2: Relative Dating Flashcards

1
Q

What is Absolute Dating and give 2 main examples

A

Provides precise dates or ranges of dates
* Ex: Radiocarbon dating (C14)
* Ex: Dendrochronology (tree ring dating)

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2
Q

What is Relative Dating and give 2 main examples

A

Determines the relative ages of sites and objects by ordering them in a sequence
* Ex: Typology and Seriation
* Ex: Stratigraphy

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3
Q

What is typology and seriation

A

groups artifacts together based on looks asnd styles to a specific time period

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4
Q

Which dating method was used primarily

A

Relative dating was used primarily before absolute dating

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5
Q

What is stratigraphy and stratum

A
  • The description or study of sediment strata
  • Stratum (pl. strat) is a layer or series of layers of sediment in the ground
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6
Q

Soil vs Sediment

A

Soil: organic and inorganic material that develops on a stable surface of the Earth and sustains life. Forms in situ

Sediment: organic and inorganic material deposited after the weathering and transport of rock. Develops as a result of movement

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7
Q

Ways sediment is transported, which ones are the main ones?

A
  • Wind: dust and sandstorm
  • Water: oceans, river, glaciers, lakes
  • Alluvial: moving water like rivers and floods
  • Lacustrine: standing water like lakes
  • Gravity
  • Humans: can deposit cultural layers like man made artifacts
  • 3 main ones are wind, water, and gravity
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8
Q

What are the Steno’s Laws of Stratigraphy

A
  • Nicolas Steno: 17th century Danish scientist who outlined 4 laws to describe how stratigraphic layers are deposited
    1. Law of Superposition
    2. Law of Original Horizontality
    3. Law of Cross-Cutting Relationships
    4. Law of Lateral Continuity
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9
Q

Law of Superposition

A

Younger strata will be deposited on top of older strata, under normal depositional conditions

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10
Q

Law of Original Horizontality

A

Strata are deposited in flat layers, if a stratum does not lie flat, some geologic even after deposition caused them to be that way

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11
Q

Law of Cross-Cutting Relationships

A

An intrusion into strata is the younger (and youngest) than the layers it intersects

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12
Q

Law of Lateral Continuity

A

Sediment layers spread horizontally until they reach an obstacle that keeps them from spreading further. If there is a depression into the flat layers of strata then it must have been hollowed out after the formation of strata

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13
Q

Law of Association

A
  • Not one of Steno’s
  • Objects found in the same archaeological layer must all date from the same time period, unless there has been some form of clear disturbance
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14
Q

How doe stratigraphy help in archaeology?

A
  • Document site formation processes
  • Reconstruct past natural landscapes
  • Determine relative or absolute dating context
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15
Q

What is vertical mapping and what does it document

A
  • Archaeological units mapped in 3D
  • Document unit walls with horizontal and vertical axes
  • Records width and depth of strata
  • Describes contents of layers
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16
Q

How is vertical mapping done

A
  • measurements are taken of each stratum change at set intervals and plotteed on grid paper
  • measurements must be both level (horizontal): using a line level and plumb (vertical): using a plumb bob
  • Connect the plotted points to show stratum transitions (boundaries)
  • All mapps need: title, labelled axes (cm/cmbs), north arrow, legeld, scale, name, and date
17
Q

What is the Harris Matrix

A
  • Used to represent stratigraphic relationships
  • Layer/feature represented by letter or number in box (from oldest to youngest going from bottom to up)
  • Direct relationships of layers (touching) indicated by line