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The Great Patriotic War (Russian: Вели́кая Оте́чественная война́, romanized: Velikaja Otečestvennaja vojna) is a term used in Russia and some other former republics of the Soviet Union to describe the conflict fought during the period from 22 June 1941 to 9 May 1945 along the many fronts of the Eastern Front of World War II, primarily between the Soviet Union and Nazi Germany. For some legal purposes, this period may be extended to 11 May 1945 to include the end of the Prague offensive.
History
The term Patriotic War refers to the Russian resistance to the French invasion of Russia under Napoleon I, which became known as the Patriotic War of 1812. In Russian, the term отечественная война originally referred to a war on one's own territory (otechestvo means "the fatherland"), as opposed to a campaign abroad (заграничная война), and later was reinterpreted as a war for the fatherland, i.e. a defensive war for one's homeland. Sometimes the Patriotic War of 1812 was also referred to as the Great Patriotic War (Великая отечественная война); the phrase first appeared in 1844 and became popular on the eve of the centenary of the Patriotic War of 1812.
After 1914, the phrase was applied to World War I. It was the name of a special war-time appendix to the magazine Theater and Life (Театр и жизнь) in Saint Petersburg, and referred to the Eastern Front of World War I, where Russia fought against the German Empire and the Austro-Hungarian Empire. The phrases Second Patriotic War (Вторая отечественная война) and Great World Patriotic War (Великая всемирная отечественная война) were also used during World War I in Russia.
The term Great Patriotic War re-appeared in the official newspaper of the CPSU, Pravda, on 23 June 1941, just a day after Germany invaded the Soviet Union. It was found in the title of "The Great Patriotic War of the Soviet People" (Velikaya Otechestvennaya Voyna Sovetskogo Naroda), a long article by Yemelyan Yaroslavsky, a member of Pravda editors' collegium. The phrase was intended to motivate the population to defend the Soviet fatherland and to expel the invader, and a reference to the Patriotic War of 1812 was seen as a great morale booster. During the Soviet period, historians engaged in huge distortions to make history fit with Communist ideology, with Marshal Mikhail Kutuzov and Prince Pyotr Bagration transformed into peasant generals, Alexander I alternatively ignored or vilified, and the war becoming a massive "People's War" fought by the ordinary people of Russia with almost no involvement on the part of the government. The invasion by Germany was called the Great Patriotic War by the Soviet government to evoke comparisons with the victory by Tsar Alexander I over Napoleon's invading army.
The term Отечественная война (Patriotic War or Fatherland War) was officially recognized by establishment of the Order of the Patriotic War on 20 May 1942, awarded for heroic deeds.
The term is not generally used outside the former Soviet Union, and the closest term is the Eastern Front of World War II (1941–1945). Neither term covers the initial phase of World War II in Eastern Europe, during which the USSR, then still in a non-aggression pact with Germany, invaded eastern Poland (1939), the Baltic states (1940), Bessarabia and Northern Bukovina (1940) and Finland (1939–1940). The term also does not cover the Soviet–Japanese War (1945) nor the Battles of Khalkhin Gol (1939).
In Russia and some other post-Soviet countries, the term is given great significance; it is accepted as a representation of the most important part of World War II. Until 2014, Uzbekistan was the only nation in the Commonwealth of Independent States that had not recognized the term, referring to it as World War II on the state holiday - the Day of Remembrance and Honour.
On 9 April 2015, the Ukrainian parliament replaced the term Great Patriotic War (1941–1945) (Velyka vitchyzniana viina) in the country's law with the "Second World War (1939–1945)" (Druha svitova viina), as part of a set of decommunization laws. Also in 2015, Ukraine's "Victory Day over Nazism in World War II" was established as a national holiday in accordance with the law of "On Perpetuation of Victory over Nazism in World War II 1939–1945". The new holiday was celebrated on May 9 and replaced the Soviet-Russian Victory Day, which is celebrated on May 9. These laws were adopted by the Ukrainian parliament within the package of laws on decommunization. In 2023 Ukraine abolished the 2015 9 May "Victory Day over Nazism" holiday and replaced it with the new public holiday "Day of Remembrance and Victory over Nazism in World War II 1939 – 1945" which is celebrated on 8 May annually.
From the May 2016 trip to Thailand and Cambodia:
As this was my first trip to Thailand, I absolutely insisted that it include some island…any island, really. Since this trip was including Bangkok and also Cambodia, an island along the eastern seaboard made the most sense and Koh Chang was the “winner.” (I’m pretty sure there are others – maybe even more beautiful ones – but, since we just had two nights, this one worked out fine, as it was quite accessible.)
Now, Koh Chang isn’t considered the prettiest island in Thailand by a long shot, however, it is quite nice all the same. I’m more than likely going to be returning to Thailand within the next 4 months, and will be visiting one of the more picturesque islands at that time (along with northern Thailand, which went completely untouched this trip).
Koh Chang (“koh” or “ko” means “island,” and “chang” means elephant…for anyone who’s curious) is the second-largest island in Thailand. I’m not sure what the largest is (Phuket, probably?). At any rate, getting here from Bangkok is very easy. Go to the eastern bus terminal and buy a bus ticket. (Lonely Planet said it’s 7 hours; the hotel said 5. Oddly, we got there in 6 hour flat.) The ticket cost…about 250 baht, from what I recall. That’s less than $10USD for a six hour bus ride. Not bad at all.
As bus rides go, it’s completely nondescript. The road doesn’t hug the sea, so there’s nothing coastal to see, nor is southeastern Thailand terribly mountainous. (The Cardamom Mountains in western Cambodia aren’t too far off, but they’re more like hills, even smaller than the Appalachians, and were far enough off that you wouldn’t even consider this hilly terrain. The only points of note on this trip (which completely bypasses Pattaya – fine by me) are the towns of Chanthaburi and Trat. Trat is the closest main city to Koh Chang. At Trat, it’s a two lane road just under an hour to the Koh Chang dock, where the bus stops and you have to buy a ferry ticket (40 baht/person). Both the Bangkok-Koh Chang buses and ferries run regularly (every thirty minutes or so), so timing isn’t a concern.
The ferry across the Gulf of Trat (Gulf of Thailand, really) is about…30-40 minutes. It’s only six kilometers or so offshore. It’s far enough that, when you’re there, you certainly forget about the rest of the world, which is rather nice. Arriving on the north shore of the island at one of 2 or 3 docks, you pay anywhere from 50-100 baht for a group tuktuk/van to take you to whichever point on the island you happen to be staying.
The island is large (and hilly) enough that there are waterfalls, ziplines, hiking, all kinds of outdoor recreation other than just being a beach bum. I, unfortunately, got rather sick late the first night there and was completely out of commission for over 24 hours. However, I’m glad to say that I did get to enjoy Hat Sai Khao (White Sand Beach) very much.
On arriving in the area – this is the most popular beach, and also nearest the docks, about 4 km away – you find your hotel/hostel/guesthouse and then, will more than likely, head straight to the beach. This is the only part of the trip where we had no hotel reservations ahead of time. There are so many options for staying that, even during peak season, getting a place to stay is pretty easy. (And May is not peak season…)
Our hotel – the Arunee Resort – was pretty much no frills and, while not directly on the beach, it was less than a three minute walk away (through the 15 Palms Restaurant, where we ate twice). For 1000 baht/night (around $30USD), it was perfect.
We got to the hotel and checked in around 4:00 in the afternoon. After getting settled, we just went over to the aforementioned 15 Palms Restaurant for a late lunch/early dinner. The view was wonderful. The beach isn’t terribly big – or long – but, it’s large enough that it wasn’t crowded at all. We just relaxed outdoors for a while and, closer to sundown, took a stroll along the beach.
As far as sunsets go, this one left a lot to be desired on the “Wow!” scale, but there was a sunset, so I can’t complain too much. Fortunately, Koh Chang is interesting in its own right. Along the beach, which I’d guess is about 500 meters long, give or take, are lots of restaurants, bars, some of the pricier resorts, a few souvenir shops, etc. I guess it’s exactly what you’d expect and hope for from a tropical beach. All of these line the main road around the west side of the island, by the way.
From a practical point of view, I’m also glad to say that there are plenty of pharmacies, massage parlors, tattoo parlors (though that’s not “practical,” so to speak), and I think there’s even an emergency clinic on the island. As I was annoyingly sick, I considered looking into that, but in the end, just waited it out. The silver lining to that cloud is that, if there were one day during this trip where I had to be completely waylaid, I’m glad it was one here, since the rest of the time involved much more tourist sites & stock shooting. Though I wish that I could have been healthy enough to possibly see other parts of the island on the one full day we had, I’m just glad I was well enough to travel on Friday morning.
Friday was a travel day that I was mildly concerned about, simply because it involved a truck, a ferry, a tuktuk/van, a bus, an international border crossing (with no prearranged visa), and indefinite transportation 300 km on the other side of the border to our final destination. More on that in the next “batch” post…
Lego's Architecture line includes a very nice rendition of Frank Lloyd Wright's Fallingwater, built in Mill Run, Pennsylvania in the 1930s and famed for incorporating the terrain and the waterfall as major architectural elements. The Lego version, rated at Age 16+ and consisting of 811 pieces, costs $99.99 and is a very nice 3-hour build.
The completed set - quite an awesome sight. This is my first Architecture set that represents something I have not seen in person, though based on photographs of the real Fallingwater, the essence is well captured in this set. To allow further appreciation of the architecture, this set was designed modularly; the terrain is one separate build, the foundation of the house a second separate build, and each of the three floors, plus the roof, are all separate builds as well, sliding out easily.
Kochi is a city in the Indian state of Kerala. Kochi is located in the district of Ernakulam. Old Kochi loosely refers to a group of islands including Willingdon Island, Fort Kochi and Mattancherry. Today Kochi includes Ernakulam, old parts of Kochi, Kumbalangi, and outlying islands.
For many centuries up to and during the British Raj, the city of Kochi was the seat of the eponymous princely state. Kochi traces its history back many centuries, when it was the centre of Indian spice trade for hundreds of years, and was known to the Yavanas (Greeks and Romans), Jews, Arabs and Chinese since ancient times. Kochi earned a significant position on the world trading map after the port at Kodungallur (Cranganore) was destroyed by massive flooding of the river Periyar in 1341.
The earliest documented references to Kochi occur in the books written by Chinese voyager Ma Huan, during his visit to Kochi in the 15th century as part of the treasure fleet of Admiral Zheng He. There are also references to Kochi in accounts written by Italian traveller Niccolò Da Conti, who visited Cochin in 1440 . Today, Kochi is the commercial hub of Kerala, and one of the fastest growing second-tier metros in India.
PREHISTORY
Not much is known about the prehistory of Kochi. There has been no clear evidence of Stone Age inhabitation. Quite ironically, Kochi forms the central part of the Megalithic belt of Kerala. The only trace of prehistoric life in the region is the menhir found in Tripunithura.
Princely rule
PRINCELY RULE
The history of Kochi prior to the Portuguese is not well documented. Though places north and south of Kochi are mentioned in quite detail in many accounts by ancient travellers, even a mention of Kochi is absent prior to the arrival of the Portuguese. Kochi's prominence as a trading port grew after the collapse of the port at Kodungallur in 1341 AD.
The Cochin State came into existence in 1102 AD after the breaking up of the Kulasekhara empire.
FOREIGN RULE
Kochi was under the rule of many foreign empires, during which the Raja of Kochi still remained the titular head.
PORTUGUESE PERIOD (1503-1663)
Kochi was the scene of the first European settlement in India. In the year 1500, Portuguese Admiral Pedro Álvares Cabral, landed at Cochin after being repelled from Calicut. The King of rival Kochi welcomed his guests and a treaty of friendship was signed. Promising his support in the conquest of Calicut, the admiral coaxed the king into allowing them to build a factory at Cochin. Assured by the support, the king called war with the Zamorins of Calicut. However, the admiral retreated in panic on seeing the powers of the Zamorin. The Zamorins, on the other hand, eager to win the favor of the Portuguese, left without a war. Another captain, João da Nova was sent in place of Cabral. However, he too faltered at the sight of the Zamorin. The consecutive retreats made the King of Portugal indignant. The king sent Vasco Da Gama, who bombed Calicut and destroyed the Arab trading posts. This invited the anger of the Zamorin, who declared a war against the Kochi Raja.
The war between Calicut and Cochin began on 1 March 1503. However, the oncoming monsoons and the arrival of a small Portuguese fleet under Francisco and Afonso de Albuquerque alarmed the Zamorin, and he called back his army. The Zamorin resorted to a retreat also because the revered festival of Onam was near, and the Zamorin intended to keep the auspicious day holy. This led to a triumph for the king of Kochi, who was later re-established in the possession of his kingdom. However, much of the kingdom was burnt and destroyed by the Zamorins.
After securing the king in his throne, the Portuguese got permission to build a fort – Fort Kochi (Fort Emmanuel) (after the reigning king of Portugal) - surrounding the Portuguese factory, in order to protect it from any further attacks. The entire work was commissioned by the Cochin Raja, who supplied workers and material. The Raja continued to rule with the help of the Portuguese. Meanwhile, the Portuguese secretly tried to enter into an alliance with the Zamorins. A few later attempts by the Zamorin at conquering the Kochi port was thwarted by the Cochin Raja with the help of the Portuguese. Slowly, the Portuguese armory at Kochi was increased, with the presumed notion of helping the raja protect Kochi. However, the measured led to decrease in the power of the Cochin Raja, and an increase in the Portuguese influence. From 1503 to 1663, Kochi was ruled by Portugal through the namesake Cochin Raja. Kochi remained the capital of Portuguese India till 1510. In 1530, Saint Francis Xavier arrived and founded a Christian mission. This Portuguese period was difficult for the Jews installed in the region, since the Inquisition was active in Portuguese India. Kochi hosted the grave of Vasco da Gama, the Portuguese viceroy, who was buried at St. Francis Church until his remains were returned to Portugal in 1539. Soon after the time of Albuquerque, the Portuguese rule in Kerala declined. The failure is attributed to several factors like intermarriages, forcible conversions, religious persecution etc.
DUTCH PERIOD (1663-1773)
The Portuguese rule was followed by that of the Dutch, who had by then conquered Quilon, after various encounters with the Portuguese and their allies. Discontented members of the Cochin Royal family called on the assistance of the Dutch for help in overthrowing the Cochin Raja. The Dutch successfully landed at Njarakal and headed on to capture the fort at Pallippuram, which they handed over to the Zamorin.
MYSORE INVASION
The 1773 conquest of the Mysore King Hyder Ali in the Malabar region descended to Kochi. The Kochi Raja had to pay a subsidy of one hundred thousand of Ikkeri Pagodas (equalling 400,000 modern rupees). Later on, in 1776, Haider captured Trichur, which was under the Kingdom of Kochi. Thus, the Raja was forced to become a tributary of Mysore and to pay a nuzzar of 100,000 of pagodas and 4 elephants and annual tribute of 30,000 pagodas. The hereditary Prime Ministership of Cochin came to an end during this period.
BRITISH PERIOD (1814–1947)
In 1814 according to the Anglo-Dutch Treaty, the islands of Kochi, including Fort Kochi and its territory were ceded to the United Kingdom in exchange for the island of Banca. Even prior to the signing of the treaty, there are evidence of English residents in Kochi. Towards the early 20th century, trade at the port had increased substantially, and the need to develop the port was greatly felt. Harbour Engineer Robert Bristow, was thus brought to Cochin in 1920 under the direction of Lord Willingdon, then the Governor of Madras. In a span of 21 years, he had transformed Cochin as the safest harbour in the peninsula, where ships berthed alongside the newly reclaimed inner harbour equipped with a long array of steam cranes. Meanwhile, in 1866, Fort Cochin was made a municipality, and its first Municipal Council election to a board of 18 members was conducted in 1883. The Maharajah of Cochin, in 1896 initiated local administration, by forming town councils in Mattancherry and Ernakulam. In 1925, Kochi legislative assembly was constituted due to public pressure on the state. The assembly consisted of 45 members, 10 of who were officially nominated. Thottakkattu Madhaviamma became the first woman to be a member of any legislature in India.
POST INDEPENDENCE ERA
In 1947, India gained independence from the British colonial rule. Cochin was the first princely state to join the Indian Union willingly. Post independence, E. Ikkanda Warrier became the first Prime Minister of Kochi. K. P. Madhavan Nair, P.T Jacob, C. Achutha Menon, Panampilly Govinda Menon were few of the other stalwarts who were in the forefront of the democratic movements. Then in 1949, Travancore-Cochin state came into being by the merger of Cochin and Travancore, with Parur T. K. Narayana Pillai as the first chief minister. Travancore-Cochin, was in turn merged with the Malabar district of the Madras State. Finally, the Government of India's 1 November 1956 States Reorganisation Act inaugurated a new state – Kerala – incorporating Travancore-Cochin, Malabar District, and the taluk of Kasargod, South Kanara. On 9 July 1960, the Mattancherry council passed a resolution that was forwarded to the government, requesting the formation of a Municipal Corporation by combining the existing municipalities of Fort Kochi, Mattancherry and Ernakulam. The proposal was condemned by the Fort Kochi municipality. However, the Ernakulam municipality welcomed the proposal, suggesting the inclusion of more suburban areas in the amalgamated Corporation. Major Balagangadhara Menon, the then Director of Local Bodies was appointed by the government to study the feasibility of the suggested merger. And based on the report submitted by him, the Kerala Legislative Assembly approved the formation of the Corporation. Thus, on 1 November 1967, exactly 11 years since the conception of the state of Kerala, the corporation of Cochin came into existence, by the merger of the municipalities of Ernakulam, Mattancherry and Fort Kochi, along with that of the Willingdon Island and four panchayats viz. Palluruthy, Vennala, Vyttila and Edappally and the small islands of Gundu and Ramanthuruth.
WIKIPEDIA
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Hong Kong Transport - Trucks
The Hong Kong Truck Culture
The number of Trucks, Vans* and Special Purpose Vehicles (Light, Medium & Heavy) registered + licenced in Hong Kong seems to fluctuate between 120,000 - 125,000 vehicles and presumably new trucks registered are offset by old trucks being retired or sold over the border in China.
*Vans are classified as Light Goods Vehicles and are not shown in this album
In Hong Kong Trucks are classified as GOODS VEHICLES By the Transport Department - see below
☛Light Goods Vehicles - Goods vehicles of permitted gross vehicle weight not exceeding 5.5 tonnes.
☛Medium Goods Vehicles - Goods vehicles of permitted gross vehicle weight exceeding 5.5 tonnes but not exceeding 24 tonnes.
☛Heavy Goods Vehicles - Goods vehicles of permitted gross vehicle weight exceeding 24 tonnes but not exceeding 38 tonnes.
The major truck types you tend to see in urban areas are trucks carrying construction materials or waste, dump trucks, concrete mixers and all sizes of delivery trucks... outside of the urban areas it is container trucks and large trucks carrying construction materials.
The following brands of Trucks can be seen on the streets of Hong Kong and include:-
Beiben ✚ Bell ✚ CAMC ✚ CNHTC ✚ DAF ✚ Dennis ✚ Dong Feng ✚ FAW ✚ Fuso ✚ Foton ✚ Ford ✚ Hino ✚ Howo ✚ Hyundai ✚ Isuzu ✚ Iveco ✚ JAC ✚ Kato ✚ KIA ✚ Liebherr ✚ MAN ✚ Mercedes Benz ✚ Mitsubishi ✚ Nissan ✚ Renault ✚ Scania ✚ Shacman ✚ Sinotruk ✚ Suzuki ✚ Toyota ✚ UD ✚ Volvo ✚ Zoomlion
Hong Kong is a brand conscious place even for trucks (!) hence the popularity of the European brands, Scania and Man are very popular and even the older trucks look the business and they are utterly reliable.
Isuzu is the market leader in terms of sale volume for all types of trucks.
(Source - The Transport Department, Hong Kong Government)
☛.... and if you want to read about my views on Hong Kong, then go to my blog, link below
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Selected Writing.
by bpNichol;
edited by Jack David & bpNichol.
Vancouver, Talonbooks, october 198o. ISBN o-88922-176-6.
5-3/16 x 8-1/4, 72 sheets tan wove newsprint perfectbound in glossy PVC white card wrappers, all except inside covers & 3 pp (2, 8, 32) printed black offset with 3-colour process additions to front cover.
cover photograph by Kim Ondaatje.
other contributors:
David Aylward, Matsuo Basho, Barbara Caruso, Gaius Catullus, Wayne Clifford, Co-Accident, Jack David, Vivien Halas, Kirby Malone, Chris Mason, Steve McCaffery, Libby Oughton, Marshall Reese, Karl Siegler, Toronto Research Group.
includes:
i) Y (p.33; poem)
ii) H (an alphhabet), lettered by Barbara Caruso (p.34; visual poem)
iii) from 'ABC: the aleph beth book' (p.35; visual poem (ie poem for "Q", "WE MUST PUT THE POEM IN OUR LIVE"))
iv) Blues, typeset by Vivien Halas (p.36; concrete poem)
v) "arrow worra worra arrow" (p.37; concrete poem)
vi) The End of the Affair (p.38; concrete poem)
vii) The Complete Works (p.39; visual poem, revised)
viii) Allegory No. 6 (p.4o; visual poem)
ix) Aleph Unit, drawn by Barbara Caruso (pp.41-48; visual poem in 8 parts, titles not here given:
–1. [Aleph Unit Closed] (p.41)
–2. [Aleph Unit Opened] (p.42)
–3. [Aleph Unit Distance] (p.43)
–4. [Aleph Unit Surface] (p.44)
–5. [Aleph Unit Observed] (p.45)
–6. [Aleph Unit Enigmatic] (p.46)
–7. [Aleph Unit in Transit] (p.47)
–8. [Aleph Unit Not] (p.48))
x) Cycle No. 22 (p.49; concrete poem)
xi) NOT WHAT THE SIREN SANG BUT WHAT THE FRAG MENT (pp.5o-51; concrete/sound poem)
xii) Dada Lama (pp.52-56; sound poem in 6 parts:
–1. "hweeeee" (p.52)
–2. "eeeeeeeeeeeeeeeeeeeeeeeeee" (p.53)
–3. "oudoo doan doanna" (pp.53-54)
–4. "AAAAAAAAAAAAAAAAAAAAA" (p.54)
–5. "tlic" (p.55)
–6. "wwwwwwwwwwwwwwwwwwwwwwwwwww" (p.56))
xii) Lament (p.57; concrete poem, revised to a single page)
xiii) from 'Trans-Continental' (pp.58-59; poetry, parts 1-4 (of 49):
–1. "an h moves past an m" (p.58)
–2. "x d" (p.58)
–3. "z" (p.59)
–4. "a d in a cloudbank" (p.59))
xiv) after hokusai (p.6o; poem)
xv) COLD MOUNTAIN (pp.61-62; poem (revision of concrete poetry object) in 2 parts:
–1. "GO" (p.61)
–2. "RETURN" (p.62))
xvi) to the memory of su t'ung po (p.63; poem)
[(xvii)-(xx) under section title 4 poems from 'Still Water']
xvii) "2 leaves touch" (p.64; poem)
xviii) "blob", translation of Matsuo Basho (p.65; concrete poem)
xix) "em ty" (p.66; concrete poem)
xx) "moon (p.67; poem)
xxi) the other side of the room (p.68; poem)
xxii) 1335 COMOX AVENUE (pp.69-7o; poem)
xxiii) Chapter 7 (pp.71-73; poetry (fromThe Captain Poetry Poems) with 2 works embedded in full:
–1. bpNichol, "Dear Rex:" (correspondence)
–2. Rex Allen, "Dear Barrie:" (correspondence))
xxiv) from 'The Plunkett Papers' (p.74; poem, "we rode the train back west in 54")
xxv) two sections from 'Mono Tones' (pp.75-76; poetry in 2 parts:
–13. "terra" (p.75)
–5o) "walk in the woods" (p.76))
xxvi) Coda: Mid-Initial Sequence (pp.77-86; poetry in 11 parts with 1o drawings of clouds by Libby Oughton:
–1. "faint edge of sleep" (p.77)
–2. "orange" (pp.77-78)
–3. "last note" (pp.78-79)
–4. "bushes" (p.79)
–5. "there is no desire for speech" (p.8o)
–6. "in vocation" (p.81)
–7. "within the difference" (p.81)
–8. (variation on a line by H.D. – in memoriam) (p.82)
–9. "whatever dies" (pp.82-83)
–1o. "11 years since i first conceived myself a writer" (pp.83-84)
–11. "'dogma i am god'" (pp.84-85))
xxvi) Scraptures: seventh sequence (pp.87-89; prose in 8 parts:
–1. "green yellow dog up. I have not. I am. green red cat" (p.87)
–2. "insect. incest. c'est in. infant. in fonts. onts. onts. ptonts." (p.87)
–3. "liturgical turge dirge dinta krak kree fintab latlina santa" (p.88)
–4. "an infinite statement. a finite statement. a statement of" (p.88)
–5. "grewat small lovers move home. red the church caught us" (p.88)
–6. "halo. hello. i cover red my sentiment. blankets return the" (p.89)
–7. "il y a là lever la lune. l'amour est le ridicule of a life sont" (p.89)
–8. "au revoir. le réveille sounds up the coach. les pieds de le" (p.89))
xxvii) from 'Andy' (pp.9o-93; prose in 1o parts:
–1. August 27, 1944 (p.9o)
–2. August 28, 1944 (p.9o)
–3. August 29, 1944 (p.9o)
–4. August 30, 1944 (p.9o)
–5. August 31, 1944 (pp.9o-91)
–6. September 2, 1944 (p.91)
–7. September 3, 1944 (p.91)
–8. September 4, 1944 (p.92)
–9. September 7, 1944 (p.92)
–1o. September 10, 1944 (pp.92-93; includes:
––a. "Received your letter & poem today. I think I will write wool-", by Andy Phillips (prose correspondence)))
xxviii) Gorg, a detective story (p.94; prose)
xxix) TWO HEROES (pp.95-99; in 11 numbered parts:
–1. "In the back garden two men sit. They are talking with one another" (p.95)
–2. "Once a long time ago they talked more easily. Once a long time" (p.95)
–3. "When the fight was over & Riel was dead & Dumont had fled into" (pp.95-96)
–4. "Time passed. No one heard much from either of them. In GRIP" (p.96)
–5. "There are some say Billy the Kid never died the story began." (pp.96-97)
–6. "Billy was in love with machines. He loved the smooth click of the" (p.97)
–7. "It was a good story as stories go. Most of their friends when" (p.97)
–8. "The problem with Africa was it was kind of damp & there was no" (p.98)
–9. "When Billy the Kid awoke the clockwork man was very still. There" (p.98)
–1o. "There are strange tales told of Billy the Kid, of what happened" (p.99)
–11. "One year the two men returned. They were both grayer & quiet." (p.99))
xxx) Twins – a history (pp.1oo-1o1; prose)
xxxi) from 'Journal' (pp.1o2-1o6; prose, part III:2, "some days i want to talk to you mommy some days i")
xxxii) Two Words: A Wedding (pp.1o7-1o8; prose)
xxxiii) Lust (a little play) (p.1o9; script)
xxxiv) Naming 3 (p.11o; concrete poem)
xxxv) probable systems 9 (pp.111-112; nonfiction in 2 parts:
–1. "problem: find [the square root of] logic to the nearest whole letter" (p.111)
–2. commentary (pp.111-112))
xxxvi) probable systems 21 (pp.113-115; nonfiction in 2 parts:
–1. the weight of speech (pp.113-114; prose with 2 graphics:
––a. "(variable member of human speech community)" (p.113)
––b. "(speech funnel)" (p.114))
–2. commentary (p.115))
xxxvi) from Catullus poem XXVIII (pp.116-117; poem in 2 parts:
–1. "Pisonis comites, cohors inanis,", by Gaius Catullus (p.116)
–2. "Piss on his committees, cohorts in inanities," (p.117))
xxxvii) The Words – Montagnais Indian (pp.118-119; sound poem)
xxxviii) Chant to the Fire-Fly (p.12o; sound poem in 2 parts:
–1. TEXT
–2. TRANSLATION)
xxxix) Translating Apollinaire (p.121; poem)
xl) Translating Translating Apollinaire 32 / Negatives 4 (p.122; poem)
xli) a poem by bill bissett (pp.123-124; poem)
[(xlii)-(xliv) under heading Three Found Poems]
xlii) "from Jacques Barzun's 'Tomorrow's Illiterates'", with David Aylward (p.125; concrete poem)
xliii) Turner's Golden Vision, with David Aylward (p.125; poem)
xliv) Puzzle, with David Aylward (p.126; poem)
xlv) from 'A Collaboration', with Wayne Clifford (pp.127-131; poem, part II:5 of Theseus ("In the garden speech continues"))
xlvi) from 'In England Now That Spring', with Steve McCaffery (p.132; poem, part 6 ("Above Ambleside the water falls"))
xlvii) Particular Music (pp.133-135; sound poetry score)
xlviii) from 'Sorrow Laid As This One', with Co-Accident & Toronto Research Group [ie Kirby Malone, Chris Mason, Steve McCaffery, Nichol, Marshall Reese] (p.136; sound poetry score, panel "in the corridor")
il) from 'The Body: In Darkness, with Steve McCaffery (p.137; sound poetry score, panel "A A")
l) Maps (pp.138-139; poem in 3 parts:
–1. 'a day' (p.138)
–2. "i don't need the framework" (pp.138-139)
–3. "the moment doesn't come" (p.139))
li) Bibliography (pp.14o-143; list of 98 titles in 1o parts:
–1. books (p.14o; 17 titles)
–2. pamphlets (pp.14o-142; 6o titles)
–3. editor (p.142; 5 titles)
–4. prints (p.142; 2 titles)
–5. radio serials (p.142; 1 title)
–6. records (pp.142-143; 4 titles)
–7. tapes (p.143; 1 title)
–8. publications as part of the Four Horsemen (p.143; 7 titles)
–9. translations (p.143; 1 title)
–1o. "has also adapted science fiction & fairy tales for the comic book" (p.143))
lii) acknowledgements (p.144; prose)
also includes:
liii) "H", by Kim Ondaatje (front cover; photograph)
liv) Introduction, by Jack David (pp.9-31; prose in 6 parts:
–1. "In 1975 I had an idea for a book: a selection of poetry from" (pp.9-12)
–2. "The writing included in this book has been chosen from Nichol's" (pp.12-13)
–3. "Nichol has said, at readings, that his favourite letter is H; in 'H" (pp.13-28)
–4. "Five years ago, I began the last paragraph of an essay entitled" (pp.28-29)
–5. A Brief Note on the Flux (p.29)
–6. Footnotes (pp.3o-31))
lv) SELECTED WRITING, by [Karl Siegler?] (rear cover; assemblage of quotes from:
–1. Douglas Barbour, This courageous poet stalks trail of saints
–2. Frank Davey, bpNichol
–3. George Woodcock, Poetry)
lvi) [untitled portrait of bpNichol], by Andy Phillips (rear cover; reduced version of the "Robert Planet Look-Alike" portrait)
"Artists represented include Matisse, Renoir, Picasso, Cocteau, Rodin, Henry Moore, Brett Whiteley, John Power, Ian Fairweather, Donald Friend, Arthur Boyd, Sydney Nolan, James Gleeson and many many more as well as the unnamed artists of four exquisite examples of naked Greek art."
