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Trumpet/Mermaid One-Shoulder Floor-Length Tulle Charmeuse Evening Dress With Lace Flower(s)
www.jjshouse.com/Trumpet-Mermaid-One-Shoulder-Floor-Lengt...
Built: 1973, Vancouver
Overall Length:33.93 m (111'4")
Maximum Displacement:371 tonnes
Car Capacity: 16
Passenger & Crew Capacity: 125
Maximum Speed:11 knots
Horsepower:680
Amenities: None
Route: Various inter-island and northern routes.
The Nimpkish is a special vessel in the BC Ferries fleet. She is the shortest ferry, at just under 34 meters. She has the lowest car capacity (16 - tied with the Mill Bay) and passenger capacity (133). She also is one of the most well-travelled ferries in the fleet, despite being only used for a relief vessel in recent years. The Nimpkish has served on routes ranging from places like Nanaimo, Bella Coola, and Cortes Island. She has three sister ships that still operate on the coast, but not as part of the BC Ferry fleet: the Nicola, Albert J. Savoie, and the Garibaldi II. The latter vessel could be returning to BC Ferries in early 2006.
Today
Your best chance of seeing the Nimpkish would be to take the ferry from Powell River to Blubber Bay, Texada Island. The Nimpkish is tied up at Blubber Bay for much of the year, alongside the Tachek. However, the Nimpkish is often used as a relief vessel on minor routes, especially in the winter time when ferries are most likely to go in for maintenance and refits. She is the main relief vessel on the Heriot Bay (Quadra Island) - Whaletown (Cortes Island) route, replacing the Tenaka when needed. She can also be sometimes found as a replacement vessel on the Denman Island - Hornby Island route and the Port McNeill - Sointula - Alert Bay route. On busier routes, the Nimpkish will sometimes run alongside another relief vessel during busy times when the larger regular vessel is out of service. nimpkish At other times, the Nimpkish will be called up to the north coast when the Queen of Prince Rupert is out of service. The Nimpkish connects some of the remote coastal communities with the Queen of the North on the regular Inside Passage run.
Surrey, British Columbia, Canada
Clipper Newark
-Built 2011
-Gross Tonnage 12795
-Dead weight 17273 T
-Length and Breadth
144.87m 22m 475Ft 72Ft
-Home Port_Nassau
Seen From Rte 218 Overlook
Storm King Mtn Overlook On Rte 218 On Storm King Mountain near Cornwall N.Y. Overlooking the Hudson River.
-Best Route to Overlook Rte 293 to Rte 218 Follow signs for West Point Golf Course.
-The Storm King Highway is a three-mile (4.8 km) segment of New York State Route 218 (NY 218) between Lee Road in the Town of Highlands at the south end and the Cornwall-on-Hudson village line in Orange County, New York, in the United States. It was built in 1916 and added to the National Register of Historic Places in 1982 in recognition of its accomplishment in civil engineering.
It is so named because it winds around the steep slopes of Storm King Mountain near its north end of the Hudson Highlands on the west bank of the Hudson River. Here it reaches heights of up to 420 feet (130 m) above the water, with panoramic views of the river and surrounding mountains such as Breakneck Ridge and Bull Hill.
Several small pullouts allow drivers to stop and enjoy the view. When originally built it took 22 miles(34 km) off the trip [1] between Cornwall and Newburgh to its north with Highland Falls and West Point to its south. It remains used by commuters today.
Madrid Maersk (largest container vessel (in tdw) in the world)
Length 399m, beam 58.60m, BRZ 214.286, tdw 210.000, TEU 20.568
One sailor on the middle of the bow!
Bellini
Length 93.97m, beam 12,5m, tdw 3046,year built 2000
A disused length of platform at Blaydon can be seen on the left as Class 156 156494 heads away from Blaydon towards Newcastle with 1N56 0741 Dumfries to Newcastle. There it will layover for just over two hours before entering a Tyne Valley circuit which sees it operating to Carlisle, to Morpeth and finally back to Carlisle where it will be attached to another Class 156 to run to Glasgow Central via the GSWR line enabling it to return to Corkerhill depot. In the distance can be seen the still operational Blaydon signal box which was sited at the junction of the lines to Newcastle via Dunston and via Scotswood. 12th May 2022.
Specs:
Overall length: 21.5cm / 8.5"
Cutting edge: 9.5cm / 3.7"
Steel: S30V
Handle: Bone linern micarta bolsters, black linen micarta handle, red liner and SS tubes.
Female found drowned on July 16th, 2008. Body length: 8 mm. Forewing length: 5.7 mm. Ovipositor length (visible part): 3.23 mm. Ovipositor 1.25x times as long as hind tibia. Ovipositor sheaths: 2.40 mm. Ovipositor sheaths 0.93 times as long as hind tibia. HEAD: Antenna with 23 flagellar segments, basal 5 flagellomeres black, 4 central flagellomeres ivory white and the 14 apical flagellomeres black. F1 length/width ratio: 29:4=7.25. F3 length/width ratio: 21:3= 7. Clypeus narrow and obviously convex, apically rounded and separated from the face by a well-defined groove. Clypeus with a medial tubercle or tooth. Mandible twice its width at midpoint. Mandible two-toothed, tooth with the same length. Cheeks 0.72 times as long as the width of the mandibular base. Frons not depressed. MESOSOMA: Mesopleuron and metapleuron distinctly wrinkled. Mesosoma black, except subalar prominence and the tip of scutellum which are ivory white. Mesoscutum convex, relatively narrow, lacking transverse rugae, with notaulices extending beyond the centre of mesoscutum. Mesoscutum densely sculpted, matte, with fine points. Mesopleuron with a sinuated sternaulus covering almost all its length. Propodeum with carinae, but only with two transverse carinae, basal longitudinal carinae unclear or unknown. Area horizontalis 1.3 times as long as area petiolaris. Propodeal spiracles almost rounded, length/width ratio less than 1,1. Metanotum without sublateral posterior projections. Postpectal carina not complete, laterally present, absent in front of mid coxae. METASOMA: Sclerotized part of 1st sternite extending to the posterior third of the segment. 1st metasomal segment narrow basally and gradually widened apically, without a basal lateral tooth. First metasomal spiracle beyond the middle, at 0.58x the length of first metasomal segment. Postpetiolus with not very noticeable points. Second metasomal tergite with very dense microsculpture and fairly dense haired. Second tergite as long as its maximum width seen from above. Seventh tergite with a big ivory spot. Eight tergite dorsally ivory white. Ovipositor sheaths thinner and flexible. Lower half of the ovipositor toothed apically. Ovipositor tip (from the notch to the apex) 3.0 times as long as high. WINGS: Fore wings with 2m-cu vein present, with one bulla, subvertical, reaching subdiscoidal vein in a right angle. Fore wing with an areolet with convergent sides. Subdiscoideus vein reaching postnervulus about its middle. Hindwing with the medial part of the medial vein slightly curved and moderately curved at the apical 0.6x part. Hind wing with axillary vein parallel to the anal margin, its apex curved to the margin. LEGS: Hind coxa with a weakly printed area. Legs mostly deep brown, with black coxae and other parts also black. Femur III length/width ratio: 5.0. Hind tibia length: 2.57 mm. Second segment of the tarsi 1.29 times as long as the fifth segment.
Kyla Pratt at the 4th Annual BET Awards - Arrivals.Kodak Theatre, Hollywood, CA.June 29, 2004 .© Sara De Boer
A former railway station building from the 19th century. It's the worlds oldest surviving monumental railway architecture.
The station opened in 1838. When New St Station was finished in 1854, Curzon St stopped being a passenger station, put holiday trips continued until 1893. It remained in use until 1966 as a goods station. It was called Birmingham Station until 1852 when they added Curzon St.
It is Grade I listed but isn't in use at the moment.
Curzon Street Station was the terminus of the London and Birmingham Railway which started at London Euston.
The line was engineered by Robert Stephenson
London and Birmingham Railway - Wikipedia
After ceasing being a station for passengers, it was later the called British Rail Goods Office. But it hasn't been that in a very long time.
It was formerly listed as the Railway Goods Office.
1838, by Philip Hardwick. The original terminus to the London-Birmingham railway Ashlar. In the Ionic style. Three storeys, 3 bays and austerely cubic. Portico of 4 really giant Ionic columns to the dentilled entablature with attic. Behind, a carved achievement of arms and swags over the glazed tympanum above the great panelled doors and 2 ground floor single windows. The first floor with 2 windows with blind balconys and cornices on brackets. Second floor with 3 windows in flat surrounds. All windows sashes mostly with glazing bars. To the rear, 2 engaged Ionic columns between square piers. To the left, a length of wall with intermittent balustrading.
