Raven Crag is a fell in the English Lake District that overlooks Thirlmere reservoir.

The ridge has been extensively planted with conifers as part of the Thirlmere Forest, the face of Raven Crag appearing as a lone oasis of naked rock amid the trees.

Raven Crag is bordered to the west by the long valley of Shoulthwaite Gill, which is a tributary of the River Greta.

Raven Crag and the Benn exhibit rock of the Birker Fell Formation, composed of plagioclase-phyric andesite lavas with subordinate sills.

The ridge between Raven Crag and High Tove can also be gained from Armboth, or an ascent can be made from 'behind' via Shoulthwaite.