Dolly Boutique 2nd anniversary outfit :)
Includes:
- Pink rose dress
- White cape with deer horns
If you're interested please send me an e-mail (at my profile)
Hope you like it ♥♥♥
Hagerstown, Indiana (September 10, 2012) The new Model T Ford Museum is slated to hold its grand opening during Richmond’s Octoberfest on September 28 at 6 p.m. The museum which was previously located in Centerville, Indiana near the Warm Glow Candle Factory for 5 years moved just a few miles east to Richmond, Indiana’s Historical Depot District this past spring.
Since the move to Richmond volunteers have been steadily preparing the museum’s new home, displays and vehicles for the event.
Today, a photo shoot for the Model T Museum’s newly acquired 1930 Pietenpol Sky Scout was held at the Hagerstown Airport.
The plan arrived at the airport around 10:00 a.m. this morning and was assembled by Model T enthusiasts and many of them brought their own Model Ts to use during the photo shoot.
One of the people there today was Mr. Jay Klehfoth who is the CEO and publisher of the Vintage Ford Magazine.
Jay is a walking encyclopedia when it comes to all things Model T. I was to learn he’s pretty knowledgeable in a lot of areas too. During our walk around of the plane Jay pointed out one of the parts for the engine had been made by a former factory in Richmond of all places. And there are many other special things about this airplane I’m sure he’ll be writing about in the next issue of the the Vintage Ford Magazine. He not only knew a lot about the Pietenpol Sky Scout plane that was being photographed for the magazine cover. He’s pretty sharp when it comes to airports too. He said that the Hagerstown airport were today’s photo shoot was done has the longest grass landing strip in the United States which to me made it the perfect place for today’s event.
This Pietenpol that will be on display at the museum is powered by a 20 HP Model T engine which was modified to include dual-ignition which is used in aviation. According to an article in the AntiqueAirfield.com website from September 10, 2012 there was only one original Pietenpol Sky Scout built by Bernard Pietenpol himself, and just two replicas. The article also said that all 3 were still flying.
The new Model T Ford Museum is going to be an exciting addition to what is one of Indiana’s grandest historical areas and a must in this part of the Midwest.
Richmond is a perfect place for any day trip. But, if you want to see all that Richmond has to offer you’ll need to plan on staying several days.
The Model T Ford Museum is located in Richmond’s Historic Depot District at 309 N 8th St, Richmond, IN 47374 - 765-488-0026.
Model T Ford Museum website: www.mtfca.com/clubpages/museum.htm
Additional Information:
The Model T Ford Club of America has nearly 8,000 families worldwide. Members are from all 50 states and 41 other countries.
The Vintage Ford Magazine is published bimonthly by the Model T Ford Club of America, 119 W. Main Street, Centerville, Indiana and is mailed to all members. Subscription rates are $35.00 per year (six issues) in the United States ($42.00 Canada and $44.00 elsewhere) and include member ship in the club.
All correspondence should be ad dressed to:
THE MODEL T FORD CLUB
OF AMERICA
P.O. Box 126
Centerville, IN 47330-0126
765-855-5248 fax 765-855-3428
e-mail: admin@mtfca.com
Raw Video: Prepping Pietenpol Sky Scout For Photo Shoot youtu.be/7_JnszAF8GA
Video: Pietenpol Sky Scout Photo Shoot youtu.be/h3m6ZWgNJMg
Video: Model T Ford Museum Grand Opening Set youtu.be/OwIiE5O1UQk
Classic Car Sunday - the theme for the August Goodwood Breakfast Club. Lots of well polished machinery on show in the sunshine.
Another fine issue of Hulton's National Weekly, this issue graced with a cover of actress Janet Leigh ("Hollywood's Happiest Housewife"). Features include coverage of the Kon Tiki expedition, a fashion feature (including a spread on dance dresses), the US presidential race and more. No more Janet Leigh, though. Shame!
Ars Electronica Home Delivery is a weekly program that includes guided tours of Ars Electronica's exhibitions, excursions to Ars Electronica Labs, visits to the Machine Learning Studio, concerts with real-time visualizations, deep space LIVE sessions, workshops with engineers and talks with artists and scientists from around the world, as well as programs for schools, universities and companies.
In order to make these streams happen, a lot of work has to be done as the light has to be porperly set up, the sound and cameras have to be adjusted, stage directions have to be given, the set has to be re-arranged, ...
Find out more about Ars Electronica Home Delivery:
ars.electronica.art/homedelivery/en/
Credit: Ars Electronica - Robert Bauernhansl
Im Winter, in der Regel von Anfang Januar bis Mitte Februar, finden in Harbin das Eis- und Schnee-Festival und das Eislaternen-Festival statt. An verschiedenen Orten im Stadtgebiet werden dann zum Teil filigran ausgearbeitete Eis- und Schneeskulpturen ausgestellt. Die größten Skulpturen sind Nachbauten berühmter Baudenkmale wie des Louvre in Paris oder des Pekinger Sommerpalastes. Dabei können die Skulpturen mehrere Meter hoch werden und sind nachts von innen mehrfarbig beleuchtet. Das Festival hat sich mittlerweile zu einer Winter-Touristenattraktion entwickelt und gehört zu den vier größten Eis- und Schneefestivals der Welt (neben dem Schneefestival in Sapporo, dem Skifestival in Oslo und der Winter-Sonnwendfeier in Québec).
Harbin is located in Northeast China under the direct influence of the cold winter wind from Siberia. The average temperature in summer is 21.2 °C (70.2 °F) and −16.8 °C (1.8 °F) in winter.
The annual Harbin International Ice and Snow Sculpture Festival has been held since 1985. Although the official start date is January 5 each year, in practice, many of the sculptures can be seen before. While there are ice sculptures throughout the city, there are two main exhibition areas: Enormous snow sculptures at Sun Island (a recreational area on the opposite side of the Songhua River from the city) and the separate "Ice and Snow World" that operates each night. Ice and Snow World features illuminated full size buildings made from blocks of 2–3 feet thick crystal clear ice directly taken from Songhua River which passes through the city. Winter activities in the festival include Yabuli Alpine Skiing, winter-swimming in Songhua River, and the ice-lantern exhibition in Zhaolin Garden. Snow carving and ice and snow recreations are world famous.
The "Harbin International Ice and Snow Festival" is one of the four largest ice and snow festivals in the world, along with Japan's Sapporo Snow Festival, Canada's Quebec City Winter Carnival, and Norway's Ski Festival.
Text: www.wikipedia.com
Spring Cottonwood and Sandstone Cliff. Zion National Park, Utah. April 4, 2012. © Copyright 2012 G Dan Mitchell - all rights reserved.
A cottonwood tree with early spring leaves stands in front of a sandstone cliff, Zion National Park, Utah.
This was my first visit to Zion National Park - believe it or not - and I had been thinking about photographing cottonwood trees against red sandstone cliffs well before we arrived. We got there in the afternoon, checked in to our lodgings, and soon went up into the main canyon on the shuttle and then hiked up toward the Narrows from there.
It was a special and unusual experience for me to be photographing in an entirely new place, and to have very little idea of the geography of the Zion at all - I had almost intentionally avoided researching ahead of time, preferring to take it for what it was when I arrived. I was so naive that when we passed over a bridge and I looked downstream I thought, "Oh, that is the Watchman." (For those who don't know, the photograph of the Watchman Tower above the Virgin River, photographed from the bridge that crosses the river just inside the park is, roughly speaking, the Zion equivalent of photographing Half Dome from Sentinel Bridge in Yosemite.) We kept going, staring up at the beautiful sandstone towers and walls as the shuttle travelled up the canyon to the very end at the Temple of Sinawava, where we got off and started to walk. The walls in this very area are beautiful, and my progress up the trail was very slow as I stopped to gawk and photograph all of these wonderful new subjects, including this almost bare tree with its first spring growth. against the backdrop of the sandstone cliffs.
G Dan Mitchell is a California photographer whose subjects include the Pacific coast, redwood forests, central California oak/grasslands, the Sierra Nevada, California deserts, urban landscapes, night photography, and more.
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Text, photographs, and other media are © Copyright G Dan Mitchell (or others when indicated) and are not in the public domain and may not be used on websites, blogs, or in other media without advance permission from G Dan Mitchell.
Known rulers of Tikal include:
* Yax Ehb' Xook c. 60 - dynastic founder
* Siyaj Chan K'awil Chak Ich'aak "Stormy Sky I" (2nd century)
* Yax Ch’aktel Xok c. 200
* Balam Ajaw "Decorated Jaguar" 292
* K'inich Ehb' c. 300
* Ix Une' B'alam "Queen Jaguar" 317
* "Leyden Plate Ruler" 320
* K'inich Muwaan Jol - died 359
* Chak Toh Ich’ak I "Jaguar Paw I" c.360 - 378
* Nun Yax Ayin (a noble from Teotihuacan), installed on Tikal's throne in 379
* Siyah K'ak', ruled to 411
* Siyah Chan K'awil II "Stormy Sky II" 411-456
* K'an-Ak "Kan Boar" 458-486
* Ma'Kin-na Chan (late 5th century)
* Chak Tok Ich'aak "Bahlum Paw Skull" 486-508
* Ix Yo K'in "Lady Tikal" 511-527
* Kalomte' Balam "Curl-Head", "19th Lord" c. 511-527
* Wak Chan K'awil "Double-Bird" - 537-562
* "Lizard Head II" 562
* K'inich Waaw 593-628
* K'inich Wayaan - (early / mid 7th century)
* K'inich Muwaan Jol II - (early / mid 7th century)
* Hasaw Chan K’awil "Double Moon", "Lord Chocolate" 682-734
* Yik’in Chan Kawil 734-766
* "Temple VI Ruler" 766-768
* Yax Nuun Ayiin II "Chitam" 768-790
* "Dark Sun" c. 810
* "Jewel K'awil" 849
* Jasaw Chan K'awiil II 869-88
More?:
Schweiz / Berner Oberland - Allmendhubel
Eiger, Mönch and Jungfrau
Eiger, Mönch und Jungfrau
The Allmendhubel (1,932 m) is a hill above Mürren, overlooking the valley of Lauterbrunnen in the canton of Bern. Its summit is easily accessible from Mürren by a funicular, the Allmendhubelbahn, which reaches a height of 1,907 metres. A restaurant is also located near the top.
In winter, the Allmendhubel is part of a ski area and includes several ski lifts.
(Wikipedia)
The Eiger (German pronunciation: [ˈaɪ̯ɡɐ]) is a 3,967-metre (13,015 ft) mountain of the Bernese Alps, overlooking Grindelwald and Lauterbrunnen in the Bernese Oberland of Switzerland, just north of the main watershed and border with Valais. It is the easternmost peak of a ridge crest that extends across the Mönch to the Jungfrau at 4,158 m (13,642 ft), constituting one of the most emblematic sights of the Swiss Alps. While the northern side of the mountain rises more than 3,000 m (10,000 ft) above the two valleys of Grindelwald and Lauterbrunnen, the southern side faces the large glaciers of the Jungfrau-Aletsch area, the most glaciated region in the Alps. The most notable feature of the Eiger is its nearly 1,800-metre-high (5,900 ft) north face of rock and ice, named Eiger-Nordwand, Eigerwand or just Nordwand, which is the biggest north face in the Alps.] This huge face towers over the resort of Kleine Scheidegg at its base, on the eponymous pass connecting the two valleys.
The first ascent of the Eiger was made by Swiss guides Christian Almer and Peter Bohren and Irishman Charles Barrington, who climbed the west flank on August 11, 1858. The north face, the "last problem" of the Alps, considered amongst the most challenging and dangerous ascents, was first climbed in 1938 by an Austrian-German expedition.The Eiger has been highly publicized for the many tragedies involving climbing expeditions. Since 1935, at least 64 climbers have died attempting the north face, earning it the German nickname Mordwand, literally "murder(ous) wall"—a pun on its correct title of Nordwand (North Wall).
Although the summit of the Eiger can be reached by experienced climbers only, a railway tunnel runs inside the mountain, and two internal stations provide easy access to viewing-windows carved into the rock face. They are both part of the Jungfrau Railway line, running from Kleine Scheidegg to the Jungfraujoch, between the Mönch and the Jungfrau, at the highest railway station in Europe. The two stations within the Eiger are Eigerwand (behind the north face) and Eismeer (behind the south face), at around 3,000 metres. The Eigerwand station has not been regularly served since 2016.
Etymology
The first mention of Eiger, appearing as "mons Egere", was found in a property sale document of 1252, but there is no clear indication of how exactly the peak gained its name. The three mountains of the ridge are commonly referred to as the Virgin (German: Jungfrau – translates to "virgin" or "maiden"), the Monk (Mönch), and the Ogre (Eiger; the standard German word for ogre is Oger). The name has been linked to the Latin term acer, meaning "sharp" or "pointed".
Geographic setting and description
The Eiger is located above the Lauterbrunnen Valley to the west and Grindelwald to the north in the Bernese Oberland region of the canton of Bern. It forms a renowned mountain range of the Bernese Alps together with its two companions: the Jungfrau (4,158 m (13,642 ft)) about 5.6 kilometres (3.5 mi) southwest of it and the Mönch (4,107 m (13,474 ft)) about in the middle of them. The nearest settlements are Grindelwald, Lauterbrunnen (795 m (2,608 ft)) and Wengen (1,274 m (4,180 ft)). The Eiger has three faces: north (or more precisely NNW), east (or more precisely ESE), and west (or more precisely WSW). The northeastern ridge from the summit to the Ostegg (lit.: eastern corner, 2,709 m (8,888 ft)), called Mittellegi, is the longest on the Eiger. The north face overlooks the gently rising Alpine meadow between Grindelwald (943 m (3,094 ft)) and Kleine Scheidegg (2,061 m (6,762 ft)), a mountain railways junction and a pass, which can be reached from both sides, Grindelwald and Lauterbrunnen/Wengen – by foot or train.
Politically, the Eiger (and its summit) belongs to the Bernese municipalities of Grindelwald and Lauterbrunnen. The Kleine Scheidegg (literally, the small parting corner) connects the Männlichen-Tschuggen range with the western ridge of the Eiger. The Eiger does not properly form part of the main chain of the Bernese Alps, which borders the canton of Valais and forms the watershed between the Rhine and the Rhône, but constitutes a huge limestone buttress, projecting from the crystalline basement of the Mönch across the Eigerjoch. Consequently, all sides of the Eiger feed finally the same river, namely the Lütschine.
Eiger's water is connected through the Weisse Lütschine (the white one) in the Lauterbrunnen Valley on the west side (southwestern face of the Eiger), and through the Schwarze Lütschine (the black one) running through Grindelwald (northwestern face), which meet each other in Zweilütschinen (lit.: the two Lütschinen) where they form the proper Lütschine. The east face is covered by the glacier called Ischmeer, (Bernese German for Ice Sea), which forms one upper part of the fast-retreating Lower Grindelwald Glacier. These glaciers' water forms a short creek, which is also confusingly called the Weisse Lütschine, but enters the black one already in Grindelwald together with the water from the Upper Grindelwald Glacier. Therefore, all the water running down the Eiger converges at the northern foot of the Männlichen (2,342 m (7,684 ft)) in Zweilütschinen (654 m (2,146 ft)), about 10 kilometres (6.2 mi) northwest of the summit, where the Lütschine begins its northern course to Lake Brienz and the Aare (564 m (1,850 ft)).
Although the north face of the Eiger is almost free of ice, significant glaciers lie at the other sides of the mountain. The Eiger Glacier flows on the southwestern side of the Eiger, from the crest connecting it to the Mönch down to 2,400 m (7,900 ft), south of Eigergletscher railway station, and feeds the Weisse Lütschine through the Trümmelbach. On the east side, the Ischmeer–well visible from the windows of Eismeer railway station–flows eastwards from the same crest then turns to the north below the impressive wide Fiescherwand, the north face of the Fiescherhörner triple summit (4,049 m (13,284 ft)) down to about 1,600 m (5,200 ft) of the Lower Grindelwald Glacier system.
The massive composition of the Eiger, Mönch, and Jungfrau constitutes an emblematic sight of the Swiss Alps and is visible from many places on the Swiss Plateau and the Jura Mountains in the northwest. The higher Finsteraarhorn (4,270 m (14,010 ft)) and Aletschhorn (4,190 m (13,750 ft)), which are located about 10 kilometres (6.2 mi) to the south, are generally less visible and situated in the middle of glaciers in less accessible areas. As opposed to the north side, the south and east sides of the range consist of large valley glaciers extending for up to 22 kilometres (14 mi), the largest (beyond the Eiger drainage basin) being those of Grand Aletsch, Fiesch, and Aar Glaciers, and is thus uninhabited. The whole area, the Jungfrau-Aletsch protected area, comprising the highest summits and largest glaciers of the Bernese Alps, was inscribed as a UNESCO World Heritage Site in 2001.
In July 2006, a piece of the Eiger, amounting to approximately 700,000 cubic metres of rock, fell from the east face. As it had been noticeably cleaving for several weeks and fell into an uninhabited area, there were no injuries and no buildings were hit.
Climbing history
While the summit was reached without much difficulty in 1858 by a complex route on the west flank, the battle to climb the north face has captivated the interest of climbers and non-climbers alike. Before it was successfully climbed, most of the attempts on the face ended tragically and the Bernese authorities even banned climbing it and threatened to fine any party that should attempt it again. But the enthusiasm which animated the young talented climbers from Austria and Germany finally vanquished its reputation of unclimbability when a party of four climbers successfully reached the summit in 1938 by what is known as the "1938" or "Heckmair" route.
The climbers that attempted the north face could be easily watched through the telescopes from the Kleine Scheidegg, a pass between Grindelwald and Lauterbrunnen, connected by rail. The contrast between the comfort and civilization of the railway station and the agonies of the young men slowly dying a short yet uncrossable distance away led to intensive coverage by the international media.
After World War II, the north face was climbed twice in 1947, first by a party of two French guides, Louis Lachenal and Lionel Terray, then by a Swiss party consisting of H. Germann, with Hans and Karl Schlunegger.
First ascent
In 1857, a first recorded attempt was made by Christian Almer, Christian Kaufmann, Ulrich Kaufmann guiding the Austrian alpinist Sigismund Porges. They did manage the first ascent of neighboring Mönch instead. Porges, however, successfully made the second ascent of the Eiger in July 1861 with the guides Christian Michel, Hans and Peter Baumann.
The first ascent was made by the western flank on August 11, 1858 by Charles Barrington with guides Christian Almer and Peter Bohren. On the previous afternoon, the party walked up to the Wengernalp hotel. From there they started the ascent of the Eiger at 3:30 a.m. Barrington describes the route much as it is followed today, staying close to the edge of the north face much of the way. They reached the summit at about noon, planted a flag, stayed for some 10 minutes and descended in about four hours. Barrington describes the reaching of the top, saying, "the two guides kindly gave me the place of first man up." After the descent, the party was escorted to the Kleine Scheidegg hotel, where their ascent was confirmed by observation of the flag left on the summit. The owner of the hotel then fired a cannon to celebrate the first ascent. According to Harrer's The White Spider, Barrington was originally planning to make the first ascent of the Matterhorn, but his finances did not allow him to travel there as he was already staying in the Eiger region.
Mittellegi ridge
Although the Mittellegi ridge had already been descended by climbers (since 1885) with the use of ropes in the difficult sections, it remained unclimbed until 1921. On the 10th of September of that year, Japanese climber Yuko Maki, along with Swiss guides Fritz Amatter, Samuel Brawand and Fritz Steuri made the first successful ascent of the ridge. The previous day, the party approached the ridge from the Eismeer railway station of the Jungfrau Railway and bivouacked for the night. They started the climb at about 6:00 a.m. and reached the summit of the Eiger at about 7:15 p.m., after an over 13 hours gruelling ascent. Shortly after, they descended the west flank. They finally reached Eigergletscher railway station at about 3:00 a.m. the next day.
Attempts on the north face
1935
In 1935, two young German climbers from Bavaria, Karl Mehringer and Max Sedlmeyer, arrived at Grindelwald to attempt the ascent of the north face. After waiting some time for the weather to improve, they set off, reaching the height of the Eigerwand station before stopping for their first bivouac. The following day, facing greater difficulties, they gained little height. On the third day, they made hardly any vertical gain. That night, the weather deteriorated, bringing snow and low cloud that shrouded the mountain from the observers below. Avalanches began to sweep the face. Two days later, the weather briefly cleared, and the two men were glimpsed a little higher and about to bivouac for the fifth night, before clouds descended again. A few days later, the weather finally cleared, revealing a completely white north face.: 225 Weeks later, the German World War I ace Ernst Udet went searching for the missing men with his aircraft, eventually spotting one of them frozen to death in what became known as the "Death Bivouac". Sedlmeyer's body was found at the foot of the face the following year by his brothers Heinrich and Martin Meier, who were part of a group looking for the victims of the 1936 climbing disaster. Mehringer's remains were found in 1962 by Swiss climbers below the "Flat Iron" (Bügeleisen) at the lefthand end of the second ice field.
1936
The next year ten young climbers from Austria and Germany came to Grindelwald and camped at the foot of the mountain. Before their attempts started one of them was killed during a training climb, and the weather was so bad during that summer that, after waiting for a change and seeing none on the way, several members of the party gave up. Of the four that remained, two were Bavarians, Andreas Hinterstoisser and Toni Kurz, and two were Austrians, Willy Angerer and Edi Rainer. When the weather improved they made a preliminary exploration of the lowest part of the face. Hinterstoisser fell 37 metres (121 ft) but was not injured. A few days later the four men finally began the ascent of the face. They climbed quickly, but on the next day, after their first bivouac, the weather changed; clouds came down and hid the group to the observers. They did not resume the climb until the following day, when, during a break, the party was seen descending, but the climbers could be seen only intermittently from the ground. The group had no choice but to retreat, since Angerer had suffered serious injuries from falling rock. The party became stuck on the face when they could not recross the difficult Hinterstoisser Traverse, from which they had taken the rope they had first used to climb it. The weather then deteriorated for two days. They were ultimately swept away by an avalanche, which only Kurz survived, hanging on a rope. Three guides started on an extremely perilous rescue attempt. They failed to reach him but came within shouting distance and learned what had happened. Kurz explained the fate of his companions: one had fallen down the face, another was frozen above him, and the third had fractured his skull in falling and was hanging dead on the rope.
In the morning the three guides came back, traversing the face from a hole near the Eigerwand station and risking their lives under incessant avalanches. Toni Kurz was still alive but almost helpless, with one hand and one arm completely frozen. Kurz hauled himself off the cliff after cutting loose the rope that bound him to his dead teammate below and climbed back onto the face. The guides were not able to pass an unclimbable overhang that separated them from Kurz. They managed to give him a rope long enough to reach them by tying two ropes together. While descending, Kurz could not get the knot to pass through his carabiner. He tried for hours to reach his rescuers who were only a few metres below him. Then he began to lose consciousness. One of the guides, climbing on another's shoulders, was able to touch the tip of Kurz's crampons with his ice-axe but could not reach higher. Kurz was unable to descend further and, completely exhausted, died slowly.
