+++ DISCLAIMER +++

Nothing you see here is real, even though the conversion or the presented background story might be based historical facts. BEWARE!

  

The KAI T-50 Golden Eagle (골든이글) is a family of South Korean supersonic advanced trainers and light combat aircraft, developed by Korea Aerospace Industries (KAI) with Lockheed Martin. The T-50 is South Korea's first indigenous supersonic aircraft and one of the world's few supersonic trainers.

 

The T-50 program started in the late Nineties and was originally intended to develop an indigenous trainer aircraft capable of supersonic flight, to train and prepare pilots for the KF-16 and F-15K, replacing trainers such as T-38 and A-37 that were then in service with the ROKAF. Prior South Korean aircraft programs include the turboprop KT-1 basic trainer produced by Daewoo Aerospace (now part of KAI), and license-manufactured KF-16.

 

The mother program, code-named KTX-2, began in 1992, but the Ministry of Finance and Economy suspended the original project in 1995 due to financial constraints. The basic design of the aircraft was set by 1999, and eventually the development of the aircraft was funded 70% by the South Korean government, 17% by KAI, and 13% by Lockheed Martin.

 

In general, the T-50 series of aircraft closely resembles the KF-16 in configuration, but it actually is a completely new design: the T-50 is 11% smaller and 23% lighter than an F-16, and in order to create enough space for the two-seat cockpit, the air intake was bifurcated and placed under the wing gloves, resembling the F/A-18's layout.

 

The aircraft was formally designated as the T-50 'Golden Eagle' in February 2000, the T-50A designation had been reserved by the U.S. military to prevent it from being inadvertently assigned to another aircraft model. Final assembly of the first T-50 took place between 15 January and 14 September 2001. The first flight of the T-50 took place in August 2002, and initial operational assessment from 28 July to 14 August 2003.

 

The trainer has a cockpit for two pilots in a tandem arrangement, both crew members sitting in "normal" election seats, not in the F-16's reclined position. The high-mounted canopy is applied with stretched acrylic, providing the pilots with good visibility, and has been tested to offer the canopy with ballistic protection against 4-lb objects impacting at 400 knots.

 

The ROKAF, as original development driver, placed an initial production contract for 25 T-50s in December 2003, with aircraft scheduled to be delivered between 2005 and 2009. Original T-50 aircraft were equipped with the AN/APG-67(v)4 radar from Lockheed Martin. The T-50 trainer is powered by a GE F404 engine built under license by Samsung Techwin. Under the terms of the T-50/F404-102 co-production agreement, GE provides engine kits directly to Samsung Techwin who produces designated parts as well as performing final engine assembly and testing.

 

The T-50 program quickly expanded beyond a pure trainer concept to include the TA-50 armed trainer aircraft, as well as the FA-50 light attack aircraft, which has already similar capabilities as the multirole KF-16. Reconnaissance and electronic warfare variants were also being developed, designated as RA-50 and EA-50.

 

The TA-50 variant is a more heavily armed version of the T-50 trainer, intended for lead-in fighter training and light attack roles. It is equipped with an Elta EL/M-2032 fire control radar and designed to operate as a full-fledged combat platform. This variant mounts a lightweight three-barrel cannon version of the M61 Vulcan internally behind the cockpit, which fires linkless 20 mm ammunition. Wingtip rails can accommodate the AIM-9 Sidewinder missile, a variety of additional weapons can be mounted to underwing hardpoints, including precision-guided weapons, air-to-air missiles, and air-to-ground missiles. The TA-50 can also mount additional utility pods for reconnaissance, targeting assistance, and electronic warfare. Compatible air-to-surface weapons include the AGM-65 Maverick missile, Hydra 70 and LOGIR rocket launchers, CBU-58 and Mk-20 cluster bombs, and Mk-82, -83, and -84 general purpose bombs.

 

Among the operators of the TA-50 are the Philippines, Thailand and the ROKAF, and the type has attracted a global interest, also in Europe. The young Republic of Scotland Air Corps (locally known as Poblachd na h-Alba Adhair an Airm) chose, soon after the country's independence from the United Kingdom, after its departure from the European Union in 2017, the TA-50 as a complement to its initial procurements and add more flexibility to its small and young air arm.

 

According to a White Paper published by the Scottish National Party (SNP) in 2013, an independent Scotland would have an air force equipped with up to 16 air defense aircraft, six tactical transports, utility rotorcraft and maritime patrol aircraft, and be capable of “contributing excellent conventional capabilities” to NATO. Outlining its ambition to establish an air force with an eventual 2,000 uniformed personnel and 300 reservists, the SNP stated the organization would initially be equipped with “a minimum of 12 interceptors in the Eurofighter/Typhoon class, based at Lossiemouth, a tactical air transport squadron, including around six [Lockheed Martin] C-130J Hercules, and a helicopter squadron”.

 

According to the document, “Key elements of air forces in place at independence, equipped initially from a negotiated share of current UK assets, will secure core tasks, principally the ability to police Scotland’s airspace, within NATO.” An in-country air command and control capability would be established within five years of a decision in favor of independence, it continues, with staff also to be “embedded within NATO structures”.

This plan was immediately set into action after the country's independence in late 2017 with the purchase of twelve refurbished Saab JAS 39A Gripen interceptors for Quick Reaction Alert duties and upgraded, former Swedish Air Force Sk 90 trainers for the RoScAC. But these second hand machines were just the initial step in the mid-term procurement plan.

 

The twelve KAI TA-50 aircraft procured as a second step were to fulfill the complex requirement for a light and cost-effective multi-purpose aircraft that could be used in a wide variety of tasks: primarily as an advanced trainer for supersonic flight and as a trainer for the fighter role (since all Scottish Gripens were single seaters and dedicated to the interceptor/air defense role), but also as a light attack and point defense aircraft.

 

Scotland was offered refurbished F-16C and Ds, but this was declined as the type was deemed to be too costly and complex. Beyond the KAI T-50, the Alenia Aermacchi M-346 Master and the BAe Hawk were considered, too, but, eventually, a modified TA-50 that was tailored to the RoScAC’s procurement plans was chosen by the Scottish government.

 

In order to fulfill the complex duty profile, the Scottish TA-50s were upgraded with elements from the FA-50 attack aircraft. They possess more internal fuel capacity, enhanced avionics, a longer radome and a tactical datalink. Its EL/M-2032 pulse-Doppler radar has been modified so that it offers now a range two-thirds greater than the TA-50's standard radar. It enables the aircraft to operate in any weather, detect surface targets and deploy AIM-120 AAMs for BVR interceptions. The machines can also be externally fitted with Rafael's Sky Shield or LIG Nex1's ALQ-200K ECM pods, Sniper or LITENING targeting pods, and Condor 2 reconnaissance pods to further improve the machine’s electronic warfare, reconnaissance, and targeting capabilities.

 

Another unique feature of the Scottish Golden Eagle is its powerplant: even though the machines are originally powered by a single General Electric F404 afterburning turbofan and designed around this engine, the RoScAC TF-50s are powered by a Volvo RM12 low-bypass afterburning turbofan. These are procured and serviced through Saab in Sweden, as a part of the long-term collaboration contract for the RoScAC’s Saab Gripen fleet. This decision was taken in order to decrease overall fleet costs through a unified engine.

 

The RM12 is a derivative of the General Electric F404-400. Changes from the standard F404 includes greater reliability for single-engine operations (including more stringent birdstrike protection) and slightly increased thrust. Several subsystems and components were also re-designed to reduce maintenance demands, and the F404's analogue Engine Control Unit was replaced with the Digital Engine Control – jointly developed by Volvo and GE – which communicates with the cockpit through the digital data buses and, as redundancy, mechanical calculators controlled by a single wire will regulate the fuel-flow into the engine.

 

Another modification of the RoScAC’s TA-50 is the exchange of the original General Dynamics A-50 3-barrel rotary cannon for a single barrel Mauser BK-27 27mm revolver cannon. Being slightly heavier and having a lower cadence, the BK-27 featured a much higher kinetic energy, accuracy and range. Furthermore, the BK-27 is the standard weapon of the other, Sweden-built aircraft in RoScAC service, so that further synergies and cost reductions were expected.

 

The Scottish Department of National Defense announced the selection of the TA-50 in August 2018, after having procured refurbished Saab Sk 90 and JAS 39 Gripen from Sweden as initial outfit of the country's small air arm with No. 1 Squadron based at Lossiemouth AB.

 

Funding for the twelve aircraft was approved by Congress on September 2018 and worth € 420 mio., making the Golden Eagle the young country’s first brand new military aircraft. Deliveries of the Golden Hawk TF.1, how the type was officially designated in Scottish service, began in November 2019, lasting until December 2020.

The first four Scottish Golden Hawk TF.1 aircraft were allocated to the newly established RoScAC No. 2 Squadron, based at Leuchars, where the RoScAC took control from the British Army. The latter had just taken over the former air base from the RAF in 2015, losing its “RAF air base” status and was consequentially re-designated “Leuchars Station”, primarily catering to the Royal Scots Dragoon Guards who have, in the meantime, become part of Scotland’s Army Corps. The brand new machines were publically displayed on the shared army and air corps facility in the RoScAC’s new paint scheme on 1st of December 2019 for the first time, and immediately took up service.

 

General characteristics:

Crew: 2

Length: 13.14 m (43.1 ft)

Wingspan (with wingtip missiles): 9.45 m (31 ft)

Height: 4.94 m (16.2 ft)

Wing area: 23.69 m² (255 ft²)

Empty weight: 6,470 kg (14,285 lb)

Max. takeoff weight: 12,300 kg (27,300 lb)

 

Powerplant:

1× Volvo RM12 afterburning turbofan, rated at 54 kN (12,100 lbf) dry thrust

and 80.5 kN (18,100 lbf) with afterburner

 

Performance:

Maximum speed: Mach 1.5 (1,640 km/h, 1,020 mph at 9,144 m or 30,000 ft)

Range: 1,851 km (1,150 mi)

Service ceiling: 14,630 m (48,000 ft)

Rate of climb: 198 m/s (39,000 ft/min)

Thrust/weight: 0.96

Max g limit: -3 g / +8 g

 

Armament:

1× 27mm Mauser BK-27 revolver cannon with 120 rounds

A total of 7 hardpoints (4 underwing, 2 wingtip and one under fuselage)

for up to 3,740 kg (8,250 lb) of payload

  

The kit and its assembly:

A rare thing concerning my builds: an alternative reality whif. A fictional air force of an independent Scotland crept into my mind after the hysterical “Brexit” events in 2016 and the former (failed) public vote concerning the independence of Scotland from the UK. What would happen to the military, if the independence would take place, nevertheless, and British forces left the country?

 

The aforementioned Scottish National Party (SNP) paper from 2013 is real, and I took it as a benchmark. Primary focus would certainly be set on air space defense, and the Gripen appears as a good and not too expensive choice. The Sk 90 is a personal invention, but would fulfill a good complementary role.

Nevertheless, another multi-role aircraft would make sense as an addition, and both M-346 and T-50 caught my eye (Russian options were ruled out due to the tense political relations), and I gave the TA-50 the “Go” because of its engine and its proximity to the Gripen.

 

The T-50 really looks like the juvenile offspring from a date between an F-16 and an F-18. There’s even a kit available, from Academy – but it’s a Snap-Fit offering without a landing gear but, as an alternative, a clear display that can be attached to the engine nozzle. It also comes with stickers instead of waterslide decals. This sounds crappy and toy-like, but, after taking a close look at kit reviews, I gave it a try.

 

And I am positively surprised. While the kit consists of only few parts, moulded in the colors of a ROCAF trainer as expected, the surfaces have minute, engraved detail. Fit is very good, too, and there’s even a decent cockpit that’s actually better than the offering of some “normal” model kits. The interior comes with multi-part seats, side consoles and dashboards that feature correctly shaped instrument details (no decals). The air intakes are great, too: seamless, with relatively thin walls, nice!

 

So far, so good. But not enough. I could have built the kit OOB with the landing gear tucked up, but I went for the more complicated route and trans-/implanted the complete landing gear from an Intech F-16, which is available for less than EUR 5,- (and not much worth, to be honest). AFAIK, there’s white metal landing gear for the T-50 available from Scale Aircraft Conversions, but it’s 1:48 and for this set’s price I could have bought three Intech F-16s…

 

But back to the conversion. This landing gear transplantation stunt sounds more complicated as it actually turned out to be. For the front wheel well I simply cut a long opening into the fuselage and added inside a styrene sheet as a well roof, attached under the cockpit floor.

For the main landing gear I just opened the flush covers on the T-50 fuselage, cut out the interior from the Intech F-16, tailored it a little and glued it into its new place.