Nikon D200
Focal Length: 70mm
Optimize Image: Custom
Color Mode: Mode II (Adobe RGB)
Long Exposure NR: Off
High ISO NR: On (Low)
2008/02/20 20:22:51
Exposure Mode: Aperture Priority
White Balance: Auto
Tone Comp.: Auto
Compressed RAW (12-bit)
Metering Mode: Center-Weighted
AF Mode: AF-S
Hue Adjustment: 0°
Image Size: Large (3872 x 2592)
1/25 sec - F/5.6
Flash Sync Mode: Not Attached
Saturation: Auto
Color
Exposure Comp.: -1.3 EV
Sharpening: Medium high
Lens: 35-70mm F/2.8D Nikkor
Sensitivity: ISO 400
Image Comment: © Gerard Prins (+56) 22758 7209
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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1987 Perini Navi Paz (antes «Andrómeda la Dea»)
Eslora total / Length overall: 141 ft / 43 m
Eslora de flotación (a plena carga) LWL full load: 113.9 ft / 34.5 m
Manga (máxima) Beam (max): 29 ft / 8.8 m
Calado (killa arriba) / Draught (keel up): 20.79 ft / 6.3 m
Calado (quilla abajo) / Draught (keel down): 9.24 ft / 2.8 m
Motores/ Engines: 2 MTU 183 TE 91
Maximum power: 2 x 441 kW
Hull construction: Steel
Construcción de la superestructura: Aluminio
Superstructure construction: Aluminium
Desplazamiento a plena carga / Displacement full load: 296 t
Velocidad a máxima / Speed at maximum power: 13 kt
Capacidad de combustible / Fuel capacity: 27,400 lt
Agua dulce / Fresh water: 10,900 lt
Altura máxima delmastil / Main mast height above DWL: 148.5 ft / 45 m
Mizzen mast height above DWL: 111.5 ft / 33.8 m
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Arquitecto / Naval Architecture: Perini Navi
Constructor / Builder: Perini Navi - Viareggio, Italy
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Joplin is a BEAUTIFUL, big, handsome boy with a very laid-back personality. He has gorgeous medium length fur, which is black on top and has a unique smokey-grey undercoat. And he has the most stunning big, bright, light-green eyes. Very pretty! He's such a good boy and interactive - he'll chat with you. When he's being petted, he'll reach up and 'make biscuits' in the air for attention. When he's very happy and content, he'll purr up a storm and he drools. Just a charming quirk he has!
This gorgeous boy is estimated to be around 4-5 years old, has been neutered and is front de-clawed. He has been vaccinated, blood tested and is negative for Feline Leukemia and FIV, has been flea treated and de-wormed. This big boy is ready to go and start a new chapter in his life. He's such a great cat and will make someone a wonderful pet.
And yes, Joplin came from the tornado devastated area. A vet from Kansas City had rushed down during the initial days of the disaster to volunteer and provide relief work at the shelter. The vet saw beautiful Joplin, and a little old Papillon dog (later named Janice, who is vision impaired and was needing dental work). Joplin had a very bad cold, had been sneezing a lot, and was so congested that he was not eating. He was placed on antibiotics, given fluids, given steam treatments for the congestion, and his food intake was monitored. He bounced back quickly with medical care, and is now over his cold.
The Joplin Humane Society is a kill facility (they have suspended this policy at the moment to help rehome displaced animals from the tornado) and the vet had fallen in love with a few of their 'special needs' animals that were already at the shelter prior to the tornado. These lucky pets are getting the TLC they need and a second chance at a new life!
Please consider adopting this gorgeous boy. His dog-friend Janice, has already been placed in her new home. Joplin's adoption fee is $50.
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*Feature-length article on Alex Kerr's foundation Iori, which restores heritage houses, primarily in Kyoto, and converts them to living space and culture centers.
*Interview with Yamai Tsunao, a young Noh actor who is working to bring the dramatic art more mainstream attention and appreciation.
*an essay on black cultural revival in America over the last 50 years and its interesting connection with Japanese culture.
*interview with and photospread by Ikeya Tomohide, who shoots stunning and often erotic pictures of Butoh dancers underwater.
*travel article on Kochi
*write-up on the Amami-Oshima island singer Kizuki Minami and her recent accomplishments in music
*the usual: art, photography, poetry, book reviews, Fair Trade topics and more...
The art and most of the photography is only available in the print version. For more information:
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Description
•Made from 95% Combed Cotton 5% Elastane (for stretch) Fabric
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A Parisian hairstylist cuts through Magi B's pony tail so it can be donated to Pantene Beautiful Lengths!
Name: M/Y A
Length: 119m
World's largest yacht number: 23
Shipyard: Blohm + Voss
Price: 255 000 000€
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Name: S/Y A
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The full length of the former 13th Street in San Francisco can be seen at the bottom of this photo, between Mission Street and Bryant Street. Only a couple stubs of this street still exist, on either side under the Central Freeway, with Division Street running directly under the freeway and dividing the stubs.
This photo is a selection from a composite image of aerial photographs at the SF Public Library, taken in 1938 and assembled here at www.davidrumsey.com.
Built: 2006
Dimensions: 130 feet length/ 25 feet beam/ 6 feet draft
Class: First class
Type: Motor Yacht
Capacity: 16 guests
Crew: 7 crew members + 1 naturalist multilingual guide
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Facilities: Bar, dining room, salon and sun deck. All cabins and public areas are fully carpeted. Snorkeling gear available for rent.
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Schweiz / Wallis - Aletschgletscher
The Aletsch Glacier (German: Aletschgletscher, German pronunciation: [ˈalɛtʃˌɡlɛtʃɐ]) or Great Aletsch Glacier (Grosser Aletschgletscher) is the largest glacier in the Alps. It has a length of about 23 km (14 mi) (2014), has about a volume of 15.4 km3 (3.7 cu mi) (2011), and covers about 81.7 km2 (31.5 square miles) (2011) in the eastern Bernese Alps in the Swiss canton of Valais. The Aletsch Glacier is composed of four smaller glaciers converging at Konkordiaplatz, where its thickness was measured by the ETH to be still near 1 km (3,300 ft). It then continues towards the Rhône valley before giving birth to the Massa. The Aletsch Glacier is – like most glaciers in the world today – a retreating glacier. As of 2016, since 1980 it lost 1.3 kilometres (0.81 mi) of its length, since 1870 3.2 kilometres (2.0 mi), and lost also more than 300 metres (980 ft) of its thickness.
The whole area, including other glaciers is part of the Jungfrau-Aletsch Protected Area, which was declared a UNESCO World Heritage Site in 2001.
Geography
The Aletsch Glacier is one of the many glaciers located between the cantons of Bern and Valais on the Bernese Alps located east of the Gemmi Pass. The whole area is considered to be the largest glaciated area in western Eurasia. The Fiescher and Aar Glaciers lying on the east have similar extensions.
Except the Finsteraarhorn, all the highest summits of the Bernese Alps are located within the drainage basin of the glacier. The Jungfrau and Mönch constitute the northern boundary; the Gross Fiescherhorn and Gross Wannenhorn lie on its east side; finally the culminating point, the Aletschhorn (4,193 m (13,757 ft)) is located on the west side.
Before reaching the maximum flow, four smaller glaciers converge at Konkordiaplatz:
From the western mouth flows the Grosser Aletschfirn, which runs along the northern foot of the Aletschhorn and Dreieckhorn. The Grosser Aletschfirn is supplied from the north by three notable firns: the Äbeni Flue-Firn, the Gletscherhornfirn, and the Kranzbergfirn. All of these firns have their starting points at around 3,800 m (12,500 ft). From the Äbeni Flue-Firn to the Konkordiaplatz, the Grosser Aletschfirn is 9 km (5.6 mi) long and is on average about 1.5 km (0.93 mi) wide. On the west, the Grosser Aletschfirn connects with the Langgletscher over the 3,158 m (10,361 ft) high glacier pass, the Lötschenlücke, into the Lötschental.
From the northwestern mouth flows the Jungfraufirn. This firn in fact represents the straight continuation of the Aletsch Glacier, yet is the shortest of the four tributary glaciers. It has its origin on the southern flank of the Mönch and at the eastern flank of the Jungfrau with the Jungfraujoch in-between. Up to the Konkordiaplatz, the Jungfraufirn is a scarce 7 km (4.3 mi) long, and returns to flank the Kranzberg in the west and the Trugberg in the east. At its highest point, it is 2 km (1.2 mi) wide, and further down it is still a good 1 km (0.62 mi) wide.
From the northern mouth flows the Ewigschneefäld ("Eternal snow field"), where its starting point takes the east flank of the Mönch. In an elbow, it flanks from Trugberg in the west and the Gross Fiescherhorn and Grünhorn in the east, flowing on to the Konkordiaplatz. Up to here, it is about 8 km (5.0 mi) long and averages about 1.2 km (0.75 mi) wide.
The mouth at the Konkordiaplatz it follows over a rise with a descent from 25 to 30 percent; here, the glacier is sharply split. Against the north is the Ewigschneefäld over the snow-covered pass of the Unners Mönchsjoch (3,518 m (11,542 ft)), connected with the catchment area of the Ischmeer (Wallis German for "Ice Sea"). Through the Obere Mönchsjoch (3,624 m (11,890 ft)) between the Mönch and the Trugberg stands a connection to the Jungfraufirn.
From the east, the smallest firn arrives at the Konkordiaplatz: the Grüneggfirn. Its northern arm begins below the Grünegghorn (3,860 m (12,660 ft)). The southern arm collects its snow and ice in the pot flanked by the Wyssnollen, Fiescher Gabelhorn (3,866 m (12,684 ft)), and the Chamm. Between the peaks Wyssnollen and Grünhörnli another glacier pass, the Grünhornlücke (3,279 m (10,758 ft)), connects to the Fieschergletscher. The Grüneggfirn enters the Konkordiaplatz in a gap between the mountainsides Grünegg to the north and the Fülberg to the south. On the western side of the Fülberg the Konkordia hut (mountain hut) overlooks the whole Konkordiaplatz at an altitude of 2,850 m (9,350 ft).
South of Konkordiaplatz, the glacier runs towards the valley of the Oberwallis (Upper Valais); on the east side, near Bettmeralp, lies a small glacier lake, Märjelensee (2,301 m (7,549 feet)); from the western side used to enter the Mittelaletschgletscher, but since the end of the 20th century the connection with the Aletsch Glacier has been lost. Further down, until about 1880, the Oberaletschgletscher did also enter the Aletsch Glacier at its mouth. But since then both glaciers have been retreating so far that they do not connect anymore (the Upper Aletsch Glacier did retreat about 1.3 km (0.81 mi) from its connecting point with the Aletsch Glacier), but both serve now only as the source of the river Massa. The river flows through the Lake Gibidum (a reservoir, and coincidentally representing the glacier's mouth region in the 19th century, which is a retreat of more than 4 km (2.5 mi)) and a gorge of the same name before reaching the Rhône near Brig.
