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physicaltherapy: 05 Feb : 06:54 pm

Is there anyone who has gone through CWT6 or type 1 evaluation with FCCPT?
If so, kindly let me know from where can the following deficiencies be fulfilled?
1. History
2. Systems Review
3. Findings that warrant referral
4. Supervision of support staff
5. Documentation

nani: 28 Sep : 04:31 am

plz pleasec tell me where to do phd in india

Nikhilphysio: 02 Jun : 03:55 am

I am working as physiotherapist in Shalby hospital ahmedabad for 4 years. I have passed out from Rajiv gandhi university of health and sciences Bangalore. I want to apply for Newzealand physiotherapy board registration so anyone there from India who got registered as physiotherapist in new zealand please help me.

Arun: 10 May : 12:36 am

Hi Priyank, welcome. Feel free to go through these forum threads returned by search [link]

Priyank: 09 May : 10:28 pm

Hi..need advice. What are the options in Australia after MPT?


Asian Tsunami Disaster

Wednesday 29 December 2004 - 08:23:57

26-12-'04, Sunday Tsunami wave, which hit India for the first time today wreaking havoc across the southern coastline of India is a known phenomenon in the Pacific Ocean region stretching from Chile in Latin America to Japan in Far East Asia. The waves, which caused by a massive earthquake on the Indian Ocean and claimed thousand of lives in India and six other countries, are usually triggered by seismic disturbances - coastal earthquakes, volcanic eruptions, or undersea landslides - that jolt the ocean floor. Often, tremors displace ground surface, sending an entire column of water in motion outward from an earthquake region - often with disastrous results thousands of kilometers from their origin. The difference between Tsunami waves and tidal waves is that while the former hit only the harbors and coastal areas even as the other parts of the sea remain calm the latter make the sea rough.
High-speed wave
The result is a deep wave that reaches from the sea's surface to the floor, travels horizontally at speeds up to 500 miles per hour, and reaches heights between 50 and 100 feet. The waves travel faster in deeper water and when it approaches shore, they rise further. It is the sharp elevation of the ocean floor near the coast that slows the bottom of the wave while the top keeps moving at the original speed. Vast quantity of water then piled up into a vertical wall that finally crashes over the shore with amazing force. In the open sea, Tsunamis are only about a meter high, but when they reach a shoreline, they can be taller than a house and weigh millions of tons.

Seismic waves
The word "Tsunami" has come from Japanese language, describing very long, low seismic sea waves. It usually found in the Pacific Ocean where there is significant movement of the earth's tectonic plates. Japan is one of the two Asian countries - the other being Indonesia - which has been frequently hit by Tsunami waves. The Japanese suffered the fury when hundreds died after a huge wave traveling at a speed of 750 km per hour smashed the country in 1960 following a series of quakes in Chile on the other side of Pacific Ocean. Major Tsunamis occur in the Pacific Ocean region only about once per decade and the major ones - the Prince William Sound, Alaska, in March 1964, and the Tsunami generated off the coast of Chile in 1960 - have been devastating over large distances

Killer wave Tsunamis have been responsible for thousands of fatalities, especially in Japan and Indonesia. In the Indian Ocean, which hit by the quake today, the Indo-Australian plate is being sub ducted beneath the Eurasian plate at its east margin. Therefore, most Tsunamis generated in this area propagated toward the southwest shores of Java and Sumatra, rather than into the Indian Ocean. The first sign of an approaching Tsunami is the sea tide draining away from the shore. A moment of silence for the departed beloveds..... Be aware though we cannot be "BEWARED” here.....

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