1937
An attempt was made in 1937 by Mathias Rebitsch and Ludwig Vörg. Although the attempt was unsuccessful, they were nonetheless the first climbers who returned alive from a serious attempt on the face. They started the climb on 11 August and reached a high point of a few rope lengths above Death Bivouac. A storm then broke and after three days on the wall they had to retreat. This was the first successful withdrawal from a significant height on the wall.
First ascent of the north face
The north face was first climbed on July 24, 1938 by Anderl Heckmair, Ludwig Vörg, Heinrich Harrer and Fritz Kasparek in a German–Austrian party. The party had originally consisted of two independent teams: Harrer (who did not have a pair of crampons on the climb) and Kasparek were joined on the face by Heckmair and Vörg, who had started their ascent a day later and had been helped by the fixed rope that the lead team had left across the Hinterstoisser Traverse. The two groups, led by the experienced Heckmair, decided to join their forces and roped together as a single group of four. Heckmair later wrote: "We, the sons of the older Reich, united with our companions from the Eastern Border to march together to victory."
The expedition was constantly threatened by snow avalanches and climbed as quickly as possible between the falls. On the third day a storm broke and the cold was intense. The four men were caught in an avalanche as they climbed "the Spider," the snow-filled cracks radiating from an ice-field on the upper face, but all possessed sufficient strength to resist being swept off the face. The members successfully reached the summit at four o'clock in the afternoon. They were so exhausted that they only just had the strength to descend by the normal route through a raging blizzard.
Other notable events
1864 (Jul 27): Fourth ascent, and first ascent by a woman, Lucy Walker, who was part of a group of six guides (including Christian Almer and Melchior Anderegg) and five clients, including her brother Horace Walker[
1871: First ascent by the southwest ridge, 14 July (Christian Almer, Christian Bohren, and Ulrich Almer guiding W. A. B. Coolidge and Meta Brevoort).
1890: First ascent in winter, Ulrich Kaufmann and Christian Jossi guiding C. W. Mead and G. F. Woodroffe.
1924: First ski ascent and descent via the Eiger glacier by Englishman Arnold Lunn and the Swiss Fritz Amacher, Walter Amstutz and Willy Richardet.
1932: First ascent of the northeast face ("Lauper route") by Hans Lauper, Alfred Zürcher, Alexander Graven and Josef Knubel
1970: First ski descent over the west flank, by Sylvain Saudan.
1986: Welshman Eric Jones becomes the first person to BASE jump from the Eiger.
1988: Original Route (ED2), north face, Eiger (3970m), Alps, Switzerland, first American solo (nine and a half hours) by Mark Wilford.
1991: First ascent, Metanoia Route, North Face, solo, winter, without bolts, Jeff Lowe.
1992 (18 July): Three BMG/UIAGM/IFMGA clients died in a fall down the West Flank: Willie Dunnachie; Douglas Gaines; and Phillip Davies. They had ascended the mountain via the Mittellegi Ridge.
2006 (14 June): François Bon and Antoine Montant make the first speedflying descent of the Eiger.
2006 (15 July): Approximately 700,000 cubic metres (20 million cubic feet) of rock from the east side collapses. No injuries or damage were reported.
2015 (23 July): A team of British Para-Climbers reached the summit via the West Flank Route. The team included John Churcher, the world's first blind climber to summit the Eiger, sight guided by the team leader Mark McGowan. Colin Gourlay enabled the ascent of other team members, including Al Taylor who has multiple sclerosis, and the young autistic climber Jamie Owen from North Wales. The ascent was filmed by the adventure filmmakers Euan Ryan & Willis Morris of Finalcrux Films.
Books and films
The 1959 book The White Spider by Heinrich Harrer describes the first successful ascent of the Eiger north face.
The Climb Up To Hell, 1962, by Jack Olson, an account of the ill-fated 1957 attempted climb of the north face by an Italian four-man team and the dramatic rescue of the sole survivor mounted by an international all-volunteer group of rescuers.
Eiger Direct, 1966, by Dougal Haston and Peter Gillman, London: Collins, also known as Direttissima; the Eiger Assault
The 1971 novel The Ice Mirror by Charles MacHardy describes the second attempted ascent of the Eiger north face by the main character.
The 1972 novel The Eiger Sanction is an action/thriller novel by Rodney William Whitaker (writing under the pseudonym Trevanian), based around the climbing of the Eiger. This was then made into the 1975 film The Eiger Sanction starring Clint Eastwood and George Kennedy. The Eiger Sanction film crew included very experienced mountaineers (e.g., Mike Hoover, Dougal Haston, and Hamish MacInnes, see Summit, 52, Spring 2010) as consultants, to ensure accuracy in the climbing footage, equipment and techniques.
The Eiger, 1974, by Dougal Haston, London: Cassell
The 1982 book Eiger, Wall of Death by Arthur Roth is an historical account of first ascents of the north face.
The 1982 book Traverse of The Gods by Bob Langley is a World War II spy thriller where a group escaping from Nazi Germany is trapped and the only possible exit route is via the Nordwand.
Eiger, 1983, a documentary film by Leo Dickinson of Eric Jones' 1981 solo ascent of the north face.
Eiger Dreams, 1990, a collection of essays by Jon Krakauer, begins with an account of Krakauer's own attempt to climb the north face.
Eiger: The Vertical Arena (German edition, 1998; English edition, 2000), edited by Daniel Anker, a comprehensive climbing history of the north face authored by 17 climbers, with numerous photographs and illustrations.
The IMAX film The Alps features John Harlin III's climb up the north face in September 2005. Harlin's father, John Harlin II, set out 40 years earlier to attempt a direct route (the direttissima) up the 6,000-foot (1,800 m) face, the so-called "John Harlin route". At 1300 m, his rope broke, and he fell to his death. Composer James Swearingen created a piece named Eiger: Journey to the Summit in his memory.
The 2007 docu/drama film The Beckoning Silence featuring mountaineer Joe Simpson, recounting—with filmed reconstructions—the ill-fated 1936 expedition up the north face of the Eiger and how Heinrich Harrer's book The White Spider inspired him to take up climbing. The film followed Simpson's eponymous 2003 book. Those playing the parts of the original climbing team were Swiss mountain guides Roger Schäli (Toni Kurz), Simon Anthamatten (Andreas Hinterstoisser), Dres Abegglen (Willy Angerer) and Cyrille Berthod (Edi Rainer). The documentary won an Emmy Award the subsequent year.
The 2008 German historical fiction film Nordwand is based on the 1936 attempt to climb the Eiger north face. The film is about the two German climbers, Toni Kurz and Andreas Hinterstoisser, involved in a competition with an Austrian duo to be the first to scale the north face of Eiger.
The 2010 documentary Eiger: Wall of Death by Steve Robinson.
(Wikipedia)
The Mönch (German pronunciation: [ˈmœnç] German: "monk") at 4,110 metres (13,480 ft) is a mountain in the Bernese Alps, in Switzerland. Together with the Eiger and the Jungfrau, it forms a highly recognisable group of mountains, visible from far away.
The Mönch lies on the border between the cantons of Valais and Bern, and forms part of a mountain ridge between the Jungfrau and Jungfraujoch to the west, and the Eiger to the east. It is west of Mönchsjoch, a pass at 3,650 metres (11,980 ft), Mönchsjoch Hut, and north of the Jungfraufirn and Ewigschneefäld, two affluents of the Great Aletsch Glacier. The north side of the Mönch forms a step wall above the Lauterbrunnen valley.
The Jungfrau railway tunnel runs right under the summit, at an elevation of approximately 3,300 metres (10,830 ft).
The summit was first climbed on record on 15 August 1857 by Christian Almer, Christian Kaufmann (1831-1861), Ulrich Kaufmann and Sigismund Porges.
(Wikipedia)
The Jungfrau (YOONG-frow, German pronunciation: [ˈjʊŋˌfʁaʊ̯], transl. "maiden, virgin"), at 4,158 meters (13,642 ft) is one of the main summits of the Bernese Alps, located between the northern canton of Bern and the southern canton of Valais, halfway between Interlaken and Fiesch. Together with the Eiger and Mönch, the Jungfrau forms a massive wall of mountains overlooking the Bernese Oberland and the Swiss Plateau, one of the most distinctive sights of the Swiss Alps.
The summit was first reached on August 3, 1811, by the Meyer brothers of Aarau and two chamois hunters from Valais. The ascent followed a long expedition over the glaciers and high passes of the Bernese Alps. It was not until 1865 that a more direct route on the northern side was opened.
The construction of the Jungfrau Railway in the early 20th century, which connects Kleine Scheidegg to the Jungfraujoch, the saddle between the Mönch and the Jungfrau, made the area one of the most-visited places in the Alps. Along with the Aletsch Glacier to the south, the Jungfrau is part of the Jungfrau-Aletsch area, which was declared a World Heritage Site in 2001.
Etymology
The name Jungfrau ("maiden, virgin"), which refers to the highest of the three prominent mountains overlooking the Interlaken region, along with the Mönch ("monk") and the Eiger ("ogre"), is most likely derived from the name Jungfrauenberg given to Wengernalp, the alpine meadow directly facing the huge northern side of the Jungfrau, across the Trummelbach gorge. Wengernalp was so named for the nuns of Interlaken Monastery, its historical owner. Contrary to popular belief, the name did not originate from the appearance of the snow-covered mountain, the latter looking like a veiled woman.
The "virgin" peak was heavily romanticized as "goddess" or "priestess" in late 18th to 19th century Romanticism. Its summit, considered inaccessible, remained untouched until the 19th century. After the first ascent in 1811 by Swiss alpinist Johann Rudolf Meyer, the peak was jokingly referred to as "Mme Meyer" (Mrs. Meyer).
Geographic setting
Politically, the Jungfrau (and its massif) is split between the municipalities of Lauterbrunnen (Bern) and Fieschertal (Valais). It is the third-highest mountain of the Bernese Alps after the nearby Finsteraarhorn and Aletschhorn, respectively 12 and 8 km (7.5 and 5 mi) away. But from Lake Thun, and the greater part of the canton of Bern, it is the most conspicuous and the nearest of the Bernese Oberland peaks; with a height difference of 3,600 m (11,800 ft) between the summit and the town of Interlaken. This, and the extreme steepness of the north face, secured for it an early reputation for inaccessibility.
The Jungfrau is the westernmost and highest point of a gigantic 10 km (6.2 mi) wall dominating the valleys of Lauterbrunnen and Grindelwald. The wall is formed by the alignment of some of the biggest north faces in the Alps, with the Mönch (4,107 m or 13,474 ft) and Eiger (3,967 m or 13,015 ft) to the east of the Jungfrau, and overlooks the valleys to its north by a height of up to 3 km (1.9 mi). The Jungfrau is approximately 6 km (3.7 mi) from the Eiger; with the summit of the Mönch between the two mountains, 3.5 km (2.2 mi) from the Jungfrau. The Jungfraujoch is the saddle between the Jungfrau and the Mönch and the Eigerjoch is the saddle between the Mönch and the Eiger. The wall is extended to the east by the Fiescherwand and to the west by the Lauterbrunnen Wall, although it follows different directions from the Jungfrau and the Eiger.
The difference of altitude between the deep valley of Lauterbrunnen (800 m or 2,600 ft) and the summit is particularly visible from the area of Mürren. From the valley floor, west of the massif, the altitude gain is more than 3 km (1.9 mi) for a horizontal distance of 4 km (2.5 mi).
The landscapes around the Jungfrau are extremely contrasted. In contrast to the vertiginous precipices of its northwest, the mountain's southeastern side emerges from the upper snows of the Jungfraufirn, one of the main feeders of the Aletsch Glacier, at around 3,500 meters (11,500 ft). The 20-kilometer-long (12 mi) valley of Aletsch on the southeast is completely uninhabited, and is surrounded by neighboring valleys with similar landscapes. The area as a whole constitutes the largest glaciated area not just in the Alps, but in Europe as well.
Climbing history
In 1811, the brothers Johann Rudolf (1768–1825) and Hieronymus Meyer, sons of Johann Rudolf Meyer (1739–1813), the head of a rich merchant family of Aarau, along with several servants and a porter picked up at Guttannen, first reached the Valais by way of the Grimsel, and crossed the Beich Pass, a glacier pass over the Oberaletsch Glacier, to the head of the Lötschen valley. There, they added two local chamois hunters, Alois Volken and Joseph Bortis, to their party and traversed the Lötschenlücke before reaching the Aletschfirn (the west branch of the Aletsch Glacier), where they established the base camp, north of the Aletschhorn. After the Guttannen porter was sent back alone over the Lötschenlücke, the party finally reached the summit of the Jungfrau by the Rottalsattel on August 3. They then recrossed the two passes named to their point of departure in Valais, and went home again over the Grimsel.
The journey was a most extraordinary one for the time, and some persons threw doubts at its complete success. To settle these, another expedition was undertaken in 1812. In this the two sons, Rudolf (1791–1833) and Gottlieb (1793–1829), of Johann Rudolf Meyer, played the chief parts. After an unsuccessful attempt, defeated by bad weather, in the course of which the Oberaarjoch was crossed twice (this route being much more direct than the long detour through the Lötschental), Rudolf, with the two Valais hunters (Alois Volker and Joseph Bortis), a Guttannen porter named Arnold Abbühl, and a Hasle man, bivouacked on a depression on the southeast ridge of the Finsteraarhorn. Next day (August 16) the whole party attempted the ascent of the Finsteraarhorn from the Studer névé on the east by way of the southeast ridge, but Meyer, exhausted, remained behind. The following day the party crossed the Grünhornlücke to the Aletsch Glacier, but bad weather then put an end to further projects. At a bivouac, probably just opposite the present Konkordia Hut, the rest of the party, having come over the Oberaarjoch and the Grünhornlücke, joined the Finsteraarhorn party. Gottlieb, Rudolf's younger brother, had more patience than the rest and remained longer at the huts near the Märjelensee, where the adventurers had taken refuge. He could make the second ascent (September 3) of the Jungfrau, the Rottalsattel being reached from the east side as is now usual, and his companions being the two Valais hunters.
The third ascent dates from 1828, when several men from Grindelwald, headed by Peter Baumann, planted their flag upon the summit. Next came the ascent by Louis Agassiz, James David Forbes, Heath, Desor, and Duchatelier in 1841, recounted by Desor in his Excursions et Séjours dans les Glaciers. Gottlieb Samuel Studer published an account of the next ascent made by himself and Bürki in 1842.
In 1863, a party consisting of three young Oxford University graduates and three Swiss guides successfully reached the summit and returned to the base camp of the Faulberg (located near the present position of the Konkordia Hut) in less than 11 hours (see the section below, The 1863 Ascent). In the same year Mrs Stephen Winkworth became the first woman to climb the Jungfrau. She also slept overnight in the Faulberg cave prior to the ascent as there was no hut at that time.
Before the construction of the Jungfraujoch railway tunnel, the approach from the glaciers on the south side was very long. The first direct route from the valley of Lauterbrunnen was opened in 1865 by Geoffrey Winthrop Young, H. Brooke George with the guide Christian Almer. They had to carry ladders with them in order to cross the many crevasses on the north flank. Having spent the night on the rocks of the Schneehorn (3,402 m or 11,161 ft) they gained next morning the Silberlücke, the depression between the Jungfrau and Silberhorn, and thence in little more than three hours reached the summit. Descending to the Aletsch Glacier they crossed the Mönchsjoch, and passed a second night on the rocks, reaching Grindelwald next day. This route became a usual until the opening of the Jungfraujoch.
The first winter ascent was made on 23 January 1874, by Meta Brevoort and W. A. B. Coolidge with guides Christian and Ulrich Almer. They used a sled to reach the upper Aletsch Glacier, and were accompanied by Miss Brevoort's favorite dog, Tschingel.
The Jungfrau was climbed via the west side for the first time in 1885 by Fritz and Heinrich von Allmen, Ulrich Brunner, Fritz Graf, Karl Schlunegger and Johann Stäger—all from Wengen. They ascended the Rottal ridge (Innere Rottalgrat) and reached the summit on 21 September. The more difficult and dangerous northeast ridge that connects the summit from the Jungfraujoch was first climbed on 30 July 1911 by Albert Weber and Hans Schlunegger.
In July 2007, six Swiss Army recruits, part of the Mountain Specialists Division 1, died in an accident on the normal route. Although the causes of the deaths was not immediately clear, a report by the Swiss Federal Institute for Snow and Avalanche Research concluded that the avalanche risk was unusually high due to recent snowfall, and that there was "no other reasonable explanation" other than an avalanche for the incident.
The 1863 Ascent
The Führerbuch of the Alpine guide Peter Baumann records an ascent of the Jungfrau made by himself with three men from England in July 1863. The foreign climbers were long thought to have been John Tyndall, J.J. Hornby and T.H. Philpott, until in 1958 the records were checked by the Alpine Club and the following conclusion was reached:
On July 23, 1963, Phillpotts, with James Robertson and H.J. Chaytor, climbed the Jungfrau (the entry shown in A.J. 32. 227 was wrongly transcribed by Montagnier, who says ‘T.H. Philpott’ for J.S. Phillpotts). The entry in Peter Baumann’s Führerbuch (facsimile in A.C. archives) says that the trio crossed the Strahlegg Pass and the Oberaarjoch, and then climbed the Jungfrau from the Eggishorn.
Tyndall, Hornby and Philpott were well-known Alpinists, but there is no record of their having attempted the Jungfrau in 1863. Robertson, Chaytor and Phillpotts were novices; they had recently graduated from Oxford University where they had all been keen members of the Oxford University Boat Club.
William Robertson (1839–1892), the leader of the expedition (wrongly called ‘James’ in the Note quoted above), was an Australian by birth, and the first non-British national to take part in the Oxford and Cambridge Boat Race. He later became a barrister and member of parliament in Australia. He and H.J. Chaytor (possibly the father of the medievalist Henry John Chaytor) were both members of the victorious Oxford team in the 1861 Boat Race. James Surtees Phillpotts (1839–1930) was the third member of the team; he would later become headmaster of Bedford School. The trio had three Swiss guides, Peter Baumann, Peter Kaufmann ("Grabipeter", father of Peter Kaufmann the younger) and Rubi.
A description of the ascent of the Jungfrau is contained in a letter dated Sunday 26 July which Phillpotts wrote to his friend Alexander Potts (later to become the first headmaster of Fettes College). The letter is now in the possession of the Alpine Club. The following extracts are from that letter.
The Virgin certainly did not smile on the poor "fools who rushed in" on her sacred heights, i.e. in plain British, we had the treadmill slog, the biting wind, the half frost-bitten feet and the flayed faces that generally attend an Alpine ascent.
We got to the Faulberg hole about dark, and enjoyed the coffee the longman (Kauffmann) made, as one would in a hole in a rock in a cold evening. The "Faulberg Nachtlager" consists of two holes and a vestibule to the upper hole. The Upper Hole in which we lodged just contained Chay[tor], the Guv [Robertson] and myself, stretched at full length on a little hay over a hard rock mattress, convex instead of concave at the point where one likes to rest one's weight. Chaytor was in the middle, and as we were very close was warm and slept. The Guv and I courted Nature's soft nurse in vain. At two we got up and methodically put our feet into the stocks, i.e. our boots, breakfasted and shivered, then started (unwashed of course, as the cold gave us malignant hydrophobia) a little after 3:30.
The hole was about 150 feet [46 m] up one of the loose stone cliffs one now knows so well. So we groped our way down it and over the moraine – the stars still lingering, as day was just dawning. We could not start at 1:30, the proper time, as there was no moon and we wanted light as we had to tramp the glacier at once. Rubi led, and off we went, roped and in Indian file, in the old treadmill way over the slippery plowed-field-like snow that lay on the upper glacier, for a pull without a check of one or two hours.
At last we came to the region of bergschrunds and crevasses. They seemed to form at first an impassable labyrinth, but gradually the guides wound in and out between the large rifts, which were exquisitely lovely with their overhanging banks of snow and glittering icicles, and then trod as on pins and needles over a snowbridge here and there, or had to take a jump over the more feasible ones – and we found ourselves at the foot of the mountain; trudged up on the snow which ought to have been crisp but was even then more or less fresh fallen and sloppy; had to creep over about three crevasses, and after a tiresome pull, dragging one leg after another out of ankle or knee deep snow, we got on a crest of snow at right angles to the slope we had just come up. That slope with its crevasses on one side, and on the other a shorter and much steeper one which led in a few steps to a precipice.
All along this crest went a snakelike long crevasse, for which we had continually to sound, and go first one side and then the other; then we got to the foot of the saddle. Some twenty or thirty steps, some cut, some uncut, soon took us up a kind of hollow, and we got on a little sloping plateau of some six feet [1.8 m] large, where we left the grub and the knapsack, keeping my small flask of cognac only. Then up a steep ice slope, very steep I should say, down which the bits of ice cut out of the steps hopped and jumped at full gallop and then bounded over to some bottomless place which we could not see down. Their pace gave one an unpleasant idea of the possible consequence of a slip.
Here we encountered a biting bitter wind. Peter Baumann cut magnificent steps, at least he and Rubi did between them, the one improving on the other's first rough blows. After Rubi came Chaytor with Kauffmann behind him, then the Guv, and then myself, the tail of the string. Each step was a long lift from the last one, and as the snow was shallow they had to be cut in the ice which was like rock on this last slope.
Suddenly there burst upon us, on lifting our heads over the ridge, the green and cheerful valleys of Lauterbrunnen and Interlaken, of Grindelwald and a distant view of others equally beautiful stretching on for ever in one vast panorama. On the other side in grim contrast there was a wild and even awful scene. One gazed about one and tried in vain to see to the bottom of dark yawning abysses and sheer cliffs of ice or rock.
Tourism
Named after the Jungfrau, the Jungfrau Region of the Bernese Oberland is a major tourist destination in the Alps and includes a large number of railways and other facilities. While the mountain peak was once difficult to access, the Jungfrau Railway, a rack railway, now goes to the Jungfraujoch railway station at 3,454 m (11,332 ft), therefore providing an easy access to the upper Aletsch Glacier and a relatively short access to the Jungfrau itself, the height difference between the station and the summit being only 704 metres and the horizontal distance being slightly less than 2 kilometres. As a result, in the popular mind, the Jungfrau has become a mountain associated with the Bernese Oberland and Interlaken, rather than with Upper Valais and Fiesch.
In 1893, Adolf Guyer-Zeller conceived of the idea of a railway tunnel to the Jungfraujoch to make the glaciated areas on its south side more accessible. The building of the tunnel took 16 years and the summit station was not opened before 1912. The goal was in fact to reach the summit of the Jungfrau with an elevator from the highest railway station, located inside the mountain. The complete project was not realized because of the outbreak of the World War I. Nevertheless, it was at the time one of the highest railways in the world and remains today the highest in Europe and the only (non-cable) railway on Earth going well past the perennial snow-line.
The Jungfrau Railway leaves from Kleine Scheidegg, which can be reached from both sides by trains from Grindelwald, and Lauterbrunnen via Wengen. The train enters the Jungfrau Tunnel running eastward through the Eiger just above Eigergletscher, which is, since 2020, also accessible by aerial tramway from Grindelwald. Before arriving at the Jungfraujoch, it stops for a few minutes at two other stations, Eigerwand (on the north face of the Eiger) and Eismeer (on the south side), where passengers can see through the holes excavated from the mountain. The journey from Kleine Scheidegg to Jungfraujoch takes approximately 50 minutes including the stops; the downhill return journey taking only 35 minutes.
A large complex of tunnels and buildings has been constructed at the Jungfraujoch, referred to as the "Top of Europe". There are several restaurants and bars, shops, multimedia exhibitions, a post office, and a research station with dedicated accommodation facilities. An elevator enables access to the top of the Sphinx and its observatory, at 3,571 m (11,716 ft), the highest viewing platform of the area. Outside, at the level of the Jungfraujoch, there is a ski school, and the "Ice Palace", a collection of elaborate ice sculptures displayed inside the Aletsch Glacier. Another tunnel leads to the east side of the Sphinx, where one can walk on the glacier up to the Mönchsjoch Hut, the only hotel infrastructure in the area.
Apart from the Jungfraujoch, many facilities have been built in the Jungfrau Region, including numerous mountain railways. In 1908, the first public cable car in the world, the Wetterhorn Elevator, opened at the foot of the Wetterhorn, but was closed seven years later. The Schilthorn above Mürren, the Männlichen above Wengen, and the Schynige Platte above Wilderswil, offer good views of the Jungfrau and the Lauterbrunnen valley. On the south side, the Eggishorn above Fiesch also offers views of the Jungfrau, across the Aletsch Glacier.
Climbing routes
The normal route follows the traces of the first climbers, but the long approach on the Aletsch Glacier is no longer necessary. From the area of the Jungfraujoch the route to the summit takes only a few hours. Most climbers start from the Mönchsjoch Hut. After a traverse of the Jungfraufirn the route heads to the Rottalsattel (3,885 m or 12,746 ft), from where the southern ridge leads to the Jungfrau. It is not considered a very difficult climb but it can be dangerous on the upper section above the Rottalsattel, where most accidents happen. The use of the Jungfrau Railway instead of the much more gradual approach from Fiesch (or Fieschertal), via the Konkordia Hut, can cause some acclimatization troubles as the difference of altitude between the railway stations of Interlaken and Jungfraujoch is almost 3 km (1.9 mi).
(Wikipedia)
Der Eiger ist ein Berg in den Berner Alpen mit einer Höhe von 3967 m ü. M. Er ist dem Hauptkamm der Berner Alpen etwas nördlich vorgelagert und steht vollständig auf dem Territorium des Schweizer Kantons Bern. Zusammen mit Mönch und Jungfrau, deren Gipfel auf der Grenze zum Kanton Wallis liegen, dominiert der Eiger die Landschaft des zentralen Berner Oberlandes. Die etwa 3000 Meter über dem Tal aufragenden Nordflanken dieser Berge stellen die Schauseite einer der bekanntesten je als ein «Dreigestirn» bezeichneten Gipfel-Dreiergruppen in den Alpen dar.
Insbesondere die Nordwand des Eigers fasziniert sowohl Bergsteiger als auch Alpin-Laien. Durch dramatische Begehungsversuche und gelungene Begehungen dieser Wand wurde der Eiger weltweit bekannt und immer wieder ins Blickfeld der Öffentlichkeit gerückt – nicht zuletzt, da die gesamte Wand von Grindelwald und der Bahnstation Kleine Scheidegg aus einsehbar ist. Die Jungfraubahn mit ihrem Tunnel durch den Eigerfels ist seit ihrer Eröffnung im Jahr 1912 ein Touristenmagnet.
Namensherkunft
Die erste urkundliche Erwähnung des Eigers stammt aus dem Jahre 1252 – dies ist die zweitfrüheste urkundliche Erwähnung eines Schweizer Bergs nach dem Bietschhorn (1233). Am 24. Juli 1252 wurde in einer Verkaufsurkunde zwischen Ita von Wädiswyl und der Propstei Interlaken ein Grundstück mit den Worten «ad montem qui nominatur Egere» (dt.: Bis zum Berg, der Eiger genannt wird) abgegrenzt. Ein halbes Jahrhundert später wird der Eiger in einem Belehnungsbrief erstmals in deutscher Sprache erwähnt: «under Eigere».
