Excavation Techniques

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    Excavation Techniques - Presentation Transcript

    1. Excavation Techniques and Analysis Applications to Paleoanthropology
    2. About Excavation and Analysis
      • Authors’ definition:
      • Study of past cultures analyzing material remains of human behavior
      • Study entails
      • Time: Date of the site and its contents
      • Space: Location of the site and its contents
      • Material remains: siting, retrieval, analysis
    3. Fundamentals of Excavation and Analysis
      • Site discovery and selection
      • Excavation of artifacts, ecofacts, and features
      • Analysis for dates, attributes, and environment
    4. An Example: Flow Chart for Combe Capelle (A Neanderthal Site)
      • Research Design
      • Discovery
      • Preparation
      • Data Collection (The Dig)
      • Analysis
      • Interpretation/Synthesis
    5. Some Definitions
      • Ecofacts: remains of plants, animals, sediments, or other materials not modified by human activity
      • Features: immovable structures, pits, posts, burial sites
      • Artifacts: all portable objects altered by human activity
      • Sites: Landscape where human activity took place, as indicated by the above
    6. How are Sites Formed?
      • Taphonomy: Study of how lifeforms or artifacts wound up at a particular location
      • Primary refuse: items left at site of use
      • Secondary refuse: Items moved elsewhere
    7. How are Items Preserved? Material
      • Some materials resist deterioration:
      • Bone: Skulls and teeth
      • Stone or Metal (tools, ornaments)
      • Seeds, with protective covers
    8. How Are Objects Preserved? Environment
      • Arid climates (Peruvian coast)
      • Water: Planks at Ozette, WA or France
      • Peat moss: the “Bog People” in Scandinavia
      • Ice: Ötzi the “Iceman” in Austrian/Italian Alps
      • Volcanic Ash, Cerén, El Salvador
    9. Site Discovery
      • Lucky finds
      • Consulting available sources: studies, records, even older informants
      • Maps and aerial photographs
      • Geographical Information Systems/Remote Sensing
    10. Site Selection
      • Learning everything possible about each site
      • Selecting as large and representative a site as possible
      • Preliminary work: surface finds, features, perhaps test pits or trenches
      • Problem-Oriented Research and Deliberate Surveys
    11. Survey: Mapping, Part 1: General
      • First principle: Digging is destructive--record everything!
      • Mapping
      • Latitude, longitude, and elevation
      • Benchmarks or features
      • Measurements
      • Horizontal
      • Vertical
    12. Surveying: Mapping Part 2: Horizontal Measurement
      • Select and draw west-east (X-axis) and north-south (Y-axis) baselines from primary site datum
      • Mark off intervals at meters and centimeters from baselines
      • Label the intervals along axes of the grid by letters, numbers, or both
      • Adapt procedure according to topographical or archaeological features
    13. Laying Out an Alternative Grid
    14. Survey: Mapping Part 3: Vertical Measurements
      • Surveying using transit or alidade and measuring rod
      • Vertical base: benchmark or permanent feature of known elevation
      • Convert measures to meters above sea level.
    15. Example: Work In Progress
    16. Virtual Dig: Mapping in Combe-Capelle
      • Retraced excavation by Henri-Marc Ami
      • Excavated sample squares of the site
      • Squares distinguished by
      • Letter (X axis)
      • Numbers (Y axis)
      • Vertical measurements by 4 strata.
