Figure 1. Locality map showing outcrops of the Imperial Formation s.l. in southern California. Outcrops of the late Miocene to Pliocene Imperial Formation s.s. include: 1) Edom Hill/ Indio Hills/Willis Palms/Thousand Palms Canyon (Powell 1985, Powell 1986, Powell et al. 2011), 2) the southern Santa Rosa Mountains (King et al. 2002), 3) Travertine Point (Powell 2008), 4) Ocotillo Wells State Vehicle Recreation area (Powell 1993), 5) Superstition Mountain (Morton 1977), 6) Fish Creek Mountains (Dibblee 1954, Morton 1977), 7) Coyote Mountains (Hanna 1926), and 8) Yuha Buttes (Hanna 1926). Outcrops of the late Miocene "Imperial" Formation s.l. occur at 9) Lions Canyon (Bramkamp 1935, Powell 1986), 10) Super Creek (Bramkamp 1935, Powell 1985, Powell 1986, Powell and LaFollette 2012), and 11) Garnet Hill (Powell 1985, Powell 1986, Rymer et al. 1995, Powell 1995).

Published as part of Raines, Bret, 2023, Caecidae (Mollusca: Gastropoda) from late Miocene exposures of the "Imperial" Formation in Riverside County, California, pp. 1-11 in PaleoBios 40 (7) on page 2, DOI: 10.5070/P940753832, http://zenodo.org/record/10913593