Answer:
Sharing with the student through the online classroom and virtual labs
Explanation:
- Education itself a leaning where the teachers can provide the student with various opportunities to learn from technology as the elementary level student are very curious to learn the can be shown the practical aspects of the basic fundamentals like the rotation of fan, the places located in various parts of the earth and made to solve various puzzles thru the help of computer screens.
- Various other opportunities like the fun and learn where they get to learn the science and reason behind the process at work like making use of projectors, presentation, and other graphical aids.
- Giving them 3D models to learn from showing them the real-time monitoring system f air pollution and the use of virtual technology can be a suitable aid for this.
Answer:
The one on the top and right is water erosion, The one on the left is caused from a rock being there for so long is starts to become thinner because of the wind. Now the middle left is a natural basin that looks like water flowed through it so again water erosion. The middle right looks like the rocks and dirt fell off a mountain from being loosened from all the water,wind,humans and others so the kind of erosion is accelerated erosion. the bottom left is strong wind erosion. and the bottom right is a landslide. Hope this helps.
Explanation:
No, The magnetic north shifts overtime due to the rotation of liquid iron in the earth! So your answer would be No they are not always the same distance apart! Hope this helps :)
The image shows the Convergent plate boundary.
<u>Explanation:
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Convergent boundaries occur wherever the Earth’s tectonic plates move or collide toward each other.
As the plates converge, the denser, thinner tectonic plate sub-ducts or dives beneath the lighter, thicker, more buoyant tectonic plate.
As shown in the picture, the plates are composed of rigid lithosphere consisting of the crust of the earth and the uppermost mantle. Movement of the plates is driven by convection in the asthenosphere and lower mantle, which are softer and warmer than the lithosphere and can flow on geologic timescales. Convection is fuelled by heat generated from radioactive decay of elements in the Earth.
