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The cemetery is behind the Luther Home on the grounds of the Luther Complex. To reach the cemetery, park in the Luther Home parking lot, walk to the back of the building and down the trail leading near the creek and into the cemetery. It is fenced in but the gate has been knocked down with other parts of the fencing by falling trees. In front of the fence is a large stone with a plaque that reads:
Maple Grove Cemetery
Established 1857
Burial records are sketchy and were never accurately maintained. It will never be known exactly how many people have been laid to rest in this "Potter's Field." All available records on file at the Kent County Clerk's Office, Kent County Library and at the Administration office of the adjoining facility.
this was the discription in 1999, this is a collage of pic's i took there today. Seems the Luther Home has put houses behind there. It looks like several graves have sunk in and no headstones, after all no one cares its just a "Potters Field"
The Third Avenue Hotel Complex, constructed in 1899, is closely associated with the commercial development of Dawson City during the Klondike Gold Rush.
They are leaning because of melting perfmafrost, and the freeze/thaw cycle.
The Third Avenue Hotel provided inexpensive accommodation for the town’s mobile and constantly fluctuating population.
Source: www.historicplaces.ca/
The Temple of Heaven, literally the Altar of Heaven is a complex of Taoist buildings situated in the southeastern part of central Beijing, in Xuanwu District. The complex was visited by the Emperors of the Ming and Qing dynasties for annual ceremonies of prayer to Heaven for good harvest. It is regarded as a Taoist temple, although Chinese Heaven worship, especially by the reigning monarch of the day, pre-dates Taoism
The temple complex was constructed from 1406 to 1420 during the reign of the Yongle Emperor, who was also responsible for the construction of the Forbidden City in Beijing. The complex was extended and renamed Temple of Heaven during the reign of the Jiajing Emperor in the 16th century. The Jiajing Emperor also built three other prominent temples in Beijing, the Temple of Sun in the east (日坛), the Temple of Earth in the north (地坛), and the Temple of Moon in the west (月坛). The Temple of Heaven was renovated in the 18th century under the Qianlong Emperor.
Gyeongju, South Korea - 22 May 2020: There are a number of Tomb complexes in Gyeongju where royal families have been buried over the centuries, at the center of them all is Daereungwon, well preserved in its own walled area with tranquil gardens.
it tried to open a raw photo on word pad (dont ask why)
and this very very very weird document came up and in my frustration and eagerness i am trying to use it as it was going to be a great shot but now its just this overlay of symbols?
Rotterdam; Zuid; Premierevoorstelling in complex Ahoy van Netherlands Military Tattoo 2006 Rotterdam. muziek, trompet, drums, Saxofoon, Bastuba, tuba, Trombone, trommel, militair, dansgroep, Nederland, Rotterdam; South; Premiere performance in the Ahoy complex of Netherlands Military Tattoo 2006 Rotterdam. music, trumpet, drums, saxophone, bass tuba, tuba, trombone, drum, military, dance group, netherlands
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
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
Taken at the 'Safety Zone' located on Jordan Hill Rd near Granit Ridge Rd. Fire burned up the hill and past the safety zone. A home across the road from the safety zone was saved by firefighter intervention, however others were lost to the fire.
Exclusive Cover #99B Once purchased the design is removed from the site and exclusive to you! To order or for more info email: design@siegeind.com
From my new set, "Dragonflies - III:"
Dragonflies – III:
www.flickr.com/photos/motorpsiclist/sets/72157636180249003/
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Dragonflies:
www.flickr.com/photos/motorpsiclist/sets/72157627417639364/
Dragonflies – II:
www.flickr.com/photos/motorpsiclist/sets/72157633160115841/
Dragonflies – III:
www.flickr.com/photos/motorpsiclist/sets/72157636180249003/
Dragonfly Mortuary/Autopsy:
www.flickr.com/photos/motorpsiclist/sets/72157630854477176/
Dragonflies in flight:
www.flickr.com/photos/motorpsiclist/sets/72157635247891642/
Dragons Munching Bugs:
www.flickr.com/photos/motorpsiclist/sets/72157635320430576/
Roseate Skimmer:
www.flickr.com/photos/motorpsiclist/sets/72157631175837296/
Carolina Saddlebags:
www.flickr.com/photos/motorpsiclist/sets/72157635534100705/
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Copyright © notice: My photographs and videos and any of my derivative works are my private property and are copyright © by me, John Russell (aka "Zoom Lens") and ALL my rights, including my exclusive rights, are reserved and protected by United States Copyright Laws and by the Berne Convention and the Universal Copyright Convention.
ANY use without my permission in writing is forbidden by law.
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The Kingsport Aquatic Center is water fun for everyone – indoors and out! For daily hours, admission prices, a map and other info, visit www.swimkingsport.com.
At MBU's new 47,000 square foot Carl and Deloris Petty Sports and Recreation Complex. October, 2011.
De poelkikker is de kleinste van de drie groene kikkers. Hij is op de rug grasgroen tot bruin van kleur (soms met donkere vlekken). Vaak heeft hij een lichte lengtestreep op de rug en een witte buik die hooguit zwak gevlekt is. Hij heeft relatief korte achterpoten. En hij wordt tot maximaal 8 cm groot. Het belangrijkste kenmerk is de grote harde halvemaanvormige graafknobbel, die symmetrisch is. Zie hiervoor de Herkenningskaart groene kikkers. Mannetjes hebben witte kwaakblazen en krijgen, in de paartijd, een ongevlekte geelgroene kleur met een goudgele iris.
Herkenning is alleen mogelijk na vangst en bestudering van de hierboven beschreven kenmerken, of wanneer de mannetjes duidelijk roepen. Maar zelfs na vangt is het soms niet mogelijk om tot soortdeterminatie te komen. Bij twijfel, en zichtwaarnemingen, altijd "groene kikker onbepaald" (Pelophylax spec.) aanhouden. Eieren, larven en juvenielen zijn sowieso niet tot op soort te determineren en kunnen als "groene kikker onbepaald" worden aangemerkt.