Magnetic declination changes over time because themagnetic poles move slowly, between 1580 and 1820, for example the direction of magnetic north in London changed by 35 degrees Written by Londyn reid 13 yrs old
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Humera Kaleem
The magnetic field of the earth is everywhere. Well, it's not everywhere! The magnetic field is surrounding the entire earth. It's like if you placed two magnets together with opposite poles touching and sprinkled iron filings on it. All the filings would line up in a semicircle around the magnets and lead from positive to negative. except in the earths case the field would be 3-dimensional. Also, the field gets weaker as you move away from the planet. I hope I helped.
The Earth's magnetic field is the result of a dynamo. Put simply, the stuff under the earth's crust (especially the earth's molten core of iron) is rotating, convecting (hot stuff rises, cooler stuff sinks), and is electrically conductive. Because of all of this, the earth's interior acts sort of like an electrical generator, creating a huge magnetic field.
Additionally, the rocks of the crust are magnetised in the same direction as the earth's magnetic field and contribute to the effect.
Previous answer (cute, but seriously folks):
Barnstable, England.
The previous answer is mostly correct, but the Earth's core is not molten. It is pretty much solid iron. Mixed with a little nickel and other elements. But it is solid. It is the act of this solid core rotating through the molten upper layer that generates the magnetic field. The core periodically changes the direction of its rotation, which accounts for the magnetic stripes in the Atlantic Ocean floor near the mid atlantic trench. Molten rock rises from the trench, then orients itself in the direction of the Earth's magnetic field, then solidifies. Every time the magnetic poles switch, the orientation of the new molten rock changes direction. Thus, we can tell how often the poles switch direction.
To clarify a little, the Earth's core is solid at the center but molten toward the outside. The mostly iron core is hot enough to be molten throughout, but the intense pressure exerted on the inner core by all the rest of the Earth pushing down on it is so great that it forces the inner core to stay solid even though it's hot enough to melt at normal pressure.
By the way, the Earth's magnetic field change polarity randomly, but usually on a scale of hundreds of thousands to millions of years. That is, it tends to maintain its polarity for a long, long time.
I dont know about it but it saves some what from strorm from Sun. It is made from inside Earth from a molton mars which has high heat which use to make direction like east, north etc. Our magnetic field is smaller in size but other gaseous planets has very big magenetic field.
The simple question "how does the Earth get its magnetic field?" does not have a simple answer. It does seem clear that the generation of the magnetic field is linked to the rotation of the earth, since Venus with a similar iron-core composition but a 243 Earth-day rotation period does not have a measurable magnetic field. It certainly seems plausible that it depends upon the rotation of the fluid metallic iron which makes up a large portion of the interior, and the rotating conductor model leads to the term "dynamo effect" or "geodynamo", evoking the image of an electric generator.
they deflect solar energetic particles caused by coronal mass ejections from our sun (deflect harmful rays of sunlight)
It changes through direction and strength. Direction changes overtime so Magnetic North becomes Magnetic South.
The magnetic field in the Earth originates in the Core.
Birds and navi-computers use the Earth's EM Field to navigate. The EM Field also protects the planet from the Sun's deadly solar radiation.
The Outer Core
The OUTER CORE
The outer liquid core produces the strong magnetic field of the Earth, through the dynamo effect.
In the Dynamo Theory, the magnetic field of the earth is created in the outer core. The fluid contained in the outer core creates and maintains the magnetic field during rotation.
core
The earth's outer core produces the magnetic field.
The Outer Core
The OUTER CORE
inner core
The outer liquid core produces the strong magnetic field of the Earth, through the dynamo effect.
The entire Earth spins. No layer has a rotation rate the differs significantly from the rest of the planet. If any layer did the results would be catastrophic. The magnetic field is the result of convection currents in the outer core.
In the Dynamo Theory, the magnetic field of the earth is created in the outer core. The fluid contained in the outer core creates and maintains the magnetic field during rotation.
The Ozone layer of the earth protects the earth from the harmful UV radiations of the sun.
core
core
core
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