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Chapter 13.2: Topographic Maps 1
Chapter 13.2: Topographic Maps 1 A map is a model or representation of objects and terrain in the actual environment. There are numerous types of maps. Some of the types of maps include mental, planimetric, topographic, and even treasure maps. The concept of mapping was introduced in the section using natural features. Maps are created for numerous purposes. A treasure map is used to find the buried treasure. Topographic maps were originally used for military purposes. Today, they have been used for planning and recreational purposes. Although other types of maps are mentioned, the primary focus of this section is on topographic maps. Types of Maps Mental Maps – The mind makes mental maps all the time. You drive to the grocery store. You turn right onto the boulevard. You identify a street sign, building or other landmark and know where this is where you turn. You have made a mental map. This was discussed under using natural features. Planimetric Maps – A planimetric map is a two dimensional representation of objects in the environment. Generally, planimetric maps do not include topographic representation. Road maps, Rand McNally ® and GoogleMaps ® (not GoogleEarth) are examples of planimetric maps. Topographic Maps – Topographic maps show elevation or three-dimensional topography two dimensionally. Topographic maps use contour lines to show elevation. A chart refers to a nautical chart. Nautical charts are topographic maps in reverse. Rather than giving elevation, they provide equal levels of water depth. Topographic Maps Topographic maps show elevation or three-dimensional topography two dimensionally. Topographic maps use contour lines to show elevation. -
General Rules for Contour Lines
6/30/2015 EASC111LabEFor Printing LAB E: Topographic Maps (for printing) MAP READING PRELAB: Any type of map is a twodimensional (flat) representation of Earth’s surface. Road maps, surveying maps, topographic maps, geologic maps can all cover the same territory but highlight different features of the area. Consider the following images from the same area in Illinois. Make a list of the types of features that are shown on each type of map. Topographic Maps The light brown lines on the topographic map are called contour lines. A contour line connects points of equal height above sea level, called elevation. For example, a 600’ (six hundred foot) contour line on a map means that every point on that contour line is 600’ above sea level. In order to understand contour lines better, imagine a box with a “mountain” in it with a clear plastic lid on top of the box. Assume the base of the mountain is at sea level. The box is slowly being filled with water. Since water automatically levels itself off, it will touch the “mountain” at the same height all the way around. If we were to peer down into the box from above, we could draw a line on the lid that marks where the water touches the “mountain”. This would be a contour line for that elevation. As the box continues to fill with water, we would draw contour lines at specific intervals, such as 1”. Each time the water level rises one inch, we will draw a line marking where the water touches the land. -
Maps and Charts
Name:______________________________________ Maps and Charts Lab He had bought a large map representing the sea, without the least vestige of land And the crew were much pleased when they found it to be, a map they could all understand - Lewis Carroll, The Hunting of the Snark Map Projections: All maps and charts produce some degree of distortion when transferring the Earth's spherical surface to a flat piece of paper or computer screen. The ways that we deal with this distortion give us various types of map projections. Depending on the type of projection used, there may be distortion of distance, direction, shape and/or area. One type of projection may distort distances but correctly maintain directions, whereas another type may distort shape but maintain correct area. The type of information we need from a map determines which type of projection we might use. Below are two common projections among the many that exist. Can you tell what sort of distortion occurs with each projection? 1 Map Locations The latitude-longitude system is the standard system that we use to locate places on the Earth’s surface. The system uses a grid of intersecting east-west (latitude) and north-south (longitude) lines. Any point on Earth can be identified by the intersection of a line of latitude and a line of longitude. Lines of latitude: • also called “parallels” • equator = 0° latitude • increase N and S of the equator • range 0° to 90°N or 90°S Lines of longitude: • also called “meridians” • Prime Meridian = 0° longitude • increase E and W of the P.M. -
Bibliographical Index
