PPT-Topographic Map Skills

Author : jane-oiler | Published Date : 2017-11-07

Topographic notes Topographic Mapincludes contour lines drawn to represent changes in elevation Topographic maps take 3 dimensional ups and downs of the terrain

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Topographic Map Skills: Transcript


Topographic notes Topographic Mapincludes contour lines drawn to represent changes in elevation Topographic maps take 3 dimensional ups and downs of the terrain and show them on 2 dimensional surface. Lidar-Derived DEMs. Stereo DTM. (Topographic Surface). R. eference image of the traditional stereo-compiled DTM. Built from Masspoints and Breaklines . Much coarser resolution than lidar. Demonstrates the familiar and usually expected character of a topographic DEM. Mon: 11:30 AM to 12:30 PM & 1:45 PM to 3:00 PM. Wed: 11:30 . A. M to 12:30 PM. Thr. : 9:15 AM to 12:30 PM. Fri: 10:00 AM to 12:00 . P. M. Lesson . 9. Topographic Profiles. Hess, . McKnight’s Physical Geography. Techniques in Active Tectonic Study. Juni 20-Juli 2, 2013. Instruktur: Prof. J Ramon Arrowsmith (JRA). Dari Arizona State University (ASU) - US. Tempat Pelaksanaan: . Ruang Pangea, Laboratorium Gempabumi (LabEarth) – Puslit Geoteknologi LIPI dan Kuliah lapangan akan dilakukan disekitar Sesar Lembang, Jawa Barat.. Topographic Maps. Contouring. Topographic contours indicating surface relief. Image taken from US Army training manual.. Solid yellow lines represent surface isobars, line of equal air pressure. Green dashed lines are geopotential heights, the altitude at which 500 millibars of air pressure are attained. These types of contour maps are used by meteorologists. The weather system shown is the Storm of the Century, a powerful winter storm called a nor’easter.. Match your cards.. Take notes in your science notebook.. Label your map.. Map Notes. topography. The study…. The study of the shapes and features of the Earth’s surface.. Topography. Shows the three dimensional shape and elevations of an area of land in two dimensions. Mapping Mechanics: . An introduction to topography . by the use of contour lines . Upon completion of this lesson, students will be able to:. define topography. define the USGS and different techniques used to study topography. Aim: To be able to interpret a topographic Map.. What is a Topographic Map?. A topographic map. shows surface features,. or topography, of the . Earth. . Topography can be natural or human-made. the following. :. Match your . cards.. Take notes in your science . notebook.. Label your . map.. Map Notes. topography. The study…. The . study of the shapes and features of the Earth’s surface.. Presented by: Eric Gamble. Eric Gamble, Randel Tom Cox. ,. . Daniel Larsen, and Cody Wallace. Presentation. Goals and Background. Previous Research. Methods. Discussion. Summary. Terraces of the Saline and Ouachita River Valleys. 25193028192030321and then create a topographic map of it14302922230282612922152812914127bMapmakers have devised an ingenious way to show three150dimensional topographysurface with the use of a topogra Yonathan Admassu, PhD. James Madison . University. Who are?. Geotechnical Engineers. Designing earth structures consistent with data. Direct projects. BS in civil engineering. Engineering Geologists. Example: Hills. Mapping Earth. Topography. :. The shape of the land.. K2, Pakistan. Napa Valley, California. Grand Canyon, Arizona. Important Vocabulary. Topographic Maps:. . Represent the shape of the land on a flat piece of paper using contour lines. a ridge. a valley. g. oing uphill. closer . contours. = steeper slope. contours farther apart = shallower slope. Imagine that the red line represents a geologic contact of some sort. Given that it doesn’t parallel contours we know it isn’t horizontal, and given that it doesn’t cut straight across contours we know it isn’t vertical. Can we tell something about its orientation? . How to read a map. Maps . are pictures of the Earth's . surface. Reference maps . just . show natural features like rivers, cities, political subdivisions and highways. .. Thematic maps . use these items only .

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