Für die Herkunft des Namens gibt es drei gängige Erklärungen. Eine erste ist der althochdeutsche Name Agiger oder Aiger, wie der erste Siedler unterhalb des Eigers geheissen haben soll. Der Berg über dessen Weiden wurde deshalb Aigers Geissberg oder auch nur Geissberg genannt. Hieraus entwickelten sich dann im Laufe der Zeit die direkten Vorgänger der heutigen Bezeichnung. Die Herkunft des Namens könnte auch von dem lateinischen Wort acer kommen, woraus sich im Französischen aigu entwickelte. Beide Worte haben die Bedeutung scharf beziehungsweise spitz – in Anlehnung an die Form des Eigers. Die dritte Erklärung stammt von der früher gebräuchlichen Schreibweise Heiger, was sich aus dem Dialektausdruck «dr hej Ger» entwickelt haben könnte (hej bedeutet hoch, Ger war ein germanischer Wurfspiess). Wiederum wäre hier die Form des Eigers ausschlaggebend für seine Bezeichnung.
Im Zusammenhang mit dem Eiger wird auch des Öfteren die Namensähnlichkeit mit dem Oger, einem menschenähnlichen Unhold, genannt. In Anlehnung an das Dreigestirn «Eiger–Mönch–Jungfrau» gibt es die Erzählung, der Unhold Eiger wolle seine lüsternen Pranken auf die Jungfrau legen, woran er aber vom fröhlichen Mönch gehindert werde. Zu dieser Geschichte sind in Grindelwald alte Karikaturen und neuere Postkarten zu kaufen.
Lage und Umgebung
Der Eiger erhebt sich direkt südwestlich von Grindelwald (Amtsbezirk Interlaken). Die bekannte Nordwand ist genaugenommen eine Nordwestwand. Neben dieser existiert in der berühmten «Eiger-Nordansicht» auch noch die Nordostwand. Sie bildet die Basis für den scharfen Mittellegigrat, der vom Unteren Grindelwaldgletscher zum Gipfel zieht. Auf der gegenüberliegenden Seite begrenzt der Westgrat die Nordwand. Ihm folgt die Westflanke, in welcher sich der Eigergletscher und der Klein Eiger befinden. An diesen schliessen sich der Südwestgrat und noch ein Stück östlicher der Südgrat an, der wiederum die Südostwand begrenzt, welche bis zum Mittellegigrat reicht. Südöstlich des Eigers liegt der Grindelwald-Fieschergletscher.
In der Umgebung des Eigers befinden sich einige Viertausender des Aarmassivs. Im Osten ist er umgeben von Schreckhorn (4078 m ü. M.) und Lauteraarhorn (4042 m ü. M.), im Südosten vom Grossen Fiescherhorn (4049 m ü. M.), und im Südwesten ist der Mönch (4107 m ü. M.) durch das Nördliche und Südliche Eigerjoch vom Eiger getrennt. Zusammen mit dem Mönch und der Jungfrau (4158 m ü. M.) bildet der Eiger das «Dreigestirn», bei dem der Eiger den nordöstlichen und die Jungfrau den südwestlichen Endpunkt bildet. Entgegen der steil abfallenden Nordseite des Berges befindet sich im Süden des Eigers die Hochfläche und Gletscherwelt der Berner Alpen. Seit Ende 2001 gehört der Eiger zum Gebiet des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.
Geologie
Der Eiger ist ein Teil des helvetischen Systems, das im Grossraum um den Thunersee die Decken des Alpennordrandes bildet. In einer späten Phase der alpidischen Gebirgsfaltung wurden die helvetischen Kalk-Sedimente von ihrer kristallinen Basis abgeschürft und in Form einer Abscherungsdecke nach Nordwesten verschoben. Während des Faltungsprozesses in der Alpenentstehung brachen die Kalkbänke auf und Kluft- sowie Faltensysteme entstanden, die später mit ausgefälltem Calcit geschlossen wurden. Wichtigste Bestandteile der Sedimente sind der Schrattenkalk der Kreidezeit und der Malmkalk. Als Füll- und Schmiermaterial dienten Mergel und Tonschiefer.
Die klar erkennbare Faltung des Helvetikums mit seinen gebänderten, plattigen Kalkschichten zeigt sich auch am Eiger. Das Massiv des Eigers besteht komplett aus Kalk der helvetischen Zone und schliesst die Flyschschichten und die Molasse des Grindelwaldbeckens steil nach Süden hin ab. Weil der Talkessel von Grindelwald so reich gegliedert ist, finden hier die verschiedensten Tiere einen Lebensraum.[6] Südlich des Eigers schliesst sich das Aarmassiv mit seinem Innertkirchner-Lauterbrunner-Kristallin an. Teilweise hat sich dieses über die Sedimente des Eiger geschoben. Im Bereich des Mönchs treffen die Sedimente auf Altkristallin. Die typischen Gesteine des helvetischen Systems im Bereich des Eigers entstanden während des Jura, dem mittleren Zeitabschnitts des Mesozoikums. Der vorherrschende Kalk ist dabei mit verschiedenen Gesteinen durchmischt. Es zeigen sich Mergel-Kalke und -Schiefer, Ton-Schiefer, Eisenoolith sowie kalkige Sandsteine.
Blick auf Eigergletscher und Klein Eiger
Die Kalkschichten des Eigers lagern auf Gneis und sind um 60–70° nach Norden geneigt. Geprägt wurde die heutige Form des Eigers durch die Eiszeiten. Während der Riss-Kaltzeit reichte die Vergletscherung bis an den Fuss der Nordwand. In der Würm-Kaltzeit war die Mächtigkeit des Eises um 200 Meter geringer. Durch die Bewegung der Gletscher wurde die Erdoberfläche umgestaltet. Vom Eis überlagerte Landschaften wurden abgeschliffen, wohingegen unbedeckte Bereiche durch Verwitterung und andere Formen der Erosion verändert wurden. Mit dem Rückzug des Eises änderten sich auch die Druckverhältnisse im Gestein, was sich durch Entlastungsbewegungen formgebend auswirkte. Prägend für den Eiger und seine Form war die allseitige Umlagerung von Eismassen, welche für einen recht gleichmässigen und markanten Abrieb aller Wände sorgte. Darüber hinaus war die Nordwand durch ihre Exposition den Abtragungsprozessen wie Frostverwitterung mehr ausgesetzt.
Felssturz
2006 ereignete sich am Eiger ein grosser Bergsturz, der öffentliches Interesse auf sich zog. An der Ostseite des Berges, unterhalb des Mittellegigrates, war durch Felsbewegungen ein rund 250 Meter langer Spalt entstanden, der eine Breite von etwa 7 Metern erreichte.Danach senkten sich die äusseren Teile mehrere Zentimeter pro Tag ab. Eine Ursache dieser Felsabspaltung könnte sowohl das massive Eindringen von Schmelzwasser in den Felsen gewesen sein, als auch eine Instabilität des Gesteins durch den Rückgang des Gletschers unterhalb des Felsabbruchs infolge der globalen Erwärmung. Am 13. Juli 2006 um 19:24 Uhr stürzten rund 500'000 Kubikmeter Felsbrocken auf den Unteren Grindelwaldgletscher. Über der Gemeinde Grindelwald schwebte stundenlang eine Staubwolke. Bereits am Nachmittag desselben Tages war die sogenannte «Madonna vom Eiger» zu Tal gestürzt. Hierbei handelte es sich um einen ungefähr 30 Meter hohen schlanken Felsturm mit rund 600 Kubikmeter Volumen.
Seit diesen Ereignissen wird die Felsnase (Gesamtvolumen: ungefähr eine Million Kubikmeter Gestein), aus der die Gesteinsmasse abbrach, von der Universität Lausanne beobachtet. Die Beobachtungen ergaben, dass sich die Nase von Juli 2007 bis August 2008 auf einer nach Osten geneigten Gleitfläche um 15 Meter talwärts bewegte. Zusätzlich kippte die Gesteinsmasse um zwei Grad nach Nordosten. Die Kluft zwischen Berg und Felsbrocken betrug im August 2008 50 Meter. Immer wieder brechen Gesteinsteile ab und stürzen zu Tal. Gebremst und stabilisiert wird die Masse vom Gletschereis, in das die Felsnase gleitet. Dies verhindert, dass die Nase als kompakte Masse zu Tal stürzt. So gilt es als wahrscheinlicher, dass der Gesteinsblock in sich selbst zusammenfallen wird.
(Wikipedia)
Der Mönch ist ein 4107 m ü. M. hoher Berg der Berner Alpen in der Schweiz. Zusammen mit dem Eiger und der Jungfrau bildet er eine markante, von weit her sichtbare Dreiergruppe, ein sogenanntes „Dreigestirn“.
Seine Erstbesteigung fand am 15. August 1857 durch Christian Almer, Christian Kaufmann, Ulrich Kaufmann und Sigismund Porges statt.
Südöstlich des Mönch liegt die Mönchsjochhütte, eine 3657 m ü. M. hoch gelegene Berghütte wenig oberhalb des oberen Mönchsjochs, das den Mönch vom Trugberg trennt.
Höhenbestimmung
1935 wurde die Höhe des Mönchs mit 4099 m ü. M. bestimmt. Diese Zahl ist noch heute häufig in der Literatur zu finden. 1993 ergaben jedoch Messungen per Luftfotogrammetrie eine Höhe von 4107 m ü. M.. Daraufhin wurde der Wert auf der Landeskarte der Schweiz korrigiert. Mit einer Messung per GPS ermittelte man 1997 eine Höhe von 4109,4 m ü. M.; und bei einer erneuten luftfotogrammetrischen Messung von 1999 resultierte sogar eine Höhe von 4110 m ü. M.. Diese neuen Messwerte wurden jedoch nicht auf den amtlichen Karten berücksichtigt. Für diese abweichenden Werte sind nicht nur Messfehler verantwortlich, sondern auch die Tatsache, dass der Mönch eine Kuppe aus Firn besitzt, welche in den letzten Jahren gewachsen ist.
Name
Am Fusse des Mönchs befinden sich Alpweiden, auf welchen früher Wallache, sogenannte „Münche“, gesömmert wurden. So hat man den über den Münchenalpen gelegenen Berg Münchenberg genannt und schliesslich nur noch Münch oder Mönch.
Routen
Südarm des Ostgrates (Normalroute)
Schwierigkeit: ZS-, mit II. UIAA-Grad Felskletterei
Zeitaufwand: 2½–3½ Std. von der Mönchsjochhütte, 3–4 Std. vom Jungfraujoch
Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Südwestgrat
Schwierigkeit: ZS-, mit III-. UIAA-Grad Felskletterei
Zeitaufwand: 3–4 Stunden
Ausgangspunkt: Jungfraujoch (3454 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Nordostarm des Ostgrates
Schwierigkeit: ZS, mit III+. UIAA-Grad Felskletterei
Zeitaufwand: 4–5 Stunden
Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Nordostgrat
Schwierigkeit: ZS
Zeitaufwand: 4–5 Stunden
Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Nordwestbollwerk (Nollen)
Schwierigkeit: S
Zeitaufwand: 6–10 Stunden
Ausgangspunkt: Guggihütte (2791 m ü. M.)
Talort: Kleine Scheidegg (2061 m ü. M.)
(Wikipedia)
Die Jungfrau ist ein Berg in der Schweiz. Sie ist mit 4158 m ü. M. der dritthöchste Berg der Berner Alpen und bildet zusammen mit Eiger und Mönch eine markante Dreiergruppe, ein sogenanntes «Dreigestirn».
Am 13. Dezember 2001 wurde die Jungfrau zusammen mit südlich angrenzenden Gebieten als Schweizer Alpen Jungfrau-Aletsch in die Liste als UNESCO-Weltnaturerbe aufgenommen.
Lage und Umgebung
Über den Jungfrau-Gipfel verläuft die Grenze zwischen den Kantonen Bern und Wallis. Der Berg ist ausserordentlich vielgestaltig. Im Norden und Nordwesten, auf ihrer „weiblichen“ Schauseite (vgl. Foto) sind ihr Wengen-Jungfrau, Schneehorn, das Silberhorn, das Chly Silberhoren und der „Schwarzmönch“ vorgelagert sowie die zerrissenen Kühlauenen- und Giessengletscher. Im Westen erhebt sie sich fast eisfrei volle 3250 Meter über dem hinteren Lauterbrunnental. Es ist dies (nach dem Mont Blanc) der zweithöchste direkte Abhang in den Alpen. Ihre Südwand erhebt sich über dem versteckten Rottalgletscher und ihre Ostwand über den Firnen am Jungfraujoch.
Die Pläne, auf die Jungfrau eine Bergbahn zu bauen, wurden aufgrund finanzieller Schwierigkeiten nicht realisiert. Die ursprünglich bis unter den Gipfel geplante Jungfraubahn wurde bis 1912 mit Endstation Jungfraujoch fertiggestellt.
Auf dem untersten Absatz des Nordostgrats haben die PTT einen Funk-Umsetzer auf 3777 m ü. M. installiert.
Geologie
Die Jungfrau liegt im nördlichen Randbereich des Aarmassivs, eines der sogenannten Zentralmassive der Schweizer Alpen. Ihre höheren Lagen (Silberhorn, Wengen-Jungfrau und Hauptgipfel) sowie ihre Westflanke bis hinunter zum oberen Ende des Lauterbrunnentals sind weit überwiegend aus kristallinem Grundgebirge (prä-triassische Gneise, Glimmerschiefer u. ä.) der Helvetischen Zone aufgebaut. Die Nordwestflanke hingegen, der ganze «Vorbau» (Schwarzmönch, Rotbrett und Schneehorn) besteht aus sedimentärem, überwiegend jurassischem und kretazischem Deckgebirge des Helvetikums. Eine Besonderheit der Jungfrau ist, dass dort zwischen dem prinzipiell autochthonen Gipfel-Kristallin und dessen Deckschichten ein Überschiebungs-kontakt besteht; somit ist das Grundgebirge geringfügig auf sein Deckgebirge überschoben worden.
Name
Der Name Jungfrau dürfte sich von der Wengernalp am Fusse des Berges ableiten, die – nach den Besitzerinnen, den Nonnen vom Kloster Interlaken – früher Jungfrauenberg genannt wurde. Einer anderen Quelle zufolge leitet sich der Name vom Aussehen des Nordhanges des Berges ab, der aus der Ferne dem Schleier eines Mädchens ähneln soll.
Nach dem Berg ist die Jungfrau-Region benannt, die Tourismusorganisation der Orte Grindelwald, Wengen, Mürren und Lauterbrunnen, ausserdem die Jungfraubahn Holding AG, die neben der Jungfraubahn selbst auch die anderen Bergbahnen in der Region betreibt.
Besteigungsgeschichte
Bergsteiger auf dem Gipfel im Jahr 1878
Erstbesteiger waren Johann Rudolf Meyer und sein Bruder Hieronymus mit den Führern Joseph Bortis und Alois Volken, die am 3. August 1811 vom Lötschental her den Berg von Süden erklommen hatten. Sie folgten ungefähr der heutigen Normalroute. Der Volksmund taufte daraufhin die bis dahin unberührte Jungfrau «Madame Meyer».
1874 erfolgte die Winter-Erstbesteigung durch die Alpinistin Margaret Claudia Brevoort.
Die Jungfrau gilt, obwohl leicht erreichbar, als unfallträchtiger Berg. Bei einem der schwersten Unglücke stürzten am 12. Juli 2007 sechs Rekruten der Gebirgsspezialisten-Rekrutenschule Andermatt vom Rottalsattel 1000 Meter auf den darunterliegenden Rottalgletscher in den Tod, nachdem sie eine Lawine ausgelöst hatten. Das urteilende Militärgericht ging von einem falsch eingeschätzten, heimtückischen Lawinenrisiko aus und sprach in der Folge die verantwortlichen Bergführer frei.
Routen
Rottalsattel und Südostgrat (Normalroute)
Schwierigkeit: ZS-
Zeitaufwand: 4–5 Std. von der Mönchsjochhütte, 3½–4½ Std. vom Jungfraujoch
Ausgangspunkt: Mönchsjochhütte (3657 m)
Talort: Grindelwald (1034 m)
Innere Rottalgrat
Schwierigkeit: ZS
Zeitaufwand: 6–7 Stunden
Ausgangspunkt: Rottalhütte (2755 m)
Talort: Stechelberg (919 m)
Nordwestgrat oder „Rotbrettgrat“
Schwierigkeit: S
Zeitaufwand: 8–12 Stunden
Ausgangspunkt: Silberhornhütte (2663 m)
Talort: Stechelberg (919 m)
Nordostgrat
Schwierigkeit: S+, mit IV. UIAA-Grad Felskletterei
Zeitaufwand: 8–10 Stunden
Ausgangspunkt: Jungfraujoch (3454 m)
Talort: Grindelwald (1034 m)
Kunst
Erwähnt ist die Jungfrau unter anderem bei Friedrich Schiller, Wilhelm Tell, Vers 628 (1804). Lord Byrons Drama Manfred (1817) spielt am Fuss und auf dem Gipfel des Massivs. Ferdinand Hodler hat die Jungfrau mehrfach gemalt, darunter die perspektivisch verfremdete «Jungfrau über dem Nebelmeer». Alex Diggelmann gab 1958 eine Lithographienmappe unter dem Titel Die Jungfrau, mein Berg heraus. Stephan Bundi gestaltete 2005 eine Schweizer Gedenkmünze mit dem Bergmotiv.
Im Januar 2012 wurde zum 100-jährigen bestehen der Jungfraubahn eine übergrosse Schweizer Flagge vom Lichtkünstler Gerry Hofstetter an den Gipfel projiziert. Zeitweise waren neben dem Schweizer Kreuz auch ein Porträt des Zürcher Unternehmers Adolf Guyer-Zeller sowie ein Bild von einem der Züge zu sehen.
(Wikipedia)
I had to include this - yet another of these now rare Revo lanterns that are for the chop in January 2009. They are so evocative of street furniture and streetscapes that are redolent of Britain in the 1960s and earlier.
Pierre -Joseph Redoute "Roses" print (Gift from my sister-in-law); and my inherited bedroom silverware from my Nanna. Includes two smelling salts bottles, perfume bottle and trinket box. These were always on my Nanna's dressing table with a vase of flowers. Checking out her dressing table (and sneaking a look through the dressing table jewellery drawers!) was always my absolute first "port of call" when we arrived at Nanna's place. Crown Staffordshire roses also Nanna's.
Georgian churches are scarcer than Victorian churches. Well known Georgian style churches in Ireland include St George’s Church in Hardwicke Place and St Stephen’s (Pepper Cannister) Church on Mount St , both in Dublin, St Peter’s Church in Drogheda and to a lesser extent St. Columba’s in Swords.
St Columba’s Church in Swords is an early 19th-century Georgian church. It was designed by Francis Johnson in the Gothic style of the Chapel Royal in Dublin Castle. The noteworthy external features are the stepped buttresses, pinnacles and crenellated parapet – all in limestone.
The interior has simple elegant plasterwork, carved timber pews and cut stone memorials which pre-date the building. The stained glass East window by Joshua Bradley is deemed to be one of the oldest stained glass windows in Ireland.
A medieval square tower and an intact 10th-century round tower are among the ecclesiastical monuments in the church grounds. Brian Boru was waked in the abbey church which adjoined the medieval tower. St Columba’s is on the list of protected structures in Fingal County Council as well as being on the National Inventory of Architectural Heritage.
A section of the ceiling collapsed in April, 2013. There are also many instances of dry rot on the ceiling and internal walls. The church was closed for use following the partial collapse of the ceiling and church services are currently held in the nearby parish centre. The West window was bricked up when a tree fell through it.
The church was re-roofed in 2007 – but not before water seeped through into the ceiling and internal rubbled walls causing extensive dry rot throughout the interior. Complete restoration costs including electrical work, conservation plasterwork and re-painting of the interior are estimated at €500,000.
The parishioners of St Columba’s have established building and fundraising committees to work towards the repair and re-opening of the church. Campaigning websites savesaintcolumbaschurch.org and helpusmakehistory.org and a restoration fund has already raised €9,000.
The Trade Facilitation Programme (TFP) currently includes almost 100 Issuing Banks in the EBRD region and more than 800 Confirming Banks worldwide. The event gave EBRD confirming and issuing banks the opportunity to review and discuss industry challenges and opportunities with leading specialists, including International Chamber of Commerce and Chief Economist Office. It also featured 25th anniversary award ceremony which will recognize most active banks in EBRD Countries of Operations.
14:30 – 14:45 Opening and Welcome Speeches
• Alexander Saveliev, Director, Financial Institutions, EBRD
• Rudolf Putz, Head of Trade Facilitation Programme, EBRD
14:50 – 15:30 Panel Discussion: Development of Trade & Trade Finance - SEMED
Moderator: Kamola Makhmudova, Senior Banker, EBRD
• Alexander Plekhanov, Office of the Chief Economist, EBRD
• Hanane El Boury, Banque Centrale Populaire (BCP), the Kingdom of Morocco
• Ahmed Benyahya, BMCE Bank, the Kingdom of Morocco
• Hossam Mustafa Rageh, Commercial International Bank (CIB), the Arab Republic of Egypt
• Anas AlMasri, Bank Al Etihad, the Hashemite Kingdom of Jordan 15:30 –
15:50 – 16:30 Panel Discussion: EBRD’s new Partner Banks
Moderator: Marco Nindl, Principal Banker, EBRD
• Sally Hamdalla, QNB Alahli, the Arab Republic of Egypt
• Malliotis Achilleas, Eurobank Cyprus, Republic of Cyprus
• Vladislav Berezhny, Credit Agricole Bank, Ukraine
• Ahu Heper Dolu, Fibabanka, Republic of Turkey
• Andrew Wood, Norton Rose Fulbright LLP, the United Kingdom
16:35 – 17:15 Panel Discussion: Trade Finance Solutions for Imports of Energy Efficient Machinery & Equipment – Gaps and Constraints
Moderator: Terry McCallion, Director, Energy Efficiency and Climate Change, EBRD
• Sergiy Kostogryz, Raiffeisen Bank Aval, Ukraine
• Gagik Sahakyan, Ameriabank, Armenia
• Maria Mogilnaya, Associate Banker, EBRD
• Holger Kautzky, Commerzbank
• Eugenia Zhiglova, KBC Bank
17:35 – 18:10 TFP Annual Awards Ceremony
Hosted by Nick Tesseyman, Managing Director, Financial Institutions, EBRD
Congratulations from Ambassador Chih-Kung Liu, Head of the Taipei Representative Office in the UK
At Pevensey Castle
Pevensey Castle: a Saxon Shore fort, Norman defences, a medieval enclosure castle, and later associated remains
The monument includes Anderita Saxon Shore fort, traces of later, Norman defences, an enclosure castle, a 16th century gun emplacement and World War II defences situated on a low spur of sand and clay which now lies around 2km north west of the present East Sussex coastline at Pevensey. During the Roman and medieval periods the spur formed a peninsula projecting into a tidal lagoon and marshland, but coastal deposition and land reclamation have gradually built up the ground around it so that it is now completely land-locked. The roughly oval, north east-south west aligned Roman fort is the earliest of the structures which make up the monument and has been dated to the first half of the fourth century AD. Covering almost 4ha, the fort survives in the form of substantial ruins and buried remains. It is enclosed by a massive defensive wall with a flint and sandstone rubble core faced by coursed greensand and ironstone blocks, interspersed with red tile bonding courses. The whole is up to 3.7m thick and survives to a height of up to 8.1m. The wall was originally topped by a wall walk and parapet. Part excavation in 1906-8 showed that the wall was constructed on footings of rammed chalk and flints underpinned by oak piles and held together by a framework of wooden beams. Investigation of the internal face indicated that this was stepped upwards from a wide base so as to provide extra strength and support. Despite these precautions, a landslip on the south eastern side of the fort has resulted in the destruction of a c.180m length of the perimeter walls and, although fragments of the fallen masonry do survive, most have been removed over the years. Smaller sections of wall have also collapsed along the north western and eastern stretches. The defensive strength provided by the perimeter wall was enhanced by irregularly-spaced, externally projecting semicircular bastions with diameters of around 5m. There were originally at least 15 of these, of which 10 survive today. The fort was entered from its south western, landward approach by way of the main gateway. In front of this a protective ditch 5.5m wide was dug, and, although this became infilled over the years, a 40m stretch located towards its south eastern end has been recut and exposed. The ditch would have been spanned originally by a wooden bridge, although this no longer survives. The main gateway takes the form of a rectangular gatehouse set back between two solid semicircular bastions 8m apart. The 2.7m wide, originally arched entrance is flanked by two oblong guardrooms and the whole gateway structure projects beyond the inner face of the perimeter wall into the fort and is thought to have been originally two or even three storeys high. On the eastern side of the fort is a more simply designed subsidiary gateway, originally a 3m wide archway entrance, giving access to part of the adjacent Roman harbour, now overlain by Pevensey village. The extant archway is a modern reconstruction of the Norman rebuilding of the original entrance. Traces of a wooden causeway which led from it into the fort have been found during partial excavation. Midway along the north western stretch of perimeter wall is a now ruined postern c.2m wide, approached by a curved passage set within the wall. Part excavation between 1906-1908 indicated that the internal buildings which housed the garrison of up to 1,000 men, along with their livestock and supplies, were constructed of timber infilled with wattle and daub. A c.1m sq timber-lined Roman well was found in the south western sector of the fort, at the bottom of which were the remains of the wooden bucket with rope still attached. The well was found to have been filled with rubbish in Roman times and the presence of the bones of cattle, sheep, red deer, wild boar, wild birds, domestic dogs and cats, along with sea shells, gives some indication of the diet and lifestyle of the fort's original inhabitants. Anderita is thought to have been abandoned by its garrison by the latter half of the 4th century AD, and although little is known of its subsequent history until the 11th century, the Anglo-Saxon Chronicle records a massacre of Britons by the invading Saxons at the fort in AD 491. The Bayeux Tapestry states that William the Conquerer landed at Pevensey in 1066, and the Norman army are believed to have made use of the Roman fort as one of their first armed camps. The defences at Pevensey and the surrounding land were granted to King William's half-brother Robert, Count of Mortain. The medieval defences then went through at least 300 years of development, culminating in the construction of a stone built enclosure castle within the largely intact walls of the earlier Roman fort. It is thought that the first Norman defences took the form of a wooden palisade surrounded by a bank and ditch, and a c.40m length of partially infilled ditch up to 9m wide which survives across the north eastern sector of the earlier fort may indicate their original extent. Limited excavations in 1993-94 showed that the ground surface in the south eastern sector of the fort, in the vicinity of the later stone-built keep, was artificially raised some time before 1200, suggesting that a motte may also have been constructed. The original Roman gateways were rebuilt and a new ditch dug in front of the south western gate. Most of the Norman defences and interior wooden buildings will now survive in buried form beneath the later medieval castle, although herringbone-pattern repairs to the Roman masonry, by then serving as the outer bailey of the medieval defences, also date from this time. Around 1100 the defences were strengthened and the accommodation improved by the addition of a masonry keep in the south eastern sector of the earlier fort. The subject of a complex history of alteration, collapse and repair, the keep utilises part of the earlier, Roman perimeter wall and bastions. It takes the form of a rectangular block measuring c.16.8m by c.9m internally, reinforced by apsidal projections on all sides. Now surviving in ruined form up to first floor level, the keep originally took the form of a tall tower with an entrance on the first floor. A rectangular building measuring 7.6m by 6m was later constructed in the south eastern angle between the keep and the Roman wall. At around 1200 work began on the construction of a smaller, stone-built inner bailey in the south eastern sector of the earlier fort. An L-shaped ditch around 20m wide was dug to define the new enclosure, and this retains water in its northern arm. The material excavated from the ditch and from the destruction of the earlier bank was spread over much of the outer bailey to a depth of up to 1.5m. The ditch was recut during extensive renovations carried out during the early 20th century. The first structure to be built in this phase was the gatehouse to the south west which has an arched entrance between twin, semicircular external towers, now ruined. The basement chambers beneath each tower have ashlar-faced walls and barrel-vaulted ceilings, the southern chamber being entered by way of a newel staircase, the northern by a trapdoor. Both were used to house prisoners. Many subsequent alterations included the replacement, during the 15th century, of the wooden bridge over the outer ditch by a stone causeway. The originally embattled curtain wall enclosing the inner bailey was built within the ditch and inner berm around 1250. This survives almost to its full original height and is faced with coursed Greensand ashlar. Three semicircular external towers provided flanking cover from the narrow embrasures which pierce their walls. Each has a narrow staircase to a basement, a branch staircase off it into the ditch and a room and garderobe, or latrine, at ground floor level. Upper rooms were entered by way of the wall walk and were heated by fireplaces. The basement of the northernmost tower has two rib-vaulted bays, the keeled ribs resting on stiff-leaf corbels. The interior castle buildings continued to be built mainly of wood and these will survive in buried form, although the stone foundations of a chapel were exposed during partial excavation of the northern sector of the inner bailey. Around 20m south east of the chapel is a large stone-lined well at least 15.5m deep, and near this is a pile of medieval stone missile-balls, a selection of those recovered from the ditch. These were thrown from trebuchets during the four sieges of the castle. William, Count of Mortain forfeited Pevensey after an unsuccessful rebellion against Henry I in 1101 and the castle, which remained in the royal gift until the later Middle Ages, passed into the hands of the de Aquila family. The most famous siege took place in 1264-65 when the supporters of Henry III, fleeing from their defeat by the Barons at Lewes, took refuge in the castle. In 1372 the castle was given to John of Gaunt, and during his period of office was used to imprison James I, King of Scotland, who had been seized in 1406, and Joan, Queen of Navarre, accused of witchcraft by her stepson, Henry V. By 1300, the sea had gradually begun to recede from around the castle and its military importance declined as a result. Contemporary records show that the castle walls were constantly in need of expensive repair and by the end of the 14th century were not being properly maintained, although the roof leads were kept intact until the middle of the 15th century. By 1500 the castle had ceased to be inhabited and fell rapidly into decay. The threat of the Spanish Armada led to some renewed interest in the defensive value of the site, and a survey of 1587 records that the castle housed two demi-culverins, or heavy guns. These were sited on the contemporary, south east orientated, M-shaped earthen gun emplacement situated in the outer bailey around 90m north east of the main Roman gateway. This takes the form of a raised level platform c.20m long bounded on the seaward side by a slight bank c.0.4m high and around 3m wide. One of the cast iron guns, manufactured in the East Sussex Weald, is now housed within the inner bailey on a modern replica carriage. From the 17th century the castle passed through the hands of various private owners. Valued as a picturesque ruin during the 18th and 19th centuries, it features in many contemporary engravings and illustrations. In 1925 the Duke of Devonshire presented the monument to the state, and extensive repairs began with a view to opening the monument to the public. These were interrupted by the outbreak of World War II, when the castle resumed its original military purpose of protecting the south coast. The castle was refortified in May 1940 as an observation and command post. It was continuously occupied by regular troops, including Canadian forces and the United States Army Air Corps, who used it as a radio direction centre, and by the Home Guard until 1944. The World War II defences include two pillboxes and three machine gun posts of concrete faced with rubble and flints, carefully concealed and camouflaged within the earlier Roman and medieval fabric. An internal tower was built just to the south of the Roman east gateway and a blockhouse housing anti-tank weapons was built in front of the main Roman gateway. The blockhouse no longer survives. Modifications carried out to the medieval mural towers included lining the interiors with brick and inserting wooden floors. In 1945 the monument was returned to peaceful use and is now in the guardianship of the Secretary of State and open to the public.