Bibliographical Index BIBLIOGRAPHICAL ACCESS TO THIS VOLUME Bacon, Roger. Opus Majus. 305, 322, 345 Basil, Saint. Homilies. 328 Three modes of access to bibliographical information are used Bede, the Venerable. De natura rerum. 137 in this volume: the footnotes; the bibliographies; and the Bib ---. De temporum ratione. 321 liographical Index. The footnotes provide the full form of a reference the first Cassiodorus. Institutiones divinarum et saecularium time it is cited in each chapter with short-title versions in litterarum. 172, 255, 259, 261 subsequent citations. In each of the short-title references, the Cato the Elder. Origines. 205 note number of the fully cited work is given in parentheses. Censorinus. De die natalie 255 The bibliographies following each chapter provide a selec Chaucer, Geoffrey. Prologue to the Canterbury Tales. 387 tive list of major books and articles relevant to its subject Cicero. Arataea (translation of Aratus's versification of matter. Eudoxus's Phaenomena). 143 The Bibliographical Index comprises a complete list, ar ---. Letters to Atticus. 255 ranged alphabetically by author's name, of all works cited in ---. De natura deorum. 160,168 the footnotes. Numbers in bold type indicate the pages on --. The Republic. 159, 160, 255 which references to these works can be found. This index is ---. Tusculan Disputations. 160 divided into two parts. The first part identifies the texts of Cleomedes. De motu circulari. 152, 154, 169 classical and medieval authors. The second part lists the mod Cosmas Indicopleustes. Christian Topography. 143, 144, ern literature. 261 Ctesias of Cnidus. Indica. 149 TEXTS OF CLASSICAL AND MEDIEVAL ---. Persica. 149 AUTHORS Dicuil. -
Topographic Maps Fields
Topographic Maps Fields • Field - any region of space that has some measurable value at every point. • Ex: temperature, air pressure, elevation, wind speed Isolines • Isolines- lines on a map that connect points of equal field value • Isotherms- lines of equal temperature • Isobars- lines of equal air pressure • Contour lines- lines of equal elevation Draw the isolines! (connect points of equal values) Isolines Drawn in Red Isotherm Map Isobar Map Topographic Maps • Topographic map (contour map)- shows the elevation field using contour lines • Elevation - the vertical height above & below sea level Why use sea level as a reference point? Topographic Maps Reading Contour lines Contour interval- the difference in elevation between consecutive contour lines Subtract the difference in value of two nearby contour lines and divide by the number of spaces between the contour lines Elevation – Elevation # spaces between 800- 700 =?? 5 Contour Interval = ??? Rules of Contour Lines • Never intersect, branch or cross • Always close on themselves (making circle) or go off the edge of the map • When crossing a stream, form V’s that point uphill (opposite to water flow) • Concentric circles mean the elevation is increasing toward the top of a hill, unless there are hachures showing a depression • Index contour- thicker, bolder contour lines on contour maps, usually every 5 th line • Benchmark - BMX or X shows where a metal marker is in the ground and labeled with an exact elevation ‘Hills’ & ‘Holes’ A depression on a contour map is shown by contour lines with small marks pointing toward the lowest point of the depression. The first contour line with the depression marks (hachures) and the contour line outside it have the same elevation. -
U.S. Coast Guard Auxiliary Nautical Chart Updating Training Guide
` U.S. Coast Guard Auxiliary Nautical Chart Updating Training Guide National Ocean Service Office of Coast Survey Chart Updating Training Guide Ver. 2.4 2016 1 Table of Contents What is New - 3 Plotting (Chart Sections) - 30 Introduction to Chartplotter and GPS Navigation Software -31 Nautical Charts and Coast Pilot - 4 Using the Raster Navigational Charts Google Objective - 4 Earth Tool – 31 Background - 4 Introduction to NOAA Nautical Discrepancy Projections – 5 Report System – 32 Latitude and Longitude Scales - 6 Nautical Chart Feature Corrections – 32 Scales - 6 Coast Pilot Items – 33 Horizontal Datum – 7 Nautical Features Report – 34 Vertical Datum - 8 Instructions – 35 Depths Used on Nautical Charts- 8 Coast Pilot Report – 38 Traditional Paper Nautical Charts – 8 Instructions – 39 Chart Title and Information Block – 9 Reporting of Particular Feature Types - 41 Color Used on Nautical Charts – 9 NOAA’s Nautical Discrepancy Report System Lettering Styles – 10 – 42 Chart Depths – 10 Create a New Report – 43 Chart Edition – 10 Charting Action – 48 Updated Charts – 11 USACE Chart Discrepancy Reporting System - Nautical Chart Catalogs – 11 49 US Coast Pilot – 12 Chart Update AUXDATA Submittals - 52 US Coast Pilot Updates – 12 Individual’s duty for the patrol - 52 Bearings in the Coast Pilot – 12 Currents in the Coast Pilot – 13 Appendices Introduction to Nautical Chart Updating- 13 1. Responsible/Knowledgeable Sources, Objectives – 13 Reportable Chart Features -53 Background – 13 2. Difference Between RNCs and ENCs, Tools and Equipment useful in Print-on-Demand Paper Charts, PDF Chart Updating -14 Nautical Charts, Chart Updates (LNM Obtaining Information from Knowledgeable and NM Corrections) and Sources - 18 BookletCharts - 67 How to determine if an object is chartable – 18 3. -
Gradual Generalization of Nautical Chart Contours with a B-Spline Snake Method
