Jacek Proniewicz travel blog

picture and movies from my travel

Posts from the ‘mountins’ category

Paliton Beach, Siquior Visayas

Considered by some to be the most beautiful beach on the island it is located just a 4 kms from San Juan close to Tambisan Port. The fine white sand and the view to Negros and Apo island make this small beach (approx. 150m long) a special location. Fishermen pull their boats out and you can find many that have found their final resting place there and make great photography subjects. At high tide you can lay in the small natural ‘pools’ that are characteristic of Paliton. To find the road to Paliton you need to look out for the small church in barangay Paliton and turn down the road towards the sea, the beach is located approximately 1.5km on the main road.

Brooklyn Ferry to Dangar Island 

Brooklyn Ferry Service is a small ferry company, operating fully restored heritage vessels that run from Brooklyn to Dangar Island and Little Wobby Beach. The service provides essential public transport for the water-access properties in this area.The ferry runs everyday to a timetable and links with trains arriving and departing from Hawkesbury River railway station.

Take a day-trip to Dangar Island and learn about this history of this unique location and the ferries themselves.

Dunedin railway station 

Built in Dunedin in 1906 when the city was New Zealand’s leading commercial centre, this magnificent railway station remains, fully restored to its former glory.An excellent tourist excursion service is the only train now using the station. Much of its ground floor is used as a restaurant, and the upper floor houses an art gallery and a sports hall of fame.

In an eclectic, revived Flemish renaissance style, (Renaissance Revival architecture), the station is constructed from dark basalt from Kokonga in the Strath-Taieri with lighter Oamaru stone facings, giving it the distinctive light and dark pattern common to many of the grander buildings of Dunedin and Christchurch. Pink granite was used for a series of supporting pillars which line a colonnade at the front of the building. The roof was tiled in terracotta shingles from Marseilles surmounted by copper-domed cupolas. The southern end of the building is dominated by the 37-metre clocktower which is visible from much of central Dunedin. The sheer size, grandiose style and rich embellishments of the station earned architect George Troup the nickname of Gingerbread George.

The booking hall features a mosaic floor of almost 750,000 Minton tiles. A frieze of Royal Doulton porcelain runs around the balcony above it from which the floor’s design (featuring a locomotive and related symbols) can be clearly seen. The station’s main platform is the country’s longest, extending one kilometre.

The building’s foundation stone was laid by the Minister of Railways Joseph Ward on June 3, 1904. The Prime Minister Richard Seddon was also present. The station was opened by Ward, by then Prime Minister, in 1906. The construction of the building was kept within budget, and cost £40,000.

Created to be the jewel in the crown of New Zealand Railways, the Dunedin Railway Station has an atmosphere and character unique to any public building in the country, and is regarded as the most photographed building in New Zealand.

Antarctica,where is Antarctica,how big is it 

Antarctica is the fifth largest of the seven continents. It is situated over the South Pole almost entirely south of latitude 66°30′ south (the Antarctic Circle). It is a very rough circular shape with the long arm of the Antarctic Peninsula stretching towards South America. There are two large indentations, the Ross and Weddell seas and their ice shelves.The nearest other land masses are South America 1000 km (600 mls) away across the roughest stretch of water in the world – the Drake passage, Australia is 2500 km (1550 mls) away, and South Africa 4000 km (2500 mls) away.

The total surface area is about 14.2 million sq km (5.5 million sq mls) in summer, approximately twice the size of Australia, half as big again as the USA and fifty times the size of the UK.

In the winter Antarctica doubles in size due to the sea ice that forms around the coasts. The true boundary of Antarctica is not the coastline of the continent itself or the outlying islands, but the Antarctic Convergence.

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