Chert is a hard, fine-grained sedimentary rock composed primarily of microcrystalline quartz, or silica. It is typically composed of the skeletons of diatoms, radiolarians, and other siliceous organisms. Chert is often found in marine sedimentary rocks but can also occur in lacustrine and terrestrial settings. Chert is typically found in nodules, concretions, or layered deposits, and it exhibits a wide range of colors, including white, gray, black, brown, and red.
Chert forms in a variety of ways, including:
Biogenic silicification: This is the most common way that chert forms. Chert can form from the accumulation of silica skeletons of tiny organisms such as diatoms, radiolarians, and silicoflagellates. These organisms live in the ocean and their silica skeletons sink to the bottom of the seafloor. Over time, the skeletons are compacted and cemented together to form chert nodules or beds.
Chemical precipitation: Chert can also form inorganically as a chemical precipitate. This can happen when seawater becomes supersaturated with silica, or when silica-rich solutions are forced upwards into the crust. Inorganically formed chert is typically found in association with hydrothermal vents or volcanic deposits.
Diagenetic replacement: Chert can also form when other minerals, such as calcite, dolomite, and clay minerals, are replaced by silica during the process of diagenesis. Diagenesis is the chemical and physical changes that rocks undergo after they are deposited. This process, known as silicification, occurs when silica-rich fluids or solutions replace the original minerals.
|Chert from the Tertiary of Utah, USA.
Photo: James St. John
Types and Varieties of Chert
Chert can be classified into several types based on its texture, composition, and origin. Some of the most common types of chert include:
Types of Chert Based on Texture
Bedded chert: This type of chert is formed when layers of chert are interbedded with layers of other rocks, such as shale or limestone. It is often found in marine sedimentary rocks.
Nodular chert: This type of chert is found in nodules, or rounded lumps, within other rocks. It is often found in chalk and other sedimentary rocks.
|Radiolarian cherts in the Mesozoic of California, USA.
Photo: James St. John
Unlithified Siliceous Sediments: Siliceous sediments that have not undergone any consolidation, remaining as loose deposits, often found in marine and freshwater environments.
Compositional Subtypes of Chert
Radiolarite: Radiolarite is a type of chert that is composed primarily of the siliceous remains of radiolarians, which are microscopic marine organisms. It is often found in deep-sea sediments.
Diatomite: Diatomite is a type of chert that is composed primarily of the siliceous remains of diatoms, which are microscopic algae that flourish in marine and freshwater environments. It is known for its light, porous texture.
Spiculite: Spiculite is a type of chert that is composed primarily of the siliceous remains of sponge spicules, which are small, needle-like structures that form the skeleton of sponges.
Jasper: Jasper is a type of chert that is hard, opaque, and often colorful. It is often reddish, yellow, or brown in color. It is formed through the precipitation of silica around iron oxide impurities.
Varieties of Chert Based on Specific Characteristics
Porcellanite: Porcellanite is a type of chert that is very hard and has a porcelain-like appearance. It is often used to make ornamental objects.
Silcrete: Silcrete is a type of chert that is formed in soils. It is often used for building materials.
Flint is a compact microcrystalline quartz. It was originally the name for chert found in chalk or marly limestone formations formed by a replacement of calcium carbonate with silica. Today, some geologists refer to any dark gray to black chert as flint. The dark color is from inclusions of organic matter.
Mozarkite is a form of chert that is found in the Ozark Mountains of Missouri. Mozarkite is named after the Missouri Ozarks, where it is found. The rock was first described in the early 1800s by geologist Henry Rowe Schoolcraft. Mozarkite is typically found in nodules or veins within other rocks, such as limestone or dolomite. Mozarkite is a popular decorative stone. It is often used in countertops, fireplaces, and other interior and exterior applications.
|Chert Nodules, Emerald Parkway Roadcut, Dublin, Ohio
Photo: James St. John
- Color: Chert can be found in a variety of colors, including white, gray, brown, red, and yellow. The color is typically determined by the impurities present in the rock, such as iron oxide or manganese oxide.
- Streak: White
- Translucency: Translucent to opaque
- Fracture: Chert typically has a conchoidal fracture, which means that it breaks into smooth, curved surfaces like a shell.
- Hardness: Chert is one of the hardest sedimentary rocks, with a Mohs hardness of 7. It is slightly softer than quartz but harder than most other sedimentary rocks.
- Texture: Chert has a fine-grained texture, with a smooth, glassy surface. It can be translucent or opaque, and it often has a distinctive conchoidal fracture, meaning it breaks with a smooth, curved surface.
- Density: 2.65 g/cm³
Chert has been used by humans for centuries for a variety of purposes, including:
|Chert tools and Arrowhead
Toolmaking: Chert was one of the first materials used to make tools by early humans. Its hardness and sharpness made it ideal for cutting, scraping, and drilling.
Firemaking: Chert can be struck against steel to produce sparks, which can be used to ignite tinder and start a fire.
Sharpening: Chert was also used to sharpen other tools, such as arrowheads and knives.
Ornament: Chert was also used to make jewelry and other ornamental objects.
Chert is a fascinating and versatile sedimentary rock with a rich geological history and diverse applications in human culture.