PDF-The origin of megaripples, long wave ripples and Hummocky Cross-Strat
Author : jane-oiler | Published Date : 2015-08-09
et al 1983 Van de Meene et al 1996 but also on the shoreface Green and Black 1999 and in the surfzone Greenwood and Sherman 1986 Except Southard et al 1990 all references
Presentation Embed Code
Download Presentation
Download Presentation The PPT/PDF document "The origin of megaripples, long wave rip..." is the property of its rightful owner. Permission is granted to download and print the materials on this website for personal, non-commercial use only, and to display it on your personal computer provided you do not modify the materials and that you retain all copyright notices contained in the materials. By downloading content from our website, you accept the terms of this agreement.
The origin of megaripples, long wave ripples and Hummocky Cross-Strat: Transcript
et al 1983 Van de Meene et al 1996 but also on the shoreface Green and Black 1999 and in the surfzone Greenwood and Sherman 1986 Except Southard et al 1990 all references are to field studi. of wave ripples. Colleagues at. Massachusetts Institute of Technology. Taylor Perron, Justin Kao, Kim Huppert, Abby Koss, Jocelyn Fuentes, and John Southard. Ripples arise from an instability in sediment transport over bed perturbations. Avalanching + settling limit growth. Section 1: What are Waves. SWBAT: . Explain . the relationship among waves, energy and matter. Science Starter. 1. Name . 3-5 types of . waves.. 2. What . do you think creates waves on the ocean?. When you are relaxing on an air mattress in a pool and someone does a cannonball dive off the diving board, you suddenly find yourself bobbing up and down.. OR. Strategy:. Relate sedimentary characteristics of ancient deposits (grain size, . sedimentary . structures, geometry) to features observed in modern rivers. Bedforms. during traction deposition from unidirectional flow. Bagherimiyab. Ulrich Lemmin. Effects of bed form structure on particle-turbulence interaction in unsteady suspended sediment-laden laboratory open-channel flows . Introduction. Experimental. . set-up. Quiz 1 (Next Tuesday). Trapezius. : . ORIGIN: occipital bone, seventh cervical and all thoracic vertebrae.. INSERTION: . acromion. process and spine of scapula, clavicle.. FUNCTION: elevation, adduction, and rotation of scapula.. Where water depth < 0.5 wavelength, water interacts with bed (=. wave base. ). Typical ocean waves have . l. = 10-30 m: . fair-weather wave base . (FWWB) is about 5-15 m depth. Large storm waves can have . Sahara Desert. Most desert areas have rocky ground cover (desert pavement) formed by deflation . (wind erosion) of . finer . sediment. Yet sand . dunes are the dominant form of preserved sediment in . Billy L. . Edge & Margery Overton. CVEN 695-02. Bathymetric . Data. Why do we need wave models?. Wave climate assessment at the project site is important to most coastal & ocean engineering projects, including. Transverse Wave . Clickers! . What does a wave carry? . Energy . Matter. Particles . Atoms . Mechanical Waves . Electromagnetic Waves . Clickers! . A transverse wave travels _______ to the direction of the wave’s motion. . Example 1. : . How long does it take a P-wave to travel 4,000 km? . 1) If . you are asked the . travel time. of a P-wave or S-wave for a given epicenter distance:. a) Go . to the epicenter . distance . Department of Anthropology, George Washington University, Washington DC, USA. 334 macropomaClupavus maroccanusSorbininardus apuliensis and Tischlingerichthys viohli(Diogo, 2007; see Fig. 1). This thus TRANSPORT MEDIA. Gravity. . is the . simplest mechanism of sediment . transport.. It includes the . movement of particles under gravity . down a . slope. .. Rock falls generate piles of sediment at . Sedimentary layer . thicknesses span . several orders of magnitude, from . mm . to more than a . meter. That continuum is arbitrarily subdivided: anything <1 cm is called a lamina, >1 cm is a . Lunar tidal bulge rotates around Earth with a period of 24 hours 50 minutes. But the simple tidal bulge is disrupted by the continents, forms several cells around . amphidromic. points. Tidal range .
Download Document
Here is the link to download the presentation.
"The origin of megaripples, long wave ripples and Hummocky Cross-Strat"The content belongs to its owner. You may download and print it for personal use, without modification, and keep all copyright notices. By downloading, you agree to these terms.
Related Documents