In my classes, I used this lesson to prepare students for the Caldecott Tunnel field trip. Therefore, the rocks described in the teacher background section relate to those found in the cliffs of the Berkeley and Oakland hills. Additional sources for identifying common rocks that might be found in your backyard are provided in the Sources section. What follows is a brief introduction to sandstone, mudstone, conglomerate, basalt and granite.
**A special note on hardness testing**
Hardness testing is an easy test to determine the relative abrasion resistance of different minerals and rocks. Using an index material, like a fingernail with a hardness of 2.5, if your fingernail can scratch the surface of the rock you are testing, the rock has a hardness of less than 2.5. However, if the rock can scratch the surface of your fingernail, then the rock has a hardness of more than 2.5. By using a variety of common objects for comparison (fingernail – 2.5, penny – 3.5, butter knife or glass – 5.5, steel file – 6.5) you can easily approximate the hardness of your mystery rock. Unfortunately for this lesson, hardness tests are most useful for minerals that are composed of a pure substance of uniform density. In contrast, the hardness of a rock that is composed of a mixture of minerals will vary depending on the type of minerals in the rock and also how tightly bound the particles are to one another. For instance, a sandstone may be composed mainly of quartz grains with a hardness of 7 that can scratch steel, yet the rock itself might crumble in your hand. Thus, while hardness testing is a standard skill for geologists that want to know the mineral content of a rock, don’t rely on the measurements to identify the rock itself.
Sandstone is probably the most well known of the sedimentary rocks. It varies in color from red to brown, grey to white, sometimes with a tinge of green or yellow. It is usually composed of rounded sand particles that are medium grained, approximately the texture of beach sand. Sand is produced from the weathering of other rocks (like granite, sandstone and basalt). The sediment in a sandstone may have come from a sandbar along a river, an ocean beach, or desert sand dunes. As more and more sand layers accumulate on top on one another, the weight of the topmost layers compacts the sediment into rock. Often, minerals dissolved in water seeps down into the sandstone, cementing the rock together. The hardness varies greatly, between 2-7, depending on how tightly the sediment was compacted and cemented together.
Mudstone is a sedimentary rock similar to sandstone except that it is made of clay and silt-sized particles. The grains are generally indistinguishable from one another with the naked eye. Technically, mudstone is a mixture of clay and silt-sized particles. Shale is entirely clay-sized particles while siltstone is entirely silt-sized particles. It forms in areas such as lakes, deltas and flood plains where water slows to a near standstill and the smallest particles of trapped sediments are able to be deposited. The hardness is generally low, between 2-3.
Conglomerate is a sedimentary rock similar to sandstone except that it contains chunks of rounded rocks and gravel. These are formed in fast-moving rivers where the water washes away all but the largest rocks. The hardness varies greatly, between 2-7, depending on how tightly the sediment was compacted and cemented together.
Basalt is the most common type of rock on the Earth’s surface. Most of the ocean floor is composed of basalt. It is an igneous rock, formed from magma that cools at the Earth’s surface as it erupts from a volcano. It is generally dark in color, from black to dark grey although the rocks near Caldecott Tunnel are weathered to a dark red-brown. It has a hardness of 5-6 and is so fine grained that you need a microscope to be able to see the crystallization pattern. If it cools quickly, it forms a glassy, obsidian surface. Often, air pockets develop within the basalt as it cools, creating a distinctive holey texture like a sea sponge.
Granite is rapidly becoming the favorite surfacing material in kitchens. It comes in nearly every color of the rainbow, from pink to green to brown to black to white depending on the minerals and inclusions in the rock. The most distinctive feature of granite is crystals of varying color and size, randomly distributed throughout the rock. Granite is very hard, between 6-8 on the Moh’s hardness scale. It forms deep under the Earth’s crust as balloons of magma become trapped under the crust and slowly cools over thousands of years. Thus, granite often forms near subduction zones, where old crust is melted and rises up under the continental shelf. Most of the Sierra Nevadas is made of granite.
A clear understanding of the rock cycle. See the Crayon Rock Cycle lesson.