Map Features PPT
... Capricorn on the south is known as the "tropics." This area does not experience seasons because the sun is always high in the sky. Only higher latitudes, north of the Tropic of Cancer and south of the Tropic of Capricorn, experience significant seasonal variation in climate. ...
... Capricorn on the south is known as the "tropics." This area does not experience seasons because the sun is always high in the sky. Only higher latitudes, north of the Tropic of Cancer and south of the Tropic of Capricorn, experience significant seasonal variation in climate. ...
Geography Handbook - Your History Site
... Maps have lines of latitude and longitude that form a grid. Lines of latitude circle the earth, either north or south of the Equator (0° latitude). Lines of longitude stretch from the North Pole to the South Pole, either east or west of the Prime Meridian (0° longitude). The distance between the lin ...
... Maps have lines of latitude and longitude that form a grid. Lines of latitude circle the earth, either north or south of the Equator (0° latitude). Lines of longitude stretch from the North Pole to the South Pole, either east or west of the Prime Meridian (0° longitude). The distance between the lin ...
geo2200_1midterm_stu..
... Latitude increases from the equator to the north pole or south pole o These are the two fixed reference points for the Earth Is strongly related to yearly patterns, like sunlight and seasons Lines are called parallels Longitude – measure of (angular) distance east or west of a point on the Earth ...
... Latitude increases from the equator to the north pole or south pole o These are the two fixed reference points for the Earth Is strongly related to yearly patterns, like sunlight and seasons Lines are called parallels Longitude – measure of (angular) distance east or west of a point on the Earth ...
Unit I - Maps
... reality is a bumpy oblate spheroid or geoid, onto a 2D surface. 3D shapes can never truly be 2D All flat maps have some distortion in their representation of distance, shape, area, or direction. ...
... reality is a bumpy oblate spheroid or geoid, onto a 2D surface. 3D shapes can never truly be 2D All flat maps have some distortion in their representation of distance, shape, area, or direction. ...
5 Themes of Geography
... When we discuss location we are talking about a specific position or point in physical space. Walkertown Middle School is on Ruxton Drive. There are two types of location Absolute and Relative. ...
... When we discuss location we are talking about a specific position or point in physical space. Walkertown Middle School is on Ruxton Drive. There are two types of location Absolute and Relative. ...
the geographical perspective
... the equator to the poles. Meridians at the equator are spaced the same as parallels Meridians at 60° (N or S) are half as far apart as parallels. Parallels and meridians cross each other at right angles The area of the surface bounded by any two parallels and two meridians (a given distance apart) i ...
... the equator to the poles. Meridians at the equator are spaced the same as parallels Meridians at 60° (N or S) are half as far apart as parallels. Parallels and meridians cross each other at right angles The area of the surface bounded by any two parallels and two meridians (a given distance apart) i ...
5 Themes of Geography
... projection map, on the left, shows real sizes and shapes of continents. The equal area map , below left, shows size accurately. The Peters projection, below, shows land and oceans areas and correct directions ...
... projection map, on the left, shows real sizes and shapes of continents. The equal area map , below left, shows size accurately. The Peters projection, below, shows land and oceans areas and correct directions ...
Chapter 2
... Sextants are mechanical devices that operate without relying on any power source (other than that provided by the human operator). A batterypowered GPS unit could fail (imagine that if you were lost in a remote area). Further, a sextant provides a good demonstration of relationships between Earth an ...
... Sextants are mechanical devices that operate without relying on any power source (other than that provided by the human operator). A batterypowered GPS unit could fail (imagine that if you were lost in a remote area). Further, a sextant provides a good demonstration of relationships between Earth an ...
5 Geography Themes - Parma City School District
... • A compass rose is a model of a compass. It tells the cardinal directions, which are north, south, east, and west. Scale • The scale on a map tells you the relative distance on the map to the real world. For example, a map’s scale may tell you that one inch on the map equals one mile in the real wo ...
... • A compass rose is a model of a compass. It tells the cardinal directions, which are north, south, east, and west. Scale • The scale on a map tells you the relative distance on the map to the real world. For example, a map’s scale may tell you that one inch on the map equals one mile in the real wo ...
National Geographic Geography Handbook
... Globes accurately represent distance and direction. A map is a flat drawing of all or part of the earth’s surface. Unlike globes, maps can show small areas in great detail. Maps can also display political boundaries, population densities, or even voting ...
... Globes accurately represent distance and direction. A map is a flat drawing of all or part of the earth’s surface. Unlike globes, maps can show small areas in great detail. Maps can also display political boundaries, population densities, or even voting ...
National Geographic Geography Handbook
... south. It helps divide the earth into half spheres in the other direction. Find this line— called the Prime Meridian on a globe. Everything east of the Prime Meridian for 180 degrees is in the Eastern Hemisphere. Everything west of the Prime Meridian is in the Western Hemisphere. ...
... south. It helps divide the earth into half spheres in the other direction. Find this line— called the Prime Meridian on a globe. Everything east of the Prime Meridian for 180 degrees is in the Eastern Hemisphere. Everything west of the Prime Meridian is in the Western