Here's why:
* Partially Molten: The asthenosphere is a zone of the upper mantle that is partially molten. This means it has a solid structure but also contains pockets of molten rock.
* Ductile Behavior: Due to the partial melting, the asthenosphere exhibits a ductile behavior, meaning it can deform and flow under pressure. This is similar to how jello can deform when pressure is applied.
* Plate Tectonics: The asthenosphere is crucial for plate tectonics. The solid but flowing nature of the asthenosphere allows the tectonic plates to move on top of it.
It's important to note that the asthenosphere is not actually liquid like jello, but its semi-solid nature with the ability to flow makes it a useful analogy.