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CSX C40-8W 7788 and AC4400CW 441 on westbound multi-level train S279 at CP 293 in Solvay NY in 2009. The detector reported 310 axles on Track 2.
You'll have to wait for my full thoughts on the iPhone 6/6 Plus and their cameras. And I haven't even looked at all of my photos yet. But I'm very pleased with many of shots I came home with today.
(OK, technically, "the shots I came to the Panera a few Green Line stops away" with.)
Level C of the Frost is the booky section of the library, a place where you can still browse. I was looking for a book on chancery hand, which I never did find, so I have reprojected the stacks into Mercator for ease of navigation. The shelving down here is both Dewey Decimal and Library of Congress, but latitude and longitude might work better.
Level 10 gymnastics girls compete in Fort Worth, Texas on January 27, 2013, in the Metroplex Challenge.
Il castello è stato costruito sulle rovine di un avamposto romano, inglobando una torre del XVI secolo.
La sua edificazione fu voluta nel 1389 da Ugone di Duino, capitano di Trieste, in sostituzione del Castelvecchio risalente al X secolo, di cui sono ancora visibili le rovine su uno sperone roccioso a picco sul mare.
Alla morte di Ugone, il castello andò in eredità a Ramberto di Walsee, fratello della prima moglie, che ne curò l'ultimazione nei primi decenni del 1400. Passò poi agli Asburgo che lo diedero a varie famiglie nobili tedesche e italiane e per ultima alla famiglia Hofer von Hoenfels il cui ultimo discendente, Matthaeus, morì nel 1587 lasciandolo a sua volta in eredità alle uniche due figlie femmine, Ludovika e Maria Clara Orsa.
Entrambe furono spose, una dopo la morte dell'altra, del conte Raimondo della Torre di Valsassina che assunse anche il cognome Hofer, adattato poi in lingua tedesca a von Thurn-Hofer und Valsassina. Il castello resta così ininterrottamente ai von Thurn-Hofer und Valsassina per oltre 250 anni.
Nel 1849 la contessa Theresa von Thurn-Hofer und Valsassina, ultima discendente diretta dei Della Torre di Valsassina ed erede del castello duinese, sposò il principe Egon zu Hohenlohe-Waldenburg-Schilligsfürst dal quale ebbe sei figli.
La quarta figlia, Maria, andò sposa a sua volta nel 1875 a Venezia del principe Alexander von Thurn und Taxis, a sua volta lontano discendente dei Della Torre e figlio di Hugo Maximilian del ramo cadetto Thurn und Taxis-Lautschin-Bohemia, portando in dote il castello.
Da loro nacque nel 1881 Alexander che ereditò a sua volta il castello; creato primo Duca di Castel Duino dal Re d'Italia Vittorio Emanuele III di Savoia, si naturalizzò italiano nel 1923 riassumendo per sé e per i suoi discendenti il cognome di Della Torre e Tasso duchi di Castel Duino, dove tutt'oggi la famiglia abita.
In quel castello lo scrittore e poeta Rainer Maria Rilke ideò e iniziò la composizione delle Elegie duinesi mentre era in visita dalla Principessa Maria della Torre e Tasso (nata principessa di Hohenlohe). Rilke successivamente dedicò la sua opera alla principessa, che fu una dei suoi maggiori patroni.
A ricordo dell'evento è stato intitolato al poeta anche un sentiero panoramico - il sentiero Rilke - lungo circa 2 km. Inaugurato dopo i lavori di restauro nel 1987, corre alto sul costone roccioso tra Duino e la baia di Sistiana, con splendidi scorci sulla Riserva naturale delle Falesie.
We finally turned Ava’s car seat to face the front that day and tested Evan to see if he was tall enough to ditch the booster seat. Spoiler alert: he was not quite tall enough. He was very very close, but he couldn’t quite sit all the way back and still have his feet flat on the floor. We ended up trading the high-backed booster for the smaller one for now, so at least there was a little sense of progress made.
Uns dels edificis més alts de la City of London. A la planta 42, tot pujant amb un ascensor exclusiu, hi ha un bar amb parets de vidre i unes vistes impressionants. El preu de les consumicions també és impressionant.
Level 42
Uno de los edificios más altos de la City of London. En la planta 42, a la cual se accede mediante un ascensor exclusivo, hay un bar con paredes de vidrio y unas vistas impresionantes. El precio de las consumiciones también es impresionante.
