Petrography and Genesis of the New Jersey Beach Sands
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Data Dictionary for Grain-Size Data Tables
Data Dictionary for Grain-Size Data Tables The table below describes the attributes (data columns) for the grain-size data tables presented in this report. The metadata for the grain-size data are not complete if they are not distibuted with this document. Attribute_Label Attribute_Definition SAMPLE ID Sediment Sample identification number DEPTH (cm) Sample depth interval, in centimeters Physical description of sediment textural group - describes the dominant grain size class of the sample (after Folk, 1954): SEDIMENT TEXTURE (Folk, 1954) Sand, Clayey Sand, Muddy Sand, Silty Sand, Sandy Clay, Sandy Mud, Sandy Silt, Clay, Mud, or Silt AVERAGED SAMPLE RUNS Number of sample runs (N) included in the averaged statistics or other relavant information MEAN GRAIN SIZE (mm) Mean grain size, in microns (after Folk and Ward, 1957) MEAN GRAIN SIZE STANDARD DEVIATION (mm) Standard deviation of mean grain size, in microns SORTING (mm) Sample sorting - the standard deviation of the grain size distribution, in microns (after Folk and Ward, 1957) SORTING STANDARD DEVIATION (mm) Standard deviation of sorting, in microns SKEWNESS (mm) Sample skewness - deviation of the grain size distribution from symmetrical, in microns (after Folk and Ward, 1957) SKEWNESS STANDARD DEVIATION (mm) Standard deviation of skewness, in microns KURTOSIS (mm) Sample kurtosis - degree of curvature near the mode of the grain size distribution, in microns (after Folk and Ward, 1957) KURTOSIS STANDARD DEVIATION (mm) Standard deviation of kurtosis, in microns MEAN GRAIN SIZE (ɸ) Mean -
Mount Mitchill Scenic Overlook
Park Hours Monmouth County Park System Welcome to Activities Mount Mitchill Scenic Overlook is open each day Mount Mitchill Scenic Overlook Visitors to Mount Mitchill can take in the of the year from 8 am to dusk, free of charge. At 266 feet, this overlook sits on the highest natural expansive views of one of our most important and famous cities; contemplate the events of Mount Mitchill elevation on the Atlantic coastal plain, providing For More Information September 11, 2001; or enjoy the playground. beautiful views of Sandy Hook, Raritan Bay and If you would like information on the Monmouth Photographers and artists may be inspired to County Park System’s more than 30 open spaces, Scenic the New York skyline. There are two viewing areas capture the amazing colors and scenery of this parks, recreation areas and golf courses or a with descriptive panels that explain the view and vista on film or paper, while geography buffs directory of the nearly 4,000 programs/activities geography of the site. This 12-acre park is also home will enjoy the unique perspective afforded by offered each year, please call (732) 842-4000 to the Monmouth County 9/11 Memorial honoring the location. C en Overlook te A r v. Sho (TTY/TDD 711) or visit us online at Blvd. re Atlantic Highlands, NJ the memory of county residents who lost their lives SANDY HOOK M o www.monmouthcountyparks.com. 1980 Hostage Memorial Port nmouth Rd. B r Por a t on September 11, 2001. y G r e BAY The seizure of the U.S. -
Evolution and Grain Size Distribution of Bahamian Ooid Shoals From
Movement and grain size distribution of Bahamian sand shoals from remote sensing Kathryn M. Stack Michael Lamb, Ralph Milliken, Sebastien Leprince, John Grotzinger California Institute of Technology KISS Monitoring Earth Surface Changes From Space II 3/30/10 Motivation: Understand how sediment moves underwater Transport Grain size Implicaons Evoluon of shallow Petroleum and natural CO2 reservoirs bathymetry gas reservoirs 2 How remote sensing data can help • Obtain a 2-D snapshot of a modern day shallow carbonate environment • Build up a time series of morphology and grain size • Quantify the distribution and movement of sediment at a variety of temporal and spatial scales –Tides versus storms? • Use the modern to better understand the 3-D patterns of porosity and permeability in the rock record The Bahamas: A modern carbonate environment Florida The Atlantic Ocean The Bahamas Cuba 100 km Google Earth Tongue of the Ocean Schooner Cays 20 km 20 km Exumas Lily Bank 2 km 2 km Tongue of the Ocean 10 km 1 Crest spacing ~ 1‐10 km Google Earth 3 Crest spacing ~ 100 m 2 1 km Crest spacing ~ 1 km ASTER, Band 1 20 m Sediment transport and bedform migration Bedform spatial scales = 5-10 cm, 1 m, 10-100 m, 1-10 km Temporal scales = Hours, days, years Δy Δx Transport Ideal Imaging Campaign • High enough spatial resolution to see bedform crests on a number of scales - Sub-meter resolution - Auto-detection system • High enough temporal resolution to distinguish between slow steady processes and storms - Image collection every 3 to 6 hours • Spectral resolution depending on bedform scale of interest Also useful: • High resolution water topography (sub-meter resolution) • Track currents, tides, and water velocity Application of COSI-Corr • Use the COSI-Corr software developed by Leprince et al. -
