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SAGE 2004 Archaeological Magnetics Survey

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Title: SAGE 2004 Archaeological Magnetics Survey


1
SAGE 2004 Archaeological Magnetics Survey
San Marcos Pueblo, New Mexico J. Mark
Hale University of Utah
2
San Marcos Pueblo, NM
3
Outline
  • Introduction to Magnetics
  • Archaeological Contributions
  • Instrumentation
  • Software and Data Analysis
  • Archaeological implications of the magnetic data
    at San Marcos Pueblo
  • Conclusions
  • Caveats and Improvements

4
Possible Sources of Remnant Magnetism
  • TRM Thermo-Remnant Magnetism, Curie point
    volcanic rocks and archaeological hearths.
  • DRM Depositional Remnant Magnetism, sedimentary
    rocks and sedimentary cores.

Dipole Profile is Dependent on the Orientation of
the Body
5
G-858 Magnetometer
  • Operating Principle Self-oscillating split-beam
    Cesium Vapor with automatic hemisphere
    switching.
  • Heading Error 1 nT
  • Sensor Height 0.5 m

Data Analysis Software
6
Pros and Cons of Magnetic Data for Archaeological
Use
Benefits - Magnetics can cover a wide area in a
short amount of time. Reduction of survey
area. - Easily obtained approximate depths.
Detriments - Approximate depths carry large
discrepencies and are subjective in nature. -
Anomaly type remains a mystery until
excavation
7
Mission Complex Magnetic Anomalies
8
Mission Site Anomaly Profiles
9
Mission Site Anomaly Depths(Acquired using
maximum slope approximation)
Maximum slope approximation
10
Mission Complex1st Horizontal Derivative(as an
estimate of depth)
11
Midden 2 Magnetic Anomalies
12
Volkswagen Anomaly
  • Strong dipole signature
  • Dipole low trends towards magnetic north
  • Reasonable depth estimate 1.5 m
  • Great profile!

13
Midden 2 Site Anomaly Profiles
14
Midden 2 Site Anomaly Depths
15
Conclusions
  • The San Marcos Pueblo has several magnetic
    anomalies with reasonable depths.
  • The Galisteo fins contribute to the DRM of the
    site.
  • The Mission site still has unearthed anomalies at
    reasonable depths
  • The Volkswagen anomaly is the strongest in the
    Midden 2 site.

16
Caveats and Improvements
Caveats
  • Depth estimates are just estimates
  • Anomalies are highly ambiguous
  • There is no such thing as untainted data

Improvements for Further Research
  • Plotting magnetometer data using real GPS data
  • Use forward modeling to determine size and shape
    of magnetic body
  • More time to conduct a proper evaluation
  • More computer power!
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