minox 35 GT-E
Minox Color-Minotar 35mm f/2.8 lens
Kentmere Pan 100 film
Shot at EI 800 and pushed +3
Developed in the Ego Lab using HC-110 (1:31, 12:11min at 88F, agitating first and each minute)
Scanned with a Coolscan 9000ED
Shot with a Minolta CLE
Leitz 40mm f/2 Summicron-C lens
Eastman Kodak Double-X film
Shot at EI 200
Developed in the Ego Lab using XTOL (1:1, 7:56min at 72F, agitated first and each minute)
Scanned on a Super Coolscan 9000ED
Active rock glacier (Marinet I) in Ubaye, France. Marinet II in the background.
Rock glaciers are landforms consisting either of angular rock debris frozen in interstitial ice, former "true" glaciers overlain by a layer of talus, or something in between. Rock glaciers may extend outward and downslope from talus cones, glaciers or terminal moraines of glaciers. There are two types of rock glaciers: periglacial glaciers, or talus-derived glaciers, and glacial rock glaciers, which are often found in the former places of glaciers.
Most glacial rock glaciers are created by the recession of debris covered glaciers. Glacial rock glaciers are often found in cirque basins where rocky debris falls off the steep sides and accumulates on ice glaciers. As the glaciers shrink, their composition changes as they become increasingly covered with debris. Eventually, the glacial ice is replaced by ice cored rocks.
With the exception of ice-cored rock glaciers, rock glaciers are a periglacial process. This means that they are a nonglacial landform associated with cold climates, particularly with various aspects of frozen ground. Periglacial rock glaciers require permafrost instead of glacial ice in order to form. Instead, they are caused by continuous freezing occurring within a talus lobe.
Facebook : Aegir Photography
500px : 500px.com/photo/171619883/angular-by-glenn-crouch
Sunrise at Bunker Bay, near Dunsborough, Western Australia.
Nikon D810 & Nikkor 16-35mm, Breakthrough 6 stop filter. PP in PS CC using Nik Software and luminosity masks.
The lower strata are the Early Oligocene Port Willunga Formation, consisting of Bryozoal limestone, silt and clays, dipping gently southwards (towards the right on the photo). About halfway up the cliff, these dipping strata are truncated by an overlying horizontal layer of strongly cemented sandstone. This is the Pliocene Hallet Cove sandstone, consiting of calcareous sandstone and sandy limestone. This angular unconformity represents a 20 myr break in deposition
Odontomyia angulata (Diptera, Stratiomyidae) female. Size: 11 mm.
Focus stacked image taken in the early morning under natural light. This work is a gift for me, regarding the weather it was made in. Stacking living insects usually requires cool and windless weather. This time it was a warm morning with 25°C! However, the fly was friendly enough and stayed still throgh the stacking sequence.
Uncropped image, 2.7x magnification with the MP-E65/2.8 lens at f/5, 1/8 sec., ISO 200. 41 shots were combined in Zerene Stacker.
I isolated this architectural corner to create a study in pure form. The converging lines and subtle gradations of light transform a utilitarian structure into an abstract composition of light and space.