The Effect of Variable Grain Size Distribution on Beach's
Delft University of Technology Faculty of Civil Engineering and Geosciences Department of Hydraulic Engineering MSc Thesis THE EFFECT OF VARIABLE GRAIN SIZE DISTRIBUTION ON BEACH’S MORPHOLOGICAL RESPONSE Graduation committee: Prof.dr.ir. A.J.H.M. Reniers Author: Dr.ir. Matthieu de Schipper Melike Koktas Ir. Tjerk Zitman Dr. Edith L. Gallagher May 2017 P a g e 2 | 67 EXECUTIVE SUMMARY Field studies with in-situ sediment sampling demonstrate the spatial variability in grain size on a sandy beach. However, conventional numerical models that are used to simulate the coastal morphodynamics ignore this variability of sediment grain size and use a uniform grain size distribution of mostly around and assumed fine grain size. This thesis study investigates the importance of variable grain size distribution in a beach’s morphological response. For this purpose, first a field experiment campaign was conducted at the USACE Field Research Facility (FRF) in Duck, USA, in the spring of 2014. This experiment campaign was called SABER_Duck as an acronym for ‘Stratigraphy And BEach Response’. During SABER_Duck, in-situ swash zone grain size distribution, the prevailing hydrodynamic conditions and the time-series of the cross-shore bathymetry data were collected. The data confirmed a highly variable grain size distribution in the swash zone both vertically and horizontally. Additionally, the two trench survey observations showed the existence of continuous layers of coarse and fine sands comprising the beach stratigraphy. Secondly, a process based numerical coastal morphology model, XBeach, was chosen to simulate the beach profile response to wave and tidal action. A 1D cross-shore profile model was built and tested with the bathymetry data and accompanying boundary conditions that were collected during SABER_Duck. -
Grain-Size Sorting in Grainflows at the Lee Side of Deltas
Sedimentology (2005) 52, 291–311 doi: 10.1111/j.1365-3091.2005.00698.x Grain-size sorting in grainflows at the lee side of deltas MAARTEN G. KLEINHANS Department of Physical Geography, Faculty of Geosciences, Universiteit Utrecht, PO Box 80115, 3508 TC Utrecht, The Netherlands (E-mail: [email protected]) ABSTRACT The sorting of sediment mixtures at the lee slope of deltas (at the angle of repose) is studied with experiments in a narrow, deep flume with subaqueous Gilbert-type deltas using varied flow conditions and different sediment mixtures. Sediment deposition and sorting on the lee slope of the delta is the result of (i) grains falling from suspension that is initiated at the top of the delta, (ii) kinematic sieving on the lee slope, (iii) grainflows, in which protruding large grains are dragged downslope by subsequent grainflows. The result is a fining upward vertical sorting in the delta. Systematic variations in the trend depend on the delta height, the migration celerity of the delta front and the flow conditions above the delta top. The dependence on delta height and migration celerity is explained by the sorting processes in the grainflows, and the dependence on flow conditions above the delta top is explained by suspension of fine sediment and settling on the lee side and toe of the delta. Large differences in sorting trends were found between various sediment mixtures. The relevance of these results with respect to sorting in dunes and bars in rivers and laboratory flumes is discussed and the elements for a future vertical sorting model are suggested. -
Appendix H Sandy Hook Gateway National Recreation Area and Sea Bright Mitigation Report
Appendix H Sandy Hook Gateway National Recreation Area and Sea Bright Mitigation Report Date: June 30, 2021 Monmouth County Authored by: Stantec Consulting Services, Inc. 1 Contents INTRODUCTION ..................................................................................................................................................... 1 1 – COMMUNICATIONS ......................................................................................................................................... 5 Communications and Website Travel Portal (SH 1.1) .................................................................................................... 5 Signage on the Garden State Parkway (SH 1.2) ........................................................................................................... 6 Signage on NJ 36 (Navesink Avenue/Memorial Parkway) – Atlantic Highlands (SH 1.3) .............................................. 7 Travel Time Signage (General) (SH 1.4) ....................................................................................................................... 9 Signage on Ocean Avenue – Sea Bright (SH 1.5) ......................................................................................................... 9 2 – TRAVEL BEHAVIOR ....................................................................................................................................... 11 Pedestrian Management (SH 1.2 and SH 1.2)............................................................................................................ -
