CONTINENTAL RIFTS
CONTINENTAL RIFTS
These are elongate depression that have the thickness of the lithosphere deformed by the influence of exponential forces (Neumann & Ramberg 1978, Burchfiel, 1980).
Rift therefore applies to major lithospheric features and does not encompass smaller scale structures associated with normal faulting.
Continental Rift caused by a rising mantle plume.
Author: DBoyd13
Presently active rift include; EAR, the Baikal Rift (South Central Siberia), The Rhine Graben (North-West Europe) The Rio Grande Rift and Basin & Range Province of Western United State of America.
Continental Rift System
They are fault-bounded valleys ranging in width from about 30-75km and in length from a few tens to thousand of Kms. They are characterized by a tensional tectonic setting which extends over 6500Km from the Western part of Asia Minor to South-East Africa.
Ranges from a simple graben or half graben to complex graben system, the complex system is mostly common. The Basin and Range province is West-North America is a multiple rift system composed of a complex series of alternating graben valley and ridges (Horst).
Rift systems may occur in rocks of any age, young system (≤30million years) are characterized by unstable tectonic conditions, some large volcanic plateau in the North-West of the United State of America and the Deccan Traps in India, also appear to be related to extensive tensional faulting.
Characteristics Of Rifts
They may be form in different tectonic environments, however exhibit common characteristics like:
• They are relatively common.
• They often contain extensive volcanic rocks.
• They are commonly, spatially associated with domal uplifts.
• The lithosphere underlying rifts is generally abnormally thin and invaded by low velocity, low density, and high temperature material, E.g Ocean Ridges.
• The location of rifts is often controlled by existing zones of crustal weakness.
• The amount of horizontal extension required to form present day rift is relatively small (<10km).
References:
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