{"id":105,"date":"2020-02-04T20:05:45","date_gmt":"2020-02-05T01:05:45","guid":{"rendered":"https:\/\/pressbooks.bccampus.ca\/earthsystems\/?post_type=chapter&p=105"},"modified":"2020-09-14T16:06:45","modified_gmt":"2020-09-14T20:06:45","slug":"chapter-2","status":"publish","type":"chapter","link":"https:\/\/pressbooks.bccampus.ca\/earthsystems\/chapter\/chapter-2\/","title":{"raw":"Chapter 2","rendered":"Chapter 2"},"content":{"raw":"

Topic 2 \u2013 Location, Location, Location<\/strong><\/span><\/p>\r\nAs a subject, Geography is sometimes briefly explained as: what is where, and why. The where is an important component of this question and geographers have several key ways to communicate location in 3-dimensional space. This is an introduction to location and how we represent location on maps.\r\n\r\n[caption id=\"attachment_66\" align=\"alignleft\" width=\"300\"]\"Looking How did an Egyptian well and camels help an ancient geographer discover the circumference of the Earth and lay the foundation for Earth measurement? Find out more here: https:\/\/www.youtube.com\/watch?v=8hZl3arO7SY<\/a>[\/caption]\r\n\r\nLocation is generally communicated using \u2018coordinate systems\u2019. These systems allow us to measure the relative location of anything in reference to an agreed\u00a0 datum (or point of origin). Globally, the most commonly used coordinate system is the \u2018[pb_glossary id=\"222\"]geographic coordinate[\/pb_glossary]<\/strong>\u2019 system based on [pb_glossary id=\"223\"]latitude[\/pb_glossary]<\/strong> and [pb_glossary id=\"224\"]longitude[\/pb_glossary]<\/strong> lines that encircle the globe. These intersecting grid lines at the surface of the Earth are measured from a specific point of origin. The equator is one such line, and represents the zero point for lines of Latitude<\/em>. Circling the globe, it is defined by the edge of a plane that bisects the Earth, perpendicular to its axis of rotation. All other lines of latitude run east\/west, parallel to the equator, increasing in value north or south, towards the poles. Lines of Longitude<\/em> (meridians) encircle the globe from north to south, increasing from zero at the Prime Meridian. Therefore the datum, or origin, for geographic coordinates are the Equator (0\u00b0 latitude), and the Prime Meridian (0\u00b0 longitude). Note:<\/em> because all lines of longitude are perpendicular to the equator, they converge on the spherical surface of the Earth at the exact point where the axis of rotation intersects the Earth\u2019s surface, creating the north and south geographic poles<\/strong>. There is a unique value for latitude north or south of the equator and longitude east or west of the Prime Meridian for each location on Earth.\r\n\r\n[caption id=\"attachment_67\" align=\"alignright\" width=\"289\"]\"a Line of longitude and the equator distributed across the surface of the Earth.[\/caption]\r\n\r\nGeographic coordinates are particularly useful at the global scale because they successfully deal with the Earth as an approximate sphere and not as a flat surface. Latitude, for example, is defined as the angle given by a line drawn from the Equator to the centre of the Earth and back to the Earth\u2019s surface for your location. So these coordinates are really angle measurements, and their unit of measurement is degrees. While they do well to measure location on a spherical surface, degrees are not that intuitive for making other geospatial measurements, such as distance. As a result, other coordinate systems have been suggested.\r\n

What happens when you flatten a spherical globe onto a flat map?<\/strong><\/h6>\r\nIn order to flatten out the Earth, a number of distortions are necessary. Flat paper maps at the global scale have significant distortion, either in shape, distance, angle or direction. The process of moving from a spherical globe to a flat paper map is called map projection. There are a multitude of \u00a0ways to project a spherical globe onto a flat surface, and the choice of projection is largely based on the needs of the mapmaker, and what type of distortion they are trying to minimize.\r\n\r\n[caption id=\"attachment_68\" align=\"aligncenter\" width=\"508\"]\"Map Example of a map projection from a spherical to a flat surface. Notice how the length of the line changes from the spherical surface to the flat paper map, illustrating distortion in distance.[\/caption]\r\n\r\nFor maps of the entire world, the spherical shape of the Earth is significant, however when a map is focused on just a small part of the world, the curved surface is less apparent. The area of the Earth represented on a given map surface is referred to as map scale. Simply defined, map scale = distance on the map\/\u00a0distance on the Earth. World maps are generally low in detail, as they have to cover a large area and are referred to as [pb_glossary id=\"225\"]small-scale[\/pb_glossary]<\/em><\/strong> maps. As the mapmaker focuses on smaller areas, more detail can be added, increasing the scale at which individual features are represented, we \u00a0call local maps that represent the Earths surface in high detail [pb_glossary id=\"226\"]large-scale[\/pb_glossary]<\/em> <\/strong>maps.\r\n\r\nWhen dealing with large-scale local maps, distortion from Earth\u2019s curvature is minimized and so we can apply other coordinate systems, such as those based on cartesian grid coordinates with an x and y value, applied on a flat (non-spherical) surface. The most common grid system applied to local maps is the Universal Tranverse Mercator (UTM) system. This system measures in metres from a specific origin (datum) point. For an in-depth explanation of the UTM system see here<\/a>\u00a0:\u00a0 Note<\/em>: keep in mind that because the lines on a grid coordinate map do not converge at the top of the map (like on a sphere), Grid North (the top of the map) is different than geographic north. Furthermore, the magnetic north pole is not perfectly aligned with either of these north\u2019s. Therefore on any given map there may be up to three different definitions of north<\/em> you should be aware of.","rendered":"

