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Complexul monahal Hurezi [Hurez, Hurezu, Horez], de la Romanii de Jos, este situat în nordul provinciei Olteniei.
În depresiunea subcarpatică Hurezu, la cca. 5 km N de drumul naţional DN 67 ce face legătura între oraşele capitală de judeţ Râmnicu Vâlcea şi Târgu-Jiu, pe malul stâng al văii Romanilor, la cca. 570 m altitudine.
Mănăstirea Hurezi este cel mai vast şi cel mai dezvoltat ansamblu monastic din Tara Româneasca.
Prin elementele de ordin arhitectural şi artistic este un unicat nu doar în arhitectura româneasca, ci şi în cea a sud-estului Europei, o sinteză post-bizantina, fidelă tradiţiei ortodoxe, edificata atât după principiile ordonatoare ale Renaşterii italiene cât şi după tipicul marilor mănăstiri de la Muntele Athos.
Mănăstirea Hurezi, ctitoria domnitorului Constantin Brâncoveanu (1688-1714) a fost începuta în 1690, completată şi extinsă de egumenii mănăstirii în mai multe etape: 1734 -1735, 1829 - 1854 şi 1854 - 1873.
Hurezii pun în evidentă un program complex, nou, niciodată reluat în Tara Româneasca, conceput potrivit unor trasee regulatoare renascentiste, după o axă orientată est-vest, cu o incinta principală de plan dreptunghiular - în centrul căreia se află "Biserica mare", catholiconul - şi patru schituri subordinate ansamblului major, amplasate în afară incintei mari, spre cele patru puncte cardinale.
"Biserica Mare", cu hramul Sfinţii Împăraţi Constantin şi Elena, era destinată să devină necropola a familiei lui Constantin Brâncoveanu.
În epoca, Hurezii devin un mare centru artistic în jurul căruia s-a născut "stilul brâncovenesc", model de referinţă, cu o mare varietate de interpretări, până după 1800.
Ansamblul de la Hurezi a încununat procesul de elaborare a unui ordin muntenesc, denumit de urmaşi "stilul brâncovenesc"
Manastirea Hurezi, renumita lavra domneasca a familiei Brancoveanu, se afla asezata la poalele line ale Muntelui Capatanii, la marginea satului Romanii de Sus, localitate aflata la o distanta de aproximativ 50 de kilometri inspre vest de Ramnicu-Valcea, pe Drumul National DN 67, in judetul Valcea.
Fiind considerata cea mai reprezentativa constructie in stil brancovenesc din intreaga tara, Manastirea Hurezi este poate si cel mai mare ansamblu monahal din Romania.
Singuratatea si linistea de odinioara a locului era tulburata doar de cantecele huhurezilor, pasari de noapte, care au si dat denumirea locului.
Ansamblul monahal de la Hurezi se intinde pe mai mult de trei hectare, cuprinzand manastirea propriu-zisa, Biserica Bolnita, Schitul Sfintilor Apostoli si Schitul Sfantul Stefan.
Acestora li se poate adauga, in mod firesc, si Biserica Sfintii Ingeri, ctitorita tot de unul dintre staretii manastirii celei mari, aflata putin mai la sud de incinta manastirii.
Incepand cu anul 1993, manastirea de la Hurezi se afla pe lista Patrimoniului Mondial UNESCO.
Numele manastirii se trage de la pasarile numite "huhurezi", pasari de noapte cu un penaj deosebit de colorat.
Potrivit legendei locale, mesterii tocmiti de Sfantul Constantin Brancoveanu, anume sa construiasca o mareata lavra, din cauza turcilor, erau nevoiti sa lucreze mai mult noaptea, cand se auzeau numai huhurezii.
Manastirea Hurezi prezinta doua incinte: prima incinta este delimitata de ziduri din caramida, nu foarte inalte, care cuprind atat manastirea, cat si schiturile acesteia, in vreme ce a doua incinta este fortificata si deosebit de inalta, avand cladiri pe trei laterale, iar spre rasarit un zid inalt.
In centrul incintei principale se afla biserica cea mare de la Hurezi. I
ntrarea principala este asezata pe latura de miazazi, sub o bolta larga care, la vreme de necazuri, se inchidea cu o poarta masiva de lemn, ferecata cu fier, existenta si astazi, in forma ei originala.
Intrarea este asezata sub turnul-clopotnita, in care se afla, pana astazi, patru clopote mari, avand intre 300 si 1.000 de kilograme.
Pe trei clopote sta scris, pana astazi, numele Sfantului Constantin Brancoveanu, credincios domnitor.
Biserica cea mare a Manastirii Hurezi, inchinata Sfintilor Imparati Constantin si Elena, a fost ctitorita, intre anii 1693-1697, de catre Sfantul Constantin Brancoveanu.
