Sandbridge Beach FONSI
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Sedimentary Processes and Geomorphic History of Wreck Shoal, an Oyster Reef of the James River, Virginia
W&M ScholarWorks Dissertations, Theses, and Masters Projects Theses, Dissertations, & Master Projects 1986 THE SEDIMENTARY PROCESSES AND GEOMORPHIC HISTORY OF WRECK SHOAL, AN OYSTER REEF OF THE JAMES RIVER, VIRGINIA Joseph T. DeAlteris College of William and Mary - Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/etd Part of the Geology Commons Recommended Citation DeAlteris, Joseph T., "THE SEDIMENTARY PROCESSES AND GEOMORPHIC HISTORY OF WRECK SHOAL, AN OYSTER REEF OF THE JAMES RIVER, VIRGINIA" (1986). Dissertations, Theses, and Masters Projects. Paper 1539616626. https://dx.doi.org/doi:10.25773/v5-af3n-wf26 This Dissertation is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Dissertations, Theses, and Masters Projects by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. INFORMATION TO USERS While the most advanced technology has been used to photograph and reproduce this manuscript, the quality of the reproduction is heavily dependent upon the quality of the material submitted. For example: • Manuscript pages may have indistinct print. In such cases, the best available copy has been filmed. • Manuscripts may not always be complete. In such cases, a note will indicate that it is not possible to obtain missing pages. • Copyrighted material may have been removed from the manuscript. In such cases, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, and charts) are photographed by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. -
Florida Designated Paddling Trails Shoal River
F ll oCR)"r 6i0i2d a D e s ii g n a tt e d Blackman P a d d ll ii n g T r a ii ll s C)"R 2 ¯ )"2 C)"R 2 S h o a ll R ii v e r CR)" 147 189 «¬ Campton 85 Cannon Town «¬ Nubbin Ridge «¬4 )"393 Auburn Baker Silver Springs 188 )" Dorcas M a p 1 «¬4 Milligan Crestview )"189 Deerland ¤£90 Mossy Head 10 Holt Galliver ¨¦§ Forest Highlands «¬85 «¬285 A N S O O T O L L A A W Designated Paddling Trail K O Wetlands Water Designated Paddling Trail Index «¬123 Niceville «¬20 0 2 4 8 Miles «¬85 S h o a ll R ii v e rr P a d d ll ii n g T rr a ii ll M a p 1 )"188 STILLWELL BLVD ¯ NO B RTH AVE R V A A C L K L I N E Y S R T D F Crestview A I L R L C O H Y I L D D S 90 R T CH ¤£ D ES NU T A Þ VE !| 2)"80A Access Point 1: Ray Barnes Boat Ramp/US 90 N: 30.7535 W: -86.5099 OKALOOSA ¨¦§10 JOHN K ING RD L I 85 V ¬ E « O Okaloosa County Shoal River A K Land Acquisition PJ AD C AMS PKWY H U R C H R D A NT Choctawhatchee IOC Choctawhatchee H R Nat'l Forest D Nat'l Forest !|*IÞ Access Point 2: Bill Duggan Jr Park/SR 85 N: 30.6976 W: -86.5712 Shoal River Paddling Trail Eglin Air Force Base !| Canoe/Kayak Launch *I Restrooms Þ Potable Water Florida Conservation Lands 0 0.5 1 2 Miles Wetlands Shoal River Paddling Trail Guide The Waterway A nature photographer’s dream, the shallow, gold-tinted Shoal River threads through a northwest Florida wilderness of high sandy hills, broad sandbars perfect for rest stops, and floodplain forest. -
Lesson 4: Sediment Deposition and River Structures
LESSON 4: SEDIMENT DEPOSITION AND RIVER STRUCTURES ESSENTIAL QUESTION: What combination of factors both natural and manmade is necessary for healthy river restoration and how does this enhance the sustainability of natural and human communities? GUIDING QUESTION: As rivers age and slow they deposit sediment and form sediment structures, how are sediments and sediment structures important to the river ecosystem? OVERVIEW: The focus of this lesson is the deposition and erosional effects of slow-moving water in low gradient areas. These “mature rivers” with decreasing gradient result in the settling and deposition of sediments and the formation sediment structures. The river’s fast-flowing zone, the thalweg, causes erosion of the river banks forming cliffs called cut-banks. On slower inside turns, sediment is deposited as point-bars. Where the gradient is particularly level, the river will branch into many separate channels that weave in and out, leaving gravel bar islands. Where two meanders meet, the river will straighten, leaving oxbow lakes in the former meander bends. TIME: One class period MATERIALS: . Lesson 4- Sediment Deposition and River Structures.pptx . Lesson 4a- Sediment Deposition and River Structures.pdf . StreamTable.pptx . StreamTable.pdf . Mass Wasting and Flash Floods.pptx . Mass Wasting and Flash Floods.pdf . Stream Table . Sand . Reflection Journal Pages (printable handout) . Vocabulary Notes (printable handout) PROCEDURE: 1. Review Essential Question and introduce Guiding Question. 2. Hand out first Reflection Journal page and have students take a minute to consider and respond to the questions then discuss responses and questions generated. 3. Handout and go over the Vocabulary Notes. Students will define the vocabulary words as they watch the PowerPoint Lesson. -