Topic 2 \u2013 Location, Location, Location<\/strong><\/span><\/p>\n

As a subject, Geography is sometimes briefly explained as: what is where, and why. The where is an important component of this question and geographers have several key ways to communicate location in 3-dimensional space. This is an introduction to location and how we represent location on maps.<\/p>\n

\"Looking
How did an Egyptian well and camels help an ancient geographer discover the circumference of the Earth and lay the foundation for Earth measurement? Find out more here: https:\/\/www.youtube.com\/watch?v=8hZl3arO7SY<\/a><\/figcaption><\/figure>\n

Location is generally communicated using \u2018coordinate systems\u2019. These systems allow us to measure the relative location of anything in reference to an agreed\u00a0 datum (or point of origin). Globally, the most commonly used coordinate system is the \u2018geographic coordinate<\/a><\/strong>\u2019 system based on latitude<\/a><\/strong> and longitude<\/a><\/strong> lines that encircle the globe. These intersecting grid lines at the surface of the Earth are measured from a specific point of origin. The equator is one such line, and represents the zero point for lines of Latitude<\/em>. Circling the globe, it is defined by the edge of a plane that bisects the Earth, perpendicular to its axis of rotation. All other lines of latitude run east\/west, parallel to the equator, increasing in value north or south, towards the poles. Lines of Longitude<\/em> (meridians) encircle the globe from north to south, increasing from zero at the Prime Meridian. Therefore the datum, or origin, for geographic coordinates are the Equator (0\u00b0 latitude), and the Prime Meridian (0\u00b0 longitude). Note:<\/em> because all lines of longitude are perpendicular to the equator, they converge on the spherical surface of the Earth at the exact point where the axis of rotation intersects the Earth\u2019s surface, creating the north and south geographic poles<\/strong>. There is a unique value for latitude north or south of the equator and longitude east or west of the Prime Meridian for each location on Earth.<\/p>\n

\"a
Line of longitude and the equator distributed across the surface of the Earth.<\/figcaption><\/figure>\n

Geographic coordinates are particularly useful at the global scale because they successfully deal with the Earth as an approximate sphere and not as a flat surface. Latitude, for example, is defined as the angle given by a line drawn from the Equator to the centre of the Earth and back to the Earth\u2019s surface for your location. So these coordinates are really angle measurements, and their unit of measurement is degrees. While they do well to measure location on a spherical surface, degrees are not that intuitive for making other geospatial measurements, such as distance. As a result, other coordinate systems have been suggested.<\/p>\n

What happens when you flatten a spherical globe onto a flat map?<\/strong><\/h6>\n

In order to flatten out the Earth, a number of distortions are necessary. Flat paper maps at the global scale have significant distortion, either in shape, distance, angle or direction. The process of moving from a spherical globe to a flat paper map is called map projection. There are a multitude of \u00a0ways to project a spherical globe onto a flat surface, and the choice of projection is largely based on the needs of the mapmaker, and what type of distortion they are trying to minimize.<\/p>\n

\"Map
Example of a map projection from a spherical to a flat surface. Notice how the length of the line changes from the spherical surface to the flat paper map, illustrating distortion in distance.<\/figcaption><\/figure>\n

For maps of the entire world, the spherical shape of the Earth is significant, however when a map is focused on just a small part of the world, the curved surface is less apparent. The area of the Earth represented on a given map surface is referred to as map scale. Simply defined, map scale = distance on the map\/\u00a0distance on the Earth. World maps are generally low in detail, as they have to cover a large area and are referred to as small-scale<\/a><\/em><\/strong> maps. As the mapmaker focuses on smaller areas, more detail can be added, increasing the scale at which individual features are represented, we \u00a0call local maps that represent the Earths surface in high detail large-scale<\/a><\/em> <\/strong>maps.<\/p>\n

When dealing with large-scale local maps, distortion from Earth\u2019s curvature is minimized and so we can apply other coordinate systems, such as those based on cartesian grid coordinates with an x and y value, applied on a flat (non-spherical) surface. The most common grid system applied to local maps is the Universal Tranverse Mercator (UTM) system. This system measures in metres from a specific origin (datum) point. For an in-depth explanation of the UTM system see here<\/a>\u00a0:\u00a0 Note<\/em>: keep in mind that because the lines on a grid coordinate map do not converge at the top of the map (like on a sphere), Grid North (the top of the map) is different than geographic north. Furthermore, the magnetic north pole is not perfectly aligned with either of these north\u2019s. Therefore on any given map there may be up to three different definitions of north<\/em> you should be aware of.<\/p>\n

definition<\/span>