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What else can I help you with?
Can S waves travel through the earths mantle?
Yes, S-waves can travel through the Earth's mantle. They are secondary seismic waves that propagate by shearing the material they pass through, making them able to travel through solid materials like the mantle. However, their velocity and amplitude might change as they move through the different layers of the Earth.
Do p waves travel through earths mantle?
Yes, P-waves (primary waves) can travel through the Earth's mantle. P-waves are a type of seismic wave that is capable of propagating through solid, liquid, and gaseous materials. They are the fastest seismic waves and can travel through the mantle, which is the layer between the Earth's crust and core.
Can p waves travel through the mantle?
Yes. Compressional waves (P-waves) can travel through solids, liquids, and gases. They can propagate through every layer of earth's interior. In contrast, shear waves (S-waves) can pass through solids but not liquids or gases. As they propagate toward the center of the earth they pass through the crust, refract through the crust-mantle interface, pass through the mantle, but cannot pass through the mantel-outer core interface because the outer core is liquid.
Give are the three ways scientist can learn about earth's mantle?
Scientists can learn about Earth's mantle through seismic studies that analyze how seismic waves travel through the mantle, laboratory experiments that simulate mantle conditions, and by studying rare mantle-derived rocks that reach the Earth's surface through volcanic eruptions.
Do seismic waves need a medium to travel through?
Seismic, or earthquake waves travel through the earth. They may travel through our crust, which is rocky, or through the more fluid parts, like the mantle, but the medium is the earth.
Do p waves travel through the crust mantle outer and inner core?
Yes, P-waves can travel through the Earth's crust, mantle, outer core, and inner core. They are the fastest seismic waves and can travel through both solid and liquid layers of the Earth, with their speed and direction changing as they encounter different materials.
What earthquakes travel through the earth's mantle?
Primary waves and secondary waves (body waves). Love waves and rayleigh waves (surface waves) do not travel through the earth's mantle. Though secondary waves do not go through liquids, the asthenosphere is only a semi-liquid, so secondary waves can still go through it.
What type of seismic wave can pass through the Earth's mantle and core?
There are two types of waves ; P waves and S waves . P waves can travel through solids , liquids , and gases . S waves can only travel through solids . The mantle is pure solid rock ; the outer core is made of liquid-iron and nickel . In other words , only P waves can travel through both the mantle and the core . Hope this helps ! Give thanks to 7th grade Earth science ! :D
What layer of earth will waves travel through faster?
The mantle of course.....because sound waves travel through liquid like surfaces better than solid rock.
Is there an empty space in the Earth's mantle?
To my knowledge, there is not known to be an empty space in the mantle. Earthquake seismic waves travel through the Earth in different ways as they change from crust to mantle. Such a void would have probably been detected by now, as the waves would NOT travel through a void - they travel through solids and liquids (but not the solid of the Earth's core).
Can you infer why p waves travel faster through He upper mantle than they do thought the crust?
P waves travel faster through the upper mantle because it is composed of denser rock materials compared to the crust. The higher density allows the seismic waves to propagate more efficiently through the upper mantle, resulting in higher velocity. Additionally, the upper mantle is composed of more solid rock material, while the crust may contain more heterogeneous and less dense materials that can slow down the waves.
Can a black hole travel through space?
Yes, a black hole could travel through space.