    17. Survey: Test pits and trenches
      • Test pits provide sample of site stratigraphy
      • Stratigraphy: profile of two or more layers of
      • Natural sediment
      • Human deposits
      • Test pits provide sample of overall site
      • Several pits suggest which part should be excavated most extensively
    18. Survey: Test Pits
      • Advantages: Provide preliminary information on site
      • Disadvantages
      • Need more pits to round out information
      • May not yield full stratigraphy
    19. Survey: Trenches
      • Uses
      • Provide full stratigraphy
      • Provide sample of artifacts to establish chronology
      • Locate features
      • Find site boundaries
      • Types
      • Slit trenches
      • Step trenches
      • Backhoe trenches
      • Wall trenches
    20. Survey: Trenches—Advantages and Drawbacks
      • Advantages:
      • Good samples of artifacts
      • Find buried features
      • Good time depth
      • Drawbacks
      • Destructive, especially with backhoe
      • Can destroy potential activity areas before knowing what’s there
      • Danger of collapse
    21. Deciding Where to Excavate
      • Sampling depends on research questions
      • Judgmental Sampling: based on prior knowledge of site; used at Combe-Capelle
      • Probabilistic Sampling
      • Random sampling
      • Stratified sampling: based on prior knowledge
      • Known trash deposits or architectural features
      • Ensure everything significant is included
    22. Tools for Excavation
      • Dental picks or paint brushes
      • Ice picks
      • Tweezers (fragile objects)
      • Trowels (pointed and square)
      • Shovels (pointed and square-nosed)
      • Heavy equipment (backhoes)
      • Buckets and Screens
    23. Tools Used for Rough Excavation
      • Shovel, Round Nose Club Hammer
      • Pick Chisel, Flat
      • Pry Bar Scraper, Long Handle
      • Sledge Hammer
    24. Tools Used for Fine Excavation
      • Top row: plastic paint trowel, rubber air puffer, large brushes, small brush, wooden/plastic sculpting tools/small paint trowel), plastic spoon Bottom row: note pad, folding ruler (in cm.), Marshalltown trowel (45-5), 8"mill bastard file, plastic spoon, plastic trowel, tape measure (3-4 m. is sufficient)
    25. Vertical Excavation: Some “Laws”
      • Law of Association:
      • Artifacts found at the same stratum (layer) are in association with one another
      • Artifacts found at different strata are not in association with one another
      • Law of Superposition: Geological layers are stratified one upon another
      • Lower strata are older than higher ones
      • Uniformitarianism: Geological processes similar throughout time
    26. The “Laws” Illustrated
      • a) Law of Association: Skeleton, dagger, and burial pit are at the same level
      • b) Law of Superposition: pot is at the higher stratum and
      • stone axe is at the lower stratum
    27. Vertical Excavation: Stratigraphy
      • Layer deposited in chronological order: lowest layer is oldest and so on.
      • Disturbances can change stratigraphy
      • Erosion from hillside: oldest is top layer
      • Structure foundation disturbs layers
      • Burrowing animals may move objects
      • Then there are golddiggers and pothunters
    28. Vertical Excavation: Procedure:
      • Each artifact is recorded and removed
      • Photographed, sketched, or described
      • Vertical and horizontal position
      • Soils analyzed for chemistry, pollen, etc
      • Associations between artifacts are recorded
      • Assumption: artifacts found at same layer occurred at same time period
    29. Vertical Excavation: Proveniencing
      • Definition: recording artifacts in three-dimensional space
      • Transit and stadia rod: record is set from a secondary datum point
      • Theolodite: Records the position of a artifact
      • Using both vertical and horizontal coordinates
    30. What is a Theolodite?
      • Left: Front View Right: Back View
      • Front Lens Viewing Lens and Focus
      • Gun Sights Adjustment knobs (v and h)
    31. Laser Theolodite
      • Adds an electronic distance meter (EDM)
      • And a laser device to the theolodite
      • It records the position of an artifact
      • Using a laser bouncing off a prism of known height
      • Results can be written down or linked to a portable computer
      • Printer can produce tags that are detached
      • And put with the artifact to be photographed before removal
    32. Horizontal Excavation: Procedure
      • As each layer or stratum is excavated, it is removed
      • Same procedure of excavation is repeated for next layer
      • One or two layers: prefer horizontal excavation to get lay of the site
      • Different samples are taken for different layers: soil, pollen, charcoal, bone
      • Some layers may be left for control
    33. Overview of Dating
      • Unifomitarianism
      • Relative Dating
        • Stratigraphy
        • Association
      • Absolute Dating
        • Calendrical
        • Natural Features
        • Isotopic
    34. Dating: Uniformitarianism
      • Uniformitarianism vs. Catastrophism
      • Uniformitarianism: All geological processes--erosion, weathering--observable today have always been present and at the same rate
      • Uniformitarianism is the basis of dating.