[Historic England]
The Miao are one of several ethnic minorities living in the
subtropical mountainous areas of southwestern China. Different groups
include the Dong, Yi, Yao, Shui, Buyi (Bouyei), Li, Gejia, and Bai among many
others. For thousands of years, these migrating peoples have developed
rich, cultural traditions and they are increasingly being recognized
for their extraordinary handcrafted textiles and silver jewelry. It is
the area of costume where mythology, technical skill, and cultural
identity coalesce in vivid aesthetic expression. Until recently, most
of these remote, ethnic villages were relatively isolated from the
majority Han Chinese population. China’s rapid modernization, however,
has penetrated even the minority districts of Guizhou, Yunnan,
Guangxi, and Guangdong provinces. The resultant economic, educational,
and social changes have already begun to erode the look and use of
traditional festive costumes worn by the Miao and other ethnic groups.
In the Spring of 2008, staff of the Minneapolis Institute of Arts
documented villages throughout Guizhou, China and the Sisters Meal
Festival in Shidong.
Explore the MIA's Ethnic Minority Textiles Collection
Photos by Dan Dennehy for the Minneapolis Institute of Arts.
This project has been funded with a grant from the The Institute of
Museum and Library Services. The Institute of Museum and Library
Services is the primary source of federal support for the nations
123,000 libraries and 17,500 museums. The Institute's mission is to
create strong libraries and museums that connect people to information
and ideas.www.imls.gov/
Copyright: Some rights reserved. Attribution Noncommercial Share Alike
Attribution-NonCommercial-ShareAlike License
The new barracks, which can house up to 320 Soldiers, include a selection of ADA-compliant rooms with roll-in showers, kitchen counters and desks to accommodate wheel chairs and wheelchair-accessible washer and dryers. All rooms are furunished with Internet access and flat-screen televisions.
Fort Hood’s new Warrior Transition Brigade Complex is a $62 million, 15-acre campus that includes a 30,137 square-foot battalion headquarters, a 15,000 square-foot company headquarters, a 192,000 square-foot 320-person barracks and a 15,000 square-foot Soldiers and Family Assistance Center that includes child-care facilities and a modern playground. The new facility, which held a ribbon-cutting ceremony June 6, improves care for wounded, injured and ill Soldiers and their Families because services are now centrally located and within walking distance. The new WTB campus allows WTB Soldiers to work, train and socialize as a group to create tighter bonds that have proven to be helpful in a Soldier’s healing.
The new barracks, which can house up to 320 Soldiers, include a selection of ADA-compliant rooms with roll-in showers, kitchen counters and desks to accommodate wheel chairs and wheelchair-accessible washer and dryers. Handrails are installed throughout hallways as well as in all private bathrooms.
All four buildings are eco friendly with design solutions that conserve energy, water efficient and self-sustainable. The buildings have solar panels that provide about 30% of energy used to heat hot water as well as standing seam metal roofs that lower the buildings' solar reflectivity index, which reduces heat and cooling costs. Other energy efficiency enhancements include motion sensing lights, high-efficiency window systems and non-water using urinals that use a biodegradable liquid for sanitary and odor free environment and dual flush toilets will save up to 30 gallons of water. The WT Operations building is LEED Silver Level certified.
Landscaping considerations include using native trees and grass that are grouped together by similar watering needs and selected for their hardiness, availability and drought tolerance.
The WT complex, by using durable finishes and efficient systems, is designed for a 25-year life span before renovation. It has an estimated 50-year life span with renovations.
Elizabeth II (Elizabeth Alexandra Mary Windsor; born 21 April 1926) is Queen of the United Kingdom and the other Commonwealth realms.
Elizabeth was born in London as the first child of the Duke and Duchess of York, later King George VI and Queen Elizabeth, and she was educated privately at home. Her father acceded to the throne on the abdication of his brother King Edward VIII in 1936, from which time she was the heir presumptive. She began to undertake public duties during the Second World War, serving in the Auxiliary Territorial Service. In 1947, she married Prince Philip, Duke of Edinburgh, a former prince of Greece and Denmark, with whom she has four children: Charles, Prince of Wales; Anne, Princess Royal; Prince Andrew, Duke of York; and Prince Edward, Earl of Wessex.
When her father died in February 1952, Elizabeth became head of the Commonwealth and queen regnant of seven independent Commonwealth countries: the United Kingdom, Canada, Australia, New Zealand, South Africa, Pakistan and Ceylon. She has reigned as a constitutional monarch through major political changes, such as devolution in the United Kingdom, Canadian patriation, and the decolonisation of Africa. Between 1956 and 1992, the number of her realms varied as territories gained independence, and as realms, including South Africa, Pakistan, and Ceylon (renamed Sri Lanka), became republics. Her many historic visits and meetings include a state visit to the Republic of Ireland and visits to or from five popes. Significant events have included her coronation in 1953 and the celebrations of her Silver, Golden, and Diamond Jubilees in 1977, 2002, and 2012 respectively. In 2017, she became the first British monarch to reach a Sapphire Jubilee. She is the longest-lived and longest-reigning British monarch as well as the world's longest-serving female head of state, oldest living monarch, longest-reigning current monarch, and the oldest and longest-serving current head of state.
en.wikipedia.org/wiki/Elizabeth_II
en.wikipedia.org/wiki/Wikipedia:Text_of_Creative_Commons_...
Pattern includes easy to follow instructions.
Materials Needed:
Straight knitting needles, size US 7 (4.5mm)
100% Cotton Medium/Worsted Weight yarn [60 yards]
In any color you choose.
Stitches: knit & purl.
Skill: Beginner
Finished Size: 7W X 7 1/4 H (18cn X 18.5 cm)
Darning needle needed for finishing.
This pattern will be delivered via email as an attached PDF file to anywhere in the world.
Pattern can be found @ www.artfire.com/users/Ezcareknits or @ www.etsy.com/shop/ezcareknits
Check Tweed outfit by Ambrosia includes skirt, lace knit half sleeve and scarf - 1L
slurl.com/secondlife/Symmetry/148/207/49
Basics pocket cardigan (blank) by Ohmai - free
slurl.com/secondlife/Cheesecake/220/174/38
Dot line tights (black) by Humming - 1L
slurl.com/secondlife/SkyBeam FirstLand/71/236/27
Suede fat heart belt (blacks) by Baby Monkey - group gift
slurl.com/secondlife/Dindrane Elfor/227/37/34
Basic flats (white) by Fri.day at Sunny - free
slurl.com/secondlife/Sunny/46/125/24
Granny bag by Pop Feel - group gift
slurl.com/secondlife/Lazy Bloom/91/101/22
Hair accessoire: bling bling by JM:Mai - lucky board
slurl.com/secondlife/Upadhyaya/104/153/237
Morning after hair (dirty blonde) by Posh - past Easter gift
slurl.com/secondlife/Liberty/233/222/22
Lucy first sight love skin (light) by Imabee - group gift
slurl.com/secondlife/Planete Terre/129/175/21
From today's Rugby match at Buckingham Park, Shoreham. Shoreham 1st XV against Hove Volunteers. Shoreham, in yellow and green came back strongly to win in a thrilling and contentious finish. Let's just say that the Hove contingent weren't too impressed with some key refereeing decisions towards the end of the match.
I include the following few photos for posterity, for once the railway left Honeybourne and ran north to Stratford it was an older and not the Honeybourne and Cheltenham Line anymore, though many trains ran through from Stratford-upon-Avon to Cheltenham. The Stratford Branch was opened by the OWW Railway on 11.7.1859 and ran for nearly 9 miles through flat country. Stations and halts existed at Pebworth, Broad Marston, Long Marston, Milcote, Chambers Crossing, Stratford Racecourse and Stratford itself. The history of the line is beyond my interest, but I include the following photos purely for interest. The bulk of the line, other than the last 3-ish miles, is now a cyclepath . The stretch from Honeybourne to Long Marston depot is now effectively a private siding but maintained to standards required for Class 66 freight. This bridge marks the Worcestershire-Warwickshire border and crosses the line at SP151469, ELR code STD 2 68. The gates beyond lead into the former MOD Depot of Long Marston.
Daulatabad Fort
Daulatabad also known as Devagiri, is a town which includes the Devagiri-Daulatabad fort It is a 14th-century fort city in Maharashtra state of India, about 16 kilometres (9.9 mi) northwest of Aurangabad. The place was originally named Devagiri when it was an important uplands city along caravan routes (ca. sixth century AD), but the intervening centuries have reduced it to a village. However it is also considered to be one of the seven wonders of Maharashtra and a developing tourist spot.
The historical triangular fort of Daulatabad was built by first Yadava king Bhillama V in 1187.
Starting 1327, it famously remained the capital of Tughlaq dynasty, under Muhammad bin Tughluq (r. 1325-1351), who also changed its name, and forcibly moved the entire population of Delhi for two years before it was abandoned for lack of water and Tughluq was constantly known to shift the capital from Delhi to Daulatabad and Daulatabad to Delhi.
There is a belief that Devagiri was built in 1203 AD by a Dhangar or herdsman who acquired vast wealth by his good fortune. He had a brother who was a shepherd named 'Raja Ram' and in correlation with it he assumed the rank of a Raja (King).
Lord Shiva is believed to have been stayed on the hills surrounding this region. Hence the fort was originally known as Devagiri, literally (Hills of Gods)
The area of the city includes the hill-fortress of Devagiri (sometimes Latinised to Deogiri). It stands on a conical hill, about 200 meters high. Much of the lower slopes of the hill has been cut away by Yadava dynasty rulers to leave 50 meter vertical sides to improve defenses. The fort is a place of extraordinary strength. The only means of access to the summit is by a narrow bridge, with passage for not more than two people abreast, and a long gallery, excavated in the rock, which has for the most part a very gradual upward slope.
About midway along this gallery, the access gallery has steep stairs, the top of which is covered by a grating destined in time of war to form the hearth of a huge fire kept burning by the garrison above. At the summit, and at intervals on the slope, are specimens of massive old cannon facing out over the surrounding countryside. Also at the mid way, there is a cave entrance meant to confuse the enemies.
The fort had the following specialities which are listed along with their advantages :
No separate exit from the fort, only one entrance/exit - This is designed to confuse the enemy soldiers to drive deep into the fort in search of an exit, at their own peril.
No parallal gates - This is designed to break the momentum of theconfusing the invading army. Also, the flag mast is on the left hill, which the enemy will try to capitualte, thus will always turn left. But the real gates of the fort are on the right & the false ones on the left, thus confusing the enemy.
Spikes on the gates - In the era before gunpowder, intoxicated elephants were used as a battering ram to break open the gates. The presence of spikes ensured that the elephants died of injury.
Complex arrangement of entryways, curved walls, false doors - Designed to confuse the enemy, false, but well-designed gates on the left side lured the enemy soldiers in & trapped them inside, eventually feeding them to crocodiles.
The hill is shaped like a smooth tortoise back - this prevented the use of mountain lizards as climbers, because they cannot stick on it.
The site had been occupied since at least 100 BCE, and now has remains of Buddhist temples similar to those at Ajanta and Ellora.
The city is said to have been founded c. 1187 by Bhillama V, a Yadava prince who renounced his allegiance to the Chalukyas and established the power of the Yadava dynasty in the west. During the rule of the Yadava king Ramachandra, Alauddin Khalji of Delhi Sultanate raided Devagiri in 1296, forcing the Yadavas to pay a hefty tribute. When the tribute payments stopped, Alauddin sent a second expedition to Devagiri in 1308, forcing Ramachandra to become his vassal.
In 1328, Muhammad bin Tughluq of Delhi Sultanate transferred the capital of his kingdom to Devagiri, and renamed it Daulatabad. Some scholars ague that it the idea behind transfer of the capital was rational, because it lied more or less in the centre of the kingdom, and geographically secured the capital from the north-west frontier attacks.
In the Daulatabad fort, he found the area arid & dry. Hence he built a huge reservoir for water storage & connected it with a far-away river. He used siphon system to fill up the reservoir. However, his capital-shift strategy failed miserably due to lack of application & other factors. Hence he shifted back to Delhi & earned him the moniker "Mad King".
The next important event in the Daulatabad fort time-line was the construction of the Chand Minar by the Bahmani ruler Hasan Gangu Bahmani, also known as Ala-ud-Din Bahman Shah (r. 3 August 1347 – 11 February 1358).
Hasan Gangu built the Chand Minar as a replica of the Qutb Minar of Delhi, of which he was a great fan of. He employed Iranian architects to built the Minar who used Lapis Lazuli & Red Ochre for coloring. Currently, the Minar is out of bounds for the tourists, because of a suicide case.
As we move further into the fort, we can see the Chini Mahal, a VIP prison built by Aurangzeb. In this prison, he kept Abul Hasan Tana Shah of the Qutb Shahi Dynasty of Hyderabad. The antecedents of Abul Hasan Tana Shah, the last Qutub Shahi king are shrouded in mystery. Although a kinsman of the Golconda royals, he spent his formative years as a disciple of renowned Sufi saint Shah Raju Qattal, leading a spartan existence away from the pomp and grandeur of royalty. Shah Raziuddin Hussaini, popularly known as Shah Raju, was held in high esteem by both the nobility and commoners of Hyderabad. Abdullah Qutub Shah, the seventh king of Golconda was among his most ardent devotees. He died in prison leaving no male heir to the throne.
In this Chini Mahal, Sambhaji, son of Shivaji was kept.
Most of the present-day fortification was constructed under the Bahmanis and the Nizam Shahs of Ahmadnagar. The Mughal Governor of the Deccan under Shah Jahan, captured the fortress in 1632 and imprisoned the Nizam Shahi prince Husain Shah.
Monuments[edit]
The outer wall, 2.75 miles (4.43 km) in circumference, once enclosed the ancient city of Devagiri and between this and the base of the upper fort are three lines of defences.
Along with the fortifications, Devagiri contains several notable monuments, of which the chief are the Chand Minar and the Chini Mahal. The Chand Minar is a tower 210 ft (64 m). high and 70 ft (21 m). in circumference at the base, and was originally covered with beautiful Persian glazed tiles. It was erected in 1445 by Ala-ud-din Bahmani to commemorate his capture of the fort. The Chini Mahal (literally: China Palace), is the ruin of a building once of great beauty. In it Abul Hasan Tana Shah, the last of the Qutb Shahi kings of Golconda, was imprisoned by Aurangzeb in 1687.
A butterfly is a mainly day-flying insect of the order Lepidoptera, which includes the butterflies and moths. Like other holometabolous insects, the butterfly's life cycle consists of four parts: egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths. The earliest known butterfly fossils date to the mid Eocene epoch, 40–50 million years ago.
Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Some species are pests because in their larval stages they can damage domestic crops or trees; however, some species are agents of pollination of some plants, and caterpillars of a few butterflies (e.g., Harvesters) eat harmful insects. Culturally, butterflies are a popular motif in the visual and literary arts.
Mr Bean's Mini - on display at Chelmsford Market - spotted before a nice lunch with brother on his 60th birthday.
The Miao are one of several ethnic minorities living in the
subtropical mountainous areas of southwestern China. Different groups
include the Dong, Yi, Yao, Shui, Buyi (Bouyei), Li, Gejia, and Bai among many
others. For thousands of years, these migrating peoples have developed
rich, cultural traditions and they are increasingly being recognized
for their extraordinary handcrafted textiles and silver jewelry. It is
the area of costume where mythology, technical skill, and cultural
identity coalesce in vivid aesthetic expression. Until recently, most
of these remote, ethnic villages were relatively isolated from the
majority Han Chinese population. China’s rapid modernization, however,
has penetrated even the minority districts of Guizhou, Yunnan,
Guangxi, and Guangdong provinces. The resultant economic, educational,
and social changes have already begun to erode the look and use of
traditional festive costumes worn by the Miao and other ethnic groups.
In the Spring of 2008, staff of the Minneapolis Institute of Arts
documented villages throughout Guizhou, China and the Sisters Meal
Festival in Shidong.
Explore the MIA's Ethnic Minority Textiles Collection
Photos by Dan Dennehy for the Minneapolis Institute of Arts.
This project has been funded with a grant from the The Institute of
Museum and Library Services. The Institute of Museum and Library
Services is the primary source of federal support for the nations
123,000 libraries and 17,500 museums. The Institute's mission is to
create strong libraries and museums that connect people to information
and ideas.www.imls.gov/
Copyright: Some rights reserved. Attribution Noncommercial Share Alike
Attribution-NonCommercial-ShareAlike License
This wonderful set includes the patterns for: basket, eggs, chicks and little color eggs.
Measures aprox.
Basket: 14 cm
Eggs and chicks: 7 cm
Little color eggs: 3.5 cm
For more information, please visit www.deliciouscrochet.com/
----------
Este maravilloso set incluye los patrones de: canasta, huevos, pollitos y huevitos de colores.
Medidas aproximadas:
Canasta: 14 cm
Huevos y pollitos: 7 cm
Huevitos de colores: 3.5 cm
Para más información, por favor visite www.deliciouscrochet.com/
The Soysambu Conservancy includes much of Lake Elementaita and borders Lake Nakuru National Park to the west. It covers 190 square km (48,000 acres). It was created on the grounds of the Soysambu Ranch in 2007 to conserve the flora, fauna, and scenery of the Soysambu Ranch; it offers a home to over 450 bird species and 50 mammal species, including the critically endangered Rothschild (or Nubian) giraffe. The land of the ranch was appropriated by Hugh Cholmondeley, 3rd Baron Delamere, in 1906. The ranch still is owned and operated by the Delamere family.
Lake Elementaita is a shallow a soda lake located on the floor of Kenya's Great Rift Valley at an altitude of 1,776 meters, 20 km southeast of the city of Nakuru. Its surface area is 18 square kilometers, although the water level fluctuates. Its deepest point is 1.9 meters; much of the lake is less than one meter deep. 450 bird species can be found here; it is an important stop for migratory birds. The lake is designated as Ramsar Site and as Important Bird Area (IBA). Lake Elementaita Wildlife Sanctuary encompasses the whole of Lake Elementaita and its riparian land; it became a UNESCO World Heritage Site as part of the Kenya Lake System in 2011.
When couples dream of their perfect wedding destination abroad, their vision often includes escaping to a far-away place that offers all of the charms one could possibly desire for their Religious or Civil Ceremony. So, if you're looking at celebrating your wedding in Sicily, Taormina is a good choice.Taormina's beauty is uncontested. Some cities are known for their art treasures, others for their natural beauties; only a few, like Taormina, own both.Visitors to this magical yet relatively undiscovered island, leave with its images of sheer beauty, its cultural simplicity, the passion and warmth of the people and historical delights etched permanently in their memories.Within its ancient stone gates, the old town has fascinating archeological monuments and medieval homes. Magnificent views of the sea complete the picture.The city is located on a cliff top overlooking the deep blue of the never ending horizon reflected in a clear turquoise sea which surrounds the bays and beaches.In fact it is Sicily's number one tourist resort, boasting magnificent scenery, architecture and great local cuisine. It's no wonder tourists flock to Taormina every year.
Its rich culture and crystal clear sea and views of Mount Etna create a magical atmosphere. Taormina has endlessly winding medieval streets and tiny passages, each with its own secrets.Some of these intriguing places are secluded gardens hidden by stone walls; others are set on terraces overlooking the coast or in more public but equally pleasant squares.Taormina is beautiful by day but in the evenings its atmosphere is simply enchanting, whether you stroll the illuminated streets or indulge in the view of the coast over an authentic Sicilian dinner. Taormina's ancient Greek splendor, medieval charm and unique views will leave you with a lasting impression of Sicily.The climate is mild even in the winter, where it feels like eternal spring time. Its air is filled with the scent of orange and lemon blossoms. Steal away on an island retreat in beautiful Sicily, as it offers a taste of the traditional with a delicate touch of the exotic.There are several charming churches here in which to have a Catholic wedding, as well as Palazzo Santo Stefano for civil weddings, which takes an exquisitely charming medieval mood. Taormina's regal Norman Byzantine, Romanesque and Baroque churches offer a beautiful venue for a religious wedding.Couples may choose to exchange their wedding vows in any of these spectacular locations!The whole Taormina experience leaves visitors breathless and enthusiastic to plan their dream wedding here.
Make the dream come true for you...
www.facebook.com/pages/Weddinginsicily-Taormina/475641052...
BRAHMINY KITE :
The Brahminy Kite (Haliastur indus) also known as the Red-backed Sea-eagle in Australia, is a medium-sized bird of prey in the family Accipitridae, which also includes many other diurnal raptors such as eagles, buzzards and harriers. They are found in the Indian subcontinent, Southeast Asia and Australia. They are found mainly on the coast and in inland wetlands where they feed on dead fish and other prey. Adults have a reddish brown plumage and a contrasting white head and breast which makes them easy to distinguish from other birds of prey.
> Description
The Brahminy Kite is distinctive and contrastingly coloured, with chestnut plumage except for the white head and breast and black wing tips. The juveniles are browner, but can be distinguished from both the resident and migratory races of Black Kite in Asia by the paler appearance, shorter wings and rounded tail. The pale patch on the underwing carpal region is of a squarish shape and separated from Buteo buzzards.
The Brahminy Kite is about the same size as the Black Kite (Milvus migrans) and has a typical kite flight, with wings angled, but its tail is rounded unlike the Milvus species, Red Kite and Black Kite, which have forked tails. The two genera are however very close. The call is a mewing keeyew.
> Taxonomy
The Brahminy Kite was first described by the Dutch naturalist Pieter Boddaert in 1783. Four subspecies are recognized:
# indus (Boddaert, 1783) is found in South Asia
# flavirostris Condon & Amadon, 1954 is found in the Solomon Islands
# girrenera (Vieillot, 1822) is found in New Guinea, Bismarck Archipelago and Australia
# intermedius Blyth, 1865 is found in the Malay Peninsula and into the islands of the Sundas, Sulawesi and the Philippines
> Distribution and status
This kite is a familiar sight in the skies of Sri Lanka, India, Pakistan, Bangladesh, and southeast Asia and as far south as New South Wales, Australia, through which region it is widespread and resident. They perform seasonal movements associated with rainfall in some parts of their range.
They are mainly seen in the plains but can sometimes occur above 5000 feet in the Himalaya.
It is evaluated as Least Concern on the IUCN Red List of Threatened Species. However the species is on the decline in some parts such as Java.