The Sense of Hearing in the Pacific Oyster, Magallana Gigas
RESEARCH ARTICLE The sense of hearing in the Pacific oyster, Magallana gigas Mohcine Charifi1,2,3, Mohamedou Sow1,2, Pierre Ciret1,2, Soumaya Benomar3, Jean- Charles Massabuau1,2* 1 University of Bordeaux, EPOC, UMR 5805, Arcachon, France, 2 CNRS, EPOC, UMR 5805, Talence, France, 3 Unit of Research on Biological Rhythms, Neuroscience and Environment, Faculty of Science, Mohammed V-Agdal University, Rabat, Morocco * [email protected] a1111111111 a1111111111 a1111111111 a1111111111 Abstract a1111111111 There is an increasing concern that anthropogenic noise could have a significant impact on the marine environment, but there is still insufficient data for most invertebrates. What do they perceive? We investigated this question in oysters Magallana gigas (Crassostrea gigas) using pure tone exposures, accelerometer fixed on the oyster shell and hydrophone in the OPEN ACCESS water column. Groups of 16 oysters were exposed to quantifiable waterborne sinusoidal Citation: Charifi M, Sow M, Ciret P, Benomar S, sounds in the range of 10 Hz to 20 kHz at various acoustic energies. The experiment was con- Massabuau J-C (2017) The sense of hearing in the ducted in running seawater using an experimental flume equipped with suspended loud- Pacific oyster, Magallana gigas. PLoS ONE 12(10): e0185353. https://doi.org/10.1371/journal. speakers. The sensitivity of the oysters was measured by recording their valve movements pone.0185353 by high-frequency noninvasive valvometry. The tests were 3 min tone exposures including a Editor: Jose A. FernaÂndez Robledo, Bigelow 70 sec fade-in period. Three endpoints were analysed: the ratio of responding individuals in Laboratory for Ocean Sciences, UNITED STATES the group, the resulting changes of valve opening amplitude and the response latency. -
Classifying Rivers - Three Stages of River Development
Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion. -
What Is Soil Erosion? Soil Erosion by Wind Or Water Is the Physical Wearing Away of the Soil Surface
Do you have a problem with: • Low yields • Time & expense to repair and gullies • Small rills and channels in your fields • Soil deposited at the base of slopes or along fence lines • Sediment in streams, lakes, and reservoirs Soil Erosion May be the Problem! Erosion from cropland What is soil erosion? Soil erosion by wind or water is the physical wearing away of the soil surface. Soil material and nutrients are removed in the process. Why be concerned? • Erosion reduces crop yields • Erosion removes topsoil, reduces soil organic matter, and destroys soil structure Signs of Erosion – Sediment entering river • Erosion decreases rooting depth • Erosion decreases the amount of water, air, and nutrients available to plants • Nutrients and sediment removed by water erosion cause water quality problems and fish kills • Blowing dust from wind erosion can affect human health and create public safety hazards • Increased production costs Erosion removes our richest soil. How much does it cost? • Technical assistance to assess and plan erosion control systems from NRCS is free • No till and mulch till may require special tillage equipment or planters if this equipment is not al- ready available • Vegetative barriers may cost $50-$100 per mile of barrier • Cover crops may cost between $10 and $40 per acre depending on the type of seed used Controlling Soil Erosion Signs of Erosion – Small rills and channels on the soil Dust clouds & “dirt devils” such as the one pictured surface are a sign of water erosion here are signs of wind erosion. How to Reduce Erosion: The key to reducing is erosion is to keep the soil covered as much as possible for both wind and water ero- sion concerns. -
4.3 Water Has a Major Role in Shaping the Earth's Surface. Enduring
4.3 Water has a major role in shaping the Earth’s surface. Enduring Understanding(s) Essential Questions (A) Water has a major role in shaping • How does water affect the Earth’s the Earth’s surface. surface? (B) Water moves in a predictable cycle. • Where does water come from? Where does it go? GRADE-LEVEL EXPECTATIONS: 1. Water is continuously moving between Earth’s surface and the atmosphere in a process called the water cycle. Water evaporates from the surface of the earth, rises into the air and cools, condenses, collects in clouds, and falls again to the surface as precipitation. The energy that causes the water cycle comes from the sun. 2. Most precipitation that falls to Earth goes directly into oceans. Some precipitation falls on land and accumulates in lakes and ponds or moves across the land. Rain or snowmelt in high elevations flows downhill in many streams which collect in lower elevations to form a river that flows downhill to an ocean. 3. Water moving across the earth in streams and rivers pushes along soil and breaks down pieces of rock in a process called erosion. The moving water carries away rock and soil from some areas and deposits them in other areas, creating new landforms or changing the course of a stream or river. 4. The amount of erosion in an area, and the type of earth material that is moved, are affected by the amount of moving water, the speed of the moving water, and by how much vegetation covers the area. 5. Rivers carve out valleys as they move between mountains or hills. -