Tourism
The area of the Aletsch Glacier and some surrounding valleys is on the UNESCO World Heritage list, thus it is protected and the facilities are mostly restricted to the external zones. The region between Belalp, Riederalp and Bettmeralp (which is called Aletsch Region) in Valais gives access to the lower part of the glacier. The Bettmerhorn and Eggishorn are popular view points and are accessible by cable car. The Massa river can be crossed since 2008 by a suspension bridge, thus allowing hikes between the left and the right part of the glacier.
The Jungfraujoch railway station (3,450 m) gives a direct access to the upper Aletsch Glacier as well as the normal route to the Jungfrau. It can be reached only from Interlaken in the canton Bern. Hiking paths pass the Konkordia Hut or the Hollandia Hut, eventually reaching other glaciers in the massif.
On the Riederfurka, at 2,065 metres between Riederalp and the glacier, is located the historic Villa Cassel, former summer residence of many famous and influential guests from the worlds of politics and finance. The house is now one of the centers of the environmental organization Pro Natura, which hosts a permanent exhibition about the site.
Panorama
Also at the mouth of the Konkordiaplatz from the east is the small but important Grüneggfirn (3 km long and averaging 600 m wide). This firn is connected in the over the glacier pass Grünhornlücke (3280 m high) to the Fiescher Glacier in the east.
From the Konkordiaplatz, the Aletsch Glacier has a width of approximately 1.5 km and moves at a rate of 180 m per year to the southeast on course with the Rhône valley, bordering the Dreieckhorn in the west and the great Wannenhorn in the east. It then takes a great right turn and bends ever closer to the southwest, running through the edge of the Eggishorn and Bettmerhorn of the Rhône valley. The lowest part of the great Aletsch Glacier is largely covered with detritus of the lateral and medial moraines. The glacier's toe currently lies about 1560 m high, far beneath the local tree line. From it springs the Massa stream, which flows through the Massa Canyon and is used to generate hydroelectric power. It continues through the upper half of the Brig, eventually entering into the Rhône.
The great Aletsch Glacier shows considerable ice cover. At the Konkordiaplatz, it has an ice cover of more than 900 m, but as it moves to the south, the greater part of the ice melts, gradually decreasing the cover to around 150 m.
The characteristically dark medial moraine, situated almost in the middle of the glacier, runs protracted in two bands from the Konkordiaplatz along the whole length to the glacier's toe-zone. This medial moraine is collected from the ice of three large ice fields, which all run together. The westernmost medial moraine has been named the Kranzbergmoräne, and the easternmost carries the name Trugbergmoräne.
Formation and evolution
The Aletsch Glacier resulted from the accumulation and compaction of snow. Glaciers generally form where snow and ice accumulation exceed snow and ice melt. As the snow and ice thicken it reaches a point where it begins to move due to a combination of gravity and pressure of the overlying snow and ice.
During the last glacial periods, the Aletsch Glacier was much larger than now. 18,000 years ago the lower part of the ridge, between Riederalp and the glacier, was completely covered by ice. Only the summits of the Bettmerhorn, Eggishorn and the Fusshörner were above the glacier. After an important retreat, the glacier again advanced 11,000 years ago during the last glacial period. The glacier reached the Rhône valley, and its ice the Riederfurka. Remaining moraines are still visible in the Aletsch Forest.
Since the last glaciation, the glacier generally retreated. However slight climatic changes happened and, in 1860, the glacier was 3 km longer and the ice level 200 m higher.
As for many other glaciers, records show a major longer-term retreat trend. The Aletsch Glacier receded by 3.2 km (2.0 mi) since 1870, including 1.3 km (0.81 mi) since 1980.[6] A record retreat of 114.6 metres (376 ft) happened in 2006 alone.
Since the end of the Little Ice Age in 1850 the glacier has lost 20 percent of its ice mass, considerably less than other glaciers in Switzerland, which have lost up to 50 percent. This is explained with the large size of the Aletsch Glacier, which reacts much slower to climate change than smaller glaciers. It is however estimated that, by 2100, the glacier will have only one tenth of its 2018 ice mass.
Photo opportunity
On August 18, 2007, photographer Spencer Tunick used hundreds of naked people in a "living sculpture" on the Aletsch Glacier in a photo shoot which he said was intended to draw attention to global warming and the shrinking of the world's glaciers. The temperature was about 10 °C (50 °F) at the time of the photo shoot. The 600 participants on the shrinking glacier said that they had volunteered for Tunick (a collaboration with Greenpeace) to let the world know about the effects of global warming on the melting Swiss glaciers.
(Wikipedia)
Der Grosse Aletschgletscher ist der flächenmässig grösste und längste Gletscher der Alpen. Er befindet sich auf der Südabdachung der Berner Alpen im Schweizer Kanton Wallis. Die Länge des Gletschers beträgt 22,6 km, die Fläche wird mit 78,49 km² angegeben. Der Aletschgletscher entwässert über die Massa in die Rhone. Die Fläche des gesamten Einzugsgebiets der Massa beträgt 195 km², wovon 1973 etwa zwei Drittel vergletschert waren. Oft werden bei der Flächenangabe der Ober- und Mittelaletschgletscher einbezogen, da diese früher mit dem Grossen Aletschgletscher verbunden waren. Die gesamte vergletscherte Fläche einschliesslich dieser Gletscher betrug 1973 etwa 128 km², für das Jahr 1863 wird eine Fläche von 163 km² angenommen.
Ursprung am Konkordiaplatz
Der Ursprung des Grossen Aletschgletschers liegt in der rund 3800 m hoch gelegenen Jungfrau-Region. Am Konkordiaplatz (♁645905 / 150101), einer 6 km² grossen und nur wenig geneigten Eisfläche, fliessen drei mächtige Firnströme zusammen:
Von Westen mündet der Grosse Aletschfirn, der entlang dem Nordfuss von Aletschhorn und Dreieckhorn fliesst. Der Grosse Aletschfirn wird von Norden her durch drei weitere bedeutende Firne gespeist, nämlich durch den Ebnefluhfirn, den Gletscherhornfirn und den Kranzbergfirn. Alle diese Firne nehmen ihren Ausgangspunkt auf rund 3800 m ü. M. Einschliesslich des Ebnefluhfirns hat der Grosse Aletschfirn bis zum Konkordiaplatz eine Länge von 9 km und ist durchschnittlich fast 1,5 km breit. Gegen Westen ist der Grosse Aletschfirn über den 3173 m ü. M. hohen Gletscherpass der Lötschenlücke mit dem Langgletscher verbunden, der ins Lötschental abfliesst.
Von Nordwesten mündet der Jungfraufirn, der zwar die gerade Fortsetzung des Aletschgletschers darstellt, jedoch der kürzeste der drei Tributärgletscher ist. Er hat seinen Ursprung an der Südflanke des Mönchs, am Jungfraujoch und an der Ostflanke der Jungfrau. Bis zum Konkordiaplatz legt der Jungfraufirn eine Wegstrecke von knapp 7 km zurück und wird dabei im Westen vom Kranzberg, im Osten vom Trugberg flankiert. Er ist in seinem oberen Teil 2 km, weiter unten noch gut 1 km breit.
Von Norden mündet das Ewigschneefeld, das seinen Ausgangspunkt an der Ostflanke des Mönchs nimmt und in einem Bogen, flankiert vom Trugberg im Westen sowie dem Gross Fiescherhorn und dem Grünhorn im Osten, zum Konkordiaplatz fliesst. Bis hierher ist es ungefähr 8 km lang und durchschnittlich 1,2 km breit. Die Mündung in den Konkordiaplatz erfolgt über einen Steilhang mit einem Gefälle von 25 bis 30 %; der Gletscher ist hier stark zerklüftet. Gegen Norden ist das Ewigschneefeld über den firnbedeckten Pass des Unteren Mönchsjochs (3529 m ü. M.) mit dem Einzugsgebiet des Unteren Grindelwaldgletschers verbunden. Durch das Obere Mönchsjoch (3627 m ü. M.) zwischen dem Mönch und dem Trugberg besteht eine Verbindung zum Jungfraufirn. Ferner mündet am Konkordiaplatz von Osten noch der wesentlich kleinere Grüneggfirn (3 km lang und durchschnittlich 600 m breit). Dieser ist nach Osten über den Gletscherpass der Grünhornlücke (3280 m ü. M.) mit dem Fieschergletscher verbunden.
Weiterer Verlauf
Vom Konkordiaplatz aus bewegt sich der Eisstrom mit einer Breite von ungefähr 1,5 km und mit einer Geschwindigkeit von bis zu 180 Metern pro Jahr nach Südosten in Richtung Rhonetal, gesäumt vom Dreieckhorn im Westen und dem Gross Wannenhorn im Osten. Er zeichnet dann eine grosse Rechtskurve und biegt immer mehr nach Südwesten ab, nun durch den Grat des Eggishorns und Bettmerhorns vom Rhonetal getrennt. Der unterste Teil des Grossen Aletschgletschers ist weitgehend durch das Geschiebematerial von Seiten- und Mittelmoränen bedeckt. Die Gletscherzunge liegt derzeit auf rund 1'560 Meter Höhe, weit unterhalb der lokalen Waldgrenze. Aus ihr entspringt der Bach Massa, welcher nach der Massaschlucht und einer Nutzung in einem Wasserkraftwerk, in Bitsch, oberhalb von Naters, in die Rhone (Rotten) fliesst.
