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Conrad
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Seismogram
Cartoon Scientists
Seismic Waves
Magma Chamber
Earth Is Layer Wikipedia
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Earth Structure
Earth Structure for Kids
Plate Tectonics
Geomorphology
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About the Earth
Discontinuidad De Mohorovicic
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The Mohorovicic Discontinuity, commonly called the “Moho” is recognized as the boundary zone between Earth's crust and the mantle. This boundary marks a change in seismic-wave velocity from the crust to the uppermost mantle within the (lithospheric) plate. This boundary was discovered by Andrija Mohorovičić, a Croatian meteorologist-turned seismologist, after an earthquake in Croatia in 1909. https://www.iris.edu/hq/inclass/animation/layers_of_the_earthwhat_is_the_moho | EarthScope Consortium
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