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Question
review questions
- how was tom basss short map an application of gis principles?
- explain why a map is simply a model of part of the earths surface.
- discuss the differences between large - scale and small - scale maps.
- how are map grid lines like landmarks? how are they different?
- which grid lines on a standard map are the vertical lines? which are the horizontal lines?
- before modern navigation methods, such as gps, how did sailors find their longitude?
- list three features on a standard map that help you use it better.
- why is a map projection needed?
- what are the advantages of plane, cylindrical, and conic projection surfaces in cartography?
- what kind of projection would show the continent of antarctica with the least amount of distortion?
- what are three types of standard maps? which would likely show glaciers and lakes?
- why are thematic maps useful?
- name the three main parts of a geographic information system (gis).
- give an example of an earth feature that could be represented by each of the gis data types.
- what is the most efficient way to collect gis data over large areas?
Brief Explanations
- A map is a model of part of the Earth's surface as it represents real - world features in a simplified way.
- Large - scale maps show a smaller area in more detail; small - scale maps show a larger area with less detail.
- Maps represent real - world features like landmarks through symbols.
- On a standard map, the vertical lines are the lines of longitude.
- Before GPS, sailors used celestial navigation (observing stars, sun, moon) to find latitude.
- Features on a standard map like scale, legend, and compass rose help in using it better.
- Map projection is needed to represent the curved surface of the Earth on a flat map.
- Plane projections are good for small areas, cylindrical projections preserve shapes well for mid - latitudes, and conic projections are useful for regions with an east - west extent.
- A polar projection would show Antarctica with the least distortion as it is centered around the poles.
- Three types of standard maps are political, physical, and topographic. Physical maps would likely show glaciers and lakes.
- Thematic maps are useful as they focus on a specific theme like population, climate, etc.
- The three main parts of a GIS are data input, data storage and management, and data output and analysis.
- For example, a river could be represented as a line in vector GIS data; a forest area could be represented as a polygon.
- Remote sensing (using satellites or aircraft) is an efficient way to collect GIS data over large areas.
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- A map is a simplified model of part of the Earth's surface.
- Large - scale maps show less area in more detail; small - scale maps show more area in less detail.
- Maps represent real - world features like landmarks using symbols.
- The vertical lines on a standard map are lines of longitude.
- Before GPS, sailors used celestial navigation to find latitude.
- Scale, legend, and compass rose are features on a standard map that help in using it better.
- Map projection is needed to represent the curved Earth on a flat surface.
- Plane projections are good for small areas, cylindrical for mid - latitudes, and conic for east - west regions.
- A polar projection would show Antarctica with least distortion.
- Political, physical, and topographic are three types of standard maps. Physical maps would show glaciers and lakes.
- Thematic maps focus on a specific theme, so they are useful.
- Data input, data storage and management, data output and analysis are the main parts of a GIS.
- A river (line) and a forest (polygon) are examples of Earth features for GIS data types.
- Remote sensing is the most efficient way to collect GIS data over large areas.