Climbing ripple cross lamination

This is a cross-sectional sedimentary structure of cm-scale climbing ripple cross stratification indicating a unidirectional current from B to A of very-fine to fine sediment, as scaled by a coin. The climbing cross laminae is due to the superimposition of migrating ripples, in which the rate of sediment deposition is greater than the rate of migration.

Digitized Date 09/07/2018

Creator Dolphin, Glenn

Digital Publisher Calgary : University of Calgary

Country Canada

Province Alberta

Municipality City of Calgary

How can you use this image?

Permitted uses are outlined in License and Usage Rights. Usage Restrictions can only be waived by the copyright holder. Add to cart and make a request if you have any questions.

Usage Rights Commercial, Education, Exhibition, Instruction, Private study, Publication, Remix and adapt, Research

Copyright Status In copyright

License URL https://creativecommons.org/licenses/by/4.0/

Attribution "Climbing ripple cross lamination", 2018, (CU124722) by , is used under . Courtesy of Collection, Libraries and Cultural Resources Digital Collections, University of Calgary.

Unique identifier: CU124722

Legacy Identifier: 20190213_geoimage_Dolphin_e_00015

Type: Geoscience Image

Size: 5184px × 3456px 51.87 MB