GRADUAL GENERALIZATION OF NAUTICAL CHART CONTOURS WITH A B-SPLINE SNAKE METHOD BY DANDAN MIAO BS in Geographic Information Systems, Wuhan University, 2009 THESIS Submitted to the University of New Hampshire in Partial Fulfillment of the Requirements for the Degree of Master of Science in Ocean Engineering September, 2014 ALL RIGHTS RESERVED © 2014 Dandan Miao This thesis has been examined and approved. Dr. Brian Calder, Associate Research Professor of Ocean Engineering Dr. Kurt Schwehr Affiliate Associate Professor of Ocean Engineering Dr. Steve Wineberg Lecturer, Mathematics and Statistics Date v ACKNOWLEDGMENTS This study was sponsored by NOAA grant NA10NOS400007, and supported by the Center for Coastal and Ocean Mapping. Professor Larry Mayer introduced me to the world of Ocean Mapping, and taught me new information about geological oceanography; Professor Brian Calder initiated this study and has always been able to selflessly help me with any questions; Professor Steven Wineberg gave me many insights of how to transfer math concepts to graphic behavior; Professor Kurt Schwehr helped me with many intelligent thoughts and suggestion about computer programming implementation. I am grateful for all their selfless help and patience, and I would like to thank all of them for their guidance, encouragement and proof-reading of this thesis: without them and CCOM’s support, this work would not have happened. Finally, I would like to thank my parents and friends, for encouragement and trust. Your love and faith gave me the strength to keep holding on and finally make it work! Love you all! With greatest thankfulness, Dandan Miao vi TABLE OF CONTENTS ACKNOWLEDGMENTS ............................................................................................................. -
Scale NOAA Nautical Chart for Small Boaters When Possible, Use the Full-Size NOAA Chart for Navigation
BookletChart™ Cumberland Head to Four Brothers Islands NOAA Chart 14782 A reduced-scale NOAA nautical chart for small boaters When possible, use the full-size NOAA chart for navigation. Included Area Published by the A special anchorage is on the west side of the lake in Deep Bay. (See 33 CFR 110.1 and 110.8(i), chapter 2, for limits and regulations.) National Oceanic and Atmospheric Administration Channels.–The south 37 miles of Lake Champlain, from Whitehall north National Ocean Service to Crown Point (44°01.8'N., 73°25.8'W.), is a narrow arm. The south 13 Office of Coast Survey miles of this arm, from Whitehall north to Benson Landing, is filled with a marshy flat traversed by a narrow channel of open water. A Federal www.NauticalCharts.NOAA.gov project provides for a 12-foot channel through this reach. In September 888-990-NOAA 2008, the controlling depths in the channel were 2 feet (7½ feet at midchannel) to Benson Landing. Above Benson Landing, natural deep What are Nautical Charts? water is available to Crown Point. The entire narrows, from Whitehall to Crown Point is well marked by lights and buoys. Nautical charts are a fundamental tool of marine navigation. They show North from Crown Point for about 75 miles to Rouses Point, Lake water depths, obstructions, buoys, other aids to navigation, and much Champlain is deep and wide. Prominent points and shoals throughout more. The information is shown in a way that promotes safe and the lake are marked by lights and buoys. efficient navigation. -
Creating a Contour Map of Your School Playground
How to Make a Contour Map of Your School Playground Source: Mountain Environments Novice On-Line Lessons http://www.math.montana.edu/~nmp/materials/ess/mountain_environments/ These instructions are for making a 4 x 4 contour map of a 6' x 6' plot of land. The number of contour intervals or size of the plot may be changed if desired. Step 1: To make a contour map, first stake out with string a plot of uneven land. Step 2: Determine the total change in elevation within your plot, from its highest point to its lowest point, in inches. (To measure this change in elevation you must place one end of a bubble stick level at the high point with the other end pointing towards the low point. Raise or lower the free end of the bubble stick until the bubble shows the stick is level.) With the yardstick, measure the vertical distance from the free end of the bubble stick to the ground. Continue measuring in this manner until you reach the low point and add up all of the vertical measurements that you took at the various points. This is your total change in elevation. Step 3: Divide this elevation change by 4 to determine the contour interval when you build 3 contour lines. (Suppose the change in elevation was 24 inches from high point to low point. If 3 contour lines are needed between the high and low point, you'd divide the 24" by 4—not 3. The contour interval would be 6 inches. ) Step 4: Now that you have a contour interval, you must locate one point for each contour line that will be the starting point for that line. -
Cartographic and Geospatial Materials