> Behaviour
The breeding season in South Asia is from December to April. In southern and eastern Australia, it is August to October, and April to June in the north and west. The nests are constructed of small branches and sticks with a bowl inside and lined with leaves, and are sited in various trees, often mangroves. They show considerable site fidelity nesting in the same area year after year. In some rare instances they have been seen to nest on the ground under trees.
A clutch of two dull white or bluish-white oval eggs measuring 52 x 41 mm is laid. Both parents take part in nest building and feeding but it is suggested that only the female incubates. The incubation period is about 26 to 27 days.
It is primarily a scavenger, feeding mainly on dead fish and crabs, especially in wetlands and marshland but occasionally hunts live prey such as hares and bats. They may also indulge in kleptoparasitism and attempt to steal prey from other birds. A rare instance of a bird feeding on honey at the hive of Apis florea has been recorded.
Young birds may indulge in play behaviour, dropping leaves and attempting to catch them in the air. When fishing over water, they may sometimes land in the water but manage to swim and take off without much trouble.
They roost communally on large and isolated trees and as many as 600 have been seen at just one location.
They may mob larger raptors such as the Aquila eagles. In some incidents where Brahminy Kites mobbed Steppe Eagles (Aquila rapax), they were attacked and injured or killed.
A number of ectoparasitic bird lice in the genera Kurodaia, Colpocephalum and Degeeriella have been reported
PHOTOGRAPHY : KAUSHIK SINGHA ROY
Brownsea Island sits in Poole harbour it is the second largest natural harbour in the world, second on to Sydney harbour in Australia. Brownsea Island ( was also known as Branksea ) is the largest of the islands in Poole Harbour in the county of Dorset, England. The island is owned by the National Trust. Much of the island is open to the public and includes areas of woodland and heath with a wide variety of wildlife, together with cliff top views across Poole Harbour and the Isle of Purbeck. The island was the location of an experimental camp in 1907 that led to the formation of the Scout movement the following year. Access is by public ferry or private boat; in 2017 the island received 133,340 visitors. The ferry trip itself is well worth the time. When I went it was £11.50 return trip. But on the way back the ferry takes a scenic route round the islands to arrive back at Poole Quay.
The island was purchased by wealthy stockbroker Charles van Raalte who used the island as a residential holiday retreat. During this time the castle was renovated and served as host to famous visitors such as Guglielmo Marconi. Robert Baden-Powell, a close friend of the van Raaltes, hosted an experimental camp for boys on the island in the summer of 1907. Brownsea was largely self-supporting, with a kitchen garden and a dairy herd. Many of the pottery factory workers had stayed on after it closed, farming and working for the owners. Charles van Raalte died in Calcutta in 1907 and his wife eventually sold the island in 1925. In 1927 it was purchased at auction by Mary Bonham-Christie for £125,000. A recluse by nature, she ordered a mass eviction of the island's residents to the mainland. The National Trust then agreed to take over responsibility for the island if enough funds were raised and in 1962 it then purchased Brownsea for £100,000. Work was carried out to prepare the island for visitors; tracks were cleared through areas overgrown with rhododendrons and firebreaks were created to prevent repetition of the 1934 fire.
Brownsea Island lies in Poole Harbour opposite the town of Poole. It is the largest of eight islands in the harbour. The island can be reached by one of the public ferries or by private boat. There is a wharf and a small dock near the main castle. The island is about 1 1⁄2 miles ( 2.4 km ) long and 3⁄4 mile ( 1.2 km ) wide and consists of 500 acres of woodland ( pine and oak trees ), heathland and salt-marsh. The entire island, except the church and a few other buildings which are leased or managed by third parties, is owned by the National Trust. Most of the buildings are situated near the small landing stage. The northern portion of the island is a Nature Reserve managed by Dorset Wildlife Trust and an important habitat for birds; this part of the island has limited public access so as not to disturb the wildlife.. A small portion to the southeast of the island, along with Brownsea Castle, is leased to the John Lewis Partnership for use as a holiday hotel for staff, and is not open to the public. The island forms part of the Studland civil parish in the Purbeck local government district. It is within the South Dorset constituency of the House of Commons and the South West England constituency of the European Parliament.
In all the time I have lived in this area I never knew there was a very lovely Church on the Island and managed to take photos and videos of my visit there both inside and out. St Mary’s Church was built in 1853, the church remains very much as it was then - its organ is pumped by hand and the only lighting comes from candles. It's a Victorian church that isfixed in the past so with no electricity or water supply. But its regular spring and summer services can attract congregations between 3 and 300 - and it remains an important part of Brownsea's small island community. A Family Service is held at St.Mary’s at 3.00pm every Sunday from May to September.
From 1st August until 8th in August 1907, Robert Baden-Powell held an experimental camp on the island, to test out his Scouting ideas. He gathered 21 boys of mixed social backgrounds ( from boy's schools in the London area and a section of boys from the Poole, Parkstone,Hamworthy, Bournemouth, and Winton Boys' Brigade units ) and held a week-long camp. The boys took part in activities such as camping, observation, woodcraft, chivalry, lifesaving and patriotism. Following the successful camp, Baden-Powell published his first book on the Scouting movement in 1908, Scouting for Boys, and the international Scouting movement grew rapidly. Boy Scouts continued to camp on the island until the 1930’s, when all public access to the island was forbidden by the island's owner. After ownership of the island transferred to the National Trust, a permanent 20 hectares or 49 acres Scout camp site was opened in 1963 by Olave Baden-Powell. In August 2007, 100 years after the first experimental camp, Brownsea Island was the focus of worldwide celebrations of the centenary of Scouting.
This is a photograph from the 60th Anniversary Commerative Half Marathon for Tullamore Harriers AC which was held on Saturday 31st August 2013 in Tullamore, Co. Offaly, Ireland at 12:00. This was a really great event and there couldn't be any fault found with any aspect of the race. There were stewarts all along the route, 3 drink stations with bottled water, superb facilities, and great after-race refreshments. The stewards along the route provided great encouragement to all of the runners. Tullamore Harriers and the local community really worked together to make this is a wonderful event.
Race event manangement and organisations was provided by PRECISION TIMING - see their website at [www.precisiontiming.net/]
This photograph is one of a set of photographs from the Tullamore Harriers Half Marathon 2013. The permanent link to the full set of photographs is [http://www.flickr.com/photos/peterm7/sets/72157635307620452/]. This set of photographs includes photographs of the start and then photographs of the finish up to the 2 HOUR finishing time.
This race celebrates the 60th Anniversary (a Diamond Anniversary) of the foundation of Tullamore Harriers AC. The club was formed in the town in November 1953. However, it was almost 1979 before facilities close to what we see today open in the present day site. Over 50 provincial and national athletics meetings are held at Tullamore Harriers every year. The facilities available combined with it's central geographical location joing routes from North, South, East, and West make it a very attractive venue. The race today brings competitive national road racing back to The Harriers. In the past there was the famous Quinnlan Cup
Festival of Races (see a link below for some nostalgia) which was one of Ireland's Blue Ribband events. Today, the facilities at Tullamore Harriers are the envy of many athletics clubs in Ireland. The facilities provided by Tullamore make it one of the premier venues for local and national level athletics in Ireland. There is an Olympic standard tartan track, a fully equipped gym, changing facilities, press and media facilities, meeting room spaces, etc. The club also provides a social center and niteclub which makes "The Harriers" a very well known on the local social scene. Esssentially, the town of Tullamore would be a different place if it weren't for the presence of Tullamore Harriers AC.
Overall Race Summary
Participants: There was about 500 participants of runners, joggers, and walkers.
Weather: The midday start seen warm pleasant conditions for running. The layout of the course meant that there was a stiff breeze into the face of competitors for the first few miles. When the race turned around to return to Tullamore the wind was more favourable to runners.
Course: The race starts on the Charleville Road just outside the entrance to Tullamore Harriers. The race proceeds south along the R421 and onto the N52 before taking a route onto local back roads. The race then completes a large rural road route before it joins to the R421 again and the final 1.5 miles are the same as the first mile of the race. The runners enter tullamore stadium and complete one lap of the tartan track before the finish line. The course is challenging in places with some undulations along the route. But overall it is fair course.
Location Map: Start/finish and registration and race HQ was all at Tullamore Harriers AC Club Grounds: goo.gl/maps/xZ4GM (Google Streetview)
Refreshments: There was a very impressive selection of refreshments including sandwiches, cakes, home-made breads, etc in the Harriers clubhouse afterwards. People were able to enjoy their post race refreshments outside in the warm pleasant sunshine.
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If you are viewing this Flickr set on a smartphone and you want to see the larger version(s) of this photograph then: scroll down to the bottom of this description under the photograph and click the "View info about this photo..." link. You will be brought to a new page and you should click the link "View All Sizes".
Some Useful Links related to the race
Race Results are available from PRECISION TIMING: www.precisiontiming.net/result/racetimer
Facebook event page: www.facebook.com/events/547723028583924/
The Tullamore Harriers AC Website: www.tullamoreharriers.com/
The Tullamore Harriers Facebook Page: www.facebook.com/tullamore.harriers (Facebook logon required)
The Tullamore Harriers Half Marathon ROUTE on MapMyRun: www.mapmyrun.com/routes/view/217165415
The Boards.ie Athletics Discussion Thread on the Race: www.boards.ie/vbulletin/showthread.php?t=2056942637
Read about Tullamore Town on Wikipedia: en.wikipedia.org/wiki/Tullamore
Quinlan Cup 1997: ireland.iol.ie/~ar5meade/quinlan97.htm
The Entrace to Tullamore Harriers AC Club Grounds: goo.gl/maps/xZ4GM (Google Streetview)
An Aerial Image of the Facilities of Tullamore Harriers AC: binged.it/12UPZ9N (Bing Aerial BirdsEye )
How can I get a full resolution copy of these photographs?
All of the photographs here on this Flickr set have a visible watermark embedded in them. All of the photographs posted here on this Flickr set are available offline, free, at no cost, at full image resolution WITHOUT watermark. We take these photographs as a hobby and as a contribution to the running community in Ireland. Our only "cost" is our request that if you are using these images: (1) on social media sites such as Facebook, Tumblr, Pinterest, Twitter,LinkedIn, Google+, etc or (2) other websites, web multimedia, commercial/promotional material that you provide a link back to our Flickr page to attribute us. This also extends the use of these images for Facebook profile pictures. In these cases please make a separate wall or blog post with a link to our Flickr page. If you do not know how this should be done for Facebook or other social media please email us and we will be happy to help suggest how to link to us.
Please email petermooney78 AT gmail DOT com with the links to the photographs you would like to obtain a full resolution copy of. We also ask race organisers, media, etc to ask for permission before use of our images for flyers, posters, etc. We reserve the right to refuse a request.
In summary please remember - all we ask is for you to link back to our Flickr set or Flickr pages. Taking the photographs and preparing them for online posting does take a significant effort. We are not posting photographs to Flickr for commercial reasons. If you really like what we do please spread the link around your social media, send us an email, leave a comment beside the photographs, send us a Flickr email, etc.
If you would like to contribute something for your photograph(s)?
Many people offer payment for our photographs. As stated above we do not charge for these photographs. We take these photographs as our contribution to the running community in Ireland. If you feel that the photograph(s) you request are good enough that you would consider paying for their purchase from other photographic providers we would suggest that you can provide a donation to any of the great charities in Ireland who do work for Cancer Care or Cancer Research in Ireland.
I ran in the race - but my photograph doesn't appear here in your Flickr set! What gives?
As mentioned above we take these photographs as a hobby and as a voluntary contribution to the running community in Ireland. Very often we have actually ran in the same race and then switched to photographer mode after we finished the race. Consequently, we feel that we have no obligations to capture a photograph of every participant in the race. However, we do try our very best to capture as many participants as possible. But this is sometimes not possible for a variety of reasons:
►You were hidden behind another participant as you passed our camera
►Weather or lighting conditions meant that we had some photographs with blurry content which we did not upload to our Flickr set
►There were too many people - some races attract thousands of participants and as amateur photographs we cannot hope to capture photographs of everyone
►We simply missed you - sorry about that - we did our best!
You can email us petermooney78 AT gmail DOT com to enquire if we have a photograph of you which didn't make the final Flickr selection for the race. But we cannot promise that there will be photograph there. As alternatives we advise you to contact the race organisers to enquire if there were (1) other photographs taking photographs at the race event or if (2) there were professional commercial sports photographers taking photographs which might have some photographs of you available for purchase. You might find some links for further information above.
Don't like your photograph here?
That's OK! We understand!
If, for any reason, you are not happy or comfortable with your picture appearing here in this photoset on Flickr then please email us at petermooney78 AT gmail DOT com and we will remove it as soon as possible. We give careful consideration to each photograph before uploading.
I want to tell people about these great photographs!
Great! Thank you! The best link to spread the word around is probably www.flickr.com/peterm7/sets
The Church of St Leonard in Rodney Stoke, Somerset, England, was built around 1175 and is a Grade I listed building.
The interior of the church contains a screen, bearing the date 1624, the gift of Sir Edward Rodney, which includes a representation of the martyrdom of St Erasmus, who was killed by having his entrails removed.
The church underwent Victorian restoration in the 1870s when a slow combustion stove was installed in a pit in the floor.
The parish is part of the Rodney Stoke with Draycott benefice which is within the Axbridge deanery.
Burials
Sir Edward Rodney (1590–1657)
Frances Rodney (d. 1659)
Rodney Stoke is a small village and civil parish, located at grid reference ST486501, 5 miles north-west of Wells, in the English county of Somerset. The village is on the A371 between Draycott and Westbury-sub-Mendip.
The parish includes the larger village of Draycott. South of the A371 the parish includes an area of the Somerset Levels, extending to the River Axe. North of the A371 the southern slopes of the Mendip Hills rise to an area of the parish on the Mendip plateau. The parish is therefore an area of high biodiversity supporting local rare species of plants and animal life.
Close to the village is Westbury Camp, which represents the remains of an Iron Age enclosed settlement and has been designated as a Scheduled Ancient Monument.
Rodney Stoke was listed in the Domesday Book of 1086 as Stoches, meaning 'a stockaded settlement' from the Old English stoc. In 1291 the place name was recorded as Stokgifford. The Giffords were Saxon nobility at the time of Edward the Confessor with Walter Gifford (then spelt Gifard) as the Earl of Buckingham.
The parish was part of the Winterstoke Hundred.
The village was the home of, and is probably named after, Sir John Rodney (d. 1400). However Ekwall indicates that Stoke Gifford was held by Richard de Rodene in 1303.
The first Baron Rodney was George Brydges Rodney (1718/19–92), a British naval admiral of Napoleonic times.
It is one of the nine Thankful Villages in Somerset which suffered no fatalities during World War I. There is a memorial window in the Parish Church together with a new plaque that testifies to the village's enduring pride in their good fortune.
The parish council has responsibility for local issues, including setting an annual precept (local rate) to cover the council's operating costs and producing annual accounts for public scrutiny. The parish council evaluates local planning applications and works with the local police, district council officers, and neighbourhood watch groups on matters of crime, security, and traffic. The parish council's role also includes initiating projects for the maintenance and repair of parish facilities, as well as consulting with the district council on the maintenance, repair, and improvement of highways, drainage, footpaths, public transport, and street cleaning. Conservation matters (including trees and listed buildings) and environmental issues are also the responsibility of the council.
The village falls within the Non-metropolitan district of Mendip, which was formed on 1 April 1974 under the Local Government Act 1972, having previously been part of Wells Rural District, which is responsible for local planning and building control, local roads, council housing, environmental health, markets and fairs, refuse collection and recycling, cemeteries and crematoria, leisure services, parks, and tourism.
Somerset County Council is responsible for running the largest and most expensive local services such as education, social services, libraries, main roads, public transport, policing and fire services, trading standards, waste disposal and strategic planning.
The village is in the 'Rodney and Westbury' electoral ward. The ward starts in the north west at Draycott and passes through Rodney Stoke to end at Westbury-sub-Mendip. The total population of the ward as at the 2011 census was 2,127.
It is also part of the Wells county constituency represented in the House of Commons of the Parliament of the United Kingdom. It elects one Member of Parliament (MP) by the first past the post system of election.
The land is noteworthy for its importance as a flight corridor and feeding ground for the Greater Horseshoe Bat. Cheddar Complex, a Site of Special Scientific Interest, lies to the north and Mascalls' Wood, an ancient woodland and Somerset Wildlife Trust Nature Reserve, lies to the west. The cross roads may be the site of an old Roman road.
Close to the village is the Rodney Stoke nature reserve, which is a Site of Special Scientific Interest (SSSI).
The church of St Leonard, was built around 1175 and is a Grade I listed building. The interior of the church contains a screen, bearing the date 1624, the gift of Sir Edward Rodney, which includes a representation of the martyrdom of St Erasmus, who was killed by having his entrails removed.
Notable residents
Edward Rodney (1590–1657), MP for Wells and Somerset at various times between 1621 and 1642, lived in Rodney Stoke and was buried there.
John Rodney (died 1400), MP for Somerset, 1391–1393, lived in Rodney Stoke.
Frances Southwell (died 1659), courtier and wife of Edward Rodney, lived in Rodney Stoke.
Thomas Tremlett (1834–1894), first-class cricketer, was born in Rodney Stoke.
Somerset is a ceremonial county in South West England. It is bordered by the Bristol Channel, Gloucestershire, and Bristol to the north, Wiltshire to the east and the north-east, Dorset to the south-east, and Devon to the south-west. The largest settlement is the city of Bath, and the county town is Taunton.
Somerset is a predominantly rural county, especially to the south and west, with an area of 4,171 km2 (1,610 sq mi) and a population of 965,424. After Bath (101,557), the largest settlements are Weston-super-Mare (82,418), Taunton (60,479), and Yeovil (49,698). Wells (12,000) is a city, the second-smallest by population in England. For local government purposes the county comprises three unitary authority areas: Bath and North East Somerset, North Somerset, and Somerset.
The centre of Somerset is dominated by the Levels, a coastal plain and wetland, and the north-east and west of the county are hilly. The north-east contains part of the Cotswolds AONB, all of the Mendip Hills AONB, and a small part of Cranborne Chase and West Wiltshire Downs AONB; the west contains the Quantock Hills AONB, a majority of Exmoor National Park, and part of the Blackdown Hills AONB. The main rivers in the county are the Avon, which flows through Bath and then Bristol, and the Axe, Brue, and Parrett, which drain the Levels.
There is evidence of Paleolithic human occupation in Somerset, and the area was subsequently settled by the Celts, Romans and Anglo-Saxons. The county played a significant part in Alfred the Great's rise to power, and later the English Civil War and the Monmouth Rebellion. In the later medieval period its wealth allowed its monasteries and parish churches to be rebuilt in grand style; Glastonbury Abbey was particularly important, and claimed to house the tomb of King Arthur and Guinevere. The city of Bath is famous for its Georgian architecture, and is a UNESCO World Heritage Site. The county is also the location of Glastonbury Festival, one of the UK's major music festivals.
Somerset is a historic county in the south west of England. There is evidence of human occupation since prehistoric times with hand axes and flint points from the Palaeolithic and Mesolithic eras, and a range of burial mounds, hill forts and other artefacts dating from the Neolithic, Bronze and Iron Ages. The oldest dated human road work in Great Britain is the Sweet Track, constructed across the Somerset Levels with wooden planks in the 39th century BCE.
Following the Roman Empire's invasion of southern Britain, the mining of lead and silver in the Mendip Hills provided a basis for local industry and commerce. Bath became the site of a major Roman fort and city, the remains of which can still be seen. During the Early Medieval period Somerset was the scene of battles between the Anglo-Saxons and first the Britons and later the Danes. In this period it was ruled first by various kings of Wessex, and later by kings of England. Following the defeat of the Anglo-Saxon monarchy by the Normans in 1066, castles were built in Somerset.
Expansion of the population and settlements in the county continued during the Tudor and more recent periods. Agriculture and coal mining expanded until the 18th century, although other industries declined during the industrial revolution. In modern times the population has grown, particularly in the seaside towns, notably Weston-super-Mare. Agriculture continues to be a major business, if no longer a major employer because of mechanisation. Light industries are based in towns such as Bridgwater and Yeovil. The towns of Taunton and Shepton Mallet manufacture cider, although the acreage of apple orchards is less than it once was.
The Palaeolithic and Mesolithic periods saw hunter-gatherers move into the region of Somerset. There is evidence from flint artefacts in a quarry at Westbury that an ancestor of modern man, possibly Homo heidelbergensis, was present in the area from around 500,000 years ago. There is still some doubt about whether the artefacts are of human origin but they have been dated within Oxygen Isotope Stage 13 (524,000 – 478,000 BP). Other experts suggest that "many of the bone-rich Middle Pleistocene deposits belong to a single but climatically variable interglacial that succeeded the Cromerian, perhaps about 500,000 years ago. Detailed analysis of the origin and modification of the flint artefacts leads to the conclusion that the assemblage was probably a product of geomorphological processes rather than human work, but a single cut-marked bone suggests a human presence." Animal bones and artefacts unearthed in the 1980s at Westbury-sub-Mendip, in Somerset, have shown evidence of early human activity approximately 700,000 years ago.
Homo sapiens sapiens, or modern man, came to Somerset during the Early Upper Palaeolithic. There is evidence of occupation of four Mendip caves 35,000 to 30,000 years ago. During the Last Glacial Maximum, about 25,000 to 15,000 years ago, it is probable that Somerset was deserted as the area experienced tundra conditions. Evidence was found in Gough's Cave of deposits of human bone dating from around 12,500 years ago. The bones were defleshed and probably ritually buried though perhaps related to cannibalism being practised in the area at the time or making skull cups or storage containers. Somerset was one of the first areas of future England settled following the end of Younger Dryas phase of the last ice age c. 8000 BC. Cheddar Man is the name given to the remains of a human male found in Gough's Cave in Cheddar Gorge. He is Britain's oldest complete human skeleton. The remains date from about 7150 BC, and it appears that he died a violent death. Somerset is thought to have been occupied by Mesolithic hunter-gatherers from about 6000 BCE; Mesolithic artefacts have been found in more than 70 locations. Mendip caves were used as burial places, with between 50 and 100 skeletons being found in Aveline's Hole. In the Neolithic era, from about 3500 BCE, there is evidence of farming.
At the end of the last ice age the Bristol Channel was dry land, but later the sea level rose, particularly between 1220 and 900 BC and between 800 and 470 BCE, resulting in major coastal changes. The Somerset Levels became flooded, but the dry points such as Glastonbury and Brent Knoll have a long history of settlement, and are known to have been occupied by Mesolithic hunters. The county has prehistoric burial mounds (such as Stoney Littleton Long Barrow), stone rows (such as the circles at Stanton Drew and Priddy) and settlement sites. Evidence of Mesolithic occupation has come both from the upland areas, such as in Mendip caves, and from the low land areas such as the Somerset Levels. Dry points in the latter such as Glastonbury Tor and Brent Knoll, have a long history of settlement with wooden trackways between them. There were also "lake villages" in the marsh such as those at Glastonbury Lake Village and Meare. One of the oldest dated human road work in Britain is the Sweet Track, constructed across the Somerset Levels with wooden planks in the 39th century BC, partially on the route of the even earlier Post Track.
There is evidence of Exmoor's human occupation from Mesolithic times onwards. In the Neolithic period people started to manage animals and grow crops on farms cleared from the woodland, rather than act purely as hunter gatherers. It is also likely that extraction and smelting of mineral ores to make tools, weapons, containers and ornaments in bronze and then iron started in the late Neolithic and into the Bronze and Iron Ages.
The caves of the Mendip Hills were settled during the Neolithic period and contain extensive archaeological sites such as those at Cheddar Gorge. There are numerous Iron Age Hill Forts, which were later reused in the Dark Ages, such as Cadbury Castle, Worlebury Camp and Ham Hill. The age of the henge monument at Stanton Drew stone circles is unknown, but is believed to be from the Neolithic period. There is evidence of mining on the Mendip Hills back into the late Bronze Age when there were technological changes in metal working indicated by the use of lead. There are numerous "hill forts", such as Small Down Knoll, Solsbury Hill, Dolebury Warren and Burledge Hill, which seem to have had domestic purposes, not just a defensive role. They generally seem to have been occupied intermittently from the Bronze Age onward, some, such as Cadbury Camp at South Cadbury, being refurbished during different eras. Battlegore Burial Chamber is a Bronze Age burial chamber at Williton which is composed of three round barrows and possibly a long, chambered barrow.
The Iron Age tribes of later Somerset were the Dobunni in north Somerset, Durotriges in south Somerset and Dumnonii in west Somerset. The first and second produced coins, the finds of which allows their tribal areas to be suggested, but the latter did not. All three had a Celtic culture and language. However, Ptolemy stated that Bath was in the territory of the Belgae, but this may be a mistake. The Celtic gods were worshipped at the temple of Sulis at Bath and possibly the temple on Brean Down. Iron Age sites on the Quantock Hills, include major hill forts at Dowsborough and Ruborough, as well as smaller earthwork enclosures, such as Trendle Ring, Elworthy Barrows and Plainsfield Camp.
Somerset was part of the Roman Empire from 47 AD to about 409 AD. However, the end was not abrupt and elements of Romanitas lingered on for perhaps a century.
Somerset was invaded from the south-east by the Second Legion Augusta, under the future emperor Vespasian. The hillforts of the Durotriges at Ham Hill and Cadbury Castle were captured. Ham Hill probably had a temporary Roman occupation. The massacre at Cadbury Castle seems to have been associated with the later Boudiccan Revolt of 60–61 AD. The county remained part of the Roman Empire until around 409 AD.
The Roman invasion, and possibly the preceding period of involvement in the internal affairs of the south of England, was inspired in part by the potential of the Mendip Hills. A great deal of the attraction of the lead mines may have been the potential for the extraction of silver.
Forts were set up at Bath and Ilchester. The lead and silver mines at Charterhouse in the Mendip Hills were run by the military. The Romans established a defensive boundary along the new military road known the Fosse Way (from the Latin fossa meaning ditch). The Fosse Way ran through Bath, Shepton Mallet, Ilchester and south-west towards Axminster. The road from Dorchester ran through Yeovil to meet the Fosse Way at Ilchester. Small towns and trading ports were set up, such as Camerton and Combwich. The larger towns decayed in the latter part of the period, though the smaller ones appear to have decayed less. In the latter part of the period, Ilchester seems to have been a "civitas" capital and Bath may also have been one. Particularly to the east of the River Parrett, villas were constructed. However, only a few Roman sites have been found to the west of the river. The villas have produced important mosaics and artifacts. Cemeteries have been found outside the Roman towns of Somerset and by Roman temples such as that at Lamyatt. Romano-British farming settlements, such as those at Catsgore and Sigwells, have been found in Somerset. There was salt production on the Somerset Levels near Highbridge and quarrying took place near Bath, where the Roman Baths gave their name to Bath.
Excavations carried out before the flooding of Chew Valley Lake also uncovered Roman remains, indicating agricultural and industrial activity from the second half of the 1st century until the 3rd century AD. The finds included a moderately large villa at Chew Park, where wooden writing tablets (the first in the UK) with ink writing were found. There is also evidence from the Pagans Hill Roman Temple at Chew Stoke. In October 2001 the West Bagborough Hoard of 4th century Roman silver was discovered in West Bagborough. The 681 coins included two denarii from the early 2nd century and 8 Miliarense and 671 Siliqua all dating to the period AD 337 – 367. The majority were struck in the reigns of emperors Constantius II and Julian and derive from a range of mints including Arles and Lyons in France, Trier in Germany and Rome.