 

This was made easy by the fact that the T-50 is a bit smaller than the F-16, so that the transplants are by tendency a little too large and offer enough “flesh” for adaptations. Once in place, the F-16 struts were mounted (also slightly tailored to fit well) and covers added. The front wheel cover was created with 0.5 mm styrene sheet, for the main covers I used the parts from the Intech F-16 kit because they were thinner than the leftover T-50 fuselage parts and feature some surface detail on the inside. They had to be adapted in size, though. But the operation worked like a charm, highly recommended!

 

Around the hull, some small details like missing air scoops, some pitots and antennae were added. In a bout of boredom (while waiting for ordered parts…) I also added static dischargers on the aerodynamic surfaces’ trailing edges – the kit comes with obvious attachment points, and they are a small detail that improves the modern look of the T-50 even more.

 

Since the Academy kit comes clean with only a ventral drop tank as ordnance, underwing pylons from a SEPECAT Jaguar (resin aftermarket parts from Pavla) and a pair of AGM-65 from the Italeri NATO Weapons set plus launch rails were added, plus a pair of Sidewinders (from a Hasegawa AAM set, painted as blue training rounds) on the wing tip launch rails.

Since the T-50 trainer comes unarmed, a gun nozzle had to be added – its position is very similar to the gun on board of the F-16, on the upper side of the port side LERX. Another addition are conformal chaff/flare dispensers at the fin’s base, adding some beef to the sleek aircraft.

  

Painting and markings:

I did not want a grey-in-grey livery, yet something “different” and rather typical or familiar for the British isles. My approach is actually a compromise, with classic RAF colors and design features inspired by camouflage experiments of the German Luftwaffe on F-4F Phantoms and Alpha Jets in the early Eighties.

 

For the upper sides I went for a classic British scheme, in Dark Green and Dark Sea Grey (Humbrol 163 and 164), colors I deem very appropriate for the Scottish landscape and for potential naval operations. These were combined with elements from late RAF interceptors: Barley Grey (Humbrol 167) for the flanks including the pylons, plus Light Aircraft Grey (Humbrol 166) for the undersides, with a relatively high waterline and a grey fin, so that a side or lower view would rather blend with the sky than the ground below.

 

Another creative field were the national markings: how could fictional Scottish roundels look like, and how to create them so that they are easy to make and replicate (for a full set for this kit, as well as for potential future builds…)? Designing and printing marking decals myself was an option, but I eventually settled for a composite solution which somewhat influenced the roundels’ design, too.

My Scottish roundel interpretationconsists of a blue disk with a white cross – it’s simple, different from any other contemporary national marking, esp. the UK roundel, and easy to create from single decal parts. In fact, the blue roundels were die-punched from blue decal sheet, and the cross consists of two thin white decal strips, cut into the correct length with the same stencil, using generic sheet material from TL Modellbau.

 

Another issue was the potential tactical code, and a small fleet only needs a simple system. Going back to a WWII system with letter codes for squadrons and individual aircraft was one option, but, IMHO, too complicated. I adopted the British single letter aircraft code, though, since this system is very traditional, but since the RoScAC would certainly not operate too many squadrons, I rather adapted a system similar to the Swedish or Spanish format with a single number representing the squadron. The result is a simple 2-digit code, and I adapted the German system of placing the tactical code on the fuselage, separated by the roundel. Keeping British traditions up I repeated the individual aircraft code letter on the fin, where a Scottish flag, a small, self-printed Fife coat-or-arms and a serial number were added, too.

 

The kit saw only light weathering and shading, and the kit was finally sealed with matt acrylic varnish (Italeri).

  

Creating this whif, based on an alternative historic timeline with a near future perspective, was fun – and it might spawn more models that circle around the story. A Scottish Sk 90 and a Gripen are certain options (and for both I have kits in the stash…), but there might also be an entry level trainer, some helicopters for the army and SAR duties, as well as a transport aircraft. The foundation has been laid out, now it’s time to fill Scotland’s history to come with detail and proof. ;-)

 

Besides, despite being a snap-fit kit, Academy’s T-50 is a nice basis, reminding me of some Hobby Boss kits but with less flaws (e .g. most of the interiors), except for the complete lack of a landing gear. But with the F-16 and Jaguar transplants the simple kit developed into something more convincing.

Rick doesn't like being on the wrong side of the lens.

My Thanks to John, Mark, Stu and all the boys for a superb day out!

 

City Palace, Udaipur, is a palace complex in Udaipur, in the Indian state Rajasthan. It was built over a period of nearly 400 years being contributed by several kings of the dynasty, starting by the Maharana Udai Singh as the capital of the Sisodia Rajput clan in 1559, after he moved from Chittor. It is located on the east bank of the Lake Pichola and has several palaces built within its complex. Udaipur was the historic capital of the former kingdom of Mewar in the Rajputana Agency and its last capital.

 

The City Palace in Udaipur was built in a flamboyant style and is considered the largest of its type in Rajasthan, a fusion of the Rajasthani and Mughal architectural styles, and was built on a hill top that gives a panoramic view of the city and its surrounding, including several historic monuments such as the Lake Palace in Lake Pichola, the Jag Mandir on another island in the lake, the Jagdish Temple close to the palace, the Monsoon Palace on top of an overlooking hillock nearby and the Neemach Mata temple. These structures are linked to the filming of the James Bond movie Octopussy, which features the Lake Palace and the Monsoon Palace. The subsequent publicity has resulted in the epithet of Udaipur as "Venice of the East". In 2009, Udaipur was rated the top city in the World's Best Awards by Travel + Leisure.

 

HISTORY

The city Palace was built concurrently with establishment of the Udaipur city by Maharana Udai Singh, in 1559 and his successor Maharanas over a period of the next 300 years. It is considered the largest royal complex in Rajasthan and is replete with history. Founding of the city and building of the palace complex can not be looked in isolation as the Maharanas lived and administered their kingdom from this palace.

 

Prior to moving their capital from Udaipur to Chittor≤≥, the Mewar kingdom had flourished initially in Nagda (30 kilometres to the north of Udaipur), established in 568 AD by Guhil, the first Mewar Maharana. In the 8th century, the capital was moved to Chittor, a hill top fort from where the Sisodias ruled for 80 years. Maharana Udai Singh II inherited the Mewar kingdom at Chittor in 1537 but by that time there were signs of losing control of the fort in wars with the Mughals. Udai Singh II, therefore, chose the site near Lake Pichola for his new kingdom because the location was well protected on all sides by forests, lakes and the Aravalli hills. He had chosen this site for his new capital, much before the sacking of Chittor by Emperor Akbar, on the advice of a hermit he had met during one of his hunting expeditions.

 

At his capital Udaipur, Maharana Udai Singh soon faced defeat at the hands of Mughal Emperor Akbar. He soon moved to Udaipur to the chosen location to establish his new capital. The earliest royal structure he built here was the Royal courtyard or 'Rai Angan', which was the beginning of the building of the City Palace complex, at the place where the hermit had advised Maharana to build his Capital.

 

After Udai Singh’s death in 1572, his son Maharana Pratap took the reins of power at Udaipur. He was successful in defeating Akbar at the battle of Haldighati in 1576 and thereafter Udaipur was peaceful for quite some years. With this, prosperity of Udaipur ensued, palaces were built on the shore and in the midst of the Pichola lake. Concurrently art, particularly miniature painting, also flourished.

 

But in 1736, the marauding Marathas attacked Udaipur and by the end of the century the Mewar state was in dire straits and in ruins. However, the British came to Mewar’s rescue in the 19th century and soon the State of Mewar got re-established and prospered under British protection, under a treaty signed with the British. However, the British were not allowed to replace them. Once India got independence in 1947, the Mewar Kingdom, along with other princely states of Rajasthan, merged with the Democratic India, in 1949. The Mewar Kings subsequently also lost their special royal privileges and titles. However, the successor Maharanas have enjoyed the trust of their people and also retained their ownership of the palaces in Udaipur. They are now running the palaces by creating a trust, called the Mewar Trust, with the income generated from tourism and the heritage hotels that they have established in some of their palaces. With the fund so generated they are running charitable hospitals, educational institutions and promoting the cause of environmental preservation.

 

LEGEND

Historical legend narrated to the selection of the site for the palace is about a hermit meeting Maharana Udai Singh when he was on a hunting trail in the Udaipur hills. The Maharana met the hermit who was meditating on top of a hill above the Pichola Lake and sought the hermit’s blessings. The hermit advised the Maharana to build his palace at that very spot and that is where the palace complex came to be established at Udaipur.

 

GEOGRAPHY

The city palace located in Udaipur city at 24.576°N 73.68°E, which is set with an average elevation of 598 metres.

 

CLIMATE

The climate of Udaipur reflects the climate at the city palace. It is tropical, with the mercury recording between a maximum of 38.3 °C and a minimum of 28.8 °C during summers. Winter is cold with the maximum temperature rising to 28 °C and the minimum dipping to 11.6 °C. The average annual rainfall is 64 cm.

 

STRUCTURES

The series of palaces packed in the city palace complex, facing east (as customarily appropriate for the Maharana dynasty – the Sun dynasty), behind an exquisite facade of 244 metres length and 30.4 metres height, were built on a ridge on the east of lake Pichola. They were built over a long period, from 1559 onwards, by 76 generations of Sisodia Rajputs or Suryavanshi Rajputs (worshippers of Sun god). Several Maharanas (the title Maharana is distinctly different from Maharajah, as the former connotes a warrior and the latter a ruler or a king) starting with Udai Mirza Singh II, have richly contributed to this edifice, which comprises an agglomeration of structures, including 11 small separate palaces. The unique aspect of this conglomeration is that the architectural design (a rich blend of Rajasthani, Mughal, Medieval, European and Chinese Architecture) is distinctly homogeneous and eye catching. The palace complex has been built entirely in granite and marble. The interiors of the palace complex with its balconies, towers and cupolas exhibit delicate mirror-work, marble-work, murals, wall paintings, silver-work, inlay-work and leftover of colored glass. The complex provides a fine view of the lake and the Udaipur city from its upper terraces.

 

Located with the picturesque backdrop of rugged mountains, beside the Pichola lake on its shore, the city palace complex painted in gleaming white color has been compared to the Greek islands, such as the Mykonos.

 

The famous structures or palaces viewed from the Lake Palace appear like a fort. They are interlinked inside the complex through a number of chowks or quadrangles with zigzag corridors (planned in this fashion to avoid surprise attacks by enemies). Erected in the complex, after entering through the main Tripolia (triple) gate, are the Suraj Gokhda (public address facade), the Mor-chowk (Peacock courtyard), the Dilkhush Mahal (heart’s delight), the Surya Chopar, the Sheesh Mahal (Palace of glass and mirrors), the Moti Mahal (Palace of Pearls), the Krishna Vilas (named after Lord Krishna), Shambu Niwas (royal residence now), the Bhim Vilas, the Amar Vilas (with a raised garden) that faces the Badi Mahal (the big palace), the Fateprakash Palace and the Shiv Niwas Palace (the latest addition to the complex); the last two have been converted into heritage hotels. Details of all these structures are elaborated. The vast collection of structures are termed to form ‘a city within a city’ set with facilities of post office, bank, travel agency, numerous craft shops and also an Indian boutique belonging to the World Wildlife Fund (WWF) for Nature. The entire complex is the property of the Mewar royal family and a number of trusts take care of the running and maintenance of the structures. The earliest royal structure built in the complex was the Royal courtyard or Rai Angan.

 

GATEWAYS

Gateways, colloquially called Pols, are set to the east of Udaipur city that was established by Maharana Udai Singh II, concurrently with the City Palace. A number of impressive gateways provide access to the palace complex.

 

The main entry from the city is through the 'Bara Pol' (Great Gate), which leads to the first courtyard. Bara Pol (built in 1600) leads to the ‘Tripolia Pol', a triple arched gate built in 1725, which provides the northern entry. The road between this gate and the palace is lined with shops and kiosks owned by craftsmen, book-binders, miniature painters, textile dealers and antique shops. Between these two gates, eight marble arches or Toranas are erected. It is said that the Maharanas used to be weighed here with gold and silver, which was then distributed among the local people. Following the Tripolia gate is an arena in front of the Toran Pol and the facade palace, where elephant fights were staged in the past to test their prowess before starting on war campaigns.

 

The main block of the city palace at Udaipur is approached through a modest door from the Ganesha Deodhi terrace. The door is flanked by whitewashed walls vibrantly painted with martial animals in the traditional Rajput style.

 

AMAR VILAS

Amar Vilas is the uppermost court inside the complex, which is a raised garden. It provides entry to the Badi Mahal. It is a pleasure pavilion built in Mughal style. It has cussed arcades enclosing a square marble tub. Amar Vilas' is the highest point of the City palace and has wonderful hanging gardens with fountains, towers and terraces.

