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[1] shale is characterized by its tendency to split into thin layers (laminae) less than one centimeter in thickness The meaning of shale is a fissile rock that is formed by the consolidation of clay, mud, or silt, has a finely stratified or laminated structure, and is composed of minerals essentially unaltered since deposition. Shale is the most abundant of the sedimentary rocks, accounting for roughly 70 percent of this rock type in the crust of the earth.

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Shale is the most abundant sedimentary rock Shale may be any color, but is generally greenish gray to grayish black. It is found in sedimentary basins worldwide.

Shale is the most common sedimentary rock type, constituting approximately 70% of exposed sedimentary rock on earth

Shale is characterized by its laminated structure, with thin, parallel layers resulting from the alignment of clay minerals during deposition. Below is a fully detailed and globally relevant overview of shale, including its formation, composition, properties, varieties, fossil content, economic significance, and geological role. Shale is one of the most common types of sedimentary rock primarily composed of clay and silt particles It forms through the compaction of these fine particles over millions of years in calm environments such as deep ocean floors, lakes, and riverbeds.

It is formed of many thim mineral layers and is typically characterized. Shale is the most abundant of all sedimentary rocks It is composed primarily of soft clay minerals, but may include variable amounts of organic matter, calcareous material, and quartz grains