In April 2010, the Frome Hoard, one of the largest-ever hoards of Roman coins discovered in Britain, was found by a metal detectorist. The hoard of 52,500 coins dated from the 3rd century AD and was found buried in a field near Frome, in a jar 14 inches (36 cm) below the surface. The coins were excavated by archaeologists from the Portable Antiquities Scheme.
This is the period from about 409 AD to the start of Saxon political control, which was mainly in the late 7th century, though they are said to have captured the Bath area in 577 AD. Initially the Britons of Somerset seem to have continued much as under the Romans but without the imperial taxation and markets. There was then a period of civil war in Britain though it is not known how this affected Somerset. The Western Wandsdyke may have been constructed in this period but archaeological data shows that it was probably built during the 5th or 6th century. This area became the border between the Romano-British Celts and the West Saxons following the Battle of Deorham in 577 AD. The ditch is on the north side, so presumably it was used by the Celts as a defence against Saxons encroaching from the upper Thames Valley. According to the Anglo-Saxon Chronicle, the Saxon Cenwalh achieved a breakthrough against the British Celtic tribes, with victories at Bradford-on-Avon (in the Avon Gap in the Wansdyke) in 652 AD, and further south at the Battle of Peonnum (at Penselwood) in 658 AD, followed by an advance west through the Polden Hills to the River Parrett.
The Saxon advance from the east seems to have been halted by battles between the British and Saxons, for example; at the siege of Badon Mons Badonicus (which may have been in the Bath region e.g. at Solsbury Hill), or Bathampton Down. During the 5th, 6th and 7th centuries, Somerset was probably partly in the Kingdom of Dumnonia, partly in the land of the Durotriges and partly in that of the Dobunni. The boundaries between these is largely unknown, but may have been similar to those in the Iron Age. Various "tyrants" seem to have controlled territories from reoccupied hill forts. There is evidence of an elite at hill forts such as Cadbury Castle and Cadbury Camp; for example, there is imported pottery. Cemeteries are an important source of evidence for the period and large ones have been found in Somerset, such as that at Cannington, which was used from the Roman to the Saxon period. The towns of Somerset seem to have been little used during that period but there continued to be farming on the villa sites and at the Romano-British villages.
There may have been effects from plague and volcanic eruption during this period as well as marine transgression into the Levels.
The language spoken during this period is thought to be Southwestern Brythonic, but only one or two inscribed stones survive in Somerset from this period. However, a couple of curse tablets found in the baths at Bath may be in this language. Some place names in Somerset seem to be Celtic in origin and may be from this period or earlier, e.g. Tarnock. Some river names, such as Parrett, may be Celtic or pre-Celtic. The religion of the people of Somerset in this period is thought to be Christian but it was isolated from Rome until after the Council of Hertford in 673 AD when Aldhelm was asked to write a letter to Geraint of Dumnonia and his bishops. Some church sites in Somerset are thought to date from this period, e.g., Llantokay Street.
Most of what is known of the history of this period comes from Gildas's On the Ruin of Britain, which is thought to have been written in Durotrigan territory, possibly at Glastonbury.
The earliest fortification of Taunton started for King Ine of Wessex and Æthelburg, in or about the year 710 AD. However, according to the Anglo-Saxon Chronicle this was destroyed 12 years later.
This is the period from the late 7th century (for most of Somerset) to 1066, though for part of the 10th and 11th centuries England was under Danish control. Somerset, like Dorset to the south, held the West Saxon advance from Wiltshire/Hampshire back for over a century, remaining a frontier between the Saxons and the Romano-British Celts.
The Saxons conquered Bath following the Battle of Deorham in 577, and the border was probably established along the line of the Wansdyke to the north of the Mendip Hills. Then Cenwalh of Wessex broke through at Bradford-on-Avon in 652, and the Battle of Peonnum possibly at Penselwood in 658, advancing west through the Polden Hills to the River Parrett. In 661 the Saxons may have advanced into what is now Devon as a result of a battle fought at Postesburh, possibly Posbury near Crediton.
Then in the period 681–85 Centwine of Wessex conquered King Cadwaladr and "advanced as far as the sea", but it is not clear where this was. It is assumed that the Saxons occupied the rest of Somerset about this time. The Saxon rule was consolidated under King Ine, who established a fort at Taunton, demolished by his wife in 722. It is sometimes said that he built palaces at Somerton and South Petherton but this does not seem to be the case. He fought against Geraint in 710. In 705 the diocese of Sherborne was formed, taking in Wessex west of Selwood. Saxon kings granted land in Somerset by charter from the 7th century onward. The way and extent to which the Britons survived under the Saxons is a debatable matter. However, King Ine's laws make provision for Britons. Somerset originally formed part of Wessex and latter became a separate "shire". Somersetshire seems to have been formed within Wessex during the 8th century though it is not recorded as a name until later. Mints were set up at times in various places in Somerset in the Saxon period, e.g., Watchet.
Somerset played an important part in defeating the spread of the Danes in the 9th century. The Anglo-Saxon Chronicle records that in 845 Alderman Eanwulf, with the men of Somersetshire (Sumorsǣte), and Bishop Ealstan, and Alderman Osric, with the men of Dorsetshire, conquered the Danish army at the mouth of the Parret. This was the first known use of the name Somersæte. The Anglo-Saxon Chronicle reports that in January 878 the King Alfred the Great fled into the marshes of Somerset from the Viking's invasion and made a fort at Athelney. From the fort Alfred was able to organize a resistance using the local militias from Somerset, Wiltshire and Hampshire.
Viking raids took place for instance in 987 and 997 at Watchet and the Battle of Cynwit. King Alfred was driven to seek refuge from the Danes at Athelney before defeating them at the Battle of Ethandun in 878, usually considered to be near Edington, Wiltshire, but possibly the village of Edington in Somerset. Alfred established a series of forts and lookout posts linked by a military road, or Herepath, so his army could cover Viking movements at sea. The Herepath has a characteristic form which is familiar on the Quantocks: a regulation 20 m wide track between avenues of trees growing from hedge laying embankments. The Herepath ran from the ford on the River Parrett at Combwich, past Cannington hill fort to Over Stowey, where it climbed the Quantocks along the line of the current Stowey road, to Crowcombe Park Gate. Then it went south along the ridge, to Triscombe Stone. One branch may have led past Lydeard Hill and Buncombe Hill, back to Alfred's base at Athelney. The main branch descended the hills at Triscombe, then along the avenue to Red Post Cross, and west to the Brendon Hills and Exmoor. A peace treaty with the Danes was signed at Wedmore and the Danish king Guthrum the Old was baptised at Aller. Burhs (fortified places) had been set up by 919, such as Lyng. The Alfred Jewel, an object about 2.5 inch long, made of filigree gold, cloisonné-enamelled and with a rock crystal covering, was found in 1693 at Petherton Park, North Petherton. Believed to have been owned by Alfred the Great it is thought to have been the handle for a pointer that would have fit into the hole at its base and been used while reading a book.
Monasteries and minster churches were set up all over Somerset, with daughter churches from the minsters in manors. There was a royal palace at Cheddar, which was used at times in the 10th century to host the Witenagemot, and there is likely to have been a "central place" at Somerton, Bath, Glastonbury and Frome since the kings visited them. The towns of Somerset seem to have been in occupation in this period though evidence for this is limited because of subsequent buildings on top of remains from this period. Agriculture flourished in this period, with a re-organisation into centralised villages in the latter part in the east of the county.
In the period before the Norman Conquest, Somerset came under the control of Godwin, Earl of Wessex, and his family. There seems to have been some Danish settlement at Thurloxton and Spaxton, judging from the place-names. After the Norman Conquest, the county was divided into 700 fiefs, and large areas were owned by the crown, with fortifications such as Dunster Castle used for control and defence.
This period of Somerset's history is well documented, for example in the Anglo-Saxon Chronicle and Asser's Life of Alfred.
This is the period from 1066 to around 1500. Following the defeat of the Saxons by the Normans in 1066, various castles were set up in Somerset by the new lords such as that at Dunster, and the manors was awarded to followers of William the Conqueror such as William de Moyon and Walter of Douai. Somerset does not seem to have played much part in the civil war in King Stephen's time, but Somerset lords were main players in the murder of Thomas Becket.
A good picture of the county in 1086 is given by Domesday Book, though there is some difficulty in identifying the various places since the hundreds are not specified. The total population given for the county, which had different boundaries to those today, was 13,399, however this only included the heads of households, so with their families this may have been around 67,000. Farming seems to have prospered for the next three centuries but was severely hit by the Black Death which in 1348 arrived in Dorset and quickly spread through Somerset, causing widespread mortality, perhaps as much as 50% in places. It re-occurred, resulting in a change in feudal practices since the manpower was no longer so available.
Reclamation of land from marsh in the Somerset Levels increased, largely under monastic influence. Crafts and industries also flourished, the Somerset woollen industry being one of the largest in England at this time. "New towns" were founded in this period in Somerset, i.e. Newport, but were not successful. Coal mining on the Mendips was an important source of wealth while quarrying also took place, an example is near Bath.
The towns grew, again often by monastic instigation, during this period and fairs were started. The church was very powerful at this period, particularly Glastonbury Abbey. After their church burnt down, the monks there "discovered" the tomb of "King Arthur" and were able rebuild their church. There were over 20 monasteries in Somerset at this period including the priory at Hinton Charterhouse which was founded in 1232 by Ela, Countess of Salisbury who also founded Lacock Abbey. Many parish churches were re-built in this period. Between 1107 and 1129 William Giffard the Chancellor of King Henry I, converted the bishop's hall in Taunton into Taunton Castle. Bridgwater Castle was built in 1202 by William Brewer. It passed to the king in 1233 and in 1245 repairs were ordered to its motte and towers. During the 11th century Second Barons' War against Henry III, Bridgwater was held by the barons against the King. In the English Civil War the town and the castle were held by the Royalists under Colonel Sir Francis Wyndham. Eventually, with many buildings destroyed in the town, the castle and its valuable contents were surrendered to the Parliamentarians. The castle itself was deliberately destroyed in 1645.
During the Middle Ages sheep farming for the wool trade came to dominate the economy of Exmoor. The wool was spun into thread on isolated farms and collected by merchants to be woven, fulled, dyed and finished in thriving towns such as Dunster. The land started to be enclosed and from the 17th century onwards larger estates developed, leading to establishment of areas of large regular shaped fields. During this period a Royal Forest and hunting ground was established, administered by the Warden. The Royal Forest was sold off in 1818.
In the medieval period the River Parrett was used to transport Hamstone from the quarry at Ham Hill, Bridgwater was part of the Port of Bristol until the Port of Bridgwater was created in 1348, covering 80 miles (130 km) of the Somerset coast line, from the Devon border to the mouth of the River Axe. Historically, the main port on the river was at Bridgwater; the river being bridged at this point, with the first bridge being constructed in 1200 AD. Quays were built in 1424; with another quay, the Langport slip, being built in 1488 upstream of the Town Bridge. A Customs House was sited at Bridgwater, on West Quay; and a dry dock, launching slips and a boat yard on East Quay. The river was navigable, with care, to Bridgwater Town Bridge by 400 to 500 tonnes (440 to 550 tons) vessels. By trans-shipping into barges at the Town Bridge the Parrett was navigable as far as Langport and (via the River Yeo) to Ilchester.
This is the period from around 1500 to 1800. In the 1530s, the monasteries were dissolved and their lands bought from the king by various important families in Somerset. By 1539, Glastonbury Abbey was the only monastery left, its abbot Richard Whiting was then arrested and executed on the orders of Thomas Cromwell. From the Tudor to the Georgian times, farming specialised and techniques improved, leading to increases in population, although no new towns seem to have been founded. Large country houses such as at Hinton St George and Montacute House were built at this time.
The Bristol Channel floods of 1607 are believed to have affected large parts of the Somerset Levels with flooding up to 8 feet (2 m) above sea level. In 1625, a House of Correction was established in Shepton Mallet and, today, HMP Shepton Mallet is England's oldest prison still in use.
During the English Civil War, Somerset was largely Parliamentarian, although Dunster was a Royalist stronghold. The county was the site of important battles between the Royalists and the Parliamentarians, notably the Battle of Lansdowne in 1643 and the Battle of Langport in 1645. The castle changed hands several times during 1642–45 along with the town. During the Siege of Taunton it was defended by Robert Blake, from July 1644 to July 1645. This war resulted in castles being destroyed to prevent their re-use.
In 1685, the Duke of Monmouth led the Monmouth Rebellion in which Somerset people fought against James II. The rebels landed at Lyme Regis and travelled north hoping to capture Bristol and Bath, puritan soldiers damaged the west front of Wells Cathedral, tore lead from the roof to make bullets, broke the windows, smashed the organ and the furnishings, and for a time stabled their horses in the nave. They were defeated in the Battle of Sedgemoor at Westonzoyland, the last battle fought on English soil. The Bloody Assizes which followed saw the losers being sentenced to death or transportation.
The Society of Friends established itself in Street in the mid-17th century, and among the close-knit group of Quaker families were the Clarks: Cyrus started a business in sheepskin rugs, later joined by his brother James, who introduced the production of woollen slippers and, later, boots and shoes. C&J Clark still has its headquarters in Street, but shoes are no longer manufactured there. Instead, in 1993, redundant factory buildings were converted to form Clarks Village, the first purpose-built factory outlet in the United Kingdom.
The 18th century was largely one of peace and declining industrial prosperity in Somerset. The Industrial Revolution in the Midlands and Northern England spelt the end for most of Somerset's cottage industries. However, farming continued to flourish, with the Bath and West of England Agricultural Society being founded in 1777 to improve methods. John Billingsley conducted a survey of the county's agriculture in 1795 but found that methods could still be improved.
Arthur Wellesley took his title, Duke of Wellington from the town of Wellington. He is commemorated on a nearby hill with a large, spotlit obelisk, known as the Wellington Monument.
In north Somerset, mining in the Somerset coalfield was an important industry, and in an effort to reduce the cost of transporting the coal the Somerset Coal Canal was built; part of it was later converted into a railway. Other canals included the Bridgwater and Taunton Canal, Westport Canal, Grand Western Canal, Glastonbury Canal and Chard Canal.[9] The Dorset and Somerset Canal was proposed, but very little of it was ever constructed.
The 19th century saw improvements to Somerset's roads with the introduction of turnpikes and the building of canals and railways. The usefulness of the canals was short-lived, though they have now been restored for recreation. The railways were nationalised after the Second World War, but continued until 1965, when smaller lines were scrapped; two were transferred back to private ownership as "heritage" lines.
In 1889, Somerset County Council was created, replacing the administrative functions of the Quarter Sessions.
The population of Somerset has continued to grow since 1800, when it was 274,000, particularly in the seaside towns such as Weston-super-Mare. Some population decline occurred earlier in the period in the villages, but this has now been reversed, and by 1951 the population of Somerset was 551,000.
Chard claims to be the birthplace of powered flight, as it was here in 1848 that the Victorian aeronautical pioneer John Stringfellow first demonstrated that engine-powered flight was possible through his work on the Aerial Steam Carriage. North Petherton was the first town in England (and one of the few ever) to be lit by acetylene gas lighting, supplied by the North Petherton Rosco Acetylene Company. Street lights were provided in 1906. Acetylene was replaced in 1931 by coal gas produced in Bridgwater, as well as by the provision of an electricity supply.
Around the 1860s, at the height of the iron and steel era, a pier and a deep-water dock were built, at Portishead, by the Bristol & Portishead Pier and Railway to accommodate the large ships that had difficulty in reaching Bristol Harbour. The Portishead power stations were coal-fed power stations built next to the dock. Construction work started on Portishead "A" power station in 1926. It began generating electricity in 1929 for the Bristol Corporation's Electricity Department. In 1951, Albright and Wilson built a chemical works on the opposite side of the dock from the power stations. The chemical works produced white phosphorus from phosphate rock imported, through the docks, into the UK. The onset of new generating capacity at Pembroke (oil-fired) and Didcot (coal-fired) in the mid-1970s brought about the closure of the older, less efficient "A" Station. The newer of the two power stations ("B" Station) was converted to burn oil when the Somerset coalfields closed. Industrial activities ceased in the dock with the closure of the power stations. The Port of Bristol Authority finally closed the dock in 1992, and it has now been developed into a marina and residential area.
During the First World War hundreds of Somerset soldiers were killed, and war memorials were put up in most of the towns and villages; only a few villages escaped casualties. There were also casualties – though much fewer – during the Second World War, who were added to the memorials. The county was a base for troops preparing for the 1944 D-Day landings, and some Somerset hospitals still date partly from that time. The Royal Ordnance Factory ROF Bridgwater was constructed early in World War II for the Ministry of Supply. It was designed as an Explosive ROF, to produce RDX, which was then a new experimental high-explosive. It obtained water supplies from two sources via the Somerset Levels: the artificial Huntspill River which was dug during the construction of the factory and also from the King's Sedgemoor Drain, which was widened at the same time. The Taunton Stop Line was set up to resist a potential German invasion, and the remains of its pill boxes can still be seen, as well as others along the coast. A decoy town was constructed on Black Down, intended to represent the blazing lights of a town which had neglected to follow the black-out regulations. Sites in the county housed Prisoner of War camps including: Norton Fitzwarren, Barwick, Brockley, Goathurst and Wells. Various airfields were built or converted from civilian use including: RNAS Charlton Horethorne (HMS Heron II), RAF Weston-super-Mare, RNAS Yeovilton (HMS Heron), Yeovil/Westland Airport, RAF Weston Zoyland, RAF Merryfield, RAF Culmhead and RAF Charmy Down.
Exmoor was one of the first British National Parks, designated in 1954, under the 1949 National Parks and Access to the Countryside Act. and is named after its main river. It was expanded in 1991 and in 1993 Exmoor was designated as an Environmentally Sensitive Area. The Quantock Hills were designated as an Area of Outstanding Natural Beauty (AONB) in 1956, the first such designation in England under the National Parks and Access to the Countryside Act 1949. The Mendip Hills followed with AONB designation in 1972.
Hinkley Point A nuclear power station was a Magnox power station constructed between 1957 and 1962 and operating until ceasing generation in 2000. Hinkley Point B is an Advanced Gas-cooled Reactor (AGR) which was designed to generate 1250 MW of electricity (MWe). Construction of Hinkley Point B started in 1967. In September 2008 it was announced, by Électricité de France (EDF), that a third, twin-unit European Pressurised Reactor (EPR) power station known as Hinkley Point C is planned, to replace Hinkley Point B which was due for closure in 2016, but has now has its life extended until 2022.
Somerset today has only two small cities, Bath and Wells, and only small towns in comparison with other areas of England. Tourism is a major source of employment along the coast, and in Bath and Cheddar for example. Other attractions include Exmoor, West Somerset Railway, Haynes Motor Museum and the Fleet Air Arm Museum as well as the churches and the various National Trust and English Heritage properties in Somerset.
Agriculture continues to be a major business, if no longer a major employer because of mechanisation. Light industries take place in towns such as Bridgwater and Yeovil. The towns of Taunton and Shepton Mallet manufacture cider, although the number of apple orchards has reduced.
In the late 19th century the boundaries of Somerset were slightly altered, but the main change came in 1974 when the county of Avon was set up. The northern part of Somerset was removed from the administrative control of Somerset County Council. On abolition of the county of Avon in 1996, these areas became separate administrative authorities, "North Somerset" and "Bath and North East Somerset". The Department for Communities and Local Government was considering a proposal by Somerset County Council to change Somerset's administrative structure by abolishing the five districts to create a Somerset unitary authority. The changes were planned to be implemented no later than 1 April 2009. However, support for the county council's bid was not guaranteed and opposition among the district council and local population was strong; 82% of people responding to a referendum organised by the five district councils rejected the proposals. It was confirmed in July 2007 that the government had rejected the proposals for unitary authorities in Somerset, and that the present two-tier arrangements of Somerset County Council and the district councils will remain.
NARMADA PARIKRAMA
The Narmada also called the Rewa, is a river in central India and the fifth longest river in the Indian subcontinent. It is the third longest river that flows entirely within India, after the Godavari and the Krishna. It is also known as "Life Line of Madhya Pradesh" for its huge contribution to the state of Madhya Pradesh in many ways. It forms the traditional boundary between North India and South India and flows westwards over a length of 1,312 km (815.2 mi) before draining through theGulf of Khambhat into the Arabian Sea, 30 km (18.6 mi) west of Bharuch city of Gujarat. It is one of only three major rivers in peninsular India that run from east to west (longest west flowing river), along with the Tapti River and the Mahi River. It is the one of the rivers in India that flows in a rift valley, flowing west between the Satpura and Vindhya ranges. The other rivers which flows through rift valley include Damodar River in Chota Nagpur Plateau and Tapti. The Tapti River and Mahi River also flow through rift valleys, but between different ranges. It flows through the states of Madhya Pradesh(1,077 km (669.2 mi)), and Maharashtra, (74 km (46.0 mi))– (35 km (21.7 mi)) then along the border between Madhya Pradesh and Maharashtra (39 km (24.2 mi) and the border between Madhya Pradesh and Gujarat and in Gujarat (161 km (100.0 mi)).
The Periplus Maris Erythraei (c. 80 AD) calls it the Nammadus, and theBritish Raj called it the Nerbudda or Narbada. Narmadā is a Sanskrit word meaning "the Giver of Pleasure".
To Hindus the Narmada is one of the five holy rivers of India; the other four beingGanges, Yamuna, Godavari and Kaveri. It is believed that a dip in any of these five rivers washes one's sins away. According to a legend, the river Ganges, polluted by millions of people bathing in it, assumes the form of a black cow and comes to the Narmada to bathe and cleanse itself in its holy waters. Legends also claim that the Narmada River is older than the river Ganges.
The river was mentioned by Ptolemy in the second century AD as Namade and by the author of the Periplus. The Ramayana, the Mahabharat, and thePuranas refer to it frequently. The Rewa Khand of Vayu Purana and the Rewa Khand of Skanda Purana are entirely devoted to the story of the birth and the importance of the river, and hence Narmada is also called the Rewa.
There are many fables about the origin of the Narmada. According to one of them, once Lord Shiva, the Destroyer of the Universe, meditated so hard that he started perspiring. Shiva's sweat accumulated in a tank and started flowing in the form of a river – the Narmada. Another legend has it that two teardrops that fell from the eyes of Lord Brahma, the creator of the universe, yielded two rivers – the Narmada and the Son.
Legends also say that for Lord Shiva, the Hindu God, the river is especially sacred on account of its origin, and it is often called Shankari, i.e., daughter of Shankar (Lord Shiva). All the pebbles rolling on its bed are said to take the shape of his emblem with the saying, "Narmada Ke Kanker utte Sankar" (a popular saying in the Hindi belt of India), which means that 'pebble stones of Narmada get a personified form of Shiva'. These lingam shaped stones (cryptocrytalline quartz), calledBanalinga also called (Banashivalingas) are much sought after for daily worship by the Hindus. The Brihadeeswara Temple in Thanjavur, Tamil Nadu, constructed by Rajaraja Chola, has one of the biggest Banalingas. Adi Shankara met his guru Govinda Bhagavatpada on the banks of the river Narmada.
Narmada is also said to have been in love with the Sonbhadra, another river flowing on the Chota Nagpur Plateau. According to the Puranas, the Narmada is also called the Rewa, from its leaping motion (from the root 'rev') through its rocky bed.
Important religious places and Ghats along the course of the river, starting from its origin at Narmadakhund at Amarkantakhill, are a) the Amarkantak (in Sanskrit: Neck of Shiva) or Teertharaj (the King of Pilgrimages), b) Omkareshwar, Maheshwar, and Mahadeo temples, Nemawar Siddeshwar Mandir in the middle reach of the river – all named after Shiva, c) Chausath Yogini (sixty four yoginis) temple, d) Chaubis Avatar temple, e) Bhojpur Shiva temple and Bhrigu Rishi temple in Bharuch. The Narmada River is also worshipped as mother goddess by Narmadeeya Brahmins.
The importance of the Narmada River as sacred is testified by the fact that the pilgrims perform a holy pilgrimage of aparikrama or circumambulation of the river.[17] The Narmada Parikrama, as it is called, is considered to be a meritorious act that a pilgrim can undertake. Many sadhus and pilgrims walk on foot from the Arabian Sea at Bharuch in Gujarat, along the river, to the source in Maikal Mountains (Amarkantak hills) in Madhya Pradesh and back along the opposite bank of the river. It is a 2,600-kilometre (1,600 mi) walk.[18] Important towns of interest in the valley are Jabalpur, Barwani, Hoshangabad, Harda, Narmada Nagar, Omkareshwar, Dewas (Nemavar, Kity, Pipri), Mandla and Maheshwar in Madhya Pradesh, andRajpipla and Bharuch in Gujarat. Some places of historical interest are Joga Ka Quilla, Chhatri of Baji Rao Peshwa andBhimbetka, and among the falls are the Dugdhdhara, Dhardi falls, Bheraghat, Dhuandhara, Kapiladhara and Sahastradhara. By Kailash Mansarovar Foundation Swami Bikash Giri www.sumeruparvat.com , www.naturalitem.com
NARMADA PARIKRAMA
The Narmada also called the Rewa, is a river in central India and the fifth longest river in the Indian subcontinent. It is the third longest river that flows entirely within India, after the Godavari and the Krishna. It is also known as "Life Line of Madhya Pradesh" for its huge contribution to the state of Madhya Pradesh in many ways. It forms the traditional boundary between North India and South India and flows westwards over a length of 1,312 km (815.2 mi) before draining through theGulf of Khambhat into the Arabian Sea, 30 km (18.6 mi) west of Bharuch city of Gujarat. It is one of only three major rivers in peninsular India that run from east to west (longest west flowing river), along with the Tapti River and the Mahi River. It is the one of the rivers in India that flows in a rift valley, flowing west between the Satpura and Vindhya ranges. The other rivers which flows through rift valley include Damodar River in Chota Nagpur Plateau and Tapti. The Tapti River and Mahi River also flow through rift valleys, but between different ranges. It flows through the states of Madhya Pradesh(1,077 km (669.2 mi)), and Maharashtra, (74 km (46.0 mi))– (35 km (21.7 mi)) then along the border between Madhya Pradesh and Maharashtra (39 km (24.2 mi) and the border between Madhya Pradesh and Gujarat and in Gujarat (161 km (100.0 mi)).
The Periplus Maris Erythraei (c. 80 AD) calls it the Nammadus, and theBritish Raj called it the Nerbudda or Narbada. Narmadā is a Sanskrit word meaning "the Giver of Pleasure".
To Hindus the Narmada is one of the five holy rivers of India; the other four beingGanges, Yamuna, Godavari and Kaveri. It is believed that a dip in any of these five rivers washes one's sins away. According to a legend, the river Ganges, polluted by millions of people bathing in it, assumes the form of a black cow and comes to the Narmada to bathe and cleanse itself in its holy waters. Legends also claim that the Narmada River is older than the river Ganges.
