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Mcnair, B.

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Hutton's Unconformity - Siccar point, showing an angular unconformity
Home » Archives for Mcnair, B.

What Is Angular aka Hutton’s or Siccar Point Unconformity?

An angular unconformity occurs when rock beds above and below the unconformity lie at an angle. The younger rock beds lie flat on tilted, folded,

Categories Stratigraphy
Precambrian-Cambrian nonconformity at Ute Trail, Manitou Springs, Colorado
Home » Archives for Mcnair, B.

What Is Nonconformity in Geology (with Examples)

Nonconformity is unconformity where younger sedimentary rock beds overlie older intrusive igneous or metamorphic rocks. It is a contact plane created when younger sediments cover

Categories Stratigraphy
Diagram illustrating disconformity - The black wavy line indicates the erosion on the contact of the lower and upper rock beds
Home » Archives for Mcnair, B.

What Is Disconformity in Geology and How Does It Form?

A disconformity is a buried erosional or non-deposition surface or boundary between parallel rock layers of different ages. It has visible, uneven erosional surfaces and

Categories Stratigraphy
Paraconformity notice parallel bedding plane with no discernable erosional features
Home » Archives for Mcnair, B.

Here Is the Easiest Explanation of What Paraconformity Is

Paraconformity in geology refers to a type of unconformity where the upper young and old lower rock layers or masses have the same orientation, i.e.,

Categories Stratigraphy
Law or principle of inclusions
Home » Archives for Mcnair, B.

Law or Principle of Inclusions State in Geology Explained

The law or principle of inclusions states that a rock containing another rock fragment is younger than the rock fragment or inclusion it encloses. For

Categories Geology Principles
A detailed diagram to illustrate the law or principle of cross-cutting relationships
Home » Archives for Mcnair, B.

Law or Principle of Cross-Cutting Relationships Explained (with Examples)

The law or principle of cross-cutting relationships states that any geologic feature or rock body that cuts across or deforms another is the younger of

Categories Geology Principles
Bryce Canyon National Park, a perfect example of the law or principle of lateral continuity
Home » Archives for Mcnair, B.

What Does the Law or Principle of Lateral Continuity State?

Steno’s law of lateral continuity states that strata or rock layers extend in all directions until they meet a barrier, tappers (or pinch-out), or grade

Categories Geology Principles
Grand Canyon Arizona USA - With the principle or law of superposition you can get relative age
Home » Archives for Mcnair, B.

Law of Superposition in Geology: Everything You Ought to Know

Steno’s law of superposition states that any rock bed in an undisturbed or undeformed sedimentary rock sequence is older than the one above and younger

Categories Geology Principles
Original horizontality as portrayed by the nearly horizontal sedimentary rock strata or layer
Home » Archives for Mcnair, B.

Law or Principle of Original Horizontality: In-depth Explanation

Nicolaus Steno first proposed the law or principle of original horizontality in the mid-17th century. It states that sediments are always deposited in horizontal (or

Categories Geology Principles
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