enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. Relative dating - Wikipedia

    en.wikipedia.org/wiki/Relative_dating

    Relative dating by biostratigraphy is the preferred method in paleontology and is, in some respects, more accurate. [1] The Law of Superposition, which states that older layers will be deeper in a site than more recent layers, was the summary outcome of 'relative dating' as observed in geology from the 17th century to the early 20th century.

  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. 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. The principle is important to the analysis of folded and tilted strata. It was first proposed by the Danish geological pioneer Nicholas Steno (1638–1686).

  5. 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.

  6. Principle of faunal succession - Wikipedia

    en.wikipedia.org/wiki/Principle_of_faunal_succession

    This principle, which received its name from the English geologist William Smith, is of great importance in determining the relative age of rocks and strata. [1] The fossil content of rocks together with the law of superposition helps to determine the time sequence in which sedimentary rocks were laid down.

  7. 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 ...

  8. Chronological dating - Wikipedia

    en.wikipedia.org/wiki/Chronological_dating

    Palynology, the study of modern-dated pollens for the relative dating of archaeological strata, also used in forensic palynology. Paleomagnetism; Paleopalynology, also spelt "Palaeopalynology", the study of fossilized pollens for the relative dating of geological strata. Principle of original horizontality; Principle of lateral continuity

  9. Seriation (archaeology) - Wikipedia

    en.wikipedia.org/wiki/Seriation_(archaeology)

    In archaeology, seriation is a relative dating method in which assemblages or artifacts from numerous sites in the same culture are placed in chronological order. Where absolute dating methods, such as radio carbon, cannot be applied, archaeologists have to use relative dating methods to date archaeological finds and features. Seriation is a ...