Slaty cleavage refers to the extremely closely spaced, parallel planes of weakness that give a rock like slate its ability to split into very thin, platy layers.
Slate is a common roofing material. Taking advantage of the natural planes of weakness within slate (slaty cleavage), it can be split into very thin slabs of uniform thickness. Photo by National Park Service.
Shale is a very fine-grained sedimentary rock that tends to break into flat, slabby pieces. Photo by NASA.
Shale is composed of very fine (sub-microscopic) mineral dust, of which clay is a significant component. Clay occurs as flat flakes which, except for their extremely small size, are similar to flakes of muscovite (shown above).
Slate contains significant quantities of muscovite, chlorite (a green mineral similar to mica) and sometimes graphite, all of which are flaky minerals (shown above).
Both shale and slate split into flat slabs. However, slate slabs tend to be thinner and flatter than shale slabs. Both shale and slate have significant quantities of flaky minerals which are oriented parallel to each other. Splitting takes place parallel to the oriented, flaky grains. Because the parallelism of the grains in the slate is more perfect than in the shale, the splitting results in flatter, thinner slabs.
|Geologists claim that slaty cleavage is a secondary structure imposed on the sedimentary rock 'shale'. That is, slate is the metamorphic equivalent of shale.|
How can the geologists' claims be justified?
Shale is considered sedimentary on the basis of the many primary structures it displays. Here are three examples of such structures:
The gentle slopes are composed of horizontal layers of shale. If you look carefully at the hills in the forground, you will see the horizontal, alternating blue and bluish-white layers. Photo by USGS. Horizontal layering is a characteristic of sedimentary rocks.
The presence of mudcracks indicates the rock formed at or near the earth's surface.
The presence of fossils indicates the rock formed at or near the earth's surface. Photo by Utah Geological Survey.
Geologists have come to conclusions about the origin of slate and slaty cleavage based upon observations of their relationship to other rock bodies in the field.