Venue & Hospitality

Welcome to the Official Attendee Housing Site for the 2ndAnnual Congress on Orthodontics and Endodontics, scheduled at Melbourne, Australia.
Accommodations will be provided at Conference Venue.


Conference Dates: October 21-22, 2019

Hotel Services & Amenities

  • Audio/Visual Equipment Rental.
  • Business Center.
  • Business Phone Service.
  • Complimentary Printing Service.
  • Express Mail.
  • Fax.
  • Meeting Rooms.
  • Office Rental.
  • Photo Copying Service.
  • Secretarial Service.
  • Telex.
  • Typewriter.
  • Video Conference.
  • Video Messaging.
  • Video Phone.
  • ATM.
  • Baggage Storage.


Mercure Melbourne Albert Park
16 The Esplanade, St Kilda VIC 3182, Australia.
Melbourne Airport
Departure Dr, Melbourne Airport VIC 3045, Australia
Continue to M2
2 min (1.5 km)
Continue on M2. Take Citylink/State Route 43 to Kings Way/Princes Hwy in Southbank. Take exit 2 from Citylink/State Route 43
20 min (23.9 km)
Drive to National Highway Alt 1 in Melbourne
5 min (2.7 km)
Mercure Melbourne Albert Park,65 Queens Rd, Melbourne VIC 3004, Australia

Route Map

About City

The city of Melbourne is known as the capital city of the state of Victoria. It is situated at the head of Port Phillip Bay, on the south-eastern coast. It is the core of a wider metropolitan area the world’s most southerly with a population over 1,000,000. In Australia, it is second to Sydney in population, and there is a good-natured rivalry among the two cities.

Melbourne city has so many beautiful parks, and an individual with an eye for architectural detail and history can find much that is varied and attractive. Melbourne has a reputation for conservatism and financial reliability attributes that have contributed to its growth and are revealed by the burgeoning skyline of the central city and the rapidly increasing eastern suburbs.

The development of Melbourne from its origins at the mouth of the Yarra River to its present shape shows a solid connection with the topography and waste of the land. The western region of the original city, basalt flows during the Cenozoic Era filled the existing valleys and left flat, uniform plains whereas the eastern region, however, consists of rolling and dissected beds of sandstones conglomerates and shales, laid down in the Silurian.

Not surprisingly, the expansion of Melbourne has been mainly eastward into the broad reaches of land between Darebin Creek, Koonung and Gardiner's creeks and the Plenty and Yarra rivers. In a strikingly asymmetrical way,

Melbourne’s climate results from the eastward flow of high-pressure cells divided by low-pressure troughs. These patterns follow a sequence that passes south of the continent in summer and over northern Victoria in winter.