Samsung Galaxy S8, S8+, S7/7Edge, S6/S6 Edge, Galaxy S5, Samsung
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"At S8 – 2019 – I // die Galluswarte im Ledermuseum / braucht die Mühl nicht heim zu tragen / denn die Steinberg wies zur Weiskirche"
(c) Drager Meurtant, 2019, in private collection
ELEPHANT PLAINS: Located in the Sabi Sand Game Reserve, neighbouring the Kruger National Park, the Elephant Plains Game Lodge promises a Big Five game viewing experience with high class luxurious and comfortable accommodation facilities. From rondavels to intimate honeymoon suites the lodge provides its guests with a vast range of options to choose from for their accommodation. Elephant Plains Game Lodge is famous for the enthralling Big Five game viewing where guests can avail two game drives a day. With amazing facilities like swimming pool, spa, gym, library, games room and much more; Elephant Plains Game Lodge serves the guests with one of the best accommodation services in South Africa. The lodge can accommodate up to 24 guests at a time and also offer wedding planning services for those who wish to celebrate the wedding in the wilderness of South Africa. www.elephantplains.co.za
KRUGER NATIONAL PARK is one of the largest game reserves in Africa. It covers an area of 19,485 km2 in the provinces of Limpopo and Mpumalanga in northeastern South Africa, and extends 360 km from north to south and 65 km from east to west. The administrative headquarters are in Skukuza. Areas of the park were first protected by the government of the South African Republic in 1898, and it became South Africa's first national park in 1926. To the west and south of the Kruger National Park are the two South African provinces of Limpopo and Mpumalanga. In the north is Zimbabwe, and to the east is Mozambique. It is now part of the Great Limpopo Transfrontier Park, a peace park that links Kruger National Park with the Gonarezhou National Park in Zimbabwe, and with the Limpopo National Park in Mozambique. The park is part of the Kruger to Canyons Biosphere an area designated by the United Nations Educational, Scientific and Cultural Organization (UNESCO) as an International Man and Biosphere Reserve (the "Biosphere"). The park has nine main gates allowing entrance to the different camps. en.wikipedia.org/wiki/Kruger_National_Park
SABI SAND: The Sabi Sand Game Reserve is situated in the southwestern corner of the world-renowned Kruger National Park in South Africa and consists of 65000 hectares. It is the most prestigious game reserve in South Africa and is famous for incredible leopard and lion sightings. www.sabisandsgamereserve.com
hathe kent msawy 3leeha test drive
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A l l R i g h t s R e s e r v e d : AbdulAziz ..}
taken By: Me
111 036 ist mit SVG 61370 von Freudenstadt nach Eutingen im Gäu bei Dornstetten als Ersatzzug für die S8 auf dem Kübelbachviadukt unterwegs.
Watkins Glen State Park is located in the village of Watkins Glen, south of Seneca Lake in Schuyler County in New York's Finger Lakes region. The park's lower part is near the village, while the upper part is open woodland. It was opened to the public in 1863 and was privately run as a tourist resort until 1906, when it was purchased by New York State. Initially known as Watkins Glen State Reservation, the park was first managed by the American Scenic and Historic Preservation Society before being turned over to full state control in 1911. Since 1924, it has been managed by the Finger Lakes Region of the New York State Office of Parks, Recreation and Historic Preservation. The centerpiece of the 778-acre (3.15 km2) park is a 400-foot-deep (120 m) narrow gorge cut through rock by a stream – Glen Creek – that was left hanging when glaciers of the Ice age deepened the Seneca valley, increasing the tributary stream gradient to create rapids and waterfalls wherever there were layers of hard rock. The rocks of the area are sedimentary of Devonian age that are part of a dissected plateau that was uplifted with little faulting or distortion. They consist mostly of soft shales, with some layers of harder sandstone and limestone. The park features three trails – open mid-May to early November – by which one can climb or descend the gorge. The Southern Rim and Indian Trails run along the wooded rim of the gorge, while the Gorge Trail is closest to the stream and runs over, under and along the park's 19 waterfalls by way of stone bridges and more than 800 stone steps. The trails connect to the Finger Lakes Trail, an 800-mile (1,300 km) system of trails within New York state. The park has comfortable camping sites, as well as picnic tables and pavilions, food, playground, a gift shop, pool, dump stations, showers, recreation programs, tent and trailer sites, fishing, hiking, hunting and cross-country skiing. The entrance fee for a day picnic is $8 per car. The park is open year-round, but not all facilities are available at all times. During the Pleistocene era, a vast area was covered by ice during the maximum extent of glacial ice in the north polar area. The movement of glaciers from the Laurentide and Wisconsin ice sheets shaped the Finger Lakes region. The lakes originated as a series of northward-flowing streams. Around two million years ago the first of many continental glaciers of the Laurentide Ice Sheet moved southward from the Hudson Bay area, initiating the Pleistocene glaciation. These glaciers widened, deepened and accentuated the existing river valleys. Glacial debris, possibly including terminal moraines, left behind by the receding ice acted as dams, allowing lakes to form. Despite the deep erosion of the valleys, the surrounding uplands show little evidence of glaciation, suggesting that the ice was thin, or at least unable to cause much erosion at these higher altitudes. The deep cutting of the valleys by the ice left some tributaries hanging high above the lakes: both Seneca and Cayuga have tributaries hanging as much as 390 feet (120 m) above the valley floors. One such hanging valley, overlooking the south end of the Seneca Lake valley, evolved into the deep gorge of Watkins Glen. The steep drop of Glen Creek into Seneca Valley created a powerful torrent that eroded the underlying rock, cutting further and further back towards the stream's headwaters. This erosion was not a uniform process: the rock here includes shale, limestone, and sandstone, and these types of rock erode at different rates, leaving behind a staircase of waterfalls, cascades, plunge pools and potholes. Watkins Glen State Park now encompasses nineteen waterfalls spaced along a trail roughly two miles (3.2 km) long.
20180507_121013. I really miss my office in the Villa. My company rented 1-3 rooms in different places inside for seven years. Fantastic workplace. Epic garden.
A London Underground S8 Stock departs from Northwood whilst on a Met Line service to Aldgate, whilst Chiltern Railways 165022 and 165024 pass on a service towards Aylesbury Vale Parkway
Taken only a few days after motorway opened after being many years in construction. People came to stare...
"Others have seen what is and asked why. I have seen what could be and asked why not." - Pablo Picasso
5x7" Title: "S8 LVIII"
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