Seastreak Wall Street with Pier 11, Lower Manhattan, New York, New York January 9, 2013
Allision of the Passenger Vessel Seastreak Wall Street with Pier 11, Lower Manhattan, New York, New York January 9, 2013 Marine Accident Report NTSB/MAR-14/01 PB2014-105712 NTIS # National Transportation Safety Board NTSB/MAR-14/01 NTIS # PB2014-105712 Notation 8473A Adopted April 8, 2014 Marine Accident Report Allision of the Passenger Vessel Seastreak Wall Street with Pier 11, Lower Manhattan, New York, New York January 9, 2013 National Transportation Safety Board 490 L’Enfant Plaza, SW Washington, DC 20594 National Transportation Safety Board. 2014. Allision of the Passenger Vessel Seastreak Wall Street with Pier 11, Lower Manhattan, New York, New York, January 9, 2013. Marine Accident Report NTSB/MAR-14/01. Washington, DC. Abstract: This report discusses the allision of the high-speed passenger ferry Seastreak Wall Street with Pier 11/Wall Street in lower Manhattan, New York City, on January 9, 2013. Four passengers were seriously injured, and 75 passengers and 1 deckhand sustained minor injuries. The estimated cost to repair the ferry was about $166,200. The total cost of repairs to the pier was $333,349. Safety issues identified in this report include oversight of vessel operations, control panel design, management of passenger access to stairwells to mitigate possible injuries, the importance of marine safety management systems, and the need for information captured by voyage data recorders in investigating and analyzing accident causes and identifying remedial actions to help prevent their recurrence. The National Transportation Safety Board (NTSB) issues new recommendations to the United States Coast Guard regarding human factors standards for critical vessel controls, the need for operator control of ferry passenger access to stairwells, and the carriage of marine voyage data recorders. -
History of Religions in Freehold Township
HISTORY OF RELIGIONS IN FREEHOLD TOWNSHIP Compiled By Father Edward Jawidzik of St. Robert Bellarmine Catholic Church For Freehold Township Historic Preservation Commission Compiled In 2003 (Updated 2016) BETHEL AFRICAN METHODIST EPISCOPAL CHURCH 3 WATERWORKS RD. PO BOX 541 FREEHOLD, N.J. 07728 PHONE 732-462-0826 FAX 732-462-7015 HISTORY Bethel African Methodist Episcopal Church was founded in 1867. A new structure was completed in 1988. The church was relocated to its present location. Bethel Church was an Episcopal form of church government where bishops of the African Methodist Episcopal Church appoint pastors. It is a worldwide church denomination with congregations in South America, Europe, Africa, Canada, Bermuda, The Caribbean Islands and the United States. Founded In 1787 By Rev. Richard Allen. This first leader was a former slave. The African Methodist Episcopal Church is divided into 19 Episcopal Districts. It was under the pastoral leadership of Rev. Malcolm S. Steele that Bethel experienced its greatest progress, development and growth. Rev. Steele was appointed to Bethel in 1966 and served until his retirement in 2000. COLTS NECK REFORMED CHURCH 72 ROUTE 537 W. P.O. BOX 57 COLTS NECK, N.J. 07722 PHONE 732-462-4555 FAX 732-866-9545 WEBSITE: http://www.cnrc.info--email: [email protected] HISTORY The First Reformed Protestant Church of Freehold, now known as Old Brick Reformed Church of Marlboro and was founded In 1699. Preaching in the area that is now Colts Neck; however was done in homes, barns and schoolhouses for the next 150 Years. The Colts Neck Reformed Church was organized as a sister congregation of the Freehold Church on Tuesday, April 22, 1856. -
Coastal Processes Study at Ocean Beach, San Francisco, CA: Summary of Data Collection 2004-2006
Coastal Processes Study at Ocean Beach, San Francisco, CA: Summary of Data Collection 2004-2006 By Patrick L. Barnard, Jodi Eshleman, Li Erikson and Daniel M. Hanes Open-File Report 2007–1217 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia 2007 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Barnard, P.L.., Eshleman, J., Erikson, L., and Hanes, D.M., 2007, Coastal processes study at Ocean Beach, San Francisco, CA; summary of data collection 2004-2006: U. S. Geological Survey Open-File Report 2007- 1217, 171 p. [http://pubs.usgs.gov/of/2007/1217/]. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Executive Summary of Major Findings..................................................................................................................................1 Chapter 2 - Beach Topographic Mapping..............................................................................................................1 -
