BH250-241d

Title

BH250-241d

Subject

Xenolith without basalt

Description

Cinder cones are beautiful volcanic features that decorate the landscape. The Split Cinder Cone in southern Death Valley is a Pleistocene-age volcano that has been split and displaced by movement along the active Southern Death Valley Fault Zone. Located near West Side Road and Highway 178, the western part of the cone has been offset approximately 225 meters north relative to the eastern portion by right-lateral strike-slip faulting, a relationship that can be observed both in the field and on satellite imagery.

In addition to the beautiful structural features visible at this site, the cinder cone preserves several notable volcanic features, including volcanic bombs and chilled margins. Another important characteristic of this outcrop is the presence of abundant xenoliths, which were brought to the surface by the lava and are exposed throughout the cinder cone. Some of these xenoliths are felsic in composition, indicating that the magma incorporated shallow granitic country rock during ascent. Five samples were collected from this site, including a volcanic bomb and several xenoliths: BH250-241a, BH250-241b, BH250-241c, and BH250-241e.

Coverage

Location: Death Valley, California, USA
Nearby Geographic Feature: Death Valley
GPS Coordinates: 35.940906, -116.732639

Creator

Bereket Haileab

Source

From the rock collection of Bereket Haileab. Sample 241d. Housed at Carleton College in Minnesota.

Type

Thin section and hand sample

Relation









Collection

Citation

Bereket Haileab, “BH250-241d,” BH250 Mineralogy Teaching Collection, accessed April 24, 2026, https://bereket-haileab.geology.sites.carleton.edu/items/show/360.

Output Formats

Geolocation