 

BADI MAHAL

Badi Mahal (Great Palace) also known as Garden Palace and is the exotic central garden palace that is situated on a 27 metres high natural rock formation bis-a-bis the rest of the palace. The rooms on the ground floor appear to be at the level of the fourth floor in view of the height difference to its surrounding buildings. There is a swimming pool here, which was then used for Holi festival (festival of colors) celebration. In an adjoining hall, miniature paintings of 18th and 19th centuries are displayed. In addition, wall paintings of Jag Mandir (as it appeared in the 18th century), Vishnu of Jagdish temple, the very courtyard and an elephant fight scene are depicted.

 

The elephant fight depicted in a painting on the wall was a representation of the real elephant fights, which used to be organized by the Maharanas. It is mentioned that the elephants used to be fed hashish (opium) before arranging the fights. An interesting observation is that the word ‘assassin’ is a derivative of the word ‘hashish’. The last such fight was reported in 1995.

 

BHIM VILAS

Bhim Vilas has a gallery of a remarkable collection of miniature paintings that depict the real life stories of Radha-Krishna.

 

CHINI CHITRASHALA

Chini Chitrashala (Chinese art place) depicts Chinese and Dutch ornamental tiles.

 

CHOTI CHITRASHALI

Choti Chitrashali or 'Residence of Little Pictures', built in early 19th century, has pictures of peacocks.

 

DILKHUSHA MAHAL

Dilkhusha Mahal or ‘Palace of Joy’ was built in 1620.

 

DURBAR HALL

Durbar Hall was built in 1909 within the Fatepraksh Palace (now a heritage hotel) Official functions such as State banquets and meetings were held here. The gallery of the hall was used by the Royal ladies to observe the Durbar proceedings. This hall has luxuriant interior with some unusually large chandeliers. Weapons of the maharanas and also some of their unique portraits are also depicted here. The foundation stone for this hall was laid by Lord Minto, the Viceroy of India, in 1909, during the rule of Maharana Fateh Singh and was then called Minto Hall.

 

FATEPRAKASH PALCE

Fateprakash Palace, which is now run as a luxury hotel, has a crystal gallery that consists of crystal chairs, dressing tables, sofas, tables, chairs and beds, crockery, table fountains which were never used. There is also a unique jewel studded carpet here. Maharaja Sajjan Singh had ordered these rare items in 1877 from F& C Osler & Co of London but he died before they arrived here. It is said that the packages containing these crystals remained unopened for 110 years.

 

JAGDISH MANDIR

Jagdish Mandir, located 150 metres north of the city palace, was built in 1652 in Indo-Aryan architectural style. It is a large and aesthetically elegant temple where an idol of Lord Jagannath, a form of Lord Vishnu made in black stone is deified in the sanctum. The temple walls and the sikhara or tower are decorated with carvings of Vishnu, scenes from Lord Krishna’s life and figurines of nymphs or apsaras. A brass image of Garuda (half-bird, half-man image, which is Lord Vishnu’s vehicle), is placed in a separate shrine in front of the temple. Flanking the steps up the temple decoration of statues of elephants are seen. The street square, where the temple is located, is also known as Jagdish Chowk from where several roads radiate in different directions.

 

KRISHNA VILAS

Krishna Vilas is another chamber, which has rich collection of miniature paintings that portray royal processions, festivals and games of the Maharanas. However, there is tragic story linked to this wing of the City Palace. In the 19th century, a royal princess was unable to choose from two suitors seeking her hand in marriage, one from the royal family of Jaipur and another from Jodhpur, and hence in a state of dilemma, she poisoned herself to death.

 

LAXMI VILAS CHOWK

Laxmi Vilas Chowk is an art gallery with a distinctive collection of Mewar paintings.

 

MANAK MAHAL

The Manek mahal approached from the Manak Chowk is an enclosure for formal audience for the Udaipur rulers. It has a raised alcove inlaid completely in mirror glass. Sun-face emblems, in gleaming brass, religious insignia of the Sisodia dynasty are a recurring display at several locations in the City Palace; one of these prominent emblems is depicted on the façade of the Manak Chowk, which can also be seen from the outermost court below. The largest of such an emblem is also seen on the wall of the Surya Chopar, a reception centre at the lower level. Surya or Sun emblem of the Mewar dynasty depicts a Bhil, the Sun, Chittor Fort and a Rajput with an inscription in Sanskrit of a quotation from the Bhagavad Gita (Hindu holy scripture), which means “God Helps those who do their duty". It was customary for the Maharanas to offer obeisance to the Sun facing east, every morning before taking breakfast.

 

MOR CHOK

Mor Chok or Peacock square is integral to the inner courts of the palace. The elaborate design of this chamber consists of three peacocks (representing the three seasons of summer, winter and monsoon) modeled in high relief and faced with coloured glass mosaic, built into successive niches in the wall area or jharoka, These were built during Maharana Sajjan Singh’s reign, 200 years after the palace was established. The peacocks have been crafted with 5000 pieces of glass, which shine in green, gold and blue colours. The apartments in front of the Chowk are picturesquely depicted with scenes of Hindu god Lord Krishna’s legends. At the upper level, there is a projecting balcony, which is flanked by inserts of coloured glass. In an adjoining chamber, called the Kanch-ki-Burj, mosaic of mirrors adorn the walls. The Badi Charur Chowk within this chowk is a smaller court for private use. Its screen wall has painted and inlaid compositions depicting European men and Indian women. Proceeding further from the Mor-Chowk, in the Zenana Mahal or women’s quarters exquisitely designed alcoves, balconies, colored windows, tiled walls and floors are seen.

 

MUSEUM

n 1974, a part of the city palace and the 'Zenana Mahal' (Ladies Chamber) were converted into a museum. The museum is open for public. There is an interesting exhibit of a freaky monkey holding a lamp and also portraits of maharajas displaying a spectacular array of mustaches. ‘Lakshmi Chowk' is an elegant white pavilion in the same precinct.

 

RANG BHAWAN

Rang Bhawan is the palace that used to contain royal treasure. There are temples of Lord Krishna, Meera Bai and Shiva, located here.

 

SHEESH MAHAL

Sheess Mahal or Palace of Mirrors and glasses was built in 1716.

 

A shrine of Dhuni Mata is also located in the complex. This location is considered as the oldest part of the Palace, where a sage spent his entire life meditating.

 

THE PALACE IN FILM & TELEVISION

The palace was used as a hotel in the 1985 James Bond film Octopussy, where Bond (played by Roger Moore) stayed as he began his quest to apprehend the villainous Kamal Khan (Louis Jordan).

 

A 1991 documentary film directed for television by Werner Herzog is called Jag Mandir and consists of footage of an elaborate theatrical performance for the Maharana Arvind Singh Mewar at the City Palace staged by André Heller.

 

The palace was used for filming part of Goliyon Ki Raasleela Ram-Leela (English: A Play of Bullets: Ram-Leela) 2013 directed by Sanjay Leela Bhansali.

 

WIKIPEDIA

www.GirlWithCurves.com

Nikon D750

AF-S Nikkor 50mm 1.8G

oocjpeg

Nikon D7100

AF-S DX VR Zoom-Nikkor 18-55mm f/3.5-5.6G

FOTO 1140 project 3: Maximum Depth of Field

 

Camera: Canon EOS REBEL T3i

Focal Length: 24mm

ISO: 200

Shutter: 1/160

Aperture: f/16

Date: 6-25-16

Time of Day: 11:20am

Intent: To capture Cincinnati's skyline with the Roebling Bridge leading to it.

Aufnahmedatum 16.03.2019

Eröffnung Rotteckring mit hist. Fahrzeugen

Fahnenbergplatz, Tw 56

This is *why* folks should never listen to me as my ideas can usually be described as hare-brained. Yes, I came up with this idea and the Deadpool cosplayer ran away with it. GMTA? lol

 

Many thanks to the vendor (name and link to be added) for letting us borrow their prop outside of their booth.

There was some real yoga position stuff going on here!

White pelicans at Leonabelle Turnbull Birding Center

Golden chalice vine (Solandra maxima), Solanaceae family, exhibits large, 20cm funnel-shaped flowers, shifting from white to orange.

en.wikipedia.org/wiki/Solandra_maxima#:~:text=Solandra%20....

[Tirages meilleurs jusqu'à 19 x 26 cm maximum]

 

[Prints best within 19 x 26 cm / 7 x 10 inches]

  

Codi von Richthofen,

Saint Joan of Arc Superstar ©

leucanthemum maximum

Recreation Room.

i have played with my camera!

 

Schweiz / Nidwalden - Vierwaldstättersee

 

seen from Stanserhorn

 

gesehen vom Stanserhorn

 

Lake Lucerne (German: Vierwaldstättersee, literally "Lake of the four forested settlements" (in English usually translated as forest cantons), French: lac des Quatre-Cantons, Italian: lago dei Quattro Cantoni) is a lake in central Switzerland and the fourth largest in the country.

 

Geography

 

The lake has a complicated shape, with several sharp bends and four arms. It starts in the south–north bound Reuss Valley between steep cliffs above the Urnersee from Flüelen towards Brunnen to the north before it makes a sharp bend to the west where it continues into the Gersauer Becken. Here is also the deepest point of the lake with 214 m (702 ft). Even further west of it is the Buochser Bucht, but the lake sharply turns north again through the narrow opening between the Unter Nas (lower nose) of the Bürgenstock to the west and the Ober Nas (upper nose) of the Rigi to the east to reach the Vitznauer Bucht. In front of Vitznau below the Rigi the lake turns sharply west again to reach the center of a four-arm cross, called the Chrütztrichter (Cross Funnel). Here converge the Vitznauer Bucht with the Küssnachtersee from the north, the Luzernersee from the west, and the Horwer Bucht and the Stanser Trichter to the south, which is to be found right below the northeast side of the Pilatus and the west side of the Bürgenstock. At the very narrow pass between the east dropper of the Pilatus (called Lopper) and Stansstad the lake reaches its southwestern arm at Alpnachstad on the steep southern foothills of the Pilatus, the Alpnachersee. The lake drains its water into the Reuss in Lucerne from its arm called Luzernersee (which literally translates as Lake of Lucerne).

 

The entire lake has a total area of 114 km² (44 sq mi) at an elevation of 434 m (1,424 ft) a.s.l., and a maximum depth of 214 m (702 ft). Its volume is 11.8 km³. Much of the shoreline rises steeply into mountains up to 1,500 m above the lake, resulting in many picturesque views including those of the mountains Rigi and Pilatus.

 

The Reuss enters the lake at Flüelen, in the part called Urnersee (Lake of Uri, in the canton of Uri) and exits at Lucerne. The lake also receives the Muota at Brunnen, the Engelberger Aa at Buochs, and the Sarner Aa at Alpnachstad.

 

It is possible to circumnavigate the lake by train and road, though the railway route circumvents the lake even on the north side of the Rigi via Arth-Goldau. Since 1980, the A2 motorway leads through the Seelisberg Tunnel in order to reach the route to the Gotthard Pass in just half an hour in Altdorf, Uri right south of the beginning of the lake in Flüelen.

 

Steamers and other passenger boats ply between the different villages and towns on the lake. It is a popular tourist destination, both for native Swiss and foreigners, and there are many hotels and resorts along the shores. In addition, the meadow of the Rütli, traditional site of the founding of the Swiss Confederation, is on the Urnersee shore. A 35 km commemorative walkway, the Swiss Path, was built around the Lake of Uri to celebrate the country's 700th anniversary in 1991.

 

Archaeologists surveying the lake-bed (during the construction of a pipeline) from 2019 to 2021 found the remains of a Bronze Age village with artifacts dating to around 1000 BC. Later, the new findings indicated that the area was settled 2,000 years earlier than historians previously thought.

 

Lake Lucerne borders on the three original Swiss cantons of Uri, Schwyz, and Unterwalden (which today is divided into the cantons of Obwalden and Nidwalden), as well as the canton of Lucerne, thus the name Vierwaldstättersee (lit.: Lake of the Four Forested Settlements). Many of the oldest communities of Switzerland are along the shore, including Küssnacht, Weggis, Vitznau, Gersau, Brunnen, Altdorf, Buochs, and Treib.

 

Lake Lucerne is singularly irregular and appears to lie in four different valleys, all related to the conformation of the adjoining mountains. The central portion of the lake lies in two parallel valleys whose direction is from west to east, the one lying north, the other south of the ridge of the Bürgenstock. These are connected through a narrow strait, scarcely one kilometre wide, between the two rocky promontories called respectively Unter Nas and Ober Nas (Lower and Upper Nose). It is not unlikely that the southern of these two divisions of the lake—called Buochser Bucht—formerly extended to the west over the isthmus whereon stands the town of Stans, thus forming an island of the Bürgenstock. The west end of the main branch of the lake, whence a comparatively shallow bay extends to the town of Lucerne, is intersected obliquely by a deep trench whose south-west end is occupied by the branch called Alpnachersee, while the north-east branch forms the long arm of Küssnacht, Küssnachtersee. These both lie in the direct line of a valley that stretches with scarcely a break in between the Uri Alps and the Emmental Alps. At the eastern end of the Gersauer Becken, where the containing walls of the lake-valley are directed from east to west, it is joined at an acute angle by the arm of Uri, or the Urnersee, lying in the northern prolongation of the deep cleft that gives a passage to the Reuss, between the Uri Alps and the Glarus Alps.

