* Layers are not uniform: The Earth's layers vary in thickness depending on location. For example, the crust is thinner under the oceans than under continents.
* Defining "layers" is complex: The Earth's structure is divided into multiple layers based on different criteria (composition, physical properties, etc.).
However, we can provide a general idea of the relative thickness of the major layers:
* Crust (thinnest): 5-70 km thick
* Mantle (thickest): 2900 km thick
* Outer core: 2200 km thick
* Inner core: 1220 km thick
If we take the crust (thinnest) and compare it to the mantle (thickest), we can approximate the fraction:
* Crust: ~5-70 km (average ~35 km)
* Mantle: ~2900 km
This would be approximately a 1:83 fraction (35 km / 2900 km).
Important Notes:
* This is a very rough estimate, and the actual fraction can vary significantly depending on the specific location and the definition of layers.
* The Earth's layers have complex relationships, and understanding the Earth's structure requires more than just looking at simple fractions.