Der Grosse Aletschgletscher weist beachtliche Eisdicken auf. Am Konkordiaplatz hat der Gletscher eine Eisdicke von mehr als 900 Metern, gegen Süden nimmt die Mächtigkeit des Eises allmählich auf rund 150 m ab. Charakteristisch sind die beiden dunklen, fast in der Mitte des Aletschgletschers gelegenen Moränenspuren, welche sich ab dem Konkordiaplatz auf der gesamten Länge bis in den Zungenbereich hinziehen. Es sind die Mittelmoränen, die das Eis der drei Hauptfirne voneinander trennen. Die westliche Mittelmoräne wird auch Kranzbergmoräne genannt, die östliche trägt den Namen Trugbergmoräne.
Gletscherschwankungen
In seinem Hochstadium während der Kleinen Eiszeit um die Mitte des 19. Jahrhunderts erstreckte sich der Grosse Aletschgletscher noch rund 2,5 km weiter talabwärts. Aufgrund der allgemeinen Erwärmung seit etwa 1870 hat er besonders unterhalb des Konkordiaplatzes massiv an Volumen eingebüsst und sowohl an den Seiten als auch im Zungenbereich Flächen von mehreren Quadratkilometern freigegeben. Der einstmalige, in der Neuzeit höchste Gletscherstand kann gut an den noch fast vegetationslosen Seitenmoränen abgeschätzt werden. Seit 1850 hat die Eisdicke um teilweise über 100 m abgenommen. Früher waren auch die Eisströme des Oberaletschgletschers und des Mittelaletschgletschers direkt mit dem Grossen Aletschgletscher verbunden.
In der Senke zwischen dem Strahlhorn und dem Eggishorn liegt der Märjelensee, der im 19. Jahrhundert beim Gletscherhochstand zu einem Gletscherrandsee aufgestaut wurde. Seine wiederholten plötzlichen Ausbrüche durch Gletscherspalten verursachten immer wieder starke Schadenshochwasser der Massa hin zum Rhonetal.
Gegen kurzfristige Klimaschwankungen ist der Gletscher aufgrund seiner grossen Masse relativ immun. Während viele andere Gletscher Ende der 1970er Jahre bis Anfang der 1980er Jahre vorstiessen, reagierte der Aletschgletscher auf die vorübergehende Abkühlung kaum – ebenso wenig wie auf die warmen Jahre seit 1983. Aufgrund der zunehmend extremen Hitze der letzten Jahre zieht er sich aber nun doch – wie alle übrigen Alpengletscher – deutlich verstärkt zurück.
Die relative Trägheit in seinen Reaktionen auf Klimaschwankungen macht den Aletschgletscher auch zu einem idealen Untersuchungsobjekt zur Erforschung der Klimaentwicklung im Alpenraum. Die Längenschwankungen des Aletschgletschers in der Vergangenheit dürften sogar eine Rekonstruktion aller grösseren Klimaveränderungen der letzten 3200 Jahre erlauben. Die Bestimmung der verschiedenen Längenstadien des Aletschgletschers in der Vergangenheit erfolgt durch die Radiokohlenstoffdatierung fossiler Baumstämme, die der Gletscher bei einem früheren Vorstoss einmal überfahren haben muss und nun während seines aktuellen Rückzuges wieder freigibt. Der Befund fossiler Böden und von Wurzelwerk garantiert dabei, dass es sich bei dem Fundort auch um den Wuchsstandort des fossilen Baumes handelt. Durch Zählung der Jahresringe der geborgenen Stämme kann sogar der Zeitraum bestimmt werden, während dessen der Aletschgletscher den Fundort nicht erreicht hat. Mit dieser Methode wurde festgestellt, dass der Aletschgletscher bis etwa 1200 v. Chr. um einiges kleiner gewesen sein muss als gegen Ende des 20. Jahrhunderts. Für die Jahre etwa von 1200 bis 1110 v. Chr., 850 bis 750 v. Chr. und 350 bis 250 v. Chr. sind Vorstösse festgestellt worden. Dabei ist der Aletschgletscher von 900 bis 400 v. Chr. jedoch kleiner gewesen als am Ende des 20. Jahrhunderts, genauso wie von etwa 100 v. Chr. bis ins Jahr 250. Um das Jahr 300 ist eine Gletscherlänge vergleichbar der des Höchststandes im 19. Jahrhundert festzustellen.
Laut der letzten Studie der Universität Erlangen-Nürnberg (Juni 2020) schmolz die Oberfläche des Grossen Aletschgletscher zwischen den Jahren 2001 und 2014 um mehr als fünf Meter pro Jahr in den unteren Lagen.
Tourismus
Der Aletschgletscher galt schon früh als besondere Sehenswürdigkeit für Reisende und als willkommenes Untersuchungsobjekt für Forschende. Forschungsstationen gibt es seit 1937 auf dem Jungfraujoch und seit 1976 auf der Riederfurka oberhalb der Riederalp. Durch zahlreiche Luftseilbahnen besonders gut erschlossen ist der Berggrat zwischen dem Riederhorn und dem Eggishorn, der sehr schöne Einblicke in den Zungenbereich und den unteren Teil des Gletschers gewährt. Mit dem Bau der Jungfraubahn auf das Jungfraujoch (auf der Sphinx 3571 m ü. M.) wurde 1912 auch für nicht berggewohnte Leute ein Blick in den oberen Teil des Gletschers ermöglicht.
Am Felshang des Faulbergs östlich des Konkordiaplatzes stehen auf 2850 m ü. M. die Konkordiahütten des Schweizer Alpen-Clubs SAC. Sie dienen als wichtiger Etappenort auf der hochalpinen Gletscherroute vom Jungfraujoch oder vom Lötschental in das Gebiet des Grimselpasses.
UNESCO-Weltnaturerbe
Das Gebiet des Grossen Aletschgletschers ist zusammen mit dem einzigartigen Aletschwald und den umliegenden Regionen seit dem 13. Dezember 2001 Bestandteil des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.
(Wikipedia)
Markings: MARQUIS JET HOLDINGS INC,OKLAHOMA CITY ,OKLAHOMA .
Serial Number RK-520
Specifications (Hawker 400XP)
General characteristics
Crew: 2 pilots
Capacity: 7 passengers
Length: 48 ft 5 in (14.8 m)
Wingspan: 43 ft 6 in (13.3 m)
Height: 13 ft 11 in (4.2 m)
Empty weight: 10,550 lb (4,786 kg)
Max takeoff weight: 16,300 lb (7,394 kg)
Powerplant: 2× Pratt & Whitney Canada JT15D-5 , 2965 lbf () each
Performance
Maximum speed: 450 kts (518 mph) 833 km/h
Cruise speed: 414 kts (476 mph) 767 km/h
Range: 1,482 nm (2,744 km)
Service ceiling: 45,000 ft (13,716 m)
The Hawker 400 is a small twin-engine corporate aircraft, designed by Raytheon's Beech Aircraft Company subsidiary, now part of Hawker Beechcraft.
The aircraft was originally designed as the Mitsubishi MU-300 Diamond, an all-new, all-jet development to complement and slot above the Mitsubishi MU-2 and provide Mitsubishi Heavy Industries with their top-of-the-line corporate aircraft model (hence the name "Diamond")[1]. Beechcraft bought the production rights and began manufacturing it as their own model, initially redesignated as the Beechjet 400. The Beechjet 400 was certified by the FAA in May 1985.
Raytheon/Beechcraft steadily developed their own improvements to the model, leading to the 400A in 1990. Improvements in the 400A include longer range, higher take-off weights and improved luxury appointments. An all-glass flight deck was also offered. Beechcraft also developed a version for the United States Air Force known as the T-1A Jayhawk, used as a trainer for large aircraft crews (such as tankers and strategic transports). A total of 180 T-1A trainers were delivered between 1992-1997. Another military variant is the Japan Air Self-Defense Force T-400 trainer which shares the same Type Certificate as the T-1A.[2]
In 1993 Raytheon purchased the Hawker business jet product line from British Aerospace. The Beechjet 400 was eventually renamed the Hawker 400 to map it into the Hawker product line. The Hawker 400XP incorporates further aerodynamic, mechanical and interior improvements gleaned from the Hawker 800XP.
In October 2008, Hawker Beechcraft announced upgrades to the design, resulting in the new model designation Hawker 450XP.[citation needed] Upgrades include new, more fuel efficient engines (Pratt & Whitney PW535D models with 2,965 pounds of thrust apiece) Collins Pro Line 21 avionics and Collins Venue cabin management/entertainment system and a complete interior upgrade.[
MFR Year 2007
The Beacon opened to the public on 28 March 2013
The Beacon is 80ft high and has seven floors
There are 132 steps (and a lift!)
The Beacon took 12 months to build
It includes a two-storey café with open terraces offering 360 degree views
There are four floors of business space
A sky lounge for meetings and events
The top floor is an open roof terrace offering fantastic views all year round
Eco features include an energy efficient heat recovery system and solar reflective glazing
The Beacon is included in a LED lights installation which runs the full length of the seafront to the bandstand
The project is part funded by the Council, One North East and the European Regional Development Fund 2007-2013.
Redcar is a seaside town on the Yorkshire Coast in the Redcar and Cleveland unitary authority in the ceremonial county of North Yorkshire, England. It is located 7 miles (11 km) east of Middlesbrough.
The Teesside built-up area's Redcar subdivision had a population of 37,073 at the 2011 Census. The town is made up of Coatham, Dormanstown, Kirkleatham, Newcomen, West Dyke, Wheatlands and Zetland.
It gained a town charter in 1922, from then until 1968 it was governed by the municipal borough of Redcar. Since the abolition of County Borough of Teesside, which existed from 1968 until 1974, the town has been unparished.
