What is metamorphic foliation how does it differ from sedimentary bedding?

Foliation is developed by stress and fire while layering is developed by the embedding of fine and coarse deposits. Foliation is caused due to an alteration of minerals from pressure and heat while layering is developed by seasonal changes. Foliation has layers while layering contains marks on them.

How are foliation and deformation related?

Your rock will develop a foliation. During deformation, old grains rotate and parallelize with each other. Eventually, new minerals will grow already oriented parallel to the foliation.

What is the main cause of foliation?

Foliation is caused by the re-alignment of minerals when they are subjected to high pressure and temperature. Individual minerals align themselves perpendicular to the stress field such that their long axes are in the direction of these planes (which may look like the cleavage planes of minerals).

What is bedding in rocks?

Bedding (also called stratification) is one of the most prominent features of sedimentary rocks, which are usually made up of ‘piles’ of layers (called ‘strata’) of sediments deposited one on top of another. These principles are useful when investigating rock strata that are involved in orogens.

What is the relationship between metamorphic foliation and sedimentary bedding?

Foliation may be formed by realignment of micas and clays via physical rotation of the minerals within the rock. Often this foliation is associated with diagenetic metamorphism and low-grade burial metamorphism. Foliation may parallel original sedimentary bedding, but more often is oriented at some angle to it.

What is the difference between bedding and foliation?

As nouns the difference between bedding and foliation is that bedding is the textiles associated with a bed, eg, sheets, pillowcases, bedspreads, blankets, etc while foliation is the process of forming into a leaf or leaves.

Is foliation associated with sedimentary rocks?

A foliation is any sort of fabric-forming planar or curved planar geologic structure in a metamorphic rock, but could additionally include sedimentary bedding or magmatic layering (Wilkerson, 2019).

What do bedding surfaces represent?

A bedding plane is defined as a surface representing a contact between a deposit and the depositing medium during a time of change. They are primary features of sedimentary rocks formed usually by the depositing media water, and atmosphere.

What is the difference between foliation and bedding?

What is the difference between bedding and foliation in geology?

The philosophy is that bedding is due to deposition and all other foliations are due to mineral alignment in deformed rocks. In greenschist facies and higher-grade metamorphic rocks, foliations (e.g. schistosity and gneissic layering) are typically the only parallel fabric present (sometimes several generations).

What is sedimentary bedding?

Sediments and sedimentary rocks are characterized by bedding, which occurs when layers of sediment, with different particle sizes are deposited on top of each other. These beds range from millimeters to centimeters thick and can even go to meters or multiple meters thick.

Are bedding planes horizontal?

The bedding planes are the horizontal layers formed as the rocks were compressed under deposits formed above.