 

The Urnersee occupies the northernmost and deep portion of the great cleft of the Reuss Valley, which has cut through the Alpine ranges from the St Gotthard Pass to the neighbourhood of Schwyz. From its eastern shore the mountains rise in almost bare walls of rock to a height of from 3,000 to 4,000 ft (910 to 1,220 m) above the water. The two highest summits are the Fronalpstock and the Rophaien (2078 m). Between them the steep glen or ravine of the Riemenstaldener Tal descends to Sisikon, the only village with Flüelen right on the shore on that side of the Urnersee. On the opposite or western shore, the mountains attain still greater dimensions. The Niederbauen Chulm is succeeded by the Oberbauenstock, and farther south, above the ridge of the Scharti, appear the snowy peaks of the Gitschen and the Uri Rotstock (2,928 m). In the centre opens the Reuss Valley, backed by the rugged summits of the Urner and Glarner Alps.

 

The breadth of these various sections of the lake is very variable, but is usually between one and two miles (3 km). The lake's surface, whose mean height above the sea is 434 metres, is the lowest point of the cantons of Uri, Obwalden and Nidwalden. Originally the lake was susceptible to variations in level and flooding along its shoreline. Between 1859 and 1860, the introduction of a needle dam in the Reuss in the city of Lucerne, just upstream from the Spreuerbrücke, allowed the lake level to be stabilised.

 

The culminating point of the lake's drainage basin, as well as Central Switzerland, is the Dammastock at 3,630 metres above sea level.

 

Name

 

The name of Vierwaldstättersee is first used in the 16th century. Before the 16th century, the entire lake was known as Luzerner See "Lake Lucerne", as remains the English (and partly Italian, as Lago di Lucerna) usage. The (three) "Waldstätte(n)" (lit.: "forested sites/settlements", in English usually translated as forest cantons[6]) since the 14th century were the confederate allies of Uri, Schwyz and Unterwalden. The notion of "Four Waldstätten" (Vier Waldstätten), with the addition of the canton of Lucerne, is first recorded in the 1450s, in an addition to the "Silver Book" of Egloff Etterlin of Lucerne.

 

The nine different parts of the lake have individual designations:

 

Urnersee ("Lake of Uri"): The first part of the lake, at the mouth of the Reuss between Flüelen and Brunnen.

Gersauer Becken ("Basin of Gersau") next to Gersau below the Rigi massif is the deepest part of the lake.

Buochser Bucht ("Bay of Buochs"): The bay of Bouchs, where the Engelberger Aa enters the lake.

Vitznauer Bucht ("Bay of Vitznau"): The part between the Bürgenstock and Rigi.

Alpnachersee ("Lake of Alpnach"): the almost separate, southern arm below the southern mountainside of Pilatus near Alpnach.

Stanser Trichter ("Funnel of Stans"): The part north of the Pilatus, west of Bürgenstock, and in front of Hergiswil and Stansstad.

Küssnachtersee ("Lake of Küssnacht"): The most northern arm, west of the Rigi with Küssnacht SZ at its northern end.

Chrütztrichter ("Cross Funnel"): The meeting point of Stanser Trichter, Luzernersee, Küssnachtersee, and Vitznauer Bucht.

Luzernersee ("Lake of Lucerne"): in German usage now limited to the bay at Lucerne as far as Meggenhorn, with its effluence of the Reuss.

 

Navigation

 

The lake is navigable, and has formed an important part of Switzerland's transport system for many centuries, and at least since the opening of the first track across the Gotthard Pass in 1230. This trade grew with the opening of a new mail coach road across the pass in 1830. This road had its northern terminus at Flüelen at the extreme eastern end of the lake, and the lake provided the only practical onward link to Lucerne, and hence the cities of northern Switzerland and beyond.

 

Whilst the development of Switzerland's road and rail networks has relieved the lake of much of its through traffic, it continues to be used by a considerable number of vessels, both private and public. Much of this usage is tourist or leisure oriented, but the lake continues to provide practical public and cargo transport links between the smaller lakeside communities.

 

Passenger boats of the Schifffahrtsgesellschaft des Vierwaldstättersees (SGV) provide services on the lake, including many run by historic paddle steamers. The SGV serves 32 places along the shore of the lake, with interchange to both main line and mountain railways at various points. Under separate management, the Autofähre Beckenried-Gersau provides a car ferry service between Beckenried, on the south bank of the lake, and Gersau on the north.

 

Cargo barges, to a local design known as Nauen, are still used on the lake. Some have been converted for use as party boats. Other barges are used by the gravel dredging industry that operates on the lake, using large dredgers to obtain sand and gravel for use in the construction industry.

 

Cultural references

 

Beethoven's Moonlight Sonata derives its name from an 1832 description of the first movement by poet and music critic Ludwig Rellstab, who compared it to moonlight shining upon Lake Lucerne.

 

Gioacchino Rossini uses this in his William Tell Overture Section A: Sunrise over the Alps.

 

Rowing

 

Lake Lucerne has twice been used as a venue for the European Rowing Championships: in 1908 and then in 1926. The nearby Rotsee has since 1933 been used for rowing regattas instead.

 

Tourism

 

On the way south, the English discovered the mountains of central Switzerland. Several spa and bathing resorts such as Weggis or Gersau were created. In 1871, the very first rack railway in Europe, the Vitznau-Rigi Railway, was opened. In 1889 the steepest cog railway in the world was built from Alpnachstad to Mount Pilatus. Mark Twain described an ascent to the Rigi, which led to the blossoming of Swiss tourism in the United States in the 19th century. One of the largest steamship fleets in Europe operates with five steamships on Lake Lucerne.

 

In the area surrounding the lake and on terraces at medium height (for example Morschach and Seelisberg) there are numerous places for tourists. The Rigi, Pilatus, the Bürgenstock, the Stanserhorn, the Buochserhorn, and the two legends, the Urirotstock and the Fronalpstock are attractive panoramic mountains near Lake Lucerne. Most of them can be reached by mountain railways, some of which have their valley station near boat stations on the lake.

 

There are numerous locations on the lake that are important in Swiss cultural and tourism history: Rütli, Tellsplatte, Tell Chapel, Carving Tower of Stansstad, Neu-Habsburg, Schillerstein, Treib, Astrid Chapel (Küssnacht) and Meggenhorn Castle.

 

Watersports

 

Different sports are possible in some separate areas due to the water and wind conditions. The lake is accessible from boat and yacht harbors, to lake resorts and pools (e.g. the Lido pool in Lucerne, built in 1929 by Arnold Berger). Therefore, the lake can be easily accessible from both shores. The See-Club Luzern was founded in 1881, which is now Switzerland's largest rowing club, as well as the Reuss Luzern rowing club (Ruderclub Reuss Luzern) in 1904. The Lucerne Yacht Club (Yachtclub Luzern) has existed since 1941 and has been running since 1966 a boathouse and buoy field on Churchill-Quai in Lucerne.

 

The Brunnen water sports club (Wassersportclub Brunnen), founded in 1958, held on Lake Lucerne in the first years of its existence international motorboat races and water ski championships. In 1965 the association chose a new name for the club: Lake Lucerne Water Sports Club (Wassersport-Club Vierwaldstättersee). The Central Switzerland Motorboat Club (Motorbootclub Zentralschweiz) was established in 1980 and the Hergiswil Water Sports Club (Wassersportclub Hergiswil) in 1986. SchweizMobil has created a canoe tour across Lake Lucerne between Brunnen and Gersau. Due to the wind in the Reuss Valley, the southern part of Lake Uri between the campground at Gruonbachstrand in Flüelen and Isleten is a center of windsurfing.

 

Diving

 

There are about ten places where you can dive without a boat in Lake Lucerne. The water is rather chilly all year round and therefore mostly very clear. In Lake Uri, at Sisikon, one can dive to a fragmented steep vertical wall, at the northern portal of the Schieferneggtunnel. The Lediwrack Bruno lies in front of Brunnen at a depth of 15 meters. Other well-known diving spots are in front of Vitznau, Weggis, Gersau and Hergiswil.

 

(Wikipedia)

 

The Stanserhorn is a mountain in Switzerland, located in the canton of Nidwalden near to the border with Obwalden, with the peak at 1,898 metres (6,227 ft) above sea level.

 

It is a popular tourist destination, which can be reached from the adjacent town of Stans by a funicular railway and cable car, or via walking routes from Stans or Dallenwil.

 

History

 

The first public transport route to the peak was started in 1891 and completed in 1893, a three section funicular railway. The builders were the business partners Franz Josef Bucher-Durrer and Josef Durrer-Gasser.

 

The first section started from Stans town, through the low pastures above the town and over three level crossings, to an intermediate station at Kälti (also sometimes spelt Chälti). The second section continued through forest to another intermediate station at Bluematt (also sometimes spelt Blumatt), then the third section crossed the high pastures and the exposed slope leading up to the summit station and hotel. This third section included a 160 metres (520 ft) long tunnel and a number of avalanche protection walls; the final section of it was carried on a stone embankment. Each section was electrically powered (making it one of the world's first electrically powered mountain railways), with the complete trip to the summit taking 45 minutes.

 

The railway ran a tourist service until 1970, when on the night of the 2/3 October the funicular cable was struck by lightning. This started a fire which destroyed the summit hotel and the driving engine for the third section in its basement. As a result of this, and also the imminent expiry of the concession, the second funicular section stopped operating in 1974. Part of the driving engine of this section can be seen today outside the summit buildings, while parts of two cars can still be seen at the former Bluematt station.

 

A new cable car was built to replace the two upper funicular sections, which started operation in May 1975. The first funicular section continued in operation, as it does to this day.

 

In 2001 a revolving restaurant was built at the summit station, and in 2003 an outside observation deck was added.

 

In 2010 construction work started on a new cable car to replace the 1975 installation. This was to be a new design, the world's first "CabriO" double deck open top cable car, built by Garaventa. Carrying 60 passengers per cabin with room for 30 on the open deck, passengers are able to observe the mountain scenery as well as the cable and engineering installations during the six-minute journey. While this new cable car was being built, the first funicular section and its original wooden cars were renovated. The final run of the former cable car was on 23 October 2011;[8] the renovated funicular and new "CabriO" were opened on 29 June 2012.

 

Visiting

 

he funicular railway and cable car normally run daily from mid-April to mid-November.

 

The journey to the top starts in Stans town at the original 1893 bottom station (450 metres (1,480 ft) elevation), close to Stans railway station on the Luzern-Engelberg line. The journey, on the original wooden funicular wagons, takes 9 minutes to the Kälti intermediate station (714 metres (2,343 ft) altitude). From here the "CabriO" cable car takes 61⁄4 minutes to the summit station (1,850 metres (6,070 ft) altitude). The cable car closely follows the route of the original second and third stage funiculars, and the remains of the track and the Bluematt station can still be seen.

 

The summit buildings include a self-service restaurant, three meeting/dining rooms, a souvenir shop, and a sun terrace and observation deck.

 

From the summit buildings, a round trip walk is available around the summit (30 minutes), or to the peak at 1,898 metres (6,227 ft) altitude. From the peak, on a clear day, as well as the mountains around there are views as far as Alsace and the Black Forest in Germany. Ten lakes in total are visible: the Zugersee, Wichelsee, Vierwaldstättersee, Sempachersee, Sarnersee, Hallwilersee, Gerzensee, Bannalpsee, Baldeggersee and Alpnachersee.

 

A variety of hiking trail routes are available down to Bluematt-Kälti-Stans, Ahornhütte-Büren, Wiesenberg-Dallenwil, or Wirzweli-Wolfenschiessen. The routes to/from the summit are closed in winter or in bad weather.

 

(Wikipedia)

 

Der Vierwaldstättersee (französisch Lac des Quatre-Cantons; italienisch Lago dei Quattro Cantoni, Lago di Lucerna; rätoromanisch Lai dals Quatter Chantuns) ist ein von Bergen der Voralpen umgebener Alpenrandsee in der Zentralschweiz. Er liegt auf dem Gebiet der Kantone Uri, Schwyz, Unterwalden (d. h. Nid- und Obwalden) und Luzern. Die grössten Orte am Ufer sind Luzern, Küssnacht, Horw und Brunnen. Der See ist 114 km² gross, liegt auf einer Höhe von 433 m ü. M. und ist 214 m tief. Da es sich um einen charakteristischen Zungenbeckensee mit mehreren Zweigbecken handelt, ist die Uferlänge im Bezug zur Seefläche mit etwa 150 km relativ gross.