Redcar occupies a low-lying site by the sea; the second element of its name is from Old Norse kjarr, meaning 'marsh', and the first may be either Old English (Anglo-Saxon) rēad meaning 'red' or OE hrēod 'reed'. The town originated as a fishing hamlet in the 14th century, trading with the larger adjacent hamlet of Coatham. Until the mid-19th century it was within the parish of Marske-by-the-Sea – mentioned in the Domesday Book of 1086.
Numerous ships have foundered off the Redcar coastline and many of their wrecks still exist. The Zetland is the world's oldest surviving lifeboat. It was built by Henry Greathead of South Shields and is housed in a volunteer-led sea-front museum. The lifeboat was first stationed at Redcar in 1802.
As seaside holidays became fashionable in the early 19th century, Redcar's facilities expanded. By 1841, Redcar had 794 inhabitants. In 1846, work was completed on the Middlesbrough and Redcar Railway and the presently named Redcar Central station, created to attract tourism and trade.
Redcar's population expansion corresponded with Middlesbrough's, with the discovery in 1850 of iron ore in the Eston area of Cleveland Hills. Redcar prospered as a seaside town drawing tourists attracted by eight miles of sands stretching from South Gare to Saltburn-by-the-Sea.
Plans for a pier were drawn up in 1866, but lay dormant until prompted by the announcement of plans to build a pier at Coatham in 1871. Coatham Pier was wrecked before it was completed when two sailing ships were driven through it in a storm. It had to be shortened because of the cost of repairs and was re-opened with an entrance with two kiosks and a roller-skating rink on the Redcar side, and a bandstand halfway along its length.
Redcar Racecourse was created in 1875. Redcar Pier, another pier as well as Coatham Pier, was built in the late 1870s. In October 1880 the brig Luna caused £1,000 worth of damage to this pier. In New Year's Eve 1885 SS Cochrane demolished the landing stage. and in 1897 the schooner Amarant went through the pier. A year later, its head and bandstand burned down.
In October 1898 the Coatham Pier was almost wrecked when the barque Birger struck it and the pier was thereafter allowed to disintegrate. An anchor from the Birger can be seen on the sea front pavement close to the Zetland Lifeboat Museum.
In 1907 a pavilion ballroom was built on Redcar Pier behind the entrance kiosks and in 1928 it was extended. A glass house for concerts was added to the remains of Coatham Pier's entrance. The presently named Redcar East railway station was built in 1929.
In 1929 Coatham Pier's glasshouse was replaced by the New Pavilion theatre. After the war, comedian and entertainer Larry Grayson coined his catchphrase "Shut that Door!" while performing there, since the stage door was open to the cold North Sea breeze.
Redcar Pier was deliberately breached (sectioned) in 1940 to prevent its use by enemy invasion forces. As a result of sectioning, damage by a mine explosion and deterioration it was never reconnected and instead allowed to become even more dilapidated.
In 1964 the New Pavilion Theatre was transformed into the Regent Cinema. The Redcar Pier pavilion continued in use after the war but storm damage led to it being declared unsafe and it was demolished in 1980–1981.
The town's main employers in the post-war era were the nearby Teesside Steelworks at Warrenby, founded by Dorman Long in 1917, and the ICI Wilton chemical works. The steel produced at Dorman Long was used to build the Sydney Harbour Bridge, Tyne Bridge, Auckland Harbour Bridge and many others. Both the Warrenby and Lackenby sites became part of Tata Steel when Corus was taken over in 2007, but continued to trade under the Corus name until at least February 2008. SSI bought the plant from Tata Steel in February 2011, for £320 million.
After a two-year hiatus following the mothballing of the plant in February 2010, steel was once again being made at Redcar. The Thai owners of the former Corus Plant at Lackenby, Sahaviriya Steel Industries (SSI), re-ignited the blast furnace, one of the largest in Europe, on 15 April 2012.
On 18 September 2015, production was paused due to the decline in steel prices. On 28 September 2015, the plant was "mothballed" amid poor steel trading conditions across the world and a drop in steel prices. On 2 October, the owner of the site, SSI UK, entered liquidation. On 12 October 2015 the administrator announced that there was no realistic prospect of finding a buyer and the ovens would be extinguished.
Wards periodically change, as of 2018 the town is made up of Coatham, Dormanstown, Kirkleatham, Newcomen, West Dyke, Wheatlands and Zetland. Redcar is made up of areas that do not lend their name to a ward: Warrenby, Lakes Estate, Redcar East, The Ings, Ings Farm, Mickledales and Westfield.
On 5 May 2011 Redcar elected its councillors to Redcar & Cleveland Borough Council. There was a by-election on 18 November 2011 for two vacant seats in the Zetland ward, held onto by the Liberal Democrats, and on 19 January 2012 there was a by-election for a vacant seat in Newcomen ward subsequently gained by Labour from the Liberal Democrats.
Redcar was formerly a township and chapelry in the parishes of Marske and Upleatham, in 1866 Redcar became a separate civil parish. A district in Redcar's name formed in 1885. Three years after the district was formed, the centuries-old Yorkshire authority was replaced by the North Riding of Yorkshire county council. The district became an urban district in 1894.
The settlement's town charter occurred in 1922, the district was able to be styled as a municipal borough and the settlement as a town. On 1 April 1974 the parish was abolished and merged with Teesside and Marske. On 1 April 1968 the municipal borough was abolished merged into the County Borough of Teesside, part also went to Saltburn and Marske by the Sea Urban District. This removed it from the administrative county however still ceremonially in the area. In 1961 the parish had a population of 31,460.
The 1974 reform created the non-metropolitan County of Cleveland, under the Langbaurgh non-metropolitan district. The county was also inserted into the North East England region. After further changes in 1996, the district became a unitary authority called Redcar & Cleveland in the ceremonial county of North Yorkshire, the county straddling two regions of England.
The North East England region was sub-divided into combined authorities, in May 2017 the Tees Valley area voted for their first mayor. The Conservative candidate, Ben Houchen, won the election and is now in his second term.
From 1987 to 2001, the local Member of Parliament (MP) was Mo Mowlam. From 2001 to 2010 the MP was Vera Baird. In the 2010 general election there was a swing to the Liberal Democrats with Ian Swales being elected. But, in the 2015 general election, Anna Turley, a Labour MP, won back Redcar. In the snap 2017 general election, Anna Turley held onto that seat. In the general election on 12 December 2019, Anna Turley lost her seat to Conservative candidate Jacob Young with a majority of 3,527 votes. Young becomes the third conservative MP to represent Redcar, the first being Royal Naval Commander Robert Tatton Bower 1931 to 1945 and Scarborough businessman Wilfred Proudfoot between 1959 and 1964 when Redcar was part of the Cleveland constituency.
The Palace Hub, on the beach front, was built by Redcar and Cleveland Council for the creative and cultural sector of the town. An art gallery and business start up centre are located in the building. The main library is in the Redcar Heart building in the centre of the town and there is a long-standing Redcar Literary Institute, which was founded in 1896.
Redcar is home to the Tuned In! Centre, which opened in 2011 and overlooks the sea front. The multi purpose venue hosts live music as well as creative workshops for young people. The annual event Clubland on the Beach, which showcases dance acts attracting visitors from across the country, has been held at Majuba Road in Redcar for the past three years.
The town has had several parks built for tourism: Coatham Enclosure, Locke Park, Zetland Park, Lily Park, an Amusement Park with a roller coaster, and a small sea front park known locally as Titty Bottle Park. The Amusement Park near the railway closed decades ago, and Titty Bottle Park was absorbed into the redeveloped sea front around Redcar Beacon.
At the west end of High Street is a Grade II listed clock tower, a memorial to King Edward VII who was a regular visitor to Redcar. The tower has now been refurbished.
Construction of the Redcar Beacon started in 2011. In 2013, when the building had been completed, it was nominated for the Building Design Carbuncle Cup for worst new building. It came third in the whole of the UK. In December 2015, the Beacon was damaged by winds from Storm Desmond, with several large pieces of panelling falling onto the beach below. It was also damaged in winter 2016, where a panel from the top fell off in a storm.
There are 23 listed buildings in Redcar. The Grade I Listed Sir William Turner's Hospital in Kirkleatham was built between 1674–1676 and listed on the 14 June 1952.
On the Esplanade is the Grade II-Listed Zetland Lifeboat Museum housing the world's oldest lifeboat Zetland Lifeboat.
The Victorian, former Coatham Hotel stands on Newcomen Terrace sea front.[36][37] The ballroom of the hotel was home to the Redcar Jazz Club, a venue for the up-and-coming bands of the late 1960s and early 1970s.
In the south-east of Redcar is an aircraft listening post built in 1916 during the First World War as part of a regional defence system to detect approaching aircraft, principally Zeppelins, and give early warning.It is an example of an acoustic mirror, of which other examples can be found along the east coast of Britain. The mirror was used up until the invention of radar and although it was built on open fields today a modern housing estate now surrounds it. Only the concrete sound mirror remains and is now a Grade II listed building.
To the east of Redcar is the grade II* listed Church of St Peter, designed by Ignatius Bonomi and built 1822–29. In 1818, Lord Dundas gave land for a church, St Peters. The foundation stone was laid by Lady Turner of Kirkleatham in 1823. Initially it was a daughter church of Marske, but became an independent parish in 1867. It has a window commemorating local benefactor Sir William Turner.
Redcar has two railway stations, on the Tees Valley line, with trains operated by Northern and TransPennine Express, namely Redcar Central and Redcar East. A third station Redcar British Steel, which closed in December 2019, served the steelworks.
The main roads through the town are the A1085 and the A1042, with the A174 bypassing. Redcar is served primarily by Arriva North East buses, connecting Redcar with the surrounding towns and villages.
The Pangea North and CANTAT-3 submarine telecommunication cables both come ashore between Redcar and Marske-by-the-Sea.
See also: List of schools in Redcar and Cleveland
The town's further education college is Redcar & Cleveland College.
