View allAll Photos Tagged liquid
Domestic Abuse and Sexual Assault Crisis Center of Warren County gets a facelift and renovation as part of the Jesus Loves Jersey outreach across NJ, courtesy of a great team of Liquid Church volunteers.
Liquid Laundry is an upscale gastro pub that also brews its own beer and brings in craft beer from all over the world, often there are special events for beer drinkers too.
“UmTi” and “APA” of Team Liquid Honda react onstage after victory against 100 Thieves at LCS Spring Split Playoffs at the Riot Games Arena in Los Angeles, CA, on March 22, 2024. (Photo by Marv Watson / Riot Games)
Liquid Church Services 2014-03-30 (Cold Case Christianity, Week 2)
Guest speaker J. Warner Wallace, Author of Cold Case Christianity
Collagen is the mechanical strength of bones, joints and the entire body structure. Liquid Collagen repairs and builds connective tissue to improve elasticity, improves vascular quality to help improve circulation, and can promote wound healing and clearer facial skin.
For more details visit - bit.ly/3qT0723
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