 

Name

 

Seinen Namen hat der Vierwaldstättersee von den vier an ihn angrenzenden Waldstätten (heutige Kantone). Bis ins 16. Jahrhundert wurde die Bezeichnung Luzerner See verwendet.

 

Entstehung

 

Der Vierwaldstättersee entstand in den Eiszeiten, u. a. der letzten Eiszeit, durch Erosion des Reussgletschers. Der See bildete sich als Gletscherrandsee am Ende der Eiszeit vor rund 12'000 Jahren. Im Gletschergarten Luzern zeigt eine Dokumentation die Geschichte der Alpen, der Eiszeiten und der Gletscher in den Zentralalpen.

 

Geographie

 

Zufluss

 

Die Hauptzuflüsse des Vierwaldstättersees sind die Reuss mit der Einmündung bei Flüelen und Seedorf, die Engelberger Aa bei Buochs, die Sarner Aa bei Alpnachstad und die Muota bei Brunnen. Die Reuss fliesst mit einem starken Gefälle aus dem Gotthardmassiv und führt grosse Mengen Geschiebe mit sich, so dass sich das Reussdelta im Laufe der Zeit um 10 km nach Norden in den Urnersee hinein erweitert hat.

 

Im Urnersee im Bereich des Reussdeltas zwischen Flüelen und Seedorf wurde von 2001 bis 2005 mit dem Ausbruchmaterial des Umfahrungstunnels Flüelen und des Gotthard-Basistunnels der Seegrund teilweise wieder aufgeschüttet. Es entstanden Flachwasserzonen, die durch den Kiesabbau verschwunden waren, und einige neue Inseln: die Neptuninseln und die Inselgruppe Lorelei. Einige der Inseln sind Vogelschutzgebiet. Im Naturschutzgebiet erlaubt der Reussdeltaturm die Beobachtung der Fauna.

 

Kleinere in den Vierwaldstättersee einmündende Gewässer sind der Gruonbach, der Isitaler Bach, der Riemenstaldnerbach, der Cholbach von Emmetten, der Lielibach bei Beckenried, der Teuffibach, der Melbach, die Kleine Schliere bei Alpnachstad, zehn Bäche am Ostabhang des Pilatus (darunter Mülibach, Steinibach bei Horw, Widenbach, Fridbach, Feldbach und Steinibach bei Hergiswil) und der Würzenbach in Luzern.

 

Gliederung

 

Der Vierwaldstättersee besteht aus mehreren Seebecken und Buchten:

 

Der Urnersee erstreckt sich von der Einmündung der Reuss bei Seedorf 11 km in nördlicher Richtung bis nach Brunnen

Der Gersauer See (auch Gersauer Becken oder Gersauerbecken) führt 14 km von Ost nach West von Brunnen nach Ennetbürgen, wo die Engelberger Aa in den See mündet. In der Mitte zwischen Beckenried und Gersau erreicht der See mit 214 m Tiefe seine tiefste Stelle.

Der Chrüztrichter (Kreuztrichter) bildet im Westen des Weggiser Beckens das eigentliche Zentrum des nördlichen Seeteils. Von ihm zweigen vier Hauptarme (Trichter) ab:

Das Weggiserbecken (östlicher Arm des Kreuztrichters) liegt südlich von Weggis und verläuft von Ost nach West. Es führt zwischen Hertenstein im Norden und dem Bürgenstock im Süden hin zur Seemitte. Es wird auch Vitznauerbecken genannt.

Der Stanser Trichter (südwestlicher Arm des Kreuztrichters). Im Südwesten davon liegen

die Horwerbucht und

der Alpnachersee, der zwischen Acheregg und Stansstad durch eine nur 100 Meter breite Engstelle, über die eine Brücke führt, vom restlichen See abgetrennt wird und am Südfuss des Pilatus liegt.

der Küssnachtersee (nordöstlicher Arm aus dem Kreuztrichter) zweigt zwischen Hertenstein und Meggenhorn in nordöstlicher Richtung nach Küssnacht, am Nordrand des Rigimassivs gelegen, ab.

der relativ kurze Luzernersee (auch Luzerner Bucht) ist zugleich nordwestlicher Arm des Kreuztrichters und Schlussteil des Sees. Er verläuft nach Nordwesten nach Luzern.

Abfluss

In Luzern verlässt die Reuss den See, kontrolliert mit einem Regulierwehr, und fliesst durch das Mittelland zur Aare.

 

Strömungen

 

Durch das verhältnismässig warme Wasser der Reuss und den Föhn, der das Wasser ständig umschichtet, ist der Urnersee am Grund wärmer und leichter als das Wasser im Gersauer Becken. Durch diesen Temperaturunterschied strömen jeden Frühling gewaltige Wassermassen vom Gersauer Becken in die Tiefen des Urnersees. Ähnliche Tiefenwasserströmungen bestehen auch vom Alpnachersee in das Gersauer Becken.

 

Wasserqualität und Temperaturen

 

Das Wasser bleibt durchschnittlich dreieinhalb Jahre im Seebecken und hat Trinkwasserqualität. Die Eidgenössische Forschungsanstalt für Limnologie der Eawag überwacht die Wasserqualität. Im Sommer erreicht der See eine Temperatur von 22 °C. 1929 und 1963 froren der Alpnachersee und die Luzerner Bucht zu. Aus dem 17. und 19. Jahrhundert sind Vereisungen des ganzen Vierwaldstättersees dokumentiert. 1684 und 1685 konnte das Gersauer Becken auf dem Eis überquert werden.

 

Klima und Vegetation

 

Das Klima rund um den föhnbegünstigten und von Bergen geschützten Vierwaldstättersee ist im Vergleich zu anderen Regionen der deutschsprachigen Schweiz relativ mild; die Vegetation gleicht zum Teil derjenigen des Kantons Tessin. Die mittlere Tageshöchst-/-tiefsttemperatur beträgt in Luzern 2,6 °C (Januar) und 23,5 °C (Juli). In Altdorf südlich des Sees liegen die Werte bei 3,9 °C (Januar) und 23,0 °C im Juli (Klimamittel der Jahre 1961–1990). An den Seeufern wachsen Hanfpalmen, Feigen, Yuccas, Zypressen, Opuntien, Edelkastanien und andere südländische Pflanzenarten.

 

Die Edelkastanien wurden bis ins 19. Jahrhundert wirtschaftlich als Nahrungsmittel genutzt. Mit der Verbreitung der Kartoffel nahm die Bedeutung der Kastanie jedoch ab. Noch heute findet in Greppen regelmässig ein Kastanienmarkt, die sogenannte Chestene-Chilbi statt. An den Marktständen werden Kastanienprodukte und regionale Spezialitäten angeboten.

 

Naturgefahren

 

Hochwasser in Luzern August 2005

 

Nach dem Erdbeben vom 18. September 1601 entstanden Tsunamis im Vierwaldstättersee mit vermutlich bis zu 4 Meter hohen Flutwellen. Ein weiteres solches Ereignis soll im Jahr 1687 stattgefunden haben. Auch vom Genfersee ist ein Binnentsunami-Ereignis aus dem Jahr 563 bekannt, und vom Lauerzersee aus dem Jahr 1806.

 

Die Folgen der allgemeinen Erderwärmung in den Alpen werden auch für den Vierwaldstättersee und seine Umgebung diskutiert. Das Hochwasser 2005 mit diversen Muren und Erdrutschen könnte als Warnsymptom verstanden werden.

 

Seit 1861 wird der Wasserspiegel des Vierwaldstättersees durch die Reusswehranlage in Luzern etwa zwei bis drei Meter über dem natürlichen mittleren Wasserstand gehalten.

 

Verkehr

 

Schifffahrt

 

Auf dem See verkehren die Schiffe der Schifffahrtsgesellschaft des Vierwaldstättersees (SGV) zu den zahlreichen Schiffstationen. Bis zum Bau der Axenstrasse in den Jahren 1863 bis 1865 war der Wasserweg die einzige aus dem Norden mögliche Verbindung zum Kanton Uri, zum Gotthardpass und damit auch der einzige Weg von den Städten im Nordwesten Europas nach Mailand und zu den italienischen Häfen am Mittelmeer. Das gilt auch für die Pilgerwege des Mittelalters nach Rom. Noch heute verkehren auf dieser Strecke die grossen Raddampfer der SGV Stadt Luzern (das Flaggschiff der SGV) Uri, Unterwalden, Gallia und Schiller.

 

Autofähre Beckenried–Gersau

 

Zwischen Beckenried und Gersau verkehrt die Autofähre Beckenried–Gersau. Auf dem See fahren ausserdem Lastschiffe privater Transportunternehmen.

 

Beim Zusammenstoss des Nauens Schwalmis mit dem Motorschiff Schwalbe vor Horw starben am 12. Oktober 1944 zwanzig Gäste einer 33-köpfigen Hochzeitsgesellschaft aus der Region Entlebuch. Die Unfallursache konnte nicht restlos geklärt werden. Es war das bislang grösste Unglück der Schweiz mit einem motorisierten Schiff.

 

Strasse und Schiene

 

Seit dem Bau der Gotthardstrasse, der Gotthardbahn (Eröffnung 1882), der Gotthardautobahn (1982) und der Eisenbahnschnellfahrstrecken von AlpTransit (NEAT) zum Gotthard-Basistunnel (2016) tangieren grosse internationale Verkehrswege die Gegend um den Vierwaldstättersee. In Flüelen wechselten vor dem Bau der Eisenbahn die Reisenden von den Bergpässen vom Maultier oder der Postkutsche auf das Schiff. Am östlichen Ufer führt die Axenstrasse mit vielen Tunnels und Galerien von Flüelen über Sisikon nach Brunnen. Sie ist Bestandteil der A4. Die Bahnlinie führt mehrheitlich unterirdisch von Flüelen nach Brunnen. Auf dem Weg nach Küssnacht erinnern alte, restaurierte Hotelbauten an die Zeit des frühen Tourismus im 19. Jahrhundert.

 

Zwischen Hergiswil und Stansstad führen Strassenbrücken (Kantonsstrasse und Autobahn A2) und eine Eisenbahnbrücke der Luzern-Stans-Engelberg-Bahn bei der Lopper-Halbinsel über eine Landenge im See.

 

Der 1991 auf alten Verkehrswegen angelegte Wanderweg mit der Bezeichnung Weg der Schweiz führt rund um den südlichsten Teil des Sees, den Urnersee.

 

Luftverkehr

 

Zwischen Buochs und Ennetbürgen bei Stans liegt der Flugplatz Buochs, der früher fast nur von der Schweizer Armee und den Pilatus-Flugzeugwerken benutzt wurde. Heute steht der Flugplatz dem zivilen Flugverkehr offen. Der Militärflugplatz Alpnach wird von der Schweizer Armee als Helikopterbasis genutzt.

 

Hängegleiter und Gleitschirme nutzen bei geeignetem Wetter die Thermik der Felswände über den steilen Ufern des Sees. Die beliebtesten Fluggebiete für Gleitschirme um den Vierwaldstättersee sind der Pilatus, die Rigi, das Gebiet von Emmetten, das Stanserhorn und das ganze Engelbergertal. Beim Fliegen sind die Kontrollzonen der Flugplätze Alpnach, Buochs und Emmen zu beachten.

 

Geschichte

 

Zu den frühesten menschlichen Spuren am See gehörten die neolithischen Seeufersiedlungen aus dem 5. bis 4. Jahrtausend v. Chr. bei Stansstad-Kehrsiten. Zahlreiche Ortsnamen weisen auf eine keltische, später gallorömische Besiedlung hin. In Alpnach fand sich eine römische Villa. Spätestens im 7. Jahrhundert liessen sich Alemannen nieder.

 

Am Ausfluss der Reuss entstand im 12. und 13. Jahrhundert die Stadt Luzern, rund um den See die Länderorte Uri, Schwyz und Unterwalden. Diese erlangten die Hoheit über das sie verbindende Gewässer bis hin zur Seemitte, sieht man von der Fläche in der Verlängerung des Bürgenbergs bis vor Hertenstein ab. Diese gelangte 1378 zusammen mit dessen Nordflanke an Luzern. Dennoch kam es bis 1967 – zwischen Nidwalden und Luzern – zu Auseinandersetzungen um Fischereirechte und Grenzstreitigkeiten. Da es extrem schwierig war, Strassen um den See zu bauen, war das Gewässer zugleich eine Hauptverkehrsader.