The town's secondary schools are: Outwood Academy Redcar, Sacred Heart Catholic Secondary and Rye Hills Academy.
There are eleven primary schools in Redcar: Coatham, Dormanstown, Green Gates, Ings Farm, John E Batty, Lakes, Newcomen, Riverdale, St Benedict's, Wheatlands and Zetland.
Local news and television programmes are provided by BBC North East and Cumbria and ITV Tyne Tees, the local television station TalkTeesside also broadcasts to the area. Television signals are received from the Bilsdale TV transmitter.
Local radio stations are BBC Radio Tees, Heart North East, Capital North East, Smooth North East, Greatest Hits Radio Teesside, and Zetland FM, a community based radio station which broadcast from its studios on Newcomen Terrace in the town.
The town is served by the local newspapers, East Cleveland Herald & Post which is published by the TeessideLive. The Northern Echo also covers the area.
In Coatham is Cleveland Golf Club, the first golf club to be formed in Yorkshire. It was established in 1887 and is a links course. Also in Coatham is Redcar Cricket Club, which play in the NYSD league, and Redcar Running Club.
In association football, Redcar Athletic currently compete in the Northern League Division One while Redcar Town play in Northern League Division Two. Redcar Rugby Union Football club play at Mackinlay Park.
Redcar Racecourse is one of nine thoroughbred horse racecourses in Yorkshire. There is also a motorcycle speedway racing team, the Redcar Bears racing in the SGB Championship. The race track is at the South Tees Motorsport Park in Southbank Street, South Bank and is unusual in that one bend is more highly banked than the other. The team was formerly captained by 1992 World Champion Gary Havelock and was formerly managed by his father Brian.
The town is set to host the 2022 Tour of Britain stage four, UCI Europe Tour cycling race. The town was previously set to host a stage of the Tour de Yorkshire, the event was affected by the COVID-19 pandemic.
Notable people
Gertrude Bell, colonial administrator and contemporary of Lawrence of Arabia spent her youthful years at Red Barns House in Coatham,[ which became, for a time, the Red Barns Hotel and a listed building.
The surviving negatives of Redcar photographer Alfred Edward Graham (1882–1945) were acquired by Redcar Urban District Council's Library and Museum Committee and are now held by the Redcar and Cleveland Museum Service.
Rex Hunt, governor of the Falkland Islands during the 1982 invasion by Argentina, attended Coatham School.
The former Secretary of State for Northern Ireland, Mo Mowlam, represented Redcar parliamentary constituency in the House of Commons.
Film and television actors Pip Donaghy June Laverick, and Wendy Hall, and actor/director/producer Robert Porter were all born in Redcar.
Actor and radio actor Felicity Finch, famous for her part in the Archers BBC Radio 4 drama series, playing Ruth Archer, was also born and grew up in Redcar.
Singer David Coverdale, lead singer with Deep Purple and Whitesnake lived in Redcar as a youth and worked in the Gentry clothes shop on Coatham Road.
Chris Norman, founder member and former lead singer of Smokie was born in Redcar.
Pete York, drummer with the Spencer Davis Group and session drummer was born in Redcar.
Paralympian, Baroness Tanni Grey-Thompson, originally from Wales, lived in Redcar for a number of years with her husband and daughter.
2011 and 2016 UCI Downhill World Champion Danny Hart was born in and currently lives in Redcar, he is frequently nicknamed "The Redcar Rocket" by commentators.
David Wheater, Bolton Wanderers and England national football team central defender, grew up and still lives in Redcar.
Snooker player Mike Dunn was born in Middlesbrough but lives in Redcar.[citation needed]
Jordan Jones, Rangers FC and Northern Ireland national football team midfielder was born in Redcar
Hayden Hackney, Middlesbrough F.C. midfielder was born in Redcar
Dylan Cartlidge, singer and multi-instrumentalist grew up in Redcar
Film and television
A location from the film Atonement
In 2006, Redcar was used as a location for the film adaptation of the Ian McEwan novel Atonement. The Coatham Hotel, Regent Cinema, a section of Newcomen Terrace and part of the beach were dressed as 1940s Dunkirk. Filming took place across three days in August 2006, with local men playing the soldiers.
In 2010, Redcar was featured on the Channel 4 television programme The Secret Millionaire. David Jamilly a humanitarian, philanthropist and self-made millionaire, visited the Redcar community and gave £25,000 to Zoë's Place for a sensory room, £25,000 to Redcar Amateur Boxing Club to start an Olympic fund, and £25,000 to Sid's Place for special counselling.
There was a subsequent visit on 14 May to a screening at Redcar's cinema, attended by the mayor and mayoress along with all the charities and people involved. The feature of the documentary involved the closure of the nearby Corus steelworks as well as the charities. On 9 December 2011, Jamilly opened the new Redcar Education Development centre in Park Avenue, Redcar. The centre provides day care for adults with learning difficulties. He also opened the Redcar Primary Care Hospital on 9 December 2011 and the new Sid's Place on 15 December 2011.
The town was filmed for the 2018 BBC television documentary The Mighty Redcar. The four-part series followed young people from Redcar and surrounding towns as they completed their studies and looked for work.
North Yorkshire is a ceremonial county in the Yorkshire and the Humber and North East regions of England. It borders County Durham to the north, the North Sea to the east, the East Riding of Yorkshire to the south-east, South Yorkshire to the south, West Yorkshire to the south-west, and Cumbria and Lancashire to the west. Northallerton is the county town.
The county is the largest in England by land area, at 9,020 km2 (3,480 sq mi), and has a population of 1,158,816. The largest settlements are Middlesbrough (174,700) in the north-east and the city of York (152,841) in the south. Middlesbrough is part of the Teesside built-up area, which extends into County Durham and has a total population of 376,663. The remainder of the county is rural, and the largest towns are Harrogate (73,576) and Scarborough (61,749). For local government purposes the county comprises four unitary authority areas — York, Middlesbrough, Redcar and Cleveland, and North Yorkshire — and part of a fifth, Stockton-on-Tees.
The centre of the county contains a wide plain, called the Vale of Mowbray in the north and Vale of York in the south. The North York Moors lie to the east, and south of them the Vale of Pickering is separated from the main plain by the Howardian Hills. The west of the county contains the Yorkshire Dales, an extensive upland area which contains the source of the River Ouse/Ure and many of its tributaries, which together drain most of the county. The Dales also contain the county's highest point, Whernside, at 2,415 feet (736 m).
North Yorkshire non-metropolitan and ceremonial county was formed on 1 April 1974 as a result of the Local Government Act 1972. It covered most of the North Riding of Yorkshire, as well as northern parts of the West Riding of Yorkshire, northern and eastern East Riding of Yorkshire and the former county borough of York. Northallerton, as the former county town for the North Riding, became North Yorkshire's county town. In 1993 the county was placed wholly within the Yorkshire and the Humber region.
Some areas which were part of the former North Riding were in the county of Cleveland for twenty-two years (from 1974 to 1996) and were placed in the North East region from 1993. On 1 April 1996, these areas (Middlesbrough, Redcar and Cleveland and Stockton borough south of the River Tees) became part of the ceremonial county as separate unitary authorities. These areas remain within the North East England region.
Also on 1 April 1996, the City of York non-metropolitan district and parts of the non-metropolitan county (Haxby and nearby rural areas) became the City of York unitary authority.
On 1 April 2023, the non-metropolitan county became a unitary authority. This abolished eight councils and extended the powers of the county council to act as a district council.
The York and North Yorkshire Combined Authority held its first meeting on 22 January 2024, assumed its powers on 1 February 2024 and the first mayor is to be elected in May 2024.
The geology of North Yorkshire is closely reflected in its landscape. Within the county are the North York Moors and most of the Yorkshire Dales, two of eleven areas in England and Wales to be designated national parks. Between the North York Moors in the east and the Pennine Hills. The highest point is Whernside, on the Cumbrian border, at 2,415 feet (736 m). A distinctive hill to the far north east of the county is Roseberry Topping.
North Yorkshire contains several major rivers. The River Tees is the most northerly, forming part of the border between North Yorkshire and County Durham in its lower reaches and flowing east through Teesdale before reaching the North Sea near Redcar. The Yorkshire Dales are the source of many of the county's major rivers, including the Aire, Lune, Ribble, Swale, Ure, and Wharfe.[10] The Aire, Swale, and Wharfe are tributaries of the Ure/Ouse, which at 208 km (129 mi) long is the sixth-longest river in the United Kingdom. The river is called the Ure until it meets Ouse Gill beck just below the village of Great Ouseburn, where it becomes the Ouse and flows south before exiting the county near Goole and entering the Humber estuary. The North York Moors are the catchment for a number of rivers: the Leven which flows north into the Tees between Yarm and Ingleby Barwick; the Esk flows east directly into the North Sea at Whitby as well as the Rye (which later becomes the Derwent at Malton) flows south into the River Ouse at Goole.
North Yorkshire contains a small section of green belt in the south of the county, which surrounds the neighbouring metropolitan area of Leeds along the North and West Yorkshire borders. It extends to the east to cover small communities such as Huby, Kirkby Overblow, and Follifoot before covering the gap between the towns of Harrogate and Knaresborough, helping to keep those towns separate.
The belt adjoins the southernmost part of the Yorkshire Dales National Park, and the Nidderdale AONB. It extends into the western area of Selby district, reaching as far as Tadcaster and Balne. The belt was first drawn up from the 1950s.
The city of York has an independent surrounding belt area affording protections to several outlying settlements such as Haxby and Dunnington, and it too extends into the surrounding districts.
