Schist in a sentence

Gold mineralization is hosted within a meta-sedimentary sequence dominated by banded (graphitic) quartzite and interbedded pelitic biotite schist that is cross-cut by numerous felsic to intermediate dikes and sills.

A couple of years ago, the museum’s tallest statue of Buddha in schist stone was transported to Switzerland for display there for 100 days at an international exhibition.

To anchor the living room the team added a fireplace with a schist surround.

Our field observations and panning gold should be generally abundant across the Asoza zone – both in quartz veins but also elsewhere in the schist and pegmatite rocks in which they are located.

View across the gold-bearing schist rocks of the Asosa zone, Benishangul-Gumuz.

A considerable amount of mica (both muscovite and biotite) is often simultaneously formed, and the resulting product has a close resemblance to many kinds of schist.

Between convert, the North Col Formation consists chiefly of biotite-quartz phyllite and chlorite-biotite phyllite intercalated with minor amounts of biotite- sericite -quartz schist.

Historical mining terminology Before the mid-19th century, the terms slate, shale and schist were not sharply distinguished.

Middle Kingdom art, "known for its gold work and statues", moved from realism to idealization; this is exemplified by the schist statue of Amenemhatankh and the wooden Offering Bearer.

One or more of the preceding sentences incorporates text from a publication now in the public domain : citation Image:Thin section of garnet-mica-schist.

Soapstone (chloritic schist) was used for the construction of these temples.

The host rock of the garnet here is garnetiferous mica schist and the total percentage of garnet is not more than 7% to 10%, which makes the material extremely costly and non-economical to extract for non-gemstone applications.

The individual mineral grains in schist, drawn out into flaky scales by heat and pressure, can be seen with the naked eye.

The major geologic exposures in the Grand Canyon range in age from the 2-billion-year-old Vishnu Schist at the bottom of the Inner Gorge to the 230-million-year-old Kaibab Limestone on the Rim.

The remainder of the North Col Formation, exposed between convert on Mount Everest, consists of interlayered and deformed schist, phyllite, and minor marble.

These features included the use of chloritic schist or soapstone as a basic building material.

The word schist is derived ultimately from the Greek word σχίζειν schízein meaning "to split", citation which is a reference to the ease with which schists can be split along the plane in which the platy minerals lie.