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  2. Inclusion (mineral) - Wikipedia

    en.wikipedia.org/wiki/Inclusion_(mineral)

    In mineralogy, an inclusion is any material trapped inside a mineral during its formation. In gemology , it is an object enclosed within a gemstone or reaching its surface from the interior. [ 1 ] According to James Hutton 's law of inclusions, fragments included in a host rock are older than the host rock itself.

  3. Law of included fragments - Wikipedia

    en.wikipedia.org/wiki/Law_of_included_fragments

    The law of included fragments is a method of relative dating in geology.Essentially, this law states that clasts in a rock are older than the rock itself. [1] One example of this is a xenolith, which is a fragment of country rock that fell into passing magma as a result of stoping.

  4. Relative dating - Wikipedia

    en.wikipedia.org/wiki/Relative_dating

    The law of included fragments is a method of relative dating in geology. Essentially, this law states that clasts in a rock are older than the rock itself. [6] One example of this is a xenolith, which is a fragment of country rock that fell into passing magma as a result of stoping.

  5. Glossary of geology - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_geology

    Principle of inclusions and components; Walther's law; Topics. ... This glossary of geology is a list of definitions of terms and ... In its geological definition, it ...

  6. Cross-cutting relationships - Wikipedia

    en.wikipedia.org/wiki/Cross-cutting_relationships

    Cross-cutting relationships can be used to determine the relative ages of rock strata and other structures. Explanations: A – folded rock strata cut by a thrust fault; B – large intrusion (cutting through A); C – erosional angular unconformity (cutting off A & B) on which rock strata were deposited; D – volcanic dike (cutting through A, B & C); E – even younger rock strata (overlying ...

  7. Law of superposition - Wikipedia

    en.wikipedia.org/wiki/Law_of_superposition

    The law of superposition is an axiom that forms one of the bases of the sciences of geology, archaeology, and other fields pertaining to geological stratigraphy.In its plainest form, it states that in undeformed stratigraphic sequences, the oldest strata will lie at the bottom of the sequence, while newer material stacks upon the surface to form new deposits over time.

  8. Xenolith - Wikipedia

    en.wikipedia.org/wiki/Xenolith

    In geology, the term xenolith is almost exclusively used to describe inclusions in igneous rock entrained during magma ascent, emplacement and eruption. [1] Xenoliths may be engulfed along the margins of a magma chamber , torn loose from the walls of an erupting lava conduit or explosive diatreme or picked up along the base of a flowing body of ...

  9. Principle of original horizontality - Wikipedia

    en.wikipedia.org/wiki/Principle_of_original...

    The principle of original horizontality states that layers of sediment are originally deposited horizontally under the action of gravity. [1] It is a relative dating technique.