North Yorkshire has a temperate oceanic climate, like most of the UK. There are large climate variations within the county. The upper Pennines border on a Subarctic climate. The Vale of Mowbray has an almost Semi-arid climate. Overall, with the county being situated in the east, it receives below-average rainfall for the UK. Inside North Yorkshire, the upper Dales of the Pennines are one of the wettest parts of England, where in contrast the driest parts of the Vale of Mowbray are some of the driest areas in the UK.
Summer temperatures are above average, at 22 °C. Highs can regularly reach up to 28 °C, with over 30 °C reached in heat waves. Winter temperatures are below average, with average lows of 1 °C. Snow and Fog can be expected depending on location. The North York Moors and Pennines have snow lying for an average of between 45 and 75 days per year. Sunshine is most plentiful on the coast, receiving an average of 1,650 hours a year. It reduces further west in the county, with the Pennines receiving 1,250 hours a year.
The county borders multiple counties and districts:
County Durham's County Durham, Darlington, Stockton (north Tees) and Hartlepool;
East Riding of Yorkshire's East Riding of Yorkshire;
South Yorkshire's City of Doncaster;
West Yorkshire's City of Wakefield, City of Leeds and City of Bradford;
Lancashire's City of Lancaster, Ribble Valley and Pendle
Cumbria's Westmorland and Furness.
The City of York Council and North Yorkshire Council formed the York and North Yorkshire Combined Authority in February 2024. The elections for the first directly-elected mayor will take place in May 2024. Both North Yorkshire Council and the combined authority are governed from County Hall, Northallerton.
The Tees Valley Combined Authority was formed in 2016 by five unitary authorities; Middlesbrough, Redcar and Cleveland Borough both of North Yorkshire, Stockton-on-Tees Borough (Uniquely for England, split between North Yorkshire and County Durham), Hartlepool Borough and Darlington Borough of County Durham.
In large areas of North Yorkshire, agriculture is the primary source of employment. Approximately 85% of the county is considered to be "rural or super sparse".
Other sectors in 2019 included some manufacturing, the provision of accommodation and meals (primarily for tourists) which accounted for 19 per cent of all jobs. Food manufacturing employed 11 per cent of workers. A few people are involved in forestry and fishing in 2019. The average weekly earnings in 2018 were £531. Some 15% of workers declared themselves as self-employed. One report in late 2020 stated that "North Yorkshire has a relatively healthy and diverse economy which largely mirrors the national picture in terms of productivity and jobs.
Mineral extraction and power generation are also sectors of the economy, as is high technology.
Tourism is a significant contributor to the economy. A study of visitors between 2013 and 2015 indicated that the Borough of Scarborough, including Filey, Whitby and parts of the North York Moors National Park, received 1.4m trips per year on average. A 2016 report by the National Park, states the park area gets 7.93 million visitors annually, generating £647 million and supporting 10,900 full-time equivalent jobs.
The Yorkshire Dales have also attracted many visitors. In 2016, there were 3.8 million visits to the National Park including 0.48 million who stayed at least one night. The parks service estimates that this contributed £252 million to the economy and provided 3,583 full-time equivalent jobs. The wider Yorkshire Dales area received 9.7 million visitors who contributed £644 million to the economy. The North York Moors and Yorkshire Dales are among England's best known destinations.
York is a popular tourist destination. A 2014 report, based on 2012 data, stated that York alone receives 6.9 million visitors annually; they contribute £564 million to the economy and support over 19,000 jobs. In the 2017 Condé Nast Traveller survey of readers, York rated 12th among The 15 Best Cities in the UK for visitors. In a 2020 Condé Nast Traveller report, York rated as the sixth best among ten "urban destinations [in the UK] that scored the highest marks when it comes to ... nightlife, restaurants and friendliness".
During February 2020 to January 2021, the average property in North Yorkshire county sold for £240,000, up by £8100 over the previous 12 months. By comparison, the average for England and Wales was £314,000. In certain communities of North Yorkshire, however, house prices were higher than average for the county, as of early 2021: Harrogate (average value: £376,195), Knaresborough (£375,625), Tadcaster (£314,278), Leyburn (£309,165) and Ripon (£299,998), for example.
This is a chart of trend of regional gross value added for North Yorkshire at current basic prices with figures in millions of British pounds sterling.
Unemployment in the county was traditionally low in recent years, but the lockdowns and travel restrictions necessitated by the COVID-19 pandemic had a negative effect on the economy during much of 2020 and into 2021. The UK government said in early February 2021 that it was planning "unprecedented levels of support to help businesses [in the UK] survive the crisis". A report published on 1 March 2021 stated that the unemployment rate in North Yorkshire had "risen to the highest level in nearly 5 years – with under 25s often bearing the worst of job losses".
York experienced high unemployment during lockdown periods. One analysis (by the York and North Yorkshire Local Enterprise Partnership) predicted in August 2020 that "as many as 13,835 jobs in York will be lost in the scenario considered most likely, taking the city's unemployment rate to 14.5%". Some critics claimed that part of the problem was caused by "over-reliance on the booming tourism industry at the expense of a long-term economic plan". A report in mid June 2020 stated that unemployment had risen 114 per cent over the previous year because of restrictions imposed as a result of the pandemic.
Tourism in the county was expected to increase after the restrictions imposed due the pandemic are relaxed. One reason for the expected increase is the airing of All Creatures Great and Small, a TV series about the vet James Herriot, based on a successful series of books; it was largely filmed within the Yorkshire Dales National Park. The show aired in the UK in September 2020 and in the US in early 2021. One source stated that visits to Yorkshire websites had increased significantly by late September 2020.
The East Coast Main Line (ECML) bisects the county stopping at Northallerton,Thirsk and York. Passenger service companies in the area are London North Eastern Railway, Northern Rail, TransPennine Express and Grand Central.
LNER and Grand Central operate services to the capital on the ECML, Leeds Branch Line and the Northallerton–Eaglescliffe Line. LNER stop at York, Northallerton and on to County Durham or spur over to the Tees Valley Line for Thornaby and Middlesbrough. The operator also branch before the county for Leeds and run to Harrogate and Skipton. Grand Central stop at York, Thirsk Northallerton and Eaglescliffe then over to the Durham Coast Line in County Durham.
Northern operates the remaining lines in the county, including commuter services on the Harrogate Line, Airedale Line and York & Selby Lines, of which the former two are covered by the Metro ticketing area. Remaining branch lines operated by Northern include the Yorkshire Coast Line from Scarborough to Hull, York–Scarborough line via Malton, the Hull to York Line via Selby, the Tees Valley Line from Darlington to Saltburn via Middlesbrough and the Esk Valley Line from Middlesbrough to Whitby. Last but certainly not least, the Settle-Carlisle Line runs through the west of the county, with services again operated by Northern.
The county suffered badly under the Beeching cuts of the 1960s. Places such as Richmond, Ripon, Tadcaster, Helmsley, Pickering and the Wensleydale communities lost their passenger services. Notable lines closed were the Scarborough and Whitby Railway, Malton and Driffield Railway and the secondary main line between Northallerton and Harrogate via Ripon.
Heritage railways within North Yorkshire include: the North Yorkshire Moors Railway, between Pickering and Grosmont, which opened in 1973; the Derwent Valley Light Railway near York; and the Embsay and Bolton Abbey Steam Railway. The Wensleydale Railway, which started operating in 2003, runs services between Leeming Bar and Redmire along a former freight-only line. The medium-term aim is to operate into Northallerton station on the ECML, once an agreement can be reached with Network Rail. In the longer term, the aim is to reinstate the full line west via Hawes to Garsdale on the Settle-Carlisle line.
York railway station is the largest station in the county, with 11 platforms and is a major tourist attraction in its own right. The station is immediately adjacent to the National Railway Museum.
The main road through the county is the north–south A1(M), which has gradually been upgraded in sections to motorway status since the early 1990s. The only other motorways within the county are the short A66(M) near Darlington and a small stretch of the M62 motorway close to Eggborough. The other nationally maintained trunk routes are the A168/A19, A64, A66 and A174.
Long-distance coach services are operated by National Express and Megabus. Local bus service operators include Arriva Yorkshire, Stagecoach, Harrogate Bus Company, The Keighley Bus Company, Scarborough & District (East Yorkshire), Yorkshire Coastliner, First York and the local Dales & District.
There are no major airports in the county itself, but nearby airports include Teesside International (Darlington), Newcastle and Leeds Bradford.
The main campus of Teesside University is in Middlesbrough, while York contains the main campuses of the University of York and York St John University. There are also two secondary campuses in the county: CU Scarborough, a campus of Coventry University, and Queen's Campus, Durham University in Thornaby-on-Tees.
Colleges
Middlesbrough College's sixth-form
Askham Bryan College of agriculture, Askham Bryan and Middlesbrough
Craven College, Skipton
Middlesbrough College
The Northern School of Art, Middlesbrough
Prior Pursglove College
Redcar & Cleveland College
Scarborough Sixth Form College
Scarborough TEC
Selby College
Stockton Riverside College, Thornaby
York College
Places of interest
Ampleforth College
Beningbrough Hall –
Black Sheep Brewery
Bolton Castle –
Brimham Rocks –
Castle Howard and the Howardian Hills –
Catterick Garrison
Cleveland Hills
Drax Power Station
Duncombe Park – stately home
Eden Camp Museum –
Embsay & Bolton Abbey Steam Railway –
Eston Nab
Flamingo Land Theme Park and Zoo –
Helmsley Castle –
Ingleborough Cave – show cave
John Smith's Brewery
Jorvik Viking Centre –
Lightwater Valley –
Lund's Tower
Malham Cove
Middleham Castle –
Mother Shipton's Cave –
National Railway Museum –
North Yorkshire Moors Railway –
Ormesby Hall – Palladian Mansion
Richmond Castle –
Ripley Castle – Stately home and historic village
Riverside Stadium
Samuel Smith's Brewery
Shandy Hall – stately home
Skipton Castle –
Stanwick Iron Age Fortifications –
Studley Royal Park –
Stump Cross Caverns – show cave
Tees Transporter Bridge
Theakston Brewery
Thornborough Henges
Wainman's Pinnacle
Wharram Percy
York Castle Museum –
Yorkshire Air Museum –
The Yorkshire Arboretum
Longer length gloves and a string of pearls perk up a dress that has been a favourite for many years.