LIBRARY OF CONGRESS COLLECTIONS POLICY STATEMENTS ±² Collections Policy Statement Index Cartographic and Geospatial Materials This document consolidates and replaces the former Maps, Atlases, and Remote Sensing Images Collections Policy Statement and Digital Geographic Data Collections Policy Statement Contents I. Scope II. Research Strengths III. Collecting Policy IV. Acquisitions Sources: Current and Future V. Collecting Levels: (Class G1000-G9980) I. Scope This Collections Policy Statement deals with analog geospatial resources presented graphically in the form of maps1, atlases, globes, charts (aeronautical and hydrographic), three-dimensional models, and aerial photography and remote sensing images; and digital geospatial data2 or spatially referenced data in the form of vector and raster representations, relational databases that incorporate common geographic features as attributes, remotely sensed digital imagery, software for the creation, retrieval, analysis and display of geospatial data, and web sites. For treatment of cartography as a subject, see the Geography and Cartography Collections Policy Statement. The majority of the Library's cartographic and geospatial materials (Library of Congress Classification Schedule G1000-G9980) is housed in the Geography and Map Division. Analog cartographic materials often complement or supplement textual works and may appear in the Library's other format or subject collection areas. In an evolving information society, cartographic representations of geographic data and geo-referenced content -
Latitude-Longitude and Topographic Maps Reading Supplement
Latitude-Longitude and Topographic Maps Reading Supplement Latitude and Longitude A key geographical question throughout the human experience has been, "Where am I?" In classical Greece and China, attempts were made to create logical grid systems of the world to answer this question. The ancient Greek geographer Ptolemy created a grid system and listed the coordinates for places throughout the known world in his book Geography. But it wasn't until the middle ages that the latitude and longitude system was developed and implemented. This system is written in degrees, using the symbol °. Latitude When looking at a map, latitude lines run horizontally. Latitude lines are also known as parallels since they are parallel and are an equal distant from each other. Each degree of latitude is approximately 69 miles (111 km) apart; there is a variation due to the fact that the earth is not a perfect sphere but an oblate ellipsoid (slightly egg-shaped). To remember latitude, imagine them as the horizontal rungs of a ladder ("ladder-tude"). Degrees latitude are numbered from 0° to 90° north and south. Zero degrees is the equator, the imaginary line which divides our planet into the northern and southern hemispheres. 90° north is the North Pole and 90° south is the South Pole. Longitude The vertical longitude lines are also known as meridians. They converge at the poles and are widest at the equator (about 69 miles or 111 km apart). Zero degrees longitude is located at Greenwich, England (0°). The degrees continue 180° east and 180° west where they meet and form the International Date Line in the Pacific Ocean. -
Arnaud-Geography2014.Pdf
CHAPTER 3 ANCIENT MARINERS BETWEEN EXPERIENCE AND COMMON SENSE GEOGRAPHY Pascal Arnaud Université Lyon 2 Abstract Although no first-hand information from ancient mariners have been preserved, their legacy to classical Greek geography has been so important that it is still pos- sible to recognise the structural impact of the material gathered from their implicit knowledge upon the patterns of presentation of space. The kind of tacit knowledge they had acquired appears very similar to that of the later Micronesians, studied by Hutchins. It was based upon durations rather than distances, and upon an original perception of orientations and directions. Thanks to that knowledge, based upon the repetition of experience through generations and apprenticeship, they were able to sail the blue sea without maps or instruments. This paper will address the issue whether – or within which limits – the mental construction of limited linear sec- tions of space may have opened the way to the construction of some coherent pre- sentation of space, a mental map in the fullest sense. In a well-known paragraph, Strabo1 establishes the direction and length of the passage between Rhodes and Alexandria and balances Eratosthenes’ calculations with ancient mariners’ experience: “The passage between Rhodes and Alexandria by north wind is about 4000 stadia; sailing along the coasts is twice this distance. Eratosthenes says that, this distance is the mere mariners’ conjecture of some, while others avow distinctly that it amounts to 5000 stadia; he himself, from observations of the shadows indicated by the gnomon, calculates it at 3750.” ‘Mariners’ were often scorned by ancient writers, when they were authors of travel narratives, but used to be considered as a main piece of evidence, when they were ano- nymous and a consensus came into being from a long-lasting verified experience of 1 2.5.24, C 168–169 = Erat.