Sleet is somewhat of a colloquial term for ice pellets. We see that in a surface observation or terminal forecast as PL (this was changed from PE since rain and ice pellets falling at the same time might get coded as RAPE).
Ice pellets (sleet) are unmistakable. It resembles small hail, but is not produced by the same process as hail. When it hits an object such as a car windshied, it will bounce off. It is formed when snow falls through a shallow melting layer (temperature slightly above 0°C). This converts the snow to a rain drop with a nucleus that still has some crystalline structure (not completely melted). When this pseudo-drop falls through a subfreezing layer below it will refreeze into a hard nugget we call an ice pellet.
Freezing rain, on the other hand, comes in two flavors. The first is produced from the same process as described above, except, the melting layer is typically deeper or warmer. This completely melts the snow. This is called classic freezing rain as I describe in my
latest member workshop. The other flavor of freezing rain can have a similar profile, except, that the process doesn't start out as snow...it's an all-liquid process as I discuss in
this IFR magazine article.
What you potentially experienced based on your description is wet snow. That is snow that has nearly melted, but not quite. Keep in mind that ice pellets, rain, freezing rain and snow can all occur together in the atmosphere. So, the presence of PL is indicative of SLD aloft.
Hope this helps.