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Transverse ridges in loess-paleosol sequences
Abstract Loess deposits in China commonly contain well-developed transverse ridges (TRs), which are transverse to the transport direction of the loess.
Site: https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2012JD017980
Pollen from an unusual charcoal layer from the Loess Plateau
Excavations of loess profiles in the Malan loess section, northern Loess Plateau, China, exposed an unusual charcoal layer (CL) with rich sediments, a sharp upper boundary, and an age of about 12.8 thousand years (ka) BP.
Site: https://www.tandfonline.com/doi/abs/10.1080/15230430.2019.1609892
Modeling the generation of transverse ridges by a viscoelastic ...
Transverse ridges are arcuate-shaped mounds with transverse orientations that occur along shorelines. They are very common along shorelines in the low- and mid-latitudes.
Site: https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2001JC001083
Ridges - Definition, Types, Formation and Characteristics
Ridges are defined as elongated elevations on the Earth's surface, often formed by the folding of the crust or by depositional processes.
Site: https://www.geomaps.com.au/geology-glossary-r.html
Ridge - an overview | ScienceDirect Topics
Ridge: A long, relatively narrow elevation of the sea floor with steep sides. Ridges are typically formed by the accretion of sediment or volcanic material.
Site: https://www.sciencedirect.com/topics/earth-and-planetary-sciences/ridge
Transverse ridges on the Diamantina River, Queensland
The Diamantina River is a major river system in central Australia. It rises in the Central Highlands of Queensland and flows west across the arid Channel Country to Lake Eyre in South Australia.
Site: https://web.archive.org/web/20140226093932/http://www.ga.gov.au/image_cache/GA7586.pdf
Morphogenesis of transverse ridges on sandy coasts: a review
1 Introduction Transverse ridges are three-dimensional morphological features that are common on sandy coasts around the world.
Site: https://link.springer.com/article/10.1007/s10021-006-0063-x
New Zealand Journal of Geology and Geophysics
The orientations of foresets and topsets within trough cross-bedded sets are compared for sediments deposited at different depths on the continental shelf to the north of New Zealand.
Site: https://www.tandfonline.com/doi/abs/10.1080/00288306.1988.10426276
Mapping transverse ridge patterns on a dissipative beach using ...
Transverse ridges are transient morphological features that form due to the interaction between waves, currents and sediment on sandy beaches.
Site: https://link.springer.com/article/10.1007/s10236-021-01422-1
Bedform morphodynamics over transverse ridges in a large ...
Bedforms are common features in many geophysical flows. In coastal environments, bedforms appear in various shapes, sizes, and organizations determined by the interplay between flow, sediment, and morphology.
Site: https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2021JF006162