Discordant
Concordant coasts have rock layers that run parallel to the shoreline, creating a straight coastline. Discordant coasts have rock layers that run perpendicular to the shoreline, leading to irregular coastlines with bays and headlands.
A discordant intrusion is known as a dyke. A larger intrusion may also be a pluton or batholith, which both also cut across rock strata. A sill is an intrusion which is concordant, and goes between the strata. This does not necessarily mean that it is horizontal.
Intrusive igneous bodies that cut across existing sedimentary beds are said to be discordant. An example of a discordant intrusion is a batholith.
A tabular concordant intrusive structure refers to a type of igneous intrusion where the orientation of the intrusive body is parallel to the existing layering or structures in the surrounding rock. This results in the intrusion appearing as a tabular or sheet-like feature that runs parallel to the rock layers. The intrusive body is typically discordant to the sedimentary or metamorphic layers but its orientation is concordant.
A stock is an irregularly shaped pluton that is smaller than a batholith. It is typically less than 40 square miles in area and can be discordant with surrounding rock formations. Stocks are often found in mountainous regions where they have intruded into the crust.
Concordant coasts have rock layers that run parallel to the shoreline, creating a straight coastline. Discordant coasts have rock layers that run perpendicular to the shoreline, leading to irregular coastlines with bays and headlands.
A discordant intrusion is known as a dyke. A larger intrusion may also be a pluton or batholith, which both also cut across rock strata. A sill is an intrusion which is concordant, and goes between the strata. This does not necessarily mean that it is horizontal.
Intrusive igneous bodies that cut across existing sedimentary beds are said to be discordant. An example of a discordant intrusion is a batholith.
Yes, batholiths are discordant intrusions of igneous rock that cut across existing rock layers. They are formed by the crystallization of magma deep below the Earth's surface and later exposed through erosion.
A tabular concordant intrusive structure refers to a type of igneous intrusion where the orientation of the intrusive body is parallel to the existing layering or structures in the surrounding rock. This results in the intrusion appearing as a tabular or sheet-like feature that runs parallel to the rock layers. The intrusive body is typically discordant to the sedimentary or metamorphic layers but its orientation is concordant.
A stock is an irregularly shaped pluton that is smaller than a batholith. It is typically less than 40 square miles in area and can be discordant with surrounding rock formations. Stocks are often found in mountainous regions where they have intruded into the crust.
concordant data is a data based on concordant
Concordant means in agreement. Their answers were roughly concordant.
Concordant Version was created in 1926.
Laccoliths are concordant intrusions, meaning they have a flat bottom and conform to the layering of the surrounding rock. They are characterized by their mushroom-shaped form with a flat base and domed top, pushing up the overlying rock layers without breaking through them.
The discordant family quarreled often.
The word discordant is an adjective. Example sentence:The discordant notes he played were grating on my nerves.