Written by students who passed Immediately available after payment Read online or as PDF Wrong document? Swap it for free 4.6 TrustPilot
logo-home
Document preview thumbnail
Preview 2 out of 6 pages
Class notes

Lecture 7 - Forensic Archeology

Document preview thumbnail
Preview 2 out of 6 pages

Organize word doc of the content from Lecture 7

Content preview

M1: Osteology, Anthropology
& Forensic Context



LECTURE 7
Forensic Archaeology
 The principal purpose of any death investigation is to RECREATE THE
Primary Principle EVENT


 Location
o Establishing the context
 Mapping
Recovery Scene o Preserving the context
 Excavation
Methods o Uncover remains
 Collection
o Remove remains for analysis


 REMOTE SENSING
o Aerial Views
o Infrared Photography
o Plant Evidence
o Magnetometer
Locating Remains o Soil Resistivity
o Ground Penetrating Radar
 TYPICAL FORENSIC INVESTIGATION
o Cadaver Dogs
o Metal Detectors
o Site Surface Survey


 Most Common Method
 Visual inspection of area for remains
Site Surface  Smells and insects
Survey  Knowledge of human skeleton
 Appreciation for Bone’s Varied Appearance


 Trained to follow the scent of a decomposing body
Cadaver Dogs  The human body puts off a lot of odors and chemicals that these dogs
will be trained to smell out


 VISUAL SEARCH INDICATORS
The Anatomy of a o Disturbed Vegetation
Clandestine o Soil Compaction
o Secondary Depression
Grave o Disturbed Soil


AREA B – plants crushed
Disturbed AREA C-B – plantd removed  time since
Vegetation burial is important here

, M1: Osteology, Anthropology
& Forensic Context



Height A Varies by environment
Mountainous Remote = Shallow
Sandy, Inhabited = Deeper



 Impossible to Replicate NATURAL GEOLOGY
 Soil compacts over time  type of soil and amount of moisture affect
timing
 Augers and Probes and
be used to feel the
difference in soil density




A – Grave Pit
Soil Compaction Depression
B – Secondary
Depression
C – Damaged
Vegetation
D – Cracks & Sloping




 Different soil types have different depression rates
 Sands generally DO NOT show depression
Soils and  Depression forms when moisture penetration is THREE FEET DEEP
Moisture  SNOW after burial usually results in depression when snow melts
 FREEZING after burial inhibits depression formation


 In some circumstances depression represents…
o Represents the abdominal cavity collapsing
Secondary o Shallow graves  24-36 inches deep
Depression o Shallower graves  more pronounced secondary depression
BUT less pronounced primary depression


 If stratification is significant and distinct, soil mixture will result in
mottling
Disturbed Soil  Incorporation of plant remains into the matrix
EX.) SOIL STRATIFICATION

Document information

Uploaded on
November 10, 2024
Number of pages
6
Written in
2024/2025
Type
Class notes
Professor(s)
Seidel
Contains
All classes
$8.49

Wrong document? Swap it for free Within 14 days of purchase and before downloading, you can choose a different document. You can simply spend the amount again.
Written by students who passed
Immediately available after payment
Read online or as PDF

Sold
0
Followers
0
Items
24
Last sold
-



Why students choose Stuvia

Created by fellow students, verified by reviews

Quality you can trust: written by students who passed their tests and reviewed by others who've used these notes.

Didn't get what you expected? Choose another document

No worries! You can instantly pick a different document that better fits what you're looking for.

Pay as you like, start learning right away

No subscription, no commitments. Pay the way you're used to via credit card and download your PDF document instantly.

Student with book image

“Bought, downloaded, and aced it. It really can be that simple.”

Alisha Student

Working on your references?

Create accurate citations in APA, MLA and Harvard with our free citation generator.

Working on your references?

Frequently asked questions