1. 11-1 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Forensic Geology The legal application of earth and soil science Characterization of earthen materials that have been transferred between objects or locations and the analysis of possible origin or sources

2. 11-2 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein History 1887–1893—Sir Arthur Conan Doyle wrote about scientific ideas and techniques for solving crimes in his writings of Sherlock Holmes. This included information about soil and its composition which had never actually been used. 1893—An Austrian criminal investigator, Hans Gross, wrote that there should be a study of “dust, dirt on shoes and spots on cloth.” He observed, “Dirt on shoes can often tell us more about where the wearer of those shoes had last been than toilsome inquiries.”

3. 11-3 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein History 1904—Georg Popp, a German forensic scientist, presented the first example of earth materials used as evidence in a criminal case, the strangulation of Eva Disch. 1910—Edmond Locard, a forensic geologist, was most interested in the fact that dust was transferred from the crime scene to the criminal. This helped to establish his principle of transfer.

4. 11-4 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Soil Naturally deposited materials that cover the earth’s surface and are capable of supporting plant growth The value of soil as evidence depends on: -its prevalence at crime scenes -its transferability between the scene and the criminal Most soils can be differentiated by their appearance.

5. 11-5 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Soil Forensic geologists will characterize and compare the mineral content of soils.

6. 11-6 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Soil Characteristics Composition: – Sand – Silt – Clay – Organic matter

7. 11-7 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Soil Characteristics

8. 11-8 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Collection of Soil Standard /reference soils are to be collected at various intervals within a 100-yard radius of the crime scene, as well as the site of the crime, for comparison to the questioned soil. Soil found on the suspect, such as adhering to a shoe or garments, must not be removed. Instead, each object should be individually wrapped in paper, and transmitted to the laboratory.

9. 11-9 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Forensic Geology Tools Binocular microscopes Petrographic microscopes X-ray diffraction Scanning electron microscopes Microchemical analysis

10. 11-10 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Soil Analysis A side-by-side visual comparison under a microscope of the color and texture of soil specimens is easy to perform and provides a way of distinguishing soils that originate from different locations.

11. 11-11 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Soil Comparisons May establish a relationship or link to the crime, the victim, or the suspect(s) Physical properties—density, magnetism, particle size, mineralogy Chemical properties—pH, trace elements

12. 11-12 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Minerals More than 2,000 have been identified. Twenty or so are commonly found in soils; most soil samples contain only three to five. Characteristics for identification—size, density, color, luster, fracture, streak, magnetism

13. 11-13 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Mineral In-Class Assignment Select a mineral off of the list and complete the following: Identify: –Soils that mineral is found in –Size (range) –Density –Color(s) –Luster – how it reflects light/sheen –Streak – the color it displays in finely powdered form. –Magnetism

14. 11-14 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Rocks Aggregates of minerals –Types Natural—like granite Man-made—like concrete Formation –Igneous –Sedimentary –Metamorphic

15. 11-15 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Sand Sand is the term applied to natural particles with a grain diameter between 1/16 mm and 2 mm. Composition is based on the material of the source, which also gives sand its color. (The photo on the right shows color differences in sand from six locations around the world.)

16. 11-16 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein Fossils Remains of plants and animals May help geologists to determine the age of rocks Some are scarce and can be used to identify regions or locations

17. 11-17 PRENTICE HALL ©2008 Pearson Education, Inc. Upper Saddle River, NJ 07458 FORENSIC SCIENCE An Introduction By Richard Saferstein True Life: Forensic Geology A nine-year-old’s body was found in a wooded area along a river in Lincoln County, South Dakota. A forensic geologist collected soil samples from the fenders of a suspect’s truck and from the area where the body was found. Both soils contained grains of a blue mineral that turned out to be gahnite, a rare mineral that had never been reported in South Dakota. As a result, the soil tied the suspect to the crime. Check out other cases at: www.forensicgeology/science.htm