Maggie Williams Particle Size, Shape and Sorting: What Grains Can Tell Us
Particle size, shape and sorting: what grains can tell us Maggie Williams Most sediments contain particles that have a range of sizes, so the mean or average grain size is used in description. Mean grain size of loose sediments is measured by size analysis using sieves Grain size >2mm Coarse grain size (Granules<pebble<cobbles<boulders) 0.06 to 2mm Medium grain size Sand: very coarse-coarse-medium-fine-very fine) <0.06mm Fine grain size (Clay<silt) Difficult to see Remember that for sediment sizes > fine sand, the coarser the material the greater the flow velocity needed to erode, transport & deposit the grains Are the grains the same size of different? What does this tell you? If grains are the same size this tells you that the sediment was sorted out during longer transportation (perhaps moved a long distance by a river or for a long time by the sea. If grains are of different sizes the sediment was probably deposited close to its source or deposited quickly (e.g. by a flood or from meltwater). Depositional environments Environment 1 Environment 2 Environment 3 Environment 4 Environment 5 Environment 6 Sediment size frequency plots from different depositional environments • When loose sediment collected from a sedimentary environment is washed and then sieved it is possible to measure the grain sizes in the sediment accurately. • The grain size distribution may then be plotted as a histogram or as a cumulative frequency curve. • Sediments from different depositional environments give different sediment size frequency plots. This shows the grain size distribution for a river sand. -
2015 Weekend in Old Monmouth Booklet Web.Indd
Welcome to Monmouth County History The Monmouth County Board of Chosen Freeholders and the Historical Commission welcome you to the Eighth Annual Weekend in Old Monmouth self-guided tour of historic sites. This year the tour includes more than 45 sites organized into four segments: North or Yellow Tour - sites 1 - 13 East or Blue Tour - sites 14 - 23 South or Green Tour - sites 24 - 33 West or Red Tour - sites 34 – 44 Experience indicates that some tour followers attempt to visit as many sites as possible while others opt for a small number, often those close to home. Regarding organization, the tour places some widely separated sites in a semblance of order. Conversely, other sites are located close together. Visitors may see the sites in any order, or no order, or reverse the sequence from the proposed starting points. Three of the sub-tours begin in proximity to county borders, while the fourth, or East, begins in a population center and is readily accessible from the Garden State Parkway. In addition, the Tour Booklet points out a number of opportunities to leave the proscribed order. The suggested routes offer logical, easy-to-follow directions, but those familiar with the local landscape or possessing GPS systems may wish to use alternate roads. We suggest making a point to visit Site 44A, the Monmouth County Historical Association Museum and Library. The Association has an incomparable, magnifi cent collection of Monmouth artifacts, extensive research holdings and features informative changing exhibitions on Monmouth County history. While there also visit a Monmouth County owned site, the Battle of Monmouth Monument in front of the Monmouth County Courthouse. -
Sandy Hook Traveler Information System
National Park Service U.S. Department of the Interior Gateway National Recreation Area – Sandy Hook Unit Highlands, New Jersey Sandy Hook Traveler Information System PMIS No. 16635C FINAL September 2010 John A. Volpe National Transportation Systems Center Research and Special Programs Administration U.S. Department of Transportation Contents Report Notes & Acknowledgements ....................................................................... iii Notice / Disclaimer .................................................................................................. v Acronyms / Definitions ........................................................................................... vi Section 1: Introduction .......................................................................................... 1 Sandy Hook Unit Overview ................................................................................................. 1 Sandy Hook Traveler Information System Concept ............................................................... 2 Existing Traveler Information System ................................................................................... 2 Section 2: Relevant Communication Platforms ....................................................... 5 Social Media / Web 2.0 ....................................................................................................... 5 Gov 2.0 ..................................................................................................................................................... 5