Biserica cea mare are o lungime de 32 de metri si o inaltime de 14 metri, fiind zidita in forma de cruce si impartita in pridvor, pronaos, naos si Altar.
Adesea s-a spus ca arhitectura acesteia a avut drept model biserica din Manastirea Curtea de Arges.
The Ricardo J. Bordallo Governor's Complex in Hagatna, Guam.
Please attribute to Gage Skidmore if used elsewhere.
At MBU's new 47,000 square foot Carl and Deloris Petty Sports and Recreation Complex. October, 2011.
Hockley Texas Hockley Recreational Complex Greater Houston Soap Box Derby NDR Rally Night Race June 16 2012 GHSBD Cars Kids Track Children Hill Soapbox Racing
About Wat Phutthai Sawan, Ayutthaya, Thailand
Wat Phutthai Sawan or the Monastery of Lord Buddha of the Heavens is located on the south bank of the Chao Phraya River in an area presently called Samphao Lom (the Capsized Junk sub-district), east of Khlong Thakian. It is situated opposite the mouth of Khlong Chakrai Yai, also called Khlong Tho, a canal linking the former Lopburi River (present Khlong Mueang or northern moat) with the Chao Phraya River and runs adjacent the former Royal Palace grounds. The temple complex faces east and is bordered on the north by the Chao Phraya River.
Wat Phutthaisawan temple was built in 1353 AD (715 CS) by King Ramathibodi I at the royal residence of "Wiang Lek", the site where he first settled before establishing Ayutthaya as the capital city in 1350. The temple was constructed after his elder brother (the ruler of Suphan) defeated the Khmers and brought them back under the control of Ayutthaya in 1352. The temple was likely built by the large number of enslaved Khmer inhabitantsforcibly removed from Angkor to Ayutthaya at that time. The monastery was one of the first temples constructed and had a preaching hall and a great holy reliquary.
The old temple complex was enclosed by an outer wall measuring 192 meters in length and 92 meters in width. The vihara has its entry to the east and measures 48 meters in length and 16 meters in width. The main Khmer-style prang is surrounded by a square cloister. The cloister is enclosed by an outer wall, which along with the pillars inside supports the roof. The floor of the terrace is one step higher than the court. The inner wall of the cloister houses rows of Buddha images on decorated bases. Porticos lead into the gallery of seated Buddha's.
The prang, representing the cosmic Mount Meru, is located in the middle of the ancient compound and is built on an indented pedestal protruding towards the north and south, resulting in a wing-like formation, which was characteristic for prangs of the early Ayutthaya period. The "cella" or central small hall inside the prang, can be accessed through a porch, located in the east and only by climbing stairs. The prang has two staircases on the east and the west side. Over the cubic "cella" rises the central tower, the bud-shaped prang. The "cella" houses a Buddha image. Decorations of the ceilings of the porch and "cella" are still visible.
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Mis en œuvre par le Programme des Nations Unies pour le développement (PNUD), le projet pilote 16/6 arrive symboliquement à terme avec l’inauguration du Complexe Communautaire et le terrain de football de Sainte Marie au Canapé Vert en présence du Président Michel Joseph Martelly et la Directrice Principale du PNUD, Yvonne Helle.
En visitant ses deux réalisations, le Président Michel Joseph Martelly a fièrement déclaré : « Mon administration a soutenu les travaux du 16/6 parce qu’ils visaient le bien-être de la population. Je suis heureux de voir les résultats aujourd’hui.».
Pour sa part, la Directrice Principale du PNUD, Yvonne Helle, voit dans le projet 16/6, une solution intégrée qui a permis la fermeture de 50 camps, la relocalisation et l’amélioration de la qualité de vie des personnes déplacées tout en répondant aux besoins urgents en matière d’infrastructures physiques et aux problèmes sociaux des communautés ciblées.
Barton Community College Men's Soccer first half photos vs Johnson County Community College in first round of Region VI playoffs on 10-26-18 at the Cougar Soccer/Track Complex on the campus of Barton Community College in Great Bend, KS.
Photos by Baleigh Griffin, student photographer for Barton Sports Information Department.
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. Rocks in this area mostly consist of inch-scale layered plagioclase feldspar and pyroxene. The layering was originally horizontal; Stillwater Complex rocks have been structurally tilted by mountain building.
Stratigraphy: 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
Aurora Complex
July 2, 2014
The Sound Factory
McAllen, TX
PLEASE DO NOT USE WITHOUT PERMISSION! CONTACT ME FOR USE!
© Patrick Panuco. Do not use without permission.
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
Wide shot of the Visitor Complex at the Kennedy Space Center. From left: Space Shuttle Explorer, a mated pair of solid rocket boosters and external tank, and the new Shuttle Launch Experience simulation (HIGHLY recommended).
This is the actual Mariners Apartment Complex, referenced in the Lana del Rey song. It's called Mariners Village in Marina Del Rey, Los Angeles, California.