Based on your description of the oceanic crust around a mid-ocean ridge, the correct observation and inference would be:
1. The crust farthest from the ridge is older compared to the crust closer to the ridge.
2. This observation supports the following process:
c. The further from the ridge, the older the crust is: this proves that sea floor spreading is occurring and new oceanic crust is being made constantly.
This option accurately describes the phenomenon observed at mid-ocean ridges, where new crust is formed as tectonic plates pull apart, causing the crust closest to the ridge to be younger than that further away.