Short Creek and Shoal Creek in the Spring River Watershed Water Quality Impairment: Total Phosphorus
NEOSHO BASIN TOTAL MAXIMUM DAILY LOAD Waterbody / Assessment Unit: Short Creek and Shoal Creek in the Spring River Watershed Water Quality Impairment: Total Phosphorus 1.0 INTRODUCTION AND PROBLEM IDENTIFICATION Subbasin: Spring Counties: Cherokee HUC8: 11070207 HUC10(12): 08(06) & 09(04) Ecoregion: Ozark Highlands, Springfield Plateau (39a) Drainage Area: Shoal Creek = approximately 10.1 square miles in Kansas Short Creek = approximately 5.94 square miles in Kansas Water Quality Limited Segments Covered Under this TMDL: Station Main Stem Segment Tributary Station SC570 Short Creek (881) Station SC212 Shoal Creek (2) Unnamed Stream (886) 2008, 2010, 2012 & 2014 303(d) Listings: Kansas Stream segments monitored by stations SC212 on Short Creek and SC570 on Shoal Creek, are cited as impaired by Total Phosphorus (TP) for the Neosho Basin. Impaired Use: Special Aquatic Life, Expected Aquatic Life, Contact Recreation and Domestic Water Supply. Water Quality Criteria: Nutrients – Narratives: The introduction of plant nutrient into surface waters designated for domestic water supply use shall be controlled to prevent interference with the production of drinking water (K.A.R. 28-16-28e(c)(3)(D)). The introduction of plant nutrients into streams, lakes, or wetlands from artificial sources shall be controlled to prevent the accelerated succession or replacement of aquatic biota or the production of undesirable quantities or kinds of aquatic life (K.A.R. 28-16- 28e(c)(2)(A)). The introduction of plant nutrients into surface waters designated for primary or secondary contact recreational use shall be controlled to prevent the development of objectionable concentrations of algae or algal by-products or nuisance growths of submersed, floating, or emergent aquatic vegetation (K.A.R. -
Understanding the Temporal Dynamics of the Wandering Renous River, New Brunswick, Canada
Earth Surface Processes and Landforms EarthTemporal Surf. dynamicsProcess. Landforms of a wandering 30, 1227–1250 river (2005) 1227 Published online 23 June 2005 in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/esp.1196 Understanding the temporal dynamics of the wandering Renous River, New Brunswick, Canada Leif M. Burge1* and Michel F. Lapointe2 1 Department of Geography and Program in Planning, University of Toronto, 100 St. George Street, Toronto, Ontario, M5S 3G3, Canada 2 Department of Geography McGill University, 805 Sherbrooke Street West, Montreal, Quebec, H3A 2K6, Canada *Correspondence to: L. M. Burge, Abstract Department of Geography and Program in Planning, University Wandering rivers are composed of individual anabranches surrounding semi-permanent of Toronto, 100 St. George St., islands, linked by single channel reaches. Wandering rivers are important because they Toronto, M5S 3G3, Canada. provide habitat complexity for aquatic organisms, including salmonids. An anabranch cycle E-mail: [email protected] model was developed from previous literature and field observations to illustrate how anabranches within the wandering pattern change from single to multiple channels and vice versa over a number of decades. The model was used to investigate the temporal dynamics of a wandering river through historical case studies and channel characteristics from field data. The wandering Renous River, New Brunswick, was mapped from aerial photographs (1945, 1965, 1983 and 1999) to determine river pattern statistics and for historical analysis of case studies. Five case studies consisting of a stable single channel, newly formed anabranches, anabranches gaining stability following creation, stable anabranches, and an abandoning anabranch were investigated in detail. -
How to Make a Meandering River
