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An unconformity. There are three main types: angular unconformity, disconformity, and nonconformity.
Anything that is not a nonconformity, angular uncomformity, and discomformity
a nonconformity
An unconformity is the contact between two layers representing a gap in the geologic record, usually from the erosion of the layers which would normally be expected to appear.
Disconformity
An unconformity. There are three main types: angular unconformity, disconformity, and nonconformity.
Anything that is not a nonconformity, angular uncomformity, and discomformity
Angular unconformity is when rocks are deformed and then eroded and then new sediment is deposited on top. Disconformity is when igneous or metamorphic rocks are eroded and then sediment is deposited on top. Nonconformity is when either there is no deposition for some time and then deposition resumes or horizontal layers are eroded (but not deformed in any way) and then deposition resumes. These create gaps in the rock record.
1. Disconformity. 2. Angular Unconformity. 3. Non-Conformity.
a nonconformity
Angular unconformities separate rock layers along nonparallel surfaces
An unconformity is defined as a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. The different types of unconformities include disconformity, nonconformity, angular unconformity, paraconformity, buttress unconformity, blended unconformity, and biconformity.
As conformity stands for sticking to or obeying to rules of a society, nonconformity means the exact opposite. Hence, the synonyms of nonconformity are the antonyms of conformity ie disobedience, unorthodox, difference and refusal etc As conformity stands for sticking to or obeying to rules of a society, nonconformity means the exact opposite. Hence, the synonyms of nonconformity are the antonyms of conformity ie disobedience, unorthodox, difference and refusal etc
An unconformity is the contact between two layers representing a gap in the geologic record, usually from the erosion of the layers which would normally be expected to appear.
this is a type of unconformity called a nonconformity characterized by a sedimentary strata overlying an igneous or metamoprhic crystalline bedrock
Nonconformity is a noun.
a break in a sedimentary sequence that does not involves a difference of inclination between the strata on each side of the break