      • Catastrophism: Changes have been sudden and have occurred at different rates in the past from those of the present.
    35. Relative Dating
      • Stratigraphy: Establishment of sequences by soil strata
        • Exceptions: soil disturbance, erosion.
      • Law of Association: Dating of finds within a stratum
    36. Chronometric Associations
      • Basic principle: Materials associated with other materials of known age are the same age range
        • Bottle styles and clay pipes .
        • Gravestones in Stoneham, MA (Deetz)
    37. Absolute Dating: Calendrical
      • Entails use of traditional calendars
        • Mayan
          • Long Count: Beginning date fixed at 3113 BC
          • Calendar Rounds: 260- and 365-day calendars
        • Egyptians:
          • 332 BC Conquest by Alexander the Great
          • Traced back through recorded dynasties
          • Astronomical events checked by present data
        • Others: Chinese, Romans, Greeks
    38. Absolute Dating: Natural Features
      • Dendrochronology: Tree ring dating
        • Tree rings vary from year to year
        • Local stumps or timber compared with master sequence (e.g., Univ. of Arizona)
      • Varve analysis: Clay deposits in lakes from melting ice.
        • Patterns also differ yearly
        • Likewise compared with master chart.
    39. Absolute Dating: Isotopic or Radiometric Techniques
      • Common Principles
        • Isotopes: Radioactive variants of elements (e.g. carbon, potassium)
        • Isotopes decay from radioactive to nonradioactive element
        • They do so at a constant rate
      • Half Life: The period in which radioactivity rate reaches half the original rate.
    40. Isotopic Techniques: Radiocarbon Dating
      • Carbon is found in all lifeforms
      • Carbon 12 is the stable element
      • All living things accumulate Carbon 14
      • At death, carbon 14 decays at a constant rate to Carbon 12
      • It reaches half the rate of original radioactivity in 5730 years
      • At 11460 years, radioactivity is half the second rate--and so on
    41. Isotopic Techniques: Accelerator Mass Spectrometry
      • In dating, a sample is cleaned then burned to produce gas
      • Proportion of C14 to C12 is then counted using Geiger counter
      • Several grams are required for the count
      • Accelerated Mass Spectrometer: counts individual molecules
      • Advantage: High accuracy, less material
    42. Isotopic Techniques: Radiopotassium Dating
      • Half life: 1.3 billion years
      • Potassium is found in granite, basalt, clay
      • Potassium 40 decays to a gas, Argon 40
      • Argon 40 accumulate when a rock is formed
      • Disadvantage: materials less than 500,000 years old cannot be dated
    43. Other Absolute Dating Techniques
      • Electronic Spin Resonance:
        • Accumulation of unpaired electrons in crystals in tooth enamel and other items with calcium (inaccurate in bone)
      • Geomagnetism:
        • Alignment of particles on magnetic rock; this is approximate and there are few labs
      • Obsidian Hydration:
        • Reaction with water; measured by thickness of accretion.
    44. Conclusion: Dating
      • All techniques are problematic
        • Appropriate labs may be rare
        • Analyzable material must be present: no volcanic rock, no radiopotassium dates
        • Inherent problems: radiocarbon dating may be off by centuries
      • Best strategy: use several techniques
        • e.g. dendrochronology with radiocarbon.
    45. Conclusion
      • All excavation involves destruction
      • Therefore, sites have to be
      • Excavated carefully, often with trowels
      • Recorded for location and elevation
      • Artifacts catalogued before removal
      • Features have to be mapped
      • Ideal: Sites could be reconstructed
      • Based on recording of data
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