The river was mentioned by Ptolemy in the second century AD as Namade and by the author of the Periplus. The Ramayana, the Mahabharat, and thePuranas refer to it frequently. The Rewa Khand of Vayu Purana and the Rewa Khand of Skanda Purana are entirely devoted to the story of the birth and the importance of the river, and hence Narmada is also called the Rewa.
There are many fables about the origin of the Narmada. According to one of them, once Lord Shiva, the Destroyer of the Universe, meditated so hard that he started perspiring. Shiva's sweat accumulated in a tank and started flowing in the form of a river – the Narmada. Another legend has it that two teardrops that fell from the eyes of Lord Brahma, the creator of the universe, yielded two rivers – the Narmada and the Son.
Legends also say that for Lord Shiva, the Hindu God, the river is especially sacred on account of its origin, and it is often called Shankari, i.e., daughter of Shankar (Lord Shiva). All the pebbles rolling on its bed are said to take the shape of his emblem with the saying, "Narmada Ke Kanker utte Sankar" (a popular saying in the Hindi belt of India), which means that 'pebble stones of Narmada get a personified form of Shiva'. These lingam shaped stones (cryptocrytalline quartz), calledBanalinga also called (Banashivalingas) are much sought after for daily worship by the Hindus. The Brihadeeswara Temple in Thanjavur, Tamil Nadu, constructed by Rajaraja Chola, has one of the biggest Banalingas. Adi Shankara met his guru Govinda Bhagavatpada on the banks of the river Narmada.
Narmada is also said to have been in love with the Sonbhadra, another river flowing on the Chota Nagpur Plateau. According to the Puranas, the Narmada is also called the Rewa, from its leaping motion (from the root 'rev') through its rocky bed.
Important religious places and Ghats along the course of the river, starting from its origin at Narmadakhund at Amarkantakhill, are a) the Amarkantak (in Sanskrit: Neck of Shiva) or Teertharaj (the King of Pilgrimages), b) Omkareshwar, Maheshwar, and Mahadeo temples, Nemawar Siddeshwar Mandir in the middle reach of the river – all named after Shiva, c) Chausath Yogini (sixty four yoginis) temple, d) Chaubis Avatar temple, e) Bhojpur Shiva temple and Bhrigu Rishi temple in Bharuch. The Narmada River is also worshipped as mother goddess by Narmadeeya Brahmins.
The importance of the Narmada River as sacred is testified by the fact that the pilgrims perform a holy pilgrimage of aparikrama or circumambulation of the river.[17] The Narmada Parikrama, as it is called, is considered to be a meritorious act that a pilgrim can undertake. Many sadhus and pilgrims walk on foot from the Arabian Sea at Bharuch in Gujarat, along the river, to the source in Maikal Mountains (Amarkantak hills) in Madhya Pradesh and back along the opposite bank of the river. It is a 2,600-kilometre (1,600 mi) walk.[18] Important towns of interest in the valley are Jabalpur, Barwani, Hoshangabad, Harda, Narmada Nagar, Omkareshwar, Dewas (Nemavar, Kity, Pipri), Mandla and Maheshwar in Madhya Pradesh, andRajpipla and Bharuch in Gujarat. Some places of historical interest are Joga Ka Quilla, Chhatri of Baji Rao Peshwa andBhimbetka, and among the falls are the Dugdhdhara, Dhardi falls, Bheraghat, Dhuandhara, Kapiladhara and Sahastradhara. By Kailash Mansarovar Foundation Swami Bikash Giri www.sumeruparvat.com , www.naturalitem.com
NARMADA PARIKRAMA
The Narmada also called the Rewa, is a river in central India and the fifth longest river in the Indian subcontinent. It is the third longest river that flows entirely within India, after the Godavari and the Krishna. It is also known as "Life Line of Madhya Pradesh" for its huge contribution to the state of Madhya Pradesh in many ways. It forms the traditional boundary between North India and South India and flows westwards over a length of 1,312 km (815.2 mi) before draining through theGulf of Khambhat into the Arabian Sea, 30 km (18.6 mi) west of Bharuch city of Gujarat. It is one of only three major rivers in peninsular India that run from east to west (longest west flowing river), along with the Tapti River and the Mahi River. It is the one of the rivers in India that flows in a rift valley, flowing west between the Satpura and Vindhya ranges. The other rivers which flows through rift valley include Damodar River in Chota Nagpur Plateau and Tapti. The Tapti River and Mahi River also flow through rift valleys, but between different ranges. It flows through the states of Madhya Pradesh(1,077 km (669.2 mi)), and Maharashtra, (74 km (46.0 mi))– (35 km (21.7 mi)) then along the border between Madhya Pradesh and Maharashtra (39 km (24.2 mi) and the border between Madhya Pradesh and Gujarat and in Gujarat (161 km (100.0 mi)).
The Periplus Maris Erythraei (c. 80 AD) calls it the Nammadus, and theBritish Raj called it the Nerbudda or Narbada. Narmadā is a Sanskrit word meaning "the Giver of Pleasure".
To Hindus the Narmada is one of the five holy rivers of India; the other four beingGanges, Yamuna, Godavari and Kaveri. It is believed that a dip in any of these five rivers washes one's sins away. According to a legend, the river Ganges, polluted by millions of people bathing in it, assumes the form of a black cow and comes to the Narmada to bathe and cleanse itself in its holy waters. Legends also claim that the Narmada River is older than the river Ganges.
The river was mentioned by Ptolemy in the second century AD as Namade and by the author of the Periplus. The Ramayana, the Mahabharat, and thePuranas refer to it frequently. The Rewa Khand of Vayu Purana and the Rewa Khand of Skanda Purana are entirely devoted to the story of the birth and the importance of the river, and hence Narmada is also called the Rewa.
There are many fables about the origin of the Narmada. According to one of them, once Lord Shiva, the Destroyer of the Universe, meditated so hard that he started perspiring. Shiva's sweat accumulated in a tank and started flowing in the form of a river – the Narmada. Another legend has it that two teardrops that fell from the eyes of Lord Brahma, the creator of the universe, yielded two rivers – the Narmada and the Son.
Legends also say that for Lord Shiva, the Hindu God, the river is especially sacred on account of its origin, and it is often called Shankari, i.e., daughter of Shankar (Lord Shiva). All the pebbles rolling on its bed are said to take the shape of his emblem with the saying, "Narmada Ke Kanker utte Sankar" (a popular saying in the Hindi belt of India), which means that 'pebble stones of Narmada get a personified form of Shiva'. These lingam shaped stones (cryptocrytalline quartz), calledBanalinga also called (Banashivalingas) are much sought after for daily worship by the Hindus. The Brihadeeswara Temple in Thanjavur, Tamil Nadu, constructed by Rajaraja Chola, has one of the biggest Banalingas. Adi Shankara met his guru Govinda Bhagavatpada on the banks of the river Narmada.
Narmada is also said to have been in love with the Sonbhadra, another river flowing on the Chota Nagpur Plateau. According to the Puranas, the Narmada is also called the Rewa, from its leaping motion (from the root 'rev') through its rocky bed.
Important religious places and Ghats along the course of the river, starting from its origin at Narmadakhund at Amarkantakhill, are a) the Amarkantak (in Sanskrit: Neck of Shiva) or Teertharaj (the King of Pilgrimages), b) Omkareshwar, Maheshwar, and Mahadeo temples, Nemawar Siddeshwar Mandir in the middle reach of the river – all named after Shiva, c) Chausath Yogini (sixty four yoginis) temple, d) Chaubis Avatar temple, e) Bhojpur Shiva temple and Bhrigu Rishi temple in Bharuch. The Narmada River is also worshipped as mother goddess by Narmadeeya Brahmins.
The importance of the Narmada River as sacred is testified by the fact that the pilgrims perform a holy pilgrimage of aparikrama or circumambulation of the river.[17] The Narmada Parikrama, as it is called, is considered to be a meritorious act that a pilgrim can undertake. Many sadhus and pilgrims walk on foot from the Arabian Sea at Bharuch in Gujarat, along the river, to the source in Maikal Mountains (Amarkantak hills) in Madhya Pradesh and back along the opposite bank of the river. It is a 2,600-kilometre (1,600 mi) walk.[18] Important towns of interest in the valley are Jabalpur, Barwani, Hoshangabad, Harda, Narmada Nagar, Omkareshwar, Dewas (Nemavar, Kity, Pipri), Mandla and Maheshwar in Madhya Pradesh, andRajpipla and Bharuch in Gujarat. Some places of historical interest are Joga Ka Quilla, Chhatri of Baji Rao Peshwa andBhimbetka, and among the falls are the Dugdhdhara, Dhardi falls, Bheraghat, Dhuandhara, Kapiladhara and Sahastradhara. By Kailash Mansarovar Foundation Swami Bikash Giri www.sumeruparvat.com , www.naturalitem.com
NARMADA PARIKRAMA
The Narmada also called the Rewa, is a river in central India and the fifth longest river in the Indian subcontinent. It is the third longest river that flows entirely within India, after the Godavari and the Krishna. It is also known as "Life Line of Madhya Pradesh" for its huge contribution to the state of Madhya Pradesh in many ways. It forms the traditional boundary between North India and South India and flows westwards over a length of 1,312 km (815.2 mi) before draining through theGulf of Khambhat into the Arabian Sea, 30 km (18.6 mi) west of Bharuch city of Gujarat. It is one of only three major rivers in peninsular India that run from east to west (longest west flowing river), along with the Tapti River and the Mahi River. It is the one of the rivers in India that flows in a rift valley, flowing west between the Satpura and Vindhya ranges. The other rivers which flows through rift valley include Damodar River in Chota Nagpur Plateau and Tapti. The Tapti River and Mahi River also flow through rift valleys, but between different ranges. It flows through the states of Madhya Pradesh(1,077 km (669.2 mi)), and Maharashtra, (74 km (46.0 mi))– (35 km (21.7 mi)) then along the border between Madhya Pradesh and Maharashtra (39 km (24.2 mi) and the border between Madhya Pradesh and Gujarat and in Gujarat (161 km (100.0 mi)).
The Periplus Maris Erythraei (c. 80 AD) calls it the Nammadus, and theBritish Raj called it the Nerbudda or Narbada. Narmadā is a Sanskrit word meaning "the Giver of Pleasure".
To Hindus the Narmada is one of the five holy rivers of India; the other four beingGanges, Yamuna, Godavari and Kaveri. It is believed that a dip in any of these five rivers washes one's sins away. According to a legend, the river Ganges, polluted by millions of people bathing in it, assumes the form of a black cow and comes to the Narmada to bathe and cleanse itself in its holy waters. Legends also claim that the Narmada River is older than the river Ganges.
The river was mentioned by Ptolemy in the second century AD as Namade and by the author of the Periplus. The Ramayana, the Mahabharat, and thePuranas refer to it frequently. The Rewa Khand of Vayu Purana and the Rewa Khand of Skanda Purana are entirely devoted to the story of the birth and the importance of the river, and hence Narmada is also called the Rewa.
There are many fables about the origin of the Narmada. According to one of them, once Lord Shiva, the Destroyer of the Universe, meditated so hard that he started perspiring. Shiva's sweat accumulated in a tank and started flowing in the form of a river – the Narmada. Another legend has it that two teardrops that fell from the eyes of Lord Brahma, the creator of the universe, yielded two rivers – the Narmada and the Son.
Legends also say that for Lord Shiva, the Hindu God, the river is especially sacred on account of its origin, and it is often called Shankari, i.e., daughter of Shankar (Lord Shiva). All the pebbles rolling on its bed are said to take the shape of his emblem with the saying, "Narmada Ke Kanker utte Sankar" (a popular saying in the Hindi belt of India), which means that 'pebble stones of Narmada get a personified form of Shiva'. These lingam shaped stones (cryptocrytalline quartz), calledBanalinga also called (Banashivalingas) are much sought after for daily worship by the Hindus. The Brihadeeswara Temple in Thanjavur, Tamil Nadu, constructed by Rajaraja Chola, has one of the biggest Banalingas. Adi Shankara met his guru Govinda Bhagavatpada on the banks of the river Narmada.
Narmada is also said to have been in love with the Sonbhadra, another river flowing on the Chota Nagpur Plateau. According to the Puranas, the Narmada is also called the Rewa, from its leaping motion (from the root 'rev') through its rocky bed.
Important religious places and Ghats along the course of the river, starting from its origin at Narmadakhund at Amarkantakhill, are a) the Amarkantak (in Sanskrit: Neck of Shiva) or Teertharaj (the King of Pilgrimages), b) Omkareshwar, Maheshwar, and Mahadeo temples, Nemawar Siddeshwar Mandir in the middle reach of the river – all named after Shiva, c) Chausath Yogini (sixty four yoginis) temple, d) Chaubis Avatar temple, e) Bhojpur Shiva temple and Bhrigu Rishi temple in Bharuch. The Narmada River is also worshipped as mother goddess by Narmadeeya Brahmins.
The importance of the Narmada River as sacred is testified by the fact that the pilgrims perform a holy pilgrimage of aparikrama or circumambulation of the river.[17] The Narmada Parikrama, as it is called, is considered to be a meritorious act that a pilgrim can undertake. Many sadhus and pilgrims walk on foot from the Arabian Sea at Bharuch in Gujarat, along the river, to the source in Maikal Mountains (Amarkantak hills) in Madhya Pradesh and back along the opposite bank of the river. It is a 2,600-kilometre (1,600 mi) walk.[18] Important towns of interest in the valley are Jabalpur, Barwani, Hoshangabad, Harda, Narmada Nagar, Omkareshwar, Dewas (Nemavar, Kity, Pipri), Mandla and Maheshwar in Madhya Pradesh, andRajpipla and Bharuch in Gujarat. Some places of historical interest are Joga Ka Quilla, Chhatri of Baji Rao Peshwa andBhimbetka, and among the falls are the Dugdhdhara, Dhardi falls, Bheraghat, Dhuandhara, Kapiladhara and Sahastradhara. By Kailash Mansarovar Foundation Swami Bikash Giri www.sumeruparvat.com , www.naturalitem.com
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Postcard
The Fay Thomas Collection includes family archives relating to the Thomas family. Moses Thomas (1825-1878) was a significant figure in the history of the area now known as the City of Whittlesea, Victoria, Australia. Thomas and Ann and their family lived at "Mayfield", Mernda, Victoria.
Miss Lily Thomas (1871-1946), Thomas and Ann’s fourth daughter lived there all her life. She collected postcards which her family and friends sent her on a very regular basis. It was an easy and enjoyable way to keep in touch. Production of postcards blossomed in the late 19th and early 20th centuries. Lily’s collection encompasses the so-called Golden Age (1890-1915) with many postmarked 1906-1907. Some were sent to other members of the family.
The collection document the natural landscape as well as the built environment—buildings, gardens, parks, and tourist sites. Topographical Postcards showing street scenes and general views from Australian and international locations, some of which are artistic views. Popular postcard manufacturers such as Tuck’s Postcards are included in the collection.
Decorative cards, many embellished with floral motives (as a nod to the receiver Lily?) and embossing. Greeting cards are common for Christmas, New Year, Easter and of course birthdays.
Regular senders can be identified from Kyneton and the Great Ocean Road area, Victoria and there is a siginifant collection from Scotland (but not sent from there).
YPRL hold digital copies of the Papers of the Moses Thomas Family held at State Library Victoria
Copyright for these images is Public domain but a credit to the Fay Thomas Collection and YPRL would be appreciated.
Enquiries: Yarra Plenty Regional Library
via
Want to know more about the Hazards of Asbestos? Asbestos is a chronic respiratory condition. The inhaled fibers irritate the lung tissues and cause scarring. Symptoms include shortness of breath and a crackling sound in the lungs when inhaling. The disease is disabling and usually fatal. Workers who have renovated or demolished buildings containing asbestos may be at risk.
Lung cancer which is one of the hazards of Asbestos is the cause of most deaths from asbestos exposure. Mining, milling, manufacturing, and use of asbestos and asbestos products put the worker at risk. Symptoms include a cough, change in breathing and shortness of breath. Smoking in combination with asbestos exposure increases the risk of lung cancer. Symptoms of stage four mesothelioma should be taken very serious as well.
What really is Asbestos?
Asbestos is the name for a group of naturally occurring mineral fibers which are strong and both heat and chemically resistant. Due to these properties, asbestos was commonly used in the past as insulation and fireproofing. It was also used as a component in other building materials. There are three main types of asbestos found in Ireland – chrysotile (white asbestos), amosite (brown asbestos) and crocidolite (blue asbestos). The risk associated with exposure to asbestos relates to the possibility that the fibers within the asbestos-containing material (ACM) can become released into the air and are then inhaled. Breathing in air containing asbestos fibers can lead to asbestos-related diseases (mainly cancers of the chest and lungs). These diseases will not occur immediately and can take from 15 – 60 years to develop.
What are the hazards of asbestos?
When talking about hazards of asbestos, breathing asbestos fibers can cause a buildup of scar-like tissue in the lungs called asbestosis and result in loss of lung function that often progresses to disability and death. Asbestos also causes cancer of the lung and other diseases such as mesothelioma of the pleura which is a fatal malignant tumor of the membrane lining the cavity of the lung or stomach. Mesothelioma cancer is regarded to be one of the deadliest hazards of asbestos. Epidemiologic evidence has increasingly shown that all asbestos fiber types, including the most commonly used form of asbestos, chrysotile, causes mesothelioma in humans.
Where is asbestos found in homes and residential buildings?
Water, hail, and wind can damage structures and contribute to the release of fibers from asbestos-containing materials (see examples below). When these materials dry out, they can break down into very small fibers, which can get into the air and be easily inhaled during cleanup work.
What’s so dangerous about asbestos?
1. Asbestos fibers are very small. If you inhale them, they go deep into your lungs, and stay there, possibly causing disease 10 to 40 years later.
2. Asbestos is (a lung disease) and mesothelioma (a rare type of cancer) are both diseases that only people exposed to asbestos get.
3. You’re 90 times more likely to develop lung cancer if you smoke and are exposed to asbestos than people who do not smoke and are not exposed to asbestos.
Can asbestos be reduced- what can be done to reduce the hazards of asbestos?
These standards reduce the risk to workers by requiring that employers provide personal exposure monitoring to assess the risk and hazard awareness training for operations where there is any potential exposure to asbestos. Airborne levels of asbestos are never to exceed legal worker exposure limits. There is no “safe” level of asbestos exposure for any type of asbestos fiber. If you or a loved one is showing signs of stage four mesothelioma symptoms, it is suggested that they speak with a professional physician as soon as possible.
Methods for Controlling Exposure:
In order to control the hazards of asbestos or its exposure, it is necessary you follow the below tips which are:
>>Avoid disturbing sources of asbestos until proper steps for assessment and control can be implemented.
>>Never smoke, eat, or drink in areas where asbestos exposure is possible.
>>Avoid dry sweeping, shoveling, or other dry clean-up of dust and debris containing asbestos.
>>Wet materials before and during cutting, breaking, or other work that might release asbestos fibers into the air.
>>Wear protective outer clothing that can be removed and cleaned or discarded.
>>If work involving asbestos-containing materials must be done, use a NIOSH-approved respirator to protect workers from inhaling asbestos fibers.
>>Wash exposed parts of the body with soap and water.
>>Avoid carrying asbestos fibers out of a work site where they can later be inhaled by others (e.g., by family members at home).
General Asbestos Awareness
Again the danger or hazards of asbestos is in its release into the air. Each of us has walked on asbestos tiles somewhere at some point in time. There is no harm it that. However, if you take the tile and drill holes in it or take a file to it, you will release asbestos fibers into the air which could enter your lungs. If you or a loved one has recently been diagnosed with stage four mesothelioma, here at the asbestos cancer organization we are fully suited to help you find treatment options and a good mesothelioma attorney.
On the other hand, it would be difficult to do anything with asbestos-based insulation without the risk of getting some of it airborne. This is called being friable.
If the material is positive for asbestos, only a properly trained crew can remove, repair, encapsulate, or enclose it. They must be appropriately trained to remove and dispose of the material. The best thing you can do if you come across some friable material that you believe may be asbestos containing is to stop and ask prior to disturbing it. This is for your safety.
The post Knowing the Hazards of Asbestos and its Prevention appeared first on Mesothelioma Cancer Information.
source umassmedicalschool.com/2019/02/23/knowing-the-hazards-of-... umassmedicalschool.blogspot.com/2019/02/knowing-hazards-o...
This is a photograph from the Forest Marathon festival 2013 which was held in the beautiful Coillte forest of Portumna in Co. Galway, Ireland on Saturday 15th June 2013. The event includes a 10k, a full marathon, a half marathon and two ultra-running events - a 50k and 100k race. The races started at 08:00 with the 100KM, the 50KM at 10:00, and subsequent races at two hour intervals onwards. All events started and finished within the forest with the exception of the half marathon and marathon which started outside of the forest. All events see participants complete 5KM loops of the forest which start and end at the car-park/amenity end of the forest. There is an official Refreshment/Handling Zones at this point on the loop.
The event was organised by international coach Sebastien Locteau from SportsIreland.ie and his fantastic team of volunteers from Galway and beyond. Congratulations to Seb on organising a very professionally run event and an event which is growing bigger and more prestigious with each passing year. There was an incredible atmosphere amongst the runners, the spectators, and the organisers. Hats off to everyone involved.
The marathon, 50KM, and 100KM events are sanctioned by Athletics Ireland and AIMS (the Association of International Marathons and Distance Races). The event has also achieved IAU (International Association of Ultrarunners) Bronze Label status for 2013.
Electronic timing was provided by RedTagTiming: www.redtagtiming.com/
Energy Bars, Gels, Drinks etc were provided by Fuel4Sport: www.fuel4sport.ie/
This is a set of photographs taken at various points on the 5KM loop in the Forest and contains photographs of competitors from all of the events except the 10KM race.
Viewing this on a smartphone device?
If you are viewing this Flickr set on a smartphone and you want to see the larger version(s) of this photograph then: scroll down to the bottom of this description under the photograph and click the "View info about this photo..." link. You will be brought to a new page and you should click the link "View All Sizes".
Overall Race Summary
Participants: Approximately 600 people took part across all of the events which were staged: 10km, half marathon, marathon, 50km, and 100KM.
Weather: The weather was unfortunately not what a summer's day in June should be like - there was rain, some breeze, but mild temperatures.
Course: This is a fast flat course depending on your event. The course is left handed around the Forest and roughly looks like a figure of 8 in terms of routing.
Location Map: Start/finish area on Google StreetView [goo.gl/maps/WWTgD] are inside the parklands and trails
Refreshments: There are no specific refreshments but the race organizers provide very adequate supplies for all participants.
Some Useful Links
Official Race Event Website: www.forestmarathon.com/
The Boards.ie Athletics Forum Thread for the 2013 Event: www.boards.ie/vbulletin/showthread.php?t=2056874371
A GPS Garmin Trace of the Course Profile (from the 50KM event) connect.garmin.com/activity/189495781
Our Flickr Photographs from the 2012 Events: www.flickr.com/photos/peterm7/sets/72157630146344494/
Our Flickr Photographs from the 2011 Events: www.flickr.com/photos/peterm7/sets/72157626865466587/
Title Sponsors Sports Ireland Website: sites.google.com/a/sportsireland.ie/welcome-sports-irelan...
A VIDEO of the Course: www.youtube.com/watch?feature=player_embedded&v=2FLxE...
Google StreetView of the Entrance to Portuma Forest: goo.gl/maps/MX62O
Wikipedia: Read about Portumna and Portumna Forest Park: en.wikipedia.org/wiki/Portumna#Portumna_Forest_Park
Coilte Ourdoors Website: www.coillteoutdoors.ie/?id=53&rec_site=115
Portumna Forest on EveryTrails: www.everytrail.com/guide/portumna-forest-park-woodland-tr...
More about the IAU Bronze Label: www.iau-ultramarathon.org/index.asp?menucode=h07&tmp=...
How can I get a full resolution copy of these photographs?
All of the photographs here on this Flickr set have a visible watermark embedded in them. All of the photographs posted here on this Flickr set are available offline, free, at no cost, at full image resolution WITHOUT watermark. We take these photographs as a hobby and as a contribution to the running community in Ireland. Our only "cost" is our request that if you are using these images: (1) on social media sites such as Facebook, Tumblr, Pinterest, Twitter,LinkedIn, Google+, etc or (2) other websites, web multimedia, commercial/promotional material that you provide a link back to our Flickr page to attribute us. This also extends the use of these images for Facebook profile pictures. In these cases please make a separate wall or blog post with a link to our Flickr page. If you do not know how this should be done for Facebook or other social media please email us and we will be happy to help suggest how to link to us.
Please email petermooney78 AT gmail DOT com with the links to the photographs you would like to obtain a full resolution copy of. We also ask race organisers, media, etc to ask for permission before use of our images for flyers, posters, etc. We reserve the right to refuse a request.
In summary please remember - all we ask is for you to link back to our Flickr set or Flickr pages. Taking the photographs and preparing them for online posting does take a significant effort. We are not posting photographs to Flickr for commercial reasons. If you really like what we do please spread the link around your social media, send us an email, leave a comment beside the photographs, send us a Flickr email, etc.
If you would like to contribute something for your photograph(s)?
Many people offer payment for our photographs. As stated above we do not charge for these photographs. We take these photographs as our contribution to the running community in Ireland. If you feel that the photograph(s) you request are good enough that you would consider paying for their purchase from other photographic providers we would suggest that you can provide a donation to any of the great charities in Ireland who do work for Cancer Care or Cancer Research in Ireland.
I ran in the race - but my photograph doesn't appear here in your Flickr set! What gives?
As mentioned above we take these photographs as a hobby and as a voluntary contribution to the running community in Ireland. Very often we have actually ran in the same race and then switched to photographer mode after we finished the race. Consequently, we feel that we have no obligations to capture a photograph of every participant in the race. However, we do try our very best to capture as many participants as possible. But this is sometimes not possible for a variety of reasons:
►You were hidden behind another participant as you passed our camera
►Weather or lighting conditions meant that we had some photographs with blurry content which we did not upload to our Flickr set
►There were too many people - some races attract thousands of participants and as amateur photographs we cannot hope to capture photographs of everyone
►We simply missed you - sorry about that - we did our best!
You can email us petermooney78 AT gmail DOT com to enquire if we have a photograph of you which didn't make the final Flickr selection for the race. But we cannot promise that there will be photograph there. As alternatives we advise you to contact the race organisers to enquire if there were (1) other photographs taking photographs at the race event or if (2) there were professional commercial sports photographers taking photographs which might have some photographs of you available for purchase. You might find some links for further information above.
Don't like your photograph here?
That's OK! We understand!
If, for any reason, you are not happy or comfortable with your picture appearing here in this photoset on Flickr then please email us at petermooney78 AT gmail DOT com and we will remove it as soon as possible. We give careful consideration to each photograph before uploading.
I want to tell people about these great photographs!
Great! Thank you! The best link to spread the word around is probably www.flickr.com/peterm7/sets