Posted on July 27, 2008 by hadda
How they can drive dynamos
We know that all information of planetary magnetic fields based on indirect measurements which are mostly obtained from the space missions. We also make Earth’s dynamo process as reference to understand other planet magnetic fields, although for the Earth itself there is no certain theory how it can generate a dynamo [...]
Filed under: Geomagnet | Tagged: Earth magnetic field, Planetary magnetic fields | Leave a Comment »
Posted on July 22, 2008 by hadda
Findings could lead to earthquake prediction
New instruments detect small changes in rocks along the San Andreas fault up to 101/2 hours before a temblor. But more research is needed.
By Thomas H. Maugh II, Los Angeles Times Staff Writer
July 12, 2008
U.S. researchers said they were able to measure small changes in the density of fractures along [...]
Filed under: Geoscience | Tagged: Add new tag, Earthquake prediction, Earthquakes, San Andreas Fault, Seismic waves | Leave a Comment »
Posted on July 20, 2008 by hadda
Introduction
The solar system can be defined as the sun with all the planets, satellites and asteroids that move around it. The bodies in the solar system which have radius greater than 1000 km are likely to have dynamos that can generate magnetic fields (Jones, 2007). These bodies are the gas giant planets: Jupiter and [...]
Filed under: Geomagnet | Tagged: Add new tag, Magnetic observations, Planetary magnetic fields, Self -sustaining dynamos | Leave a Comment »
Posted on July 18, 2008 by hadda
The magnetic field of the Earth consists of magnetic fields coming from several sources both internal and external source. The external magnetic field of the Earth is mainly from the interaction between the solar wind and geomagnetic field. The solar wind can be described as the movement of particles particularly H+, Helium and electron which [...]
Filed under: Geomagnet | Tagged: External magnetic field, Magnetopause, Magnetosheat, Plasmasphere | 3 Comments »