Level 42
One of the tallest buidings in the City of London. You can take a direct lift up to the 42th floor. There is an amazing bar with glass walls and awesome views. The prices are also awesome.
Image ©Licensed to Jon Parker Lee
Students at Manchester High School for Girls celebrate their A-Level results on the morning of Thursday 18 August 2016. Pictured, Sarah Strickland (3 A*s)
Looks better pressing L
Thanks for your visit and comments.
Please don't use this image on websites, blogs or other media without my explicit permission.
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Leaving Poppleton station on the train to Harrogate. The level crossing gates are stilll operated manually by the signalman.
This is low level but looking up. As was not sure it would qualify, posting it as General and still looking for my low level subject.
The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.
The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.
Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.
Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.
ETYMOLOGY
The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"
ECOLOGY
The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.
The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.
GEOLOGY
The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.
During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.
Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.
During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.
HYDROLOGY
The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).
Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:
- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.
- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.
The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.
The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.
LAKES
The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.
Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.
The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.
IMPACT ON CLIMATE
The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.
RELIGIOUS OF THE REGION
In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.
Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.
A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.
RESOURCES
The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.
Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.
Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).
The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).
CULTURE
There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).
The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).
The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).
WIKIPEDIA
I blame that Kulu. I was quite happy on the level but he kept wittering on about forbidden fruit.
The original parish church of Broadway actually lies almost a mile outside of the village. Nevertheless, the Church of St Eadburgha has been a Christian place of worship since the 12th century and continues to be a significant aspect of village life. The dedication of a Christian church to Eadburgha is not common. Eadburgha was the grand-daughter of Alfred the Great. The story is told that as a child Eadburgha was asked to choose between receiving jewels or her own Bible, she chose the Bible.
The Church of St Eadburgha is listed as Grade I by English Heritage (Building ID: 400976). The current structure was built circa 1400 but there are elements that remain of the original 12th century building.
Farranfore to Valentia Railway Line - MP Farranfore Junction 2 1/4.
Level Crossing in Firies, Kerry 23rd June 2012, looking towards Farranfore.
The view from the end of the closed lower level of the 152m long Whitby West Pier extension of 1905-14, towards the West Lighthouse.
The 25.3m tall West Lighthouse, completed in 11 weeks in 1831, stands on the main West Pier rebuilt in 1814. It contained a green (starboard) harbour entrance light which was visible for more than 16km for over 80 years (until being retired from navigation use in 1914 when the pier extension light was brought into service).
The college was founded by the Jesuits in 1582, which became the foundation for the University of Fribourg.
A Classic autumn view of Somerset Levels. It is common to find mist on the Levels after a cold, clear night during spring and autumn. As the sun rises in the morning layers of mist start fleeting across the plains towards the coast.
I decided to go with a b&w approach this time as the color version was a bit too yellow. Also b&w improved the visibility slightly making the mansion in the foreground appear clearer.
Thanks for views & comments.
DB Class 66 Co-Co 66143 heads through a rain soaked Tamworth on 6M13 01.04 Dollands Moor - Ditton, aluminium in cargowaggons and containers from Neuss, Germany.
9th May 2019
1Q16 09.31 Derby RTC - Marylebone - Derby RTC (Radio Survey Train) speeds through Tamworth. DRS Class 37 Co-Co 37604 leading, 37611 rear.
11th August 2015
Bloxwich Signal Box seen in this picture controls the level crossing, the two track Cannock lines (between Walsall and Rugeley Trent Valley) through this location, and the sidings. The sidings themselves have remained unused for several years, and the company owning the private siding off to the left of the picture have gone into administration.
Several people have commented to me that the signal box looks like the model formerly supplied by Hornby in its catalogue of OO gauge accessories.
The Somerset Levels are a coastal plain and wetland area of Somerset, England, running south from the Mendips to the Blackdown Hills.
The Somerset Levels have an area of about 160,000 acres and are bisected by the Polden Hills; the areas to the south are drained by the River Parrett, and the areas to the north by the rivers Axe and Brue. The Mendip Hills separate the Somerset Levels from the North Somerset Levels. The Somerset Levels consist of marine clay "levels" along the coast and inland peat-based "moors"; agriculturally, about 70 per cent is used as grassland and the rest is arable. Willow and teazel are grown commercially and peat is extracted.