Last Airing of QuakeWatchTV...

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A great Site For Earthquake Information found HERE

Latest QuakeWatchTV Broadcast:

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Latest QuakeWatch TV Broadcast Appealing For Details or A-Z List of Towns Cities And Countries Within Known Seismic Areas;


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QuakeWatchTV Report Aired Sat 23rd April 2011..

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Proof that Earthquake Swarms can and Do exist as 11 Quakes Hit Baja California Mexico


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Northern Carolina U.S.A. Tornados Strike.

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Austrailia Has Two Quakes

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Another Area Full Of Seismic Activity..


The Septentrional-Orient fault zone (SOFZ) is a system of coaxial left lateral-moving strike slip faults which runs along the northern side of the island of Hispaniola where the Dominican Republic and Haiti are located. The SOFZ shares approximately half of the relative motion between the North American and Caribbean tectonic plates with the Enriquillo-Plantain Garden fault zone which runs along the southern side of Hispaniola. Both faults merge into the Cayman Trench to the west. Some researchers believe that the Enriquillo-Plantain Garden fault zone and the SOFZ bound a microplate, dubbed the Gonâve Microplate, a 190,000 km2 (73,000 sq mi) area of the northern Caribbean Plate that is in the process of shearing off the Caribbean Plate and accreting to the North America Plate.

A major tremor on this fault destroyed the city of Cap-Haïtien and other cities in the northern part of Haiti and the Dominican Republic on 7 May 1842.

An Area Full Of Seismic Activity is The Puerto Rico Trench.


The Puerto Rico Trench is an oceanic trench located on the boundary between the Caribbean Sea and the Atlantic Ocean. The trench is associated with a complex transition between the subduction zone to the south along the Lesser Antilles island arc and the major transform fault zone or plate boundary that extends west between Cuba and Hispaniola through the Cayman Trench to the coast of Central America. Scientific studies have concluded that an earthquake occurring along this fault zone could generate a significant tsunami.

The island of Puerto Rico lies immediately to the south of the fault zone and the trench. The trench is 800 kilometres (500 mi) long and has a maximum depth of 8,605 metres (28,232 ft) at Milwaukee Deep, which is the deepest point in the Atlantic Ocean.

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QuakeWatch TV


Earth In The Future.
Question: Is this what will become of the Earth's surface? Answer: The surface of the Earth is broken up into several large plates that are slowly shifting. About 250 million years ago, the plates on which the present-day continents rest were positioned quite differently, so that all the landmasses were clustered together in one supercontinent now dubbed Pangea. About 250 million years from now, the plates are again projected to reposition themselves so that a single landmass dominates. Known As Pangea Ultima. At that time, the Atlantic Ocean will be just a distant memory, and whatever beings inhabit Earth will be able to walk from North America to Africa. Now Thats Food For Thought.

Some Great Video Shots Of The Mid Atlantic Ridge.

Details Of The New Madrid Fault.

Nice Video Of The Golden Triangle Laos and Burma(Myanmar)

Some Great Photos Around The Extremely Active Ring Of Fire.

Heres A Video Showing The Fault At The Surface..

What Im Broadcasting on QuakeWatch TV..

QuakeWatch TV- Broadcast your self LIVE

My first live cast on Blog TV.

blogtv 1 - Broadcast your self LIVE

Sunday Mornings LiveCast.

My 10th Livecast on Kwakewatch...

Are these images of Niburu setting.
..............Setting............




Do these images show Niburu Rising and Setting..You Decide..
....................Rising...................




Niburu get a Mention

Repeat of morning broadcast due to audio failure

Puerto Rico (Cont)

Puerto Rico Seismic Sensation.

Latest Broadcast.

The Christchurch Disaster


Neighbourhood Video

Footage Of Chiles Worst Ever Quake.


And The Tsunami That Followed..

Kesennuma Port Miyagi Terrifying Footage


California


San Francisco

Could This Really Happen.....Scientists Seem To Think It Will !!!!!!


And This Is From The Movie 'Deep Impact'......

This was the latest Broadcast I Did Monday 28th March 2011

Heres The First of Two Broadcasts I Did on Saturday 26/03/11


And Heres The Second...

Heres The 5th Broadcast

Just a I Came Off The Air This Happened:
MAG 6.8 2011/03/24 13:55:12 20.705 99.949 10.0 MYANMAR
MAG 4.8 2011/03/24 14:23:53 20.595 99.862 10.2 MYANMAR
Thailand Has Two Quakes In Quick Concession....

Indonesia 2004.



Japan 2011.



I Dont Think Anyone Will Ever Forget These Images...

Heres Kwakewatch 3 Livecast Recording:

 This list makes Magnitude Strengths Easy To Follow.

Less than 2.0     Micro     Micro earthquakes, not felt. ..About 8,000 per day
2.0–2.9     Minor     Generally not felt, but recorded.     About 1,000 per day
3.0–3.9     Often felt, but rarely causes damage.     49,000 per year (est.)
4.0–4.9     Light     Noticeable shaking of indoor items, rattling noises. Significant damage unlikely.     6,200 per year (est.)
5.0–5.9     Moderate     Can cause major damage to poorly constructed buildings over small regions. At most slight damage to well-designed buildings.     800 per year
6.0–6.9     Strong     Can be destructive in areas up to about 160 kilometres (100 mi) across in populated areas.     120 per year
7.0–7.9     Major     Can cause serious damage over larger areas.     18 per year
8.0–8.9     Great     Can cause serious damage in areas several hundred kilometres across.     1 per year
9.0–9.9     Devastating in areas several thousand kilometres across.
    1 per 20 years
10.0+     Massive     Never recorded, widespread devastation across very large areas; see below for equivalent seismic energy yield.
    Extremely rare (Unknown)

And heres the second broadcast ...

Heres the introduction i did in my first attempt at Live casting.

Kwakewatch is a Ustream production where i broadcast information based in real time with the latest earthquakes and just about anything else mother nature deams fit to throw at us...ive done two Livecasts up to yet and hope to capture a worldwide audience in time.....

Heres The Introduction:

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