 

Kirchlich bildete der Raum vom Hochmittelalter bis 1821 das Dekanat Luzern bzw. das Vierwaldstätterkapitel im Bistum Konstanz. Danach wurde der Raum auf die Bistümer Chur und Basel aufgeteilt. Über den See oder an ihm entlang führten früher Pilgerwege nach Rom. Auch der westwärts nach Santiago de Compostela führende Jakobsweg führt von Einsiedeln nach Brunnen. Von hier führt er weiter westlich mit dem Schiff nach Luzern oder über den Alpnachersee nach Süden zum Brünigpass.

 

Im Gegensatz zum offenen See, auf dem frei gefischt werden durfte, gehörten die Uferstreifen zur Gemeinmarch der Siedlungsgenossen. Nur ihre Fischer durften dort ausfahren. Daneben bestanden herrschaftliche Rechte wie die Fischämter von St. Leodegar in Luzern. Aus derlei Organisationsformen gingen etwa 1465 die Luzerner Rohrgesellen oder 1607 die St.-Niklausen-Bruderschaft von Stansstad hervor. Auch hier konnten Fischereirechte zu heftigen Auseinandersetzungen führen, wie 1655 zwischen Luzern und Nidwalden. Statuten für den Fischmarkt finden sich in Luzern schon im ältesten Ratsbüchlein (um 1318).

 

Nach der Helvetik wurde die Fischerei in allen Orten zu einem Hoheitsrecht der Kantone. 1890 schlossen sich die Kantone zum Fischereikonkordat Vierwaldstättersee zusammen. Noch Ende des 20. Jahrhunderts beschäftigten 27 Betriebe rund 40 Vollzeitarbeitskräfte.

 

Der regionale Markt mit Luzern als Mittelpunkt und der Verkehr über den Gotthard führten zum Aufbau eines Transportwesens. In Flüelen wurde 1313 ein Reichszoll erwähnt, Anfang des 14. Jahrhunderts sind in Luzern Lagerhäuser bezeugt, ähnlich wie in anderen Orten.

 

Im 17. Jahrhundert bestanden in Alpnach fünf Fahrrechte, in Brunnen arbeiteten 60 Schiffsleute. 1687 kam es zum Abschluss eines Schifffahrtsvertrags, der bis ins 19. Jahrhundert Bestand hatte. 1837 begann die Dampfschifffahrt, 1870 entstand die Schifffahrtsgesellschaft des Vierwaldstättersees. Sie verdrängte die lokalen Schifffahrtsgenossenschaften. Ab 1859 entstand im Einzugsgebiet des Sees ein Eisenbahn-, Bergbahn- und Strassennetz, was den Tourismus stark anwachsen liess und eine entsprechende Infrastruktur hervorbrachte. Ab Ende des 19. Jahrhunderts wurde die Sand- und Kiesgewinnung zu einem expandierenden Industriezweig.

 

1859–1860 wurde mit dem Bau des Luzerner Nadelwehrs die Basis für eine Regulierung des Wasserpegels gelegt. Zugleich belasteten Kiesabbau, das Wachstum der Orte und der unkontrollierte Häuserbau, dazu Gewässerverschmutzung und Wassersport den See. Daher entstand 1916 das Hydrobiologische Laboratorium (1960 in die ETH Zürich integriert), das im Bereich des Gewässerschutzes tätig wurde und bis heute die Kantone berät. 1953 wurde der Gewässerschutz in der Bundesverfassung verankert, aber erst das revidierte Gewässerschutzgesetz von 1971 ermöglichte es schliesslich die Sanierung des Sees bis 1987 voranzutreiben. Bereits ab 1980 versorgten sich Luzern, Bürgenstock sowie Küssnacht, Horw und Weggis mit Trinkwasser aus dem See. 1973 setzten die Uferkantone einen Landschaftsschutzplan in Kraft, dessen Umsetzung der 1984 gegründete Landschaftsschutzverband Vierwaldstättersee vorantreibt.

 

Kulturelle und historische Eigenheiten des Seegebietes sind der Kommunalismus, die eigenständige Rezeption der italienischen Renaissance und des Barock oder der Einfluss der Gegenreformation, aber auch die Kleinräumigkeit des lokalen Brauchtums und der Mundarten.

 

Tourismus

 

Fremdenverkehr

 

Auf dem Weg in den Süden entdeckten Engländer die Bergwelt der Innerschweiz. Es entstanden mehrere Kur- und Badeorte wie Weggis oder Gersau. 1871 eröffnete man die allererste Zahnradbahn Europas, die Vitznau-Rigi-Bahn. 1889 baute man von Alpnachstad auf den Pilatus die heute immer noch steilste Zahnradbahn der Welt. Einen Aufstieg auf die Rigi beschrieb Mark Twain, was in den USA des 19. Jahrhunderts zum Aufblühen des Schweizer Tourismus führte. Auf dem Vierwaldstättersee verkehrt mit fünf Dampfschiffen eine der grössten Dampfschiffflotten Europas.

 

In der Umgebung des Sees und auf Terrassen in mittlerer Höhe (wie z. B. Morschach und Seelisberg) liegen zahlreiche Tourismusorte. Attraktive Aussichtsberge nahe am Vierwaldstättersee sind die Rigi, der Pilatus, der Bürgenstock, das Stanserhorn, das Buochserhorn, die beiden Mythen, der Uri Rotstock und der Fronalpstock. Die meisten davon sind mit Bergbahnen erreichbar, die teilweise ihre Talstation in der Nähe von Schiffstationen am See haben.

 

Am See befinden sich zahlreiche Örtlichkeiten mit Bedeutung in der Schweizer Kultur- und Tourismusgeschichte: Rütli, Tellsplatte, Tellskapelle, Schnitzturm von Stansstad, Neu-Habsburg, Schillerstein, Treib, Astrid-Kapelle (Küssnacht) und Schloss Meggenhorn.

 

Wassersport

 

In den einzelnen Seebereichen sind wegen den Wasser- und den Windverhältnissen verschiedene Sportarten möglich.Von Boots- und Yachthäfen, See- und Strandbädern (z. B. das 1929 von Arnold Berger gebaute Strandbad Lido in Luzern) und von andern Uferabschnitten aus ist der See zugänglich. 1881 wurde der See-Club Luzern gegründet, der heute der grösste Ruderclub der Schweiz ist, 1904 der Ruderclub Reuss Luzern. Seit 1941 besteht der Yachtclub Luzern, der am Churchill-Quai in Luzern seit 1966 ein Bootshaus und ein Bojenfeld betreibt. Der im Jahr 1958 gebildete Wassersportclub Brunnen führte in den ersten Jahren seines Bestehens auf dem Vierwaldstättersee internationale Motorbootrennen und Wasserskimeisterschaften durch. 1965 wählte der Verein den neuen Namen Wassersport-Club Vierwaldstättersee. 1980 entstand der Motorbootclub Zentralschweiz, 1986 der Wassersportclub Hergiswil. SchweizMobil hat eine Kanutour über den Vierwaldstättersee zwischen Brunnen und Gersau beschrieben. Der südliche Teil des Urnersees zwischen dem Campingplatz am Gruonbachstrand in Flüelen und Isleten ist wegen des Windes im Reusstal ein Zentrum des Windsurfens.

 

Tauchsport

 

Es gibt etwa zehn Plätze, an denen man ohne Boot im Vierwaldstättersee tauchen kann. Das Wasser ist ganzjährig eher kühl und deshalb meist sehr klar. Die zerklüftete Steilwand bei Sisikon, am nördlichen Portal des Schieferneggtunnels, kann man seit einem Erdrutsch und dem Verschütten eines Parkplatzes, der auch als Einstieg genutzt wurde, nicht mehr von Land aus betauchen. Vor Brunnen liegt das Lediwrack Bruno auf 15 Meter Tiefe. Weiter bekannte Tauchplätze liegen vor Vitznau, Weggis, Gersau und Hergiswil.

 

Wirtschaft

 

In mehreren Gemeinden am Vierwaldstättersee befinden sich an den leicht zugänglichen Bergflanken im Uferbereich seit Jahrhunderten Steinbrüche, die teilweise noch heute genutzt werden. Das Gestein gelangt auf dem Seeweg kostengünstig zu Verbrauchern oder Bahnhöfen. Die auffälligen Eingriffe in die Naturlandschaft stiessen schon früh auf Kritik seitens der Landschaftschutzorganisationen. 1930 wies ein Bericht auf die Zunahme der Grossanlagen hin: «Zwei Steinbrüche [liegen] im Urner See zwischen Seedorf und Isleten, vier zwischen Beckenried und Treib, einer in der Matt unter dem Bürgenstock, einer zwischen Kehrsiten und Stansstad, fünf im Alpnachersee, einer am Lopperberg zwischen Stansstad und Hergiswil, einer bei Greppen, einer zwischen Vitznau und Gersau, zwei zwischen Gersau und Brunnen». Bei Kehrsiten am Bürgenstock baut die Holcim in einem Schotterwerk harten Kieselkalk ab, der auch in den Brüchen Schwibogen und Rotzloch gewonnen wird, während vier andere Nidwaldner Steinbrüche im Uferbereich aufgelassen sind. Der Landschaftschutzverband Vierwaldstättersee begleitet die Entwicklung einzelner Steinbruchprojekte.

 

Seit 1891 baut das Unternehmen Arnold & Co. Sand- und Kieswerk AG bei Flüelen mit Schwimmbaggern Kies aus dem Schwemmfächer vor dem Delta der Reuss ab, wofür sie dem Kanton Uri Konzessionsgebühren entrichtet. Heute sind nur noch der vierte und fünfte Schwimmbagger aus den 1950er und 1960er Jahren in umgebautem Zustand im Einsatz. Die Flotte der Arnold + Co. AG umfasst etwa fünfzehn Nauen. Zwischen 2001 und 2005 legte das Unternehmen im Urnersee mit Schutt aus dem NEAT-Stollen Amsteg und der Umfahrung Flüelen sechs Inseln an.

 

Auch bei Beckenried und anderen Stellen wird vor den Flussmündungen Kies abgebaut.

 

Mitte April 1957 wurde ein Telefonkabel von Spissenegg nach Stansstad im See verlegt. Die Teilverkabelung des Vierwaldstättersees hatte zwei Gründe: Die damalige Bezirkskabelanlage war durch den Bau des neuen Autobahnabschnittes Horw-Stans erheblich gefährdet. Der Schutz der Kabel hätte aber zu kostspieligen Sicherungsmassnahmen geführt. Da die Seekabellegung in diesem Fall preiswerter und der Bedarf an zusätzlichen Leitungen gross war, bewilligte die Telefondirektion in Bern das Projekt.

 

100 Jahre zuvor, 1854, wurde exakt auf dieser Strecke das erste, in den Telegrafenwerkstätten in Bern eigens hergestellte Seetelefonkabel verlegt. Es diente zur Verbindung der anschliessenden oberirdischen Telegrafenlinien Luzern-Brünig-Interlaken.

 

Belastung mit Munition

 

Zwischen 1918 und 1967 entsorgten Schweizer Munitionsfabriken ihre Produktionsabfälle im Vierwaldstätter-, Brienzer- sowie Thunersee. Die Gesamtmenge, welche in bis zu 200 Metern Tiefe im Vierwaldstättersee versenkt wurde, wird auf 3'300 Tonnen geschätzt, 2'800 Tonnen im Urnersee sowie 500 Tonnen im Gersauer Becken.

 

Namensverwandtschaften

 

Der Jacobiweiher im Stadtwald von Frankfurt am Main wird im Volksmund seiner Form wegen Vierwaldstättersee genannt.

Auch ein künstlicher See im Zoo Berlin wird aus dem gleichen Grund Vierwaldstättersee genannt.

 

(Wikipedia)

 

Das Stanserhorn ist ein 1897 m ü. M. hoher Berg im Schweizer Kanton Nidwalden, der Hausberg von Stans und liegt in den Urner Alpen an der Grenze zum Kanton Obwalden.

 

Geographie

 

Das Stanserhorn liegt zwischen den Ortschaften Stans, Ennetmoos, Kerns, Dallenwil und Oberdorf, südlich des Vierwaldstättersees und somit (gemäss SOIUSA) in den Unterwaldner Voralpen. An der Südostflanke des Stanserhorns liegt auf einer Höhe von 1226 m ü. M. der kleine Ferienort Wirzweli.

 

Die Rundsicht reicht von den nahen Alpengipfeln bis hin zu den Vogesen im Elsass (Frankreich) und zum Feldberg im Schwarzwald (Deutschland). Dazwischen sind zehn grössere Seen auszumachen: Zugersee, Wichelsee, Vierwaldstättersee, Sempachersee, Sarnersee, Hallwilersee, Gerzensee, Bannalpsee, Baldeggersee und Alpnachersee.