COMMENTARY How to make a meandering river Alan D. Howard1 Department of Environmental Sciences, P.O. Box 400123, University of Virginia, Charlottesville, VA 22904-4123 espite the ubiquity of mean- dering rivers in nature, only recently have appropriate ex- perimental conditions been Dproduced to replicate a stably meander- ing stream in the laboratory, as de- scribed in a recent issue of PNAS (1). Meandering channels occur in a wide variety of sedimentary environments, including on deep sea fans formed by turbidity currents (2), as relict meanders on Mars (3) (Fig. 1), and as channels formed by flowing alkenes on Titan. The mechanics of formation of mean- ders is reasonably well understood (4). When flow enters a channel bed, a heli- cal secondary current is set up that in- creases flow velocity and channel depth along the outer bank in proportion to bed curvature, which encourages bank erosion. The secondary current has an intrinsic downstream scale related to flow velocity and depth; this results in gradual increase in bend amplitude and propagation of the meandering pattern upstream and downstream. Linear the- ory of flow in bends (5) has permitted construction of simulation models that replicate many aspects of meandering Fig. 1. Fossil highly sinuous meandering channel and floodplain on Mars. Red arrows point to repre- behavior, including meander cutoffs, sentative locations along channel. The channel bed is now a ridge (in inverted relief) because wind erosion creation of oxbow lakes, and patterns of has removed finer sediment from the floodplain and surrounding terrain. The low curvilinear ridges floodplain sedimentation (6, 7). -
Interpretation of Fish Shoal Indications in the Arabian Sea
INTERPRETATION OF FISH SHOAL INDICATIONS IN THE ARABIAN SEA V. A. Puthran & V. Narayana Pillai Central institute of Fisheries Operatives, Cachill. Jntroduction Some knowledge regardir.g the pre sence of similar fishable concentrations Availability of resources is perhaps of fish and other marine life is of great one of the most il1)p~rt2nt factors which importance to the technical ski:] working determines the success of any industry. on board fishing vess" ls. Their technical In the case of the fishing industry, at the knowledoe in fishing could be put to basic production level. the availability use more-eifectively ..,>,hen posit ive indi of fishable concentrations of fishes and cations with regard to the avaiiability of other mHine life is the decisive factor shoals are known to them. The correct which c~ntrols the economy of the whole and quick interpretation of these indi system. Even when well e quipped cations would Dlace them in a better vessel, fishing gear an d trained person position from where they can use their nelare available, the success of the indu judgment towards achieving great stry is dependent on the availability of success in this endeavour. fishable concentrations of commercially important marine life at the appropriate In India, only very little werk seems time. By the word' fishable concentra to have been done along these lines tions', the implication is availability of especially to arrive at a positive corre sizeable quantities of fishes which could lation between certain natural indica be definitely caught using a particular tions and presence of fishable concent type of craft and gear in a particular rations of comITl "rciallv important area at a particular time. -
Effects of a Shallow Flood Shoal and Friction on Hydrodynamics of A
PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Effects of a shallow flood shoal and friction on hydrodynamics 10.1002/2016JC012502 of a multiple-inlet system Key Points: Mara M. Orescanin1 , Steve Elgar2 , Britt Raubenheimer2 , and Levi Gorrell2 A flood shoal can act as a tidal reflector and limit the influence of an 1Oceanography Department, Naval Postgraduate School, Monterey, California, USA, 2Applied Ocean Physics and inlet in a multiple-inlet system Engineering, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA The effects of inertia, friction, and the flood shoal can be separated with a lumped element model As an inlet lengthens, narrows, and Abstract Prior studies have shown that frictional changes owing to evolving geometry of an inlet in a shoals, the lumped element model multiple inlet-bay system can affect tidally driven circulation. Here, a step between a relatively deep inlet shows the initial dominance of the and a shallow bay also is shown to affect tidal sea-level fluctuations in a bay connected to multiple inlets. shoal is replaced by friction To examine the relative importance of friction and a step, a lumped element (parameter) model is used that includes tidal reflection from the step. The model is applied to the two-inlet system of Katama Inlet (which Correspondence to: M. M. Orescanin, connects Katama Bay on Martha’s Vineyard, MA to the Atlantic Ocean) and Edgartown Channel (which con- [email protected] nects the bay to Vineyard Sound). Consistent with observations and previous numerical simulations, the lumped element model suggests that the presence of a shallow flood shoal limits the influence of an inlet.