BH250-175e

Title

BH250-175e

Subject

Bass Limestone

Description

Major Mineral: calcite
Minor Mineral: chert

In thin section, the Bass Limestone contains low-birefringence, low-relief minerals identified as chert (microcrystalline quartz), which formed through diagenetic recrystallization. As the oldest sedimentary unit in the Grand Canyon, the Bass Limestone has experienced low-grade metamorphism, leading to the recrystallization of both calcite and chert.

The calcite grain size in the Bass Limestone is substantially larger than that of younger limestones in the region, such as the Muav Limestone, reflecting the prolonged effects of metamorphism and diagenesis. This contrasts with younger and less-altered limestones like samples BH250-122, 125, 128, 140, 175f, 122wc, and 128c, which retain finer-grained textures.

You will find many calcite grains in Bass Limestone thin sections are cut perpendicular to sub-perpendicular to the c-axis, producing optic axis figures or off-centered uniaxial negative interference figures when viewed under crossed polars.

Coverage

Location: Mile 132 Stone Creek, Grand Canyon, Arizona, USA
Nearby Geographic Feature: Grand Canyon

Date

August 2021

Creator

Bereket Haileab

Source

From the rock collection of Bereket Haileab. Sample BH250-175e. Housed at Carleton College in Minnesota.

Contributor

Bereket Haileab

Type

Thin section and hand sample

Relation


View on ArcGIS Online here











  





Collection

Citation

Bereket Haileab, “BH250-175e,” BH250 Mineralogy Teaching Collection, accessed April 25, 2026, https://bereket-haileab.geology.sites.carleton.edu/items/show/231.

Output Formats

Geolocation