 

Erschliessung

 

Die beiden Bergbahnpioniere Franz Josef Bucher-Durrer und Josef Durrer-Gasser begannen im Juni 1891 mit dem Bau der Stanserhorn-Bahn, die wegen der grossen Streckenlänge von knapp 4 km in drei getrennten Standseilbahn-Sektionen von Stans über Kälti und Alp Blumatt auf den Gipfel führte. Die Bahn wurde am 23. August 1893 eröffnet, gleichzeitig mit dem ebenfalls neu errichteten Hotel Stanserhorn Kulm. 1895 wurde auf dem Gipfel ein elektrischer Scheinwerfer mit der «Kraft von 22'000 Normalkerzen» installiert, um damit auf das Stanserhorn als Attraktion aufmerksam zu machen. Durch einen Kurzschluss in der Station Blumatt wurde am 2. Oktober 1970 ein Brand ausgelöst, wodurch der Antrieb der 3. Sektion, das Hotel und das Scheinwerferaggregat zerstört wurden. Anstatt des Hotels wird seitdem ein Restaurant auf dem Gipfel betrieben.

 

Nachdem 1974 der Betrieb der Standseilbahn eingestellt worden war, wurde 1975 die Luftseilbahn Kälti–Stanserhorn eröffnet, die nun zusammen mit der ursprünglichen 1. Sektion den Berg erschloss. Seit 2012 kann man mit der doppelstöckigen «CabriO-Bahn» auf das Stanserhorn fahren. Das offene Oberdeck der Seilbahnkabine kann während der Fahrt über eine Wendeltreppe erreicht werden, die Kabine fasst 60 Personen, das Oberdeck davon 30.

 

Als Touristenattraktion wurde 2001 das Drehrestaurant Rondorama eröffnet. Von der sich im Innern des Gebäudes drehenden Plattform hat man eine Rundsicht auf die umliegenden Berge und Seen. Ein Murmeltiergehege und ein ausgeschilderter Gipfelrundgang von rund 30 Minuten ergänzen das Angebot auf dem Stanserhorn, das auch als 5-Sterne-Berg und Faulenzer-Berg vermarktet wird. Auf der Route vom Stanserhorn zur Wirzweli befindet sich der Geo-Weg (Bergwanderung im Schwierigkeitsgrad T2 gemäss SAC-Wanderskala), der gemeinsam durch die Organisationen Nidwaldner Wanderwege, Pro Natura und WWF Unterwalden realisiert wurde.

 

Das Stanserhorn wird von Drachenfliegern und Gleitschirmpiloten benutzt, es gilt als Hausberg des grössten und ältesten noch aktiven Drachenfliegerclubs der Schweiz, des Deltaclubs Stans. An sonnigen Tagen – vor allem an den Wochenenden – finden von April bis Oktober jeweils um die Mittagszeit viele Starts statt.

 

(Wikipedia)

Aufnahmedatum 16.03.2019

Eröffnung Rotteckring mit hist. Fahrzeugen

H.-von Stephan Straße, Tw 56

Type : Bell 429

Longueur : 13,1 m

Largeur : 11 m

Poids maximum : 7500 lbs

Vitesse maximale : 155 nœuds

Vitesse de croisière : 130 nœuds

Passagers : 7 + 1 pilote

 

Mention de source : Pêches et Océans Canada P. Dionne

--

Type: Bell 429

Length: 13.1 m

Breadth: 11 m

Maximum weight: 7,500 lbs

Maximum speed: 155 knots

Cruising speed: 130 knots

Passengers: 7 + 1 pilot

 

Credit: Fisheries and Oceans Canada P. Dionne

--

www.ccg-gcc.gc.ca/fleet-flotte/index-fra.html

This gothic maxi really is a bit of a stunner, being made of multiple layers of black and pink tulle, and several tiers. This might be the last photo for the day, but I’ll probably bring it out again on Halloween.

Guidelines widely ignored in this Bar

Lake Urmia is a salt lake in North Iran. At its greatest extent, it was the largest saltwater lake on Earth, with a surface area of approximately 5,200 km2, a length of 140 km (87 mi), a width of 55 km (34 mi), and a maximum depth of 16 m (52 ft). The lake has shrunk to 10% of its former size due to damming of the rivers that flow into it, and the pumping of groundwater from the surrounding area. The salinity has particularly increased in the half of the lake north of the Urmia Lake Bridge.

 

Lake Urmia, along with its once approximately 102 islands, is protected as a national park.

 

The prospect that Lake Urmia might dry up entirely has drawn protests in Iran and abroad. On May 5, 2016, Leonardo Di Caprio posted a photo of "a dilapidated ship dock remains on dried up Urmia Lake" on his Instagram page stating: "It used to be the biggest salt lake in the Middle East, but it now contains five percent of the amount of water it did two decades ago due to climate change, dam construction and decrease in precipitiation."

(Wikipedia)

Taken & edited by: Me

Location: International Motor Show in Qatar (1st time)

 

Motor Type

W16

 

Power Output

1001 HP

 

Speed

400km/h+

 

Maximum Torque

1,250 Nm

 

Cylinder Capacity

7,993 cm

 

Length/Width/Height

4,462/1,998/1,204 mm

 

Tyres (Front)

265-680 ZR 500A / Michelin Pilot Sport Pax

 

Tyres (Rear)

365-710 ZR 540A / Michelin Pilot Sport Pax

 

----------------------------------------------

 

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هلا ياجماعه .. .. هاي صفحه فيس بوكي اليديد . القديم تصكر .. سولي لايك علي اليدي .. ثنكس

 

Hey everyone, this is my new facebook page. My old one is closed so please like it .. thanks

Big version of our 'Maximum Baby Shower ' cake. At 34" across, it makes quite the statement. Complete with all edible decoration of a quilted pillow with y shoes , blocks, present box filled with flowers and a French fry in diapers ( what the mom was craving :) ), this cake pushes the limits of over the top cake decoration. Jasmine

Beach volleyball with maximum effort to reach the ball.

  

3 Likes on Instagram

 

1 Comments on Instagram:

 

ktchn: Haha. Nice!

  

One of the first Hybrid buses to be permanently allocated to York, LK58 ECW is a Wright Gemini 2HEV 10.4m integral double decker bus (based on VDL (DAF) DB300 Hybrid Technology components, but Wrights chassis) due to operate in York after a refurbishment following their retirement from London (Ex Travel for London TfL), former WNH class... they have been given the new firstgroup standard Olympia livery, so could theoretically see use on any First route in York - but will initially work the number 4 service. These utilise Siemens ELFA traction components, with energy having originally been provided by a Ford Puma 2.4 litre diesel engine - this has been removed and replaced by a Cummins unit in the refurbishment which has extended the rear overhang of the bus slightly. The last bus still outstanding is ironically the first bus of this type ever built - it was due on the weekend of April 5/6, but is still nowhere to be seen almost a month later. 39002 is here at Heslington Field Lane on its very first day of passenger cayying service in its new home - following a road test yesterday, it is now on route 4 to the University of York and then on to the city centre, Foxwood, and Acomb. This was the only Hybrid out today, the rest were confined to depot. It's worth noting the bus wasn't causing that massive queue of traffic - Green Dykes Lane currently has no access to/from Hull Road and so Field lane is the only access to the University from Hull Road and beyond - however the council has done nothing about the traffic lights at the junction of Field Lane and Lakeside was to help ease the traffic, instead they were only staying on green for traffic on this direction for 10 seconds average (19 seconds absolute maximum)

A class 390 Pendolino approaches Abington in glorious weather with my 70-300mm lens at its maximum. 11/3/14

“they tried to talk but it was no good

they said you’d leave and I knew you would

 

I knew the time and I knew the place

but through the eyes of another face” C. Devlin

 

Hurricane Dorian made landfall over Cape Hatteras, N.C., at 8:35 a.m. EDT Friday, Sept. 6, 2019, with maximum sustained winds near 90 mph. NOAA’s GOES East captured this view of the strong Category 1 storm at 8:20 a.m. EDT, just 15 minutes before the center of the storm moved across the barrier islands.

 

Life-threatening storm surge, inland flooding and strong gusty winds remain the primary hazards as the storm continues moving toward the northeast, according to the National Hurricane Center (NHC). Video footage from Frying Pan Tower — which sits approximately 32 miles from Bald Head Island, N.C. — shows the storm’s violent winds ripping apart an American flag that sits atop the decommissioned lighthouse. Around this time last year, Hurricane Florence battered the tower and a previously retired flag.

 

As of 9:30 a.m. EDT Friday, more than 350,000 homes and businesses along the North and South Carolina coasts were in the dark. At 6 a.m. EDT the North Carolina Department of Transportation tweeted, saying at least 73 roads, 17 of which are considered primary routes, were closed due to Dorian.

 

Dorian is expected to continue lashing the North Carolina coast for several hours before heading northward where the storm’s center is forecast to pass southeast of southeastern New England tonight and Saturday morning. By the time Dorian reaches Newfoundland, Canada, it is forecast to become a post-tropical cyclone with tropical-storm-force winds, according to the NHC.

 

www.nesdis.noaa.gov/content/goes-east-sees-dorian-moments...

Home based Class 37 37109 heads out of Ramsbottom with the 15.25 departure to Rawtenstall (14.30 ex-Heywood). This locomotive provided one of the highlights of the day with a terrific full-powered English Electric 'thrash' from Bury up to Ramsbottom. An extremely busy service - standing room only.

DISCLAIMER

Nothing you see here is real, even though the conversion or the presented background story might be based historical facts. BEWARE!

 

Some background:

The Northrop Grumman-IAI F-24 is the latest reincarnation of the USAF "Lightweight Fighter Program" which dates back to the 1950ies and started with the development of Northrop's F-5 "Freedom Fighter".

 

The 1st generation F-5 became very successful in the export market and saw a long line of development, including the much more powerful F-5E "Tiger II" and the F-20 Tigershark (initially called F-5G). Northrop had high hopes for the F-20 in the international market; however, policy changes following Ronald Reagan's election meant the F-20 had to compete for sales against aircraft like the F-16, the USAF's latest fighter design (which was politically favored). The F-20 development program was eventually abandoned in 1986 after three prototypes had been built and a fourth partially completed.

 

But this was not the end for Northrop’s Lightweight Fighter. In the early 1980s, two X-29As experimental aircraft were built by Grumman from two existing Northrop F-5A Freedom Fighter airframes. The Grumman X-29 was a testbed for forward-swept wings, canard control surfaces, and other novel aircraft technologies. The aerodynamic instability of this arrangement increased agility but required the use of computerized fly-by-wire control. Composite materials were used to control the aeroelastic divergent twisting experienced by forward-swept wings, also reducing the weight. The NASA test program continued from 1984 to 1991 and the X-29s flew 242 times, gathering valuable data and breaking ground for new aerodynamic technologies of 4th and 5th generation fighters.

 

Even though no service aircraft directly evolved from the X-29, its innovative FBW system as well as the new material technologies also opened the door for an updated F-20 far beyond the 1990ies. It became clear that ever expensive and complex aircraft could not be the answer to modern, asymmetrical warfare in remote corners of the world, with exploding development costs and just a limited number of aircraft in service that could not generate true economies of scale, esp. when their state-of-the-art design would not permit any export.

Anyway, a global market for simpler fighter aircraft was there, as 1st generation F-16s as well as the worldwide, aging F-5E fleet and types of Soviet/Russian origin like the MiG-29 provided the need for a modern, yet light and economical jet fighter. Contemporary types like the Indian HAL Tejas, the Swedish Saab Gripen, the French Dassault Rafale and the Pakistani/Chinese FC-1/JF-17 ”Thunder” proved this trend among 4th - 4.5th generation fighter aircraft.

 

Northrop Grumman (Northrop bought Grumman in 1994) initiated studies and basic design work on a respective New Lightweight Fighter (NLF) as a private venture in 1995. Work on the NLF started at a slow pace, as the company was busy with re-structuring.

The idea of an updated lightweight fighter was fueled by another source, too: Israel. In 1998 IAI started looking in the USA for a development partner for a new, light fighter that would replace its obsolete Kfir fleet and partly relieve its F-16 and F-15 fleet from interception tasks. The domestic project for that role, the IAI Lavi, had been stillborn, but lots of its avionics and research were still at hand and waited for an airframe for completion.

The new aircraft for the IAF was to be superior to the MiG-29, at least on par with the F-16C/D, but easier to maintain, smaller and overall cheaper. Since the performance profiles appeared to be similar to what Northrop Grumman was developing under the NLF label, the US company eventually teamed up with IAI in 2000 and both started the mutual project "Namer" (=נמר, “Tiger” in Hebrew), which eventually lead to the F-24 I for the IAF which kept its project name for service and to the USAF’s F-24A “Tigershark”.

 

The F-24, as the NLF, was based on the F-20 airframe, but outwardly showed only little family heritage, onle the forward fuselage around the cockpit reminds of the original F-5 design . Many aerodynamic details, e. g. the air intakes and air ducts, were taken over from the X-29, though, as the experimental aircraft and its components had been developed for extreme maneuvers and extra high agility. Nevertheless, the X-29's forward-swept wing was considered to be too exotic and fragile for a true service aircraft, but the F-24 was to feature an Active Aeroelastic Wing (AAW) system.

