You can't actually *see* the asthenosphere, because it's a layer of Earth's mantle that lies beneath the crust. However, the effects of the asthenosphere are visible in the form of tectonic plate movement.

Here's a simplified explanation:

1. Imagine a giant, hot, gooey layer of taffy: That's the asthenosphere. It's solid rock, but at such high temperatures and pressures, it behaves like a very viscous fluid.

2. The Earth's crust sits on top of this taffy: The rigid plates of the Earth's crust (like the North American Plate) move slowly across the asthenosphere.

3. This movement causes earthquakes, volcanoes, and mountain formation: Think of the taffy being pushed and pulled, creating movement on the surface.

So, the asthenosphere itself isn't something you can see, but its effects are observable around the world.

Here are some specific examples of how we see the asthenosphere in action:

* Mid-ocean ridges: These underwater mountain ranges are formed as magma from the asthenosphere rises to the surface, pushing plates apart.

* Volcanoes: Volcanoes often occur at plate boundaries where the asthenosphere is pushing up magma.

* Earthquakes: The movement of tectonic plates across the asthenosphere creates friction, which causes earthquakes.

Let me know if you'd like me to elaborate on any of these examples!