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Prince Durbhajan of Bundelkhand royal family fell in love with a muslim girl long back in the 17th century. He was given options either to choose the girl or the throne. He opted for the first and built their own palace far away from the city, which was known as Sundar Mahal.
People worship them and till date many pay visit to this ruined palace to seek blessings.
Taken in Orchha, Madhyapradesh, Indialo
Tiny hair-like structures of salt grow and combine to form the salt flats at Badwater in Death Valley. Here is a wider view of the same area showing how the salt combines to form geometric pools.
Photo taken in the Badwater area of Death Valley National Park (California, USA).
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Photographer Spotlight Nov 2024 : Blog
ND Awards Brons Medal :
ndawards.net/winners-gallery/nd-awards-2024/non-professio...
An outbound Metro-North Railroad train to New Haven is seen approaching New Rochelle Station, the Kawasaki M8 cars standing out nicely in the snow.
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品川シーズンテラス - 建築グラビア Architecture Gravure
Gallery : photowork.jp/christinayan01/architectural/archives/2255
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Shinagawa Season Terrace (品川シーズンテラス).
Architect : NTT Facilities (設計：ＮＴＴファシリティーズ).
Contractor : Taisei Corporation (施工：大成建設).
Completed : February 2015 (竣工：2015年2月).
Structured : Steel frames (構造：地上S造（柱CFT造）).
Height : 509 ft (高さ：155.27m).
Floor : 32nd (階数：32階).
Floor area : 2,217,635 sq.ft. (延床面積：206,025.07㎡).
Location : 1-2-70 Konan, Minato Ward, Tokyo, Japan (所在地：日本国東京都港区港南1-2-70).
Referenced :
www.nttud.co.jp/business/office/detail/id/443
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"Wooden structure"
Hôtel particulier Chambellan au 34 rue des Forges à Dijon. (Bourgogne - Côte d'Or)
Website : www.fluidr.com/photos/pat21
www.flickriver.com/photos/pat21/sets/
"Copyright © – Patrick Bouchenard
The reproduction, publication, modification, transmission or exploitation of any work contained here in for any use, personal or commercial, without my prior written permission is strictly prohibited. All rights reserved."
A different angle of The Wave structure in Arizona. What a place to see! But don't forget to get a permit to go there.
Shot in Nantes, France.
Ondu 4x5 pinhole Camera
5 sec exposure, deep red filter
Kodak Tmax 100
developed in D76. 20°c, 10'45min
Larger is better
Daylight version: www.flickr.com/photos/kayodeok/133554123/
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Vauxhall Bridge is a steel arched bridge for road and foot traffic, crossing the River Thames in a north-west south-east orientation, between Lambeth Bridge and Grosvenor Bridge, in central London.
On the north bank is Westminster, with Tate Britain and the Millbank Tower to the north-east, and Pimlico and its tube station to the north and east.
On the south bank, Vauxhall Cross, site of Vauxhall station and the headquarters of MI6, lies immediately to the south-east; Kennington is to the east, Vauxhall to the south-east and Nine Elms to the south west.
The River Effra, one of the Thames's many underground tributaries, empties into the main river just to the east of the bridge on the south bank.
The current bridge was designed by Sir Alexander Binnie, with modifications by Maurice Fitzmaurice, to replace a previous cast-iron structure.
It was completed in 1906, and opened on the May 26 by the Prince of Wales, and was the first bridge to carry trams across the Thames. It measures 80ft wide by 809ft long, has five steel arches mounted on granite piers, and its most striking feature is a series of bronze female figures on the bridge abutments, both upstream and downstream, commemorating the arts and sciences.
Multiple levels (parallel planes; rock surface curves down to right) of slickensided fault surfaces in an outcrop of Marron Fm. andesitic volcanic rock (in south-central British Columbia), with one of my fingers for scale. Above my finger, the lighter coloured material is a mineral vein (fluid flowed along a fault plane and mineral precipitated from solution) with a patchy distribution now because it is partly eroded away.
The slickenlines present have two different groove lineation directions, diagonal down to the left and down to the right in both the purplish-brown host rock and the light brown vein material. They record two different steep (sub-vertical) directions of fault motion at this site back in the Eocene (ca. 50 million years ago), a time of post-orogenic normal faulting in this part of western Canada.
C. J.R. Devaney