 

AAW Technology integrates wing aerodynamics, controls, and structure to harness and control wing aeroelastic twist at high speeds and dynamic pressures. By using multiple leading and trailing edge controls like "aerodynamic tabs", subtle amounts of aeroelastic twist can be controlled to provide large amounts of wing control power, while minimizing maneuver air loads at high wing strain conditions or aerodynamic drag at low wing strain conditions. This system was initially tested on the X-29 and later on the X-53 research aircraft, a modified F-18, until 2006.

 

Both USAF and IAF versions feature this state-of-the-art aerodynamic technology, but it is uncertain if other customers will receive it. While details concerning the F-24's system have not been published yet, it is assumed that its AAW is so effective that canard foreplanes could be omitted without sacrificing lift and maneuverability, and that drag is effectively minimized as the wing profile can be adjusted according to the aircraft’s speed, altitude, payload and mission – much like a VG wing, but without its clumsy and heavy swiveling mechanism which has to bear high g forces. As a result, the F-24 is, compared to the F-20, which could carry an external payload of about 3.5 tons, rumored to be able to carry up to 5 tons of ordnance.

 

The delta wing shape proved to be a perfect choice for the required surface and flap actuators inside of the wings, and it would also offer a very good compromise between lift and drag for a wide range of performance. Anyway, there was one price to pay: in order to keep the wing profile thin and simple, the F-24’s landing gear retracts into the lower fuselage, leaving the aircraft with a relatively narrow track.

 

Another major design factor for the outstanding performance of this rather small aircraft was weight reduction and structural integrity – combined with simplicity, ruggedness and a modular construction which would allow later upgrades. Instead of “going big” and expensive, the new F-24 was to create its performance through dedicated loss of weight, which was in some part also a compensation for the AAW system in the wings and its periphery.

 

Weight was saved wherever possible, e .g. a newly developed, lightweight M199A1 gatling gun. This 20mm cannon is a three-barreled, heavily modified version of the already “stripped” M61A2 gun in the USAF’s current F-18E and F-22. One of the novel features is a pneumatic drive instead of the traditional electric mechanism, what not only saves weight but also improves trigger response. The new gun weighs only a mere 65kg (the six-barreled M61A2 weighs 92kg, the original M61A1 112 kg), but still reaches a burst rate of fire of 1.800 RPM (about 800 RPM under cyclic fire, standard practice is to fire the cannon in 30 to 50-round bursts, though) and a muzzle velocity of 1.050 metres per second (3,450 ft/s) with a PGU-28/B round.

 

While the F-16 was and is still made from 80% aluminum alloys and only from 3% composites, the F-24 makes major use of carbon fiber and other lightweight materials, which make up about 40% of the aircraft’s structure, plus an increased share of Titanium and Magnesium alloys. As a consequence and through many other weight-saving measures like keeping stealth capabilities to a minimum (even though RAM was deliberately used and many details designed to have a natural low radar signature, resulting in modest radar cross-section (RCS) reductions), a single, relatively small engine, a fuel-efficient F404-GE-402 turbofan, is enough to make the F-24 a fast and very agile aircraft, coupled with a good range. The F-24’s thrust/weight ratio is considerably higher than 1, and later versions with a vectored thrust nozzle (see below) will take this level of agility even further – with the pilot becoming the limiting factor for the aircraft’s performance.

 

USAF and IAF F-24s are outfitted with Northrop Grumman's AN/APG-80 Active Electronically Scanned Array (AESA) radar, also used in the F-16 Block 60 aircraft. Other customers might only receive the AN/APG-68, making the F-24 comparable to the F-16C/D.

 

The first prototype, the YF-24, flew on 8th of March 2008, followed by two more aircraft plus a static airframe until summer 2010. In early 2011 the USAF placed an initial order of 101 aircraft (probably also to stir export sales – the earlier lightweight fighters from Northrop suffered from the fact that the manufacturer’s country would not use the aircraft in its own forces). These initial aircraft will replace older F-16 in the interceptor role, or free them for fighter bomber tasks. The USN and USMC also showed interest in the aircraft for their aggressor squadrons, for dissimilar air combat training. A two-seater, called the F-24B, is supposed to follow soon, too, and a later version for 2020 onwards, tentatively designated F-24C, is to feature an even stronger F404 engine and a 3D vectoring nozzle.

 

Israel is going to produce its own version domestically from late 2014 on, which will exclusively be used by the IAF. These aircraft will be outfitted with different avionics, built by Elta in Israel, and cater to national requirements which focus more on multi-purpose service, while the USAF focusses with its F-24A on aerial combat and interception tasks.

 

International interest for the F-24A is already there: in late 2013 Grumman stated that initial talks have been made with various countries, and potential export candidates from 2015 on are Taiwan, Singapore, Thailand, Finland, Norway, Australia and Japan.

  

General F-24A characteristics:

Crew: 1 pilot

Length: 47 ft 4 in (14.4 m)

Wingspan: 27 ft 11.9 in / 8.53 m; with wingtip missiles (26 ft 8 in/ 8.13 m; without wingtip missiles)

Height: 13 ft 10 in (4.20 m)

Wing area: 36.55 m² (392 ft²)

Empty weight: 13.150 lb (5.090 kg)

Loaded weight: 15.480 lb (6.830 kg)

Max. take-off weight: 27.530 lb (12.500 kg)

 

Powerplant

1× General Electric F404-GE-402 turbofan with a dry thrust of 11,000 lbf (48.9 kN) and 17,750 lbf (79.2 kN) with afterburner

 

Performance

Maximum speed: Mach 2

Combat radius: 300 nmi (345 mi, 556 km); for hi-lo-hi mission with 2 × 330 US gal (1,250 L) drop tanks

Ferry range: 1,490 nmi (1715 mi, 2759 km); with 3 × 330 US gal (1,250 L) drop tanks

Service ceiling: 55,000 ft (16,800 m)

Rate of climb: 52,800 ft/min (255 m/s)

Wing loading: 70.0 lb/ft² (342 kg/m²)

Thrust/weight: 1.09 (1.35 with loaded weight & 50% fuel)

 

Armament

1× 20 mm (0.787 in) M199A1 3-barreled Gatling cannon in the lower fuselage with 400 RPG

Eleven external hardpoints (two wingtip tails, six underwing hardpoints, three underfuselage hardpoints) and a total capacity of 11.000 lb (4.994 kg) of missiles (incl. AIM 9 Sidewinder and AIM 120 AMRAAM), bombs, rockets, ECM pods and drop tanks for extended range.

  

The kit and its assembly:

A spontaneous project. This major kitbash was inspired by fellow user nighthunter at whatifmodelers.com, who came up with a profile of a mashed-up US fighter, created “out of boredom”. The original idea was called F-21C, and it was to be a domestic successor to the IAI Kfirs which had been used by the US as aggressor aircraft in USN and USMC service for a few years.

 

As a weird(?) coincidence I had many of the necessary ingredients for this fictional aircraft in store, even though some parts and details were later changed. This model here is an interpretation of the original design. The idea was spun further, and the available parts that finally went into the model also had some influence on design and background.

I thank nighthunter for sharing the early ideas, inviting me to take the design to the hardware stage (sort of…) and adapting my feedback into new design sketches, too, which, in return, inspired the model building process.

 

Well, what went into this thing? To cook up a F-24 à la Dizzyfugu you just need (all in 1:72):

● Fuselage from a Hasegawa X-29, including the cockpit and the landing gear

● Fin and nose cone from an Italeri F-16A

● Inner wings from a (vintage) Hasegawa MiG-21F

● Outer wings from a F-4 (probably a J, Hasegawa or Fujimi)

 

The wing construction deviates from nighthunter’s original idea. The favorite ingredients would have been F-16XL or simple Mirage III wings, but I found the composite wing to be more attractive and “different”. The big F-16XL wings, despite their benefit of a unique shape, might also have created scale/size problems with a F-20 style fuselage? So I built hybrid wings: The MiG-21 landing gear wells were filled with putty and the F-4 outer wings simply glued onto the MiG inner wing sections, which were simply cut down in span. It sounds like an unlikely combo, but these parts fit together almost perfectly! In order to hide the F-4 origins I modified them to carry wingtip launch rails, though, which were also part of nighthunter’s original design.

 

The AAW technology detail mentioned in the background came in handy as it explains the complicated wing shape and the fact that the landing gear retracts into the fuselage, not into the wings, which would have been more plausible… Anyway, there’s still room for a simpler export version, with Mirage III or Kfir C.2/7 wings, and maybe canards?

 

Using the X-29 as basis also made fitting the new wings onto the area-ruled fuselage pretty easy, as I could use the wing root parts from the X-29 to bridge the gap. The original, forward-swept wings were just cut away, and the remains used as consoles for the new hybrid delta wings. Took some SERIOUS putty work, but the result is IMHO fine.

 

The bigger/square X-29 air intakes were taken over, and they change the look of the aircraft, making it look less F-5-ish than a true F-20 fuselage. For the same reason I kept the large fairing at the fin base, combining it with a bigger F-16 tail, though, as a counter-balance to the new, bigger wings. Again, the F-16 fin was/is part of nighthunter’s idea, so the model stays true to the original concept.

 

For the same reason I omitted the original X-29 nose, which is rather pointy, sports vanes and a large sensor boom. The F-16 nose was a plausible choice, as the AN/APG-80 is also carried by late Fighting Falcons, and its shape fits well, too.

 

All around the hull, some small details like radar warning sensors, pitots and air scoops were added. Not really necessary, but such thing add IMHO to the overall impression of such a fictional aircraft beyond the prototype stage.

 

Cockpit and landing gear were taken OOB, I just added a pilot figure and slightly modified the seat.

 

The ordnance was puzzled together from the scrap box, the AIM-9Ls come from the same F-4 kit which donated its outer wings, the AIM-120s come from an Italeri NATO weapons kit. The drop tanks belong to an F-16.

  

Painting and markings:

At first I considered an F-24I in IAF markings, or even a Japanese aircraft, but then reverted to one of nighthunter’s initial, simple ideas: an USAF aircraft in the “Hill II” paint scheme (F-16 style), made up from three shades of gray (FS 36118, 36270 and 36375) with low-viz markings and stencils. Dutch/Turkish NF-5A/Bs in the “Hill II” scheme were used as design benchmarks, too. It’s a simple livery, but on this delta wing aircraft it looks pretty interesting. I used enamels, what I had at hand: Humbrol 127 and 126, and Modelmaster's 1723.

 

A light black ink wash was applied, in order to em,phasize the engraved panel lines, in contrast to that, panels were manually highlighted through dry-brushed, lighter shades of gray (Humbrol 27, 166 and 167).

 

“Hill II” also adds to a generic, realistic touch for this whif. Doing an exotic air force thing is rather easy, but creating a convincing whif for a huge military machinery like the USAF’s takes more subtlety, I think.

 

The cockpit was painted in medium Gray (Dark Gull Grey, FS 36231, Humbrol 140), as well as the radome. The landing gear and the air intakes were painted white. The radome was painted with Revell 47 and dry-brushed with Humbrol 140.

 

Decals were puzzled together from various USAF aircraft, including sheets from an Airfix F-117, an Italeri F-15E and even an Academy OV-10D.

  

Tadah: a hardware tribute to an idea, born from boredom - and the aircraft does not look even bad at all? What I wanted to achieve was to make the F-24 neither look like a F-20, nor a Saab Gripen clone, as the latter comes close in overall shape, size and design.

Applying the absolute maximum amount of moxie possible, on 17th st, Potrero Hill.

 

Taken with the flippant bendycam 19.

131201 JKT48

 

#NgayogyakarLove

Sportorium UMY Yogyakarta

 

Image taken by TPJJ and owned by AnkoruMagz

1958 VW pick up spent most of her life on a farm in Oklahoma. Over the last 4 years the truck has undergone a total nut and bolt restoration and has been re-engineered to introduce modern components. The Rolls Royce Viper 535 jet engine is from a fighter jet with an afterburner added to produce a maximum power output of 5000 lbs of thrust which can be roughly translated to 5000 BHP.

Hillcrest San Diego California

Schweiz / Wallis - Aletschgletscher

 

In the background you can see the Olmenhorn (3,314 m).

 

Im Hintergrund sieht man das Olmenhorn (3.314 m).

 

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)

Recently refurbished Citaro 3901 (BX56 VTU) arrives into Guildford on the 37. Enviro 4013 (GN58 BTV), itself recently retrimmed and repainted, brings in the 101 behind.

 

From 30th August 2015, the Sunday service on the 36 and 37 was increased to hourly on each route. Previously it was two-hourly each way around.

 

Friary bus station, Guildford, Surrey.