Organic sedimentary rocks form from the accumulation and lithification of organic debris, such as leaves, roots, and other plant or animal material. Rocks that were once swampy sediments or peat beds contain carbon and are black, soft, and fossiliferous. Rich enough in carbon to burn, coal is an organic sedimentary rock that is a widespread and important fuel source. Coquina, bioclastic limestone, and skeletal limestone are also technically organic sedimentary rocks but are usually grouped with the other limestones as being chemically precipitated.
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- History of Physical Geology
- The Earth's Origin
- The Earth's Structure
- The Earth's Exterior
- Geologic Time
- The Earth Today
- Magmatic Differentiation
- Volcanoes and Lavas
- Extrusive Rock Types
- Rock Textures
- Intrusive Rock Types
- Intrusive Structures
- How Different Magmas Form
- Igneous Rocks and Plate Tectonics
- How Sedimentary Rocks Form
- Clastic Sedimentary Rocks
- Chemical Sedimentary Rocks
- Organic Sedimentary Rocks
- Sedimentary Features
- Sedimentary Environments
- Metamorphism Defined
- Factors Controlling Metamorphism
- Types of Metamorphism
- Metamorphic Rock Types
- Hydrothermal Rocks
- Metamorphism and Plate Tectonics
- Geologic Structures Defined
- Tectonic Forces
- Interpreting Structures
- Mapping in the Field
- Folding
- Fracturing
- Unconformities
- Types of Water Flow
- Stream Dynamics
- Stream Erosion
- Sediment Load
- Stream Deposition
- Stream Valleys
- Regional Erosion
- Introduction to Glaciation
- Types of Glaciers
- How Glaciers Develop
- Glacier Movement
- Glacial Erosion
- Glacial Landforms
- Glacial Deposits
- Glaciers in the Past
- North American Glaciation
- Groundwater and Infiltration
- Porosity
- Permeability
- The Water Table
- Streams and Springs
- Effects of Groundwater Flow
- Groundwater Pollution
- Geothermal Energy
- How Earthquakes Form
- Seismic Waves
- Monitoring Earthquakes
- Effects of Earthquakes
- Earthquakes and Plate Tectonics
- Control and Prediction
- Geophysics Defined
- Seismic Waves: Methods of Detection
- The Structure of the Earth
- The Crust
- The Mantle
- Isostatic Equilibrium
- The Core
- Magnetic Fields
- Gravity
- Geothermal Gradients
- Investigative Technologies
- Continental Margins
- Ocean Floor Sediments
- Active Continental Margins
- Passive Continental Margins
- Reefs
- Midoceanic Ridges
- Oceanic Crust
- Early Evidence for Plate Tectonics
- Paleomagnetic Evidence
- Sea Floor Evidence
- How Plates Move
- Types of Plate Boundaries
- Why Plates Move
- Mantle Plumes
- Pangaea
- Introduction to Mountains
- Features of Mountain Belts
- Types of Mountains
- How Mountains Form
- How Continents Form
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Organic Sedimentary Rocks
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Introduction to Physical Geology
Sedimentary Rocks
