I am working to constrain the distribution of asteroids that show evidence of past partial melting (i.e. a surface with basaltic material) by discovering new V-type asteroids that are not dynamically associated with the Vestoid family. The results of this spectroscopic survey have implications for understanding the past thermal history of Main Belt planetesimals, which in turn can help to establish a more robust relationship between asteroidal surface properties and the measured composition of meteorite samples.