Lecture Notes on Concretions
Definition and Formation
- Concretion: A hard, compact mass formed by mineral precipitation within the spaces between particles in sedimentary rock or soil.
- Typically found in sedimentary strata, forming early in the burial history of sediments.
- Concretionary cement often makes them harder and more resistant to weathering than the host rock.
- Formed by mineral precipitation around a nucleus, often organic (e.g., leaf, tooth, shell).
Distinction from Nodules
- Concretions: Formed from mineral precipitation around a nucleus.
- Nodules: Replacement bodies, different formation process.
Historical and Geological Curiosity
- Long regarded as geological curiosities.
- Misinterpreted as dinosaur eggs, pseudofossils, extraterrestrial debris, or artifacts.
Growth and Environmental Conditions
- Can grow by concentric or pervasive growth:
- Concentric Growth: Successive layers of mineral around a core.
- Pervasive Growth: Cementation occurs throughout the volume simultaneously.
Shapes and Sizes
- Varied shapes: Spheres, disks, tubes, grape-like or soap bubble-like aggregates.
- Range in size from microscopic to several meters in diameter.
Composition
- Commonly composed of a mineral present as a minor component of the host rock.
- Examples:
- Sandstone/shale concretions: Often carbonate minerals like calcite.
- Limestone concretions: Silica forms like chert or flint.
- Black shale concretions: Pyrite.
Notable Concretion Types
Septarian Concretions
- Rich in carbonates, with angular cavities or cracks (septaria).
- Found in various mudstones, often marine shales.
- Formation debated; may involve dehydration, syneresis, or excess pore pressure.
Cannonball Concretions
- Large spherical concretions, resemble cannonballs.
- Found in North Dakota, Utah, Wyoming; formed by early cementation by calcite.
Elongate Concretions
- Form parallel to sedimentary strata.
- Provide information on past fluid flow and local permeability trends.
Additional Types and Features
- Hiatus Concretions: Stratigraphic history of exhumation, exposure, and reburial; encrusted and bored by marine organisms.
- Claystones/Fairy Stones: Disc concretions found in proglacial lake deposits; various forms and sizes.
Concretion Examples
- Moeraki Boulders: New Zealand, large septarian concretions.
- Martian Spherules: Found by Opportunity rover on Mars; hematite concretions.
Environmental and Geological Significance
- Concretions record information about early diagenesis and environmental conditions during their formation.
- Studied for their insights into past geological and environmental processes.
These notes summarize key points about the formation, types, and significance of concretions in geology, providing a comprehensive understanding of these intriguing geological features.