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Lower Antelope Canyon, Page, Arizona
visitors: 1h Guided Tour
photographers: 2h photo pass (only SLR, medium or large format WITH a tripod)
The name of the village of Lower Slaughter stems from the Old English name for a wet land 'slough' or 'slothre' (Old English for muddy place) upon which it lies. This quaint village sits beside the little Eye stream and is known for it's unspoilt limestone cottages in the traditional Cotswold style.
The stream running through the village is crossed by two small bridges and the local attraction is a converted mill with original water wheel selling craft type products.
Lower Than Atlantis
Opening for All Time Low
Glasgow o2 Academy
Saturday February 9th 2013
All photos taken by Stacey @ Music Box Unwinds
All rights reserved.
DO NOT REMOVE WATERMARK/CREDIT OR EDIT IN ANY WAY!
The lower level of Miller Park, looking towards the umpire and visitor clubhouses and the leftfield area.
Inch-scale layered plagioclase feldspar and pyroxene in the Precambrian of Montana, USA.
Southern Montana’s Beartooth Mountains has one of the few platinum mines in North America. There, platinum and palladium are mined from the 2.71 billion-years-old Stillwater Complex, a classic example of an LLI (large, layered igneous province). LLIs are large intrusive bodies that display large-scale and small-scale layering, even including cross bedding, ripples, graded bedding, channelforms, and other sedimentary-like features. The Stillwater originated as a large subsurface mass of slowly cooling magma. As various minerals crystallized, they settled to the bottom of the magma chamber - this resulted in layering. Igneous rocks that formed this way have a cumulate texture. Currents in the still-liquid portions of the magma chamber produced the sedimentary structures mentioned above. Most of the Stillwater displays only large-scale layering.
The rocks in the Stillwater are mafic and ultramafic, intrusive igneous rocks. Common lithologies include gabbro, norite, harzburgite, anorthosite, troctolite, chromitite, pyroxenite, and dunite. Portions of the Stillwater have been metamorphosed. Olivine is the most commonly altered component - it's usually been metamorphosed to serpentine.
The main platinum (Pt) and palladium (Pd) occurrence is in the Johns-Manville Reef (J-M Reef), an interval in the lower part of the Lower Banded Series. The Pt and Pd occur in intercumulate sulfides, typically pyrrhotite (Fe1-xS) and chalcopyrite (CuFeS2). Platinum ores in the J-M Reef are principally sulfidic anorthosites, but other lithologies also occur. The J-M Reef is the highest grade deposit known for platinum-group elements (PGEs).
The outcrop seen here does not have platinum ore. The layering consists of alternating bands of plagioclase feldspar and pyroxene. The layering was originally horizontal; Stillwater Complex rocks have been structurally tilted by mountain building.
Stratigraphy: Lower Banded Series, Stillwater Complex, Neoarchean, 2.71 Ga
Locality: roadcut along West Fork Stillwater Road (= Forest Service Road 2846), near & above the Stillwater Mine, Beartooth Mountains, southern Montana, USA
This is the Lower Yosemite Falls - we 'hiked' up to it (everything is a 'trail' or a 'hike' here, when ost of the time it's just a stroll along the path). We did have to scrable over some slippery rocks, but it was worth it when we got here.
These falls are not so impressive in the summer - they're a bit dried up.
just cracked it open, inspecting the damage. Actually didn't look that bad, I guess I was expecting something more dramatic. At this point I had never seen inside an engine in a really hands on way, so this was pretty sweet. You can see the tops of the pistons are black...wanted to clean them but wasn't sure how to do so without contaminating the engine with debris. I think getting a shop vac hooked up with a stiff brush would have done the trick.
Getting to this point was very difficult for me. To remove the upper head the cams have to be aligned, and then held as the springs from the valves release tension as the upper head is unbolted and lifted off. But, I was able to do it by myself.
Five years after Katrina the Lower Ninth Ward still has block upon block of blighted property. Photo courtesy Claire Menck
Select photos and a corresponding article were published in Anthropology News (52:4), official newspaper of the American Anthropological Association.
Lower Gledfield
View looking East.
ID:MHG9165
Type of record:Monument
Name:1 Church Street, Lower Gledfield
Grid Reference:NH 59275 90970
Map Sheet:NH59SE
Civil Parish:KINCARDINE
Geographical Area:SUTHERLAND
Site Type COTTAGE(S)
Canmore ID 13048
Site Number NH59SE 14
NGR NH 5929 9096
Council HIGHLAND
Parish KINCARDINE (SUTHERLAND)
Former Region HIGHLAND
Former District SUTHERLAND
Former County ROSS AND CROMARTY
ID:MHG9166
Type of record:Monument
Name:2 Church Street, Lower Gledfield
Grid Reference:NH 59289 90966
Map Sheet:NH59SE
Civil Parish:KINCARDINE
Geographical Area:SUTHERLAND
Site Type COTTAGE
Canmore ID 13049
Site Number NH59SE 15
NGR NH 59305 90947
Council HIGHLAND
Parish KINCARDINE (SUTHERLAND)
Former Region HIGHLAND
Former District SUTHERLAND
Former County ROSS AND CROMARTY
ID:MHG9167
Type of record:Monument
Name:3 Church Street, Lower Gledfield
Grid Reference:NH 59302 90963
Map Sheet:NH59SE
Civil Parish:KINCARDINE
Geographical Area:SUTHERLAND
Site Type GENERAL VIEW
Canmore ID 13050
Site Number NH59SE 16
NGR NH 5904 9092
Council HIGHLAND
Parish KINCARDINE (SUTHERLAND)
Former Region HIGHLAND
Former District SUTHERLAND
Former County ROSS AND CROMARTY