Relative Dating Techniques 1 Stratigraphic Record i principle
- Slides: 41
• Relative Dating Techniques 1. Stratigraphic Record i. principle of original horizontality ii. principle of superposition
• Relative Dating Techniques 1. Stratigraphic Record iii. Law of Lateral Continuity iv. Law of Inclusions v. Cross-cutting relations
• Relative Dating Techniques 1. Stratigraphic Record v. unconformities (1) disconformity: erosion removes a part of otherwise undisturbed rock (2) angular unconformity: rocks below are at an angle in relation to those above (3) nonconformity: sedimentary rocks lie on top of igneous rocks
2. Determining absolute time i. radiometric dating (2) half-life
• Deposition of ? , E, D • Superposition
• Deposition of ? , E, D • Intrusion F • Superposition • Cross Cutting Relations
• Deposition of ? , E, D • Intrusion F • Tilting • Superposition • Cross Cutting Relations • Original Horizontality
• Deposition of ? , E, D • Intrusion F • Tilting • Erosion • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity
• Deposition of ? , E, D • Intrusion F • Tilting • Erosion • Deposition of C, B, A • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition
• Deposition of ? , E, D • Intrusion F • Tilting • Erosion • Deposition of C, B, A • Intrusion of G • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations
• Deposition of E, G, L, C • Superposition
• Deposition of E, G, L, C • Fault H • Superposition • Cross Cutting Relations
• Deposition of E, G, L, C • Fault H • Tilting • Superposition • Cross Cutting Relations • Original Horizontality
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Intrusion of A • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Intrusion of A • Erosion • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Intrusion of A • Erosion • Deposition of N, K, B • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity • Superposition
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Intrusion of A • Erosion • Deposition of N, K, B • Tilting • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity • Superposition • Original Horizontality
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Intrusion of A • Erosion • Deposition of N, K, B • Tilting • Erosion • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity • Superposition • Original Horizontality • Unconformity
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Intrusion of A • Erosion • Deposition of N, K, B • Tilting • Erosion • Deposition of F • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity • Superposition • Original Horizontality • Unconformity • Superposition
• Deposition of E, G, L, C • Fault H • Tilting • Erosion • Deposition of M, D, J • Intrusion of A • Erosion • Deposition of N, K, B • Tilting • Erosion • Deposition of F • Erosion • Superposition • Cross Cutting Relations • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity • Superposition • Original Horizontality • Unconformity • Superposition • Unconformity
• Deposition of A, B, C, D, E, F, G • Superposition
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Superposition • Original Horizontality
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Erosion I • Superposition • Original Horizontality • Unconformity
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Erosion I • Deposition of J, K, and L • Superposition • Original Horizontality • Unconformity • Superposition
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Erosion I • Deposition of J, K, and L • M (an igneous intrusion which cross cuts all older features) • Superposition • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Erosion I • Deposition of J, K, and L • M (an igneous intrusion which cross cuts all older features) • Erosion N • Superposition • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Erosion I • Deposition of J, K, and L • M (an igneous intrusion which cross cuts all older features) • Erosion N • Deposition of P and Q • Superposition • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Unconformity • Superposition
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Erosion I • Deposition of J, K, and L • M (an igneous intrusion which cross cuts all older features) • Erosion N • Deposition of P and Q • Both R (an igneous intrusion) and S (a lava flow) must come after Q but it is impossible to say whether R came before or after S since they do not cross cut • Superposition • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations
• Deposition of A, B, C, D, E, F, G • Tilting of these strata; H (a fault which cuts across the strata) • Erosion I • Deposition of J, K, and L • M (an igneous intrusion which cross cuts all older features) • Erosion N • Deposition of P and Q • Both R (an igneous intrusion) and S (a lava flow) must come after Q but it is impossible to say whether R came before or after S since they do not cross cut • Deposition of T • Superposition • Original Horizontality • Unconformity • Superposition • Cross Cutting Relations • Superposition
Do A, B, C in lab manual. Skip Parts D and E Do Fossil age dating exercise at front of class as graded assignment.
- Obj dating
- Paraconformity
- Lithostratigraphy
- Tilting
- Stratigraphic clause
- Colusuem
- Relative dating
- Relative dating
- Conformity
- Relative dating
- Relative age dating
- Relative dating
- Relative age
- Relative dating
- Discomformities
- Relative dating
- Specimen record observation
- Adjusting accounts for financial statements chapter 3
- Relative clauses and relative pronouns stage 15
- What is a joint relative frequency
- Relative clauses jeopardy
- Relative pronoun
- Fonctions et solutions techniques
- Circumciality
- Undefined status sociology definition
- Dating patterns
- Developmental tasks for adolescent
- The adolescent in society guided reading section 2
- 2 week dating challenge
- Ordinary dating method
- Msn dating
- Relationship stages
- Absolute dating examples
- Open dating
- Friendship to relationship stages
- Dating
- Dating definition relationship
- Eukaryotic cell with labels
- Archaeological dating
- Radiometric dating formula
- Speedy match dating
- Radioactive dating worksheet