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"Montgomery level measures angles, slope or pitch as well as has plum and level indicators; improved bubble level. Produced by www.montgomerylevelcompany.com
Sheringham Level Crossing update. This banner says it all. Congratulations to everybody that has made this connection possible.
52주를 통해 52명의 고전화가를 만나는 알파벳 수업.
지금까지 배웠던 A for Apple이 아닌 미술적인 관점인
A for Albers (색채이론가) 를 배우는 과정으로써
세계적인 화가들을 26개의 알파벳을 통해,
창의융합형 1년 프로그램!
High Level Bridge
The Grade 1 listed High Level Bridge was constructed between 1846 to 49. It is a double deck structure of arch and suspension design. The upper railway deck is carried on 6 ribbed arches supported by stone piers; the road suspended from the arches by wrought iron rods.
Following a restoration in 2008 the roadway on the lower deck is now open for southbound (Newcastle to Gateshead) buses and taxis only, reducing the loads on the bridge. Pedestrians and cyclists still use the original footpaths at each side of the roadway.
what3words///supper.panels.wishes
World Summit on the Information Society (WSIS)+20 Forum High-Level Event 2024
Network of Women Ministers and Leaders in ICT
27-31 May 2024
Geneva, Switzerland
©ITU/D.Woldu
Collin and mom having it out in the hotel room. Mom frantically tries to reload as Collin prepares to fire.
At one time the CP rail line ran down centre of top deck with north/south streetcars on the outside edges. Streetcars crossed-over at either end to put doors to the centre of the bridge. Currently a seasonal tourist streetcar runs on rails on the top deck at the bridge centre. Otherwise southbound vehicle and pedestrian use only today.
A work force on Bario Highland.
The Kelabit Highlands is tucked in the north eastern of Sarawak and is very close to the international border between Kalimantan and Sarawak. Bario is located on the Kelabit Highlands, 3280 feet above sea level. It is the unofficial capital of the Kelabit Highlands. All roads lead to Bario. Due to geographical barrier, this wonderful place is isolated from the rest of the world.
Bario is a very peaceful and beautiful place. everywhere you go you can expect find breathtaking sights.
Planovergang ved Bjørgo stasjon på den nå nedlagte Valdresbanen
Level crossing near Bjørgo station on the Valdres line, disused since 1989
On my walk around Christchurch city, February 16, 2012. The building on the right is to come down as it is realy unsafe!
The one year anniversary this Wenesday, Feb 22 of the deadly earthquake
A magnitude 5.8 followed by a 6.0 magnitude earthquake struck off the coast of Lyttelton on Friday afternoon the 23rd December, 2011, causing liquefaction to once again erupt from the earth and leaving sewerage, water and power out of action in pockets of eastern Christchurch.
A series of intense'' aftershocks have followed, and hundreds and hundreds'' were recorded by GNS in the 24 hours following the two major quakes, said seismologist Bill Fry.)
Taken from the New Zealand Herald New paper
The February 22, 2011 Christchurch earthquake was a magnitude 6.3 (ML) earthquake that struck the Canterbury region in New Zealand's South Island at 12:51 pm on Tuesday, 22 February 2011 local time (23:51 21 February UTC), The earthquake was centred 2 kilometres (1.2 mi) west of the town of Lyttelton, and 10 kilometres (6 mi) south-east of the centre of Christchurch, New Zealand's second-most populous city. It followed nearly six months after the magnitude 7.1 4 September 2010 Canterbury earthquake, which caused significant damage to Christchurch and the central Canterbury region, but no direct fatalities.
The earthquake caused widespread damage across Christchurch, especially in the central city and eastern suburbs, with damage exacerbated by buildings and infrastructure already being weakened by the 4 September 2010 earthquake and its aftershocks. Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt. The earthquake was reported to be felt across the South Island and the lower and central North Island.
In total, 184 (as from Jan, 2012) people were killed in the earthquake, making the earthquake the second-deadliest natural disaster recorded in New Zealand (after the 1931 Hawke's Bay earthquake), and fourth-deadliest disaster of any kind recorded in New Zealand, with nationals from more than 20 countries among the victims. Over half of the deaths occurred in the six-storey Canterbury Television (CTV) Building, which collapsed and caught fire in the quake. The government declared a state of national emergency, which stayed in force until 30 April 2011.
It has been estimated that the total cost of rebuilding to insurers to be around NZ$15–16 billion, making it by far New Zealand's costliest natural disaster, and the third-costliest earthquake (nominally) worldwide.
The earthquake would ultimately be one of three major earthquakes in a year-long earthquake swarm affecting the Christchurch area, and was followed by a large aftershock on 13 June 2011, which caused considerable additional damage.
Examples of water levels during completion of the Three Gorges Dam project. Photo taken in 2002. First stage of flooding has already occurred
Viaduct taking the train line over the flat area known as the Somerset Levels close to the town of Langport.