Key points are not available for this paper at this time.
The La Sal Mountains, in central-eastern Utah, comprise 3 of the 15 laccolithic mountain groups on the Colorado Plateau. The mountains include 3 masses that are distinct topographically and geologically; each of the 3 consists of a stock surrounded by a cluster of laccoliths that radiate from the stock.
Chris Hunt (1958) studied this question.