![Elements of geology : a text-book for colleges and for the general reader. Geology. Fig. 139.—Oblique Lamination.. Fig. 140.—Section on Mississippi Central Railroad at Oxford (after Hilgard): Oblique Lamination. originally (and Elements of geology : a text-book for colleges and for the general reader. Geology. Fig. 139.—Oblique Lamination.. Fig. 140.—Section on Mississippi Central Railroad at Oxford (after Hilgard): Oblique Lamination. originally (and](https://c8.alamy.com/comp/RCK6K7/elements-of-geology-a-text-book-for-colleges-and-for-the-general-reader-geology-fig-139oblique-lamination-fig-140section-on-mississippi-central-railroad-at-oxford-after-hilgard-oblique-lamination-originally-and-in-the-cases-represented-in-the-figures-are-still-hori-zontal-while-the-laminae-are-oblique-elevated-inclined-and-folded-stratawe-may-assume-with-con-fidence-that-stratified-rocks-were-deposited-as-sediments-at-the-bottom-of-water-and-in-a-horizontal-or-nearly-horizontal-position-but-we-do-not-now-find-them-usually-in-this-condition-place-or-position-some-RCK6K7.jpg)
Elements of geology : a text-book for colleges and for the general reader. Geology. Fig. 139.—Oblique Lamination.. Fig. 140.—Section on Mississippi Central Railroad at Oxford (after Hilgard): Oblique Lamination. originally (and
![California Division of Mines and Geology: Special Report 106 - Geologic Features—Death Valley, California California Division of Mines and Geology: Special Report 106 - Geologic Features—Death Valley, California](http://npshistory.com/publications/geology/state/ca/cdmg-sr-106/images/fig3-9.jpg)
California Division of Mines and Geology: Special Report 106 - Geologic Features—Death Valley, California
![PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/775c705484476c8cce90c5e6bdb348cae5dadbb1/2-Figure1-1.png)
PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar
![geology sedimentary sandstone lamination bedding example Stock Footage Video (100% Royalty-free) 7906984 | Shutterstock geology sedimentary sandstone lamination bedding example Stock Footage Video (100% Royalty-free) 7906984 | Shutterstock](https://ak.picdn.net/shutterstock/videos/7906984/thumb/1.jpg)
geology sedimentary sandstone lamination bedding example Stock Footage Video (100% Royalty-free) 7906984 | Shutterstock
![Architecture and morphodynamics of subcritical sediment waves in an ancient channel–lobe transition zone - Hofstra - 2018 - Sedimentology - Wiley Online Library Architecture and morphodynamics of subcritical sediment waves in an ancient channel–lobe transition zone - Hofstra - 2018 - Sedimentology - Wiley Online Library](https://onlinelibrary.wiley.com/cms/asset/afbd7006-1db5-4c73-b024-245abcf8adcc/sed12468-fig-0004-m.jpg)
Architecture and morphodynamics of subcritical sediment waves in an ancient channel–lobe transition zone - Hofstra - 2018 - Sedimentology - Wiley Online Library
![Eye and sheath folds in turbidite convolute lamination: Aberystwyth Grits Group, Wales - ScienceDirect Eye and sheath folds in turbidite convolute lamination: Aberystwyth Grits Group, Wales - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0191814111000873-gr4.jpg)