Field Trip #2 - Creating a Model for a Progradational Barrier Island System Field Area: Shackleford Banks, North Carolina Introd
![Figure 10 | Microencrusters from the Upper Jurassic–Lower Cretaceous İnaltı Formation (Central Pontides, Turkey): remarks on the development of reefal/peri-reefal facies | SpringerLink Figure 10 | Microencrusters from the Upper Jurassic–Lower Cretaceous İnaltı Formation (Central Pontides, Turkey): remarks on the development of reefal/peri-reefal facies | SpringerLink](https://media.springernature.com/full/springer-static/image/art%3A10.1007%2Fs10347-015-0445-5/MediaObjects/10347_2015_445_Fig10_HTML.gif)
Figure 10 | Microencrusters from the Upper Jurassic–Lower Cretaceous İnaltı Formation (Central Pontides, Turkey): remarks on the development of reefal/peri-reefal facies | SpringerLink
![Depositional environment of the Hunton Group (Modified from Stanley,... | Download Scientific Diagram Depositional environment of the Hunton Group (Modified from Stanley,... | Download Scientific Diagram](https://www.researchgate.net/publication/316048073/figure/fig1/AS:482361541435398@1492015361680/Depositional-environment-of-the-Hunton-Group-Modified-from-Stanley-2001-NWB-and.png)
Depositional environment of the Hunton Group (Modified from Stanley,... | Download Scientific Diagram
![Short-Term Assessment of Retreating vs. Advancing Microtidal Beaches Based on the Backshore/Foreshore Length Ratio: Examples from the Basilicata Coasts (Southern Italy) Short-Term Assessment of Retreating vs. Advancing Microtidal Beaches Based on the Backshore/Foreshore Length Ratio: Examples from the Basilicata Coasts (Southern Italy)](http://html.scirp.org/file/11-1470173x5.png)
Short-Term Assessment of Retreating vs. Advancing Microtidal Beaches Based on the Backshore/Foreshore Length Ratio: Examples from the Basilicata Coasts (Southern Italy)
![Wave and storm signals in a lacustrine succession and their relationship to paleowind direction (Tanan Depression, Mongolia, early Cretaceous) - ScienceDirect Wave and storm signals in a lacustrine succession and their relationship to paleowind direction (Tanan Depression, Mongolia, early Cretaceous) - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0037073821000634-gr12.jpg)
Wave and storm signals in a lacustrine succession and their relationship to paleowind direction (Tanan Depression, Mongolia, early Cretaceous) - ScienceDirect
![A small sea-level drop may cause important and variable facies changes... | Download Scientific Diagram A small sea-level drop may cause important and variable facies changes... | Download Scientific Diagram](https://www.researchgate.net/publication/222909488/figure/fig2/AS:305270552055808@1449793579167/A-small-sea-level-drop-may-cause-important-and-variable-facies-changes-in-shallow.png)
A small sea-level drop may cause important and variable facies changes... | Download Scientific Diagram
![Wave-Dominated Coasts. In open water, waves are purely an oscillatory motion Where water depth < 0.5 wavelength, water interacts with bed (=wave base) - ppt download Wave-Dominated Coasts. In open water, waves are purely an oscillatory motion Where water depth < 0.5 wavelength, water interacts with bed (=wave base) - ppt download](https://images.slideplayer.com/28/9386989/slides/slide_3.jpg)
Wave-Dominated Coasts. In open water, waves are purely an oscillatory motion Where water depth < 0.5 wavelength, water interacts with bed (=wave base) - ppt download
![Oligocene storm-induced lacustrine deposits in the Yaxi Area of the Jiuxi Basin, northeastern margin of the Tibetan Plateau - ScienceDirect Oligocene storm-induced lacustrine deposits in the Yaxi Area of the Jiuxi Basin, northeastern margin of the Tibetan Plateau - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S1367912018301640-gr17.jpg)