A. Bedding 1. The term that refers to a three- dimensional feature common in sedimentary rocks. B. Disturbed rock 2. A layering in sedimentary rock that has thickness greater than 1 cm. C. Graded bedding 3. Layering in sedimentary rocks characterized by thickness of less than 1 cm. D. Lamination 4. It refers to the layering in sedimentary rocks. E. Layer 5. The term for the description of the distribution of sediment sizes. F. Roundness 6. The term which refers to the degree of smoothing of the surface of a sediment due to abrasion. G. Sorting 7. The type of bedding in which sediments are deposited from suspension, coarser, and denser materials setle first then followed by finer grained material. H. Stratification Stratigraphy: 8. The word referring to the study of stratified/ layered rocks. J. Superposition 9. The principle which states that the bottom layer of a rock was formed before the top layer if it is undisturbed. K Undisturbed rock 10. The rock that may be subjected to deformation caused by folding and faulting, in which sedimentary beds may be overturned.
A. Bedding 1. The term that refers to a three- dimensional feature common in sedimentary rocks. B. Disturbed rock 2. A layering in sedimentary rock that has thickness greater than 1 cm. C. Graded bedding 3. Layering in sedimentary rocks characterized by thickness of less than 1 cm. D. Lamination 4. It refers to the layering in sedimentary rocks. E. Layer 5. The term for the description of the distribution of sediment sizes. F. Roundness 6. The term which refers to the degree of smoothing of the surface of a sediment due to abrasion. G. Sorting 7. The type of bedding in which sediments are deposited from suspension, coarser, and denser materials setle first then followed by finer grained material. H. Stratification Stratigraphy: 8. The word referring to the study of stratified/ layered rocks. J. Superposition 9. The principle which states that the bottom layer of a rock was formed before the top layer if it is undisturbed. K Undisturbed rock 10. The rock that may be subjected to deformation caused by folding and faulting, in which sedimentary beds may be overturned.
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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