As a country bordered by the Indo-Australian Plate and Pacific Plate.
Indo-Australian Plates is the name for the 2nd plate tectonics including the Australian continent and surrounding ocean extending northwest to include the Indian subcontinent and in surrounding waters. Divided into 2 plates along the border are less active: Australian plate and the Indian plate are smaller. The two plates were joined together between 50 to 55 million years of the century, before that, the two plates that move independently
biplanes Pacific tectonic plate is at the bottom of the ocean of the
With the two plates such activities can provide the effect of pressure on rocks in the bowels of the earth. Pressure will result in the occurrence of a fault or rock mass movement that can be up to the surface of the earth in the form of vibrations or shocks commonly known as earthquakes.
With advances in technology and science, then the earthquake vibrations can be detected using a tool (detector) if the land is called detector whereas if the geophone on the sea called hydrophone (buoy).
Current earthquake information can be obtained in real-time, as well such earthquake along our country, meaning if there are earthquakes in the Indonesian region would then directly detected by seismic detectors (buoy) and then record the results of data transmitted to the satellite, the satellite will sent to the centers of seismic data processing are connected to each other throughout the world, so large or scale earthquake vibrations can be known.
The problem we often face is sometimes the data (earthquake info) late known, probably due to the seismic data acquired by the agency pending BMKG, or maybe you did not get to see the news on television then you can still see in real time earthquake information.
If you want to know the data / events in real time earthquake (real time data is not corrected by seismic experts), but the data you can use for reference to be wary of the disaster.