SUNDANCE CANYON HIKE
Trail Length — 4.3 km (2.7 mi)
Half-day trip, allow 1.5 hours
Elevation gain: 145 m (470 ft)
Maximum elevation: 1545 m (5,070 ft)
Maps: Banff 82 O/4; Banff Up-Close (Gem Trek)
Access: From the intersection at the south end of the Bow River bridge in Banff, follow Cave Avenue 1.2 km to the parking area for the Cave and Basin Centennial Centre. A paved walkway leads to the Cave and Basin complex and continues 200 m beyond to the trailhead kiosk. Check the trail conditions before you go.
Throughout most of its long history, the short 2 km loop trail leading through Sundance Canyon was accessible by road from the town of Banff. In the mid 1980s, the road beyond the Cave and Basin was converted to a paved walking and cycling path, which made the trip longer but more scenically varied. Many people bike to the canyon on the broad, paved trail, but the first half of the trip is an open and pleasant route for walkers as well.
From the Cave and Basin, the trail descends gradually through forest to the Bow River. For the next 1.5 km it follows along the river and its side channels with views of the rugged peaks to the north, including the sharp spire of Mount Edith. The final stretch to the canyon climbs gradually through forest.
Pavement and bike access end at the Sundance Canyon picnic area, where a foot trail climbs into this pleasant little canyon and then loops back through forest to the picnic area.
Marsh Trail
The 1.6 km trail around the north side of the Cave and Basin marsh is an interesting way to return from Sundance Canyon.
Follow the trail that branches right from the Sundance trail at km 0.7 (where the paved trail first meets the river). It runs downstream along the banks of the Bow River to the marsh, skirts the edge of this wetland, then turns right at a junction and crosses an earthen dike to return to the Cave and Basin parking lot. Also see: Marsh Loop Trail.
Healy Creek
This roadbed branches right from the Sundance Canyon trail at 2.2 km and rolls through forest along the south side of the Bow Valley to Brewster Creek junction (2.9 km) and the Sunshine Road (4.6 km). The smooth, broad track is of more interest to mountain bikers (and cross-country skiers) than hikers.
----------------
BANFF
Banff is a town within Banff National Park in Alberta, Canada. It is located in Alberta's Rockies along the Trans-Canada Highway, approximately 126 km (78 mi) west of Calgary and 58 km (36 mi) east of Lake Louise. At an elevation of 1,400 m (4,600 ft) to 1,630 m (5,350 ft),[3] Banff is the community with the second highest elevation in Alberta after Lake Louise.
The Town of Banff was the first municipality to incorporate within a Canadian national park. The town is a member of the Calgary Regional Partnership.
Banff is a resort town and one of Canada's most popular tourist destinations, known for its mountainous surroundings and hot springs. It is a destination for outdoor sports and features extensive hiking, biking, scrambling and skiing areas within the area. Sunshine Village, Ski Norquay and Lake Louise Mountain Resort are the three nearby ski resorts located within the national park.
excerpt From Wikipedia, the free encyclopedia
For FGR - Arm's length portraits.
Merry Christmas everyone!!
You know why I tend to like myself? Because the typical almost-21-year-old well built, moderately attractive female with a photo entitled "Bad Santa" would probably be wearing some slutty Mrs. Claus outfit and trying to look seductive. As for me? I do this. :-D
Kathleen del Muerto - breakin' the mold since 1987.
Fun fact:
Right before this I went to the mall with my best friend in the world, with the intent of laughing at all the frantic last-minute shoppers (if that's you, I apologize....wait, no I don't. Why on earth would you wait so long to buy stuff, you silly twat?!). Anyways, we ended up buying each other CD's, so I'm now the proud owner of Kings of Leon - Only By the Night. Listen. LOVE.
Make your evening with this short strapless knee-length dress. It’s in a rising trend possessing a quality of easy to wear, flaunting your legs & shoulders and designs from flirty and sexy to elegant and sophisticated to fit your style. Broad belt at the waist is very sportive.
Buy Online : www.onlygowns.com
MF手動鏡頭 - 室外散景測試 [ Large Size (1024 x 683)∣Original Size (3504 x 2336) ]
Canon EOS 30D + Tamron SP 35-105mm f/2.8 ( for Nikon Mount )
Exposure：0.001 sec (1/2000)
Aperture：f/2.8
Focal Length：105 mm
ISO Speed：100
April 18, 2007
Tested by Yueh-Hua
Giacomo Ceruti (1698-1767) - Portrait of Donna Alba Regina del Ferro three quarter length in a black dress holding a book
The Chicago River is a system of rivers and canals with a combined length of 156 miles (251 km) that runs through the city of Chicago, including its center (the Chicago Loop). Though not especially long, the river is notable for being a reason why Chicago became an important location, with the related Chicago Portage being a link between the Great Lakes and the Mississippi Valley waterways and eventually the Gulf of Mexico.
The River is also noteworthy for its natural and man-made history. In 1887, the Illinois General Assembly, partly in response to concerns arising out of an extreme weather event in 1885 that threatened the city's water supply, decided to reverse the flow of the Chicago River through civil engineering by taking water from Lake Michigan and discharging it into the Mississippi River watershed. In 1889, the Illinois General Assembly created the Chicago Sanitary District (now The Metropolitan Water Reclamation District) to replace the Illinois-Michigan Canal, which had become inadequate to carry the city's increasing sewage and commercial navigation needs, with the Chicago Sanitary and Ship Canal, a much larger waterway. The District completed this man-made hydrologic connection between the Great Lakes and Mississippi watershed in 1900 by reversing the flow of the Main Stem and South Branch of the river using a series of canal locks, and increasing the river's flow from Lake Michigan, causing it to empty into the new Canal. In 1999, this system was named a 'Civil Engineering Monument of the Millennium' by the American Society of Civil Engineers (ASCE). The river is also noted for the local custom of dyeing it green on St. Patrick's Day.
The river is memorialized, in part, by two horizontal blue stripes on the Municipal Flag of Chicago. The river also serves as inspiration for one of Chicago's ubiquitous symbols: a three-branched, Y-shaped symbol (called the municipal device) is found on many buildings and other structures throughout Chicago; it represents the three branches of the Chicago River.
en.wikipedia.org/wiki/Chicago_river
en.wikipedia.org/wiki/Wikipedia:Text_of_Creative_Commons_...
Practising how to get arrested without resisting and hence avoid provoking police violence, Occupy Toronto © Linda Dawn Hammond / IndyFoto.com 2011, protest camp, Canada, November 15, 2011.
Day of visit by renowned folk singer Gordon Lightfoot, whose 17 year old daughter Meredith is among the protesters. He spoke at length with the media in support of the cause. Later, he greeted my sister, who lives nearby in a group home, and shook her hand. After I saw him, I couldn't get the song, 'In the Early morning Rain' out of my mind. My late father had bought me my first album - by Gordon Lightfoot- when I was a bit younger than his Meredith, and that song was on it. It was a day of fathers and daughters, and memories...
I hear too often people saying that the protesters have made their point and now "should get a job', as if that's an easy thing to achieve. Not to mention that when you can find them, most jobs these days are underpaid, part-time positions with no future, benefits or stability. Many of those protesting are either undereducated or overqualified- and all in the same sinking boat, with the exception of crippling debts attached to the latter group. At the camp is a mix of politically motivated people who have chosen to be there, and others who evidently have no where else to go, but have found at the Occupy Camp a renewed sense of purpose, camaraderie and security- food and a safe place to sleep. They stand to lose the most when this is finally over.
People were asked to come by at 11pm that night to show solidarity as the protest had received an eviction notice and the police were expected to break up the camp. Fortunately there was an injunction and the eviction is now expected to take place at a later date- possibly on Saturday.
Most people at the camp reacted positively to the journalists taking photographs. An exception was Lightfoot's daughter, whom it appears didn't want to be identified as such, and another woman from Quebec, who was initially angry that I had been invited by a protester to photograph inside one of the tents, until she understood that I am a freelance photographer and don't work for any particular mainstream newspaper. Though at times I wish I did, as perhaps then I wouldn't be in this dismal, insecure financial situation, something which appears to be a shared concern with many of the protesters.
I just can't win. As i was leaving, I was berated once again for the act of taking photos of Occupy Toronto, but this time by a man waiting at the streetcar stop. He saw my Stop Ford button and my camera. On his way home from "working 7 days a week", he complained to me about his taxes, crowed about the ' warm, 5 bedroom house in High Park" awaiting him which his "hard-earned money had provided" (as he cast a dismissive eye towards the tent city behind him), showed me the callous hands of "a real worker" . He didn't believe that the police would consider using tear gas and tried to suggest it hadn't happened in Quebec City during the Summit protests, which I can verify as I was there. 5,000 canisters- I told him to look it up. His idiotic response was to ask if I work for Pravda (the Russian Communist party run newspaper, defunct since 1991 and now a tabloid)... hmmm... I wasn't actually aware that there was still a Cold War going on in 2011 Canada, but then again, neither is Toronto's Mayor Ford and company, who have been known to refer to some of "his" constituents as left wing, cycling Pinkos... (the people who didn't vote for him) , all of which explains the sprinkling of anti-Ford messages at the Occupy Toronto site. Here I was thinking only the suburbs had voted Ford in- but he has at least 1 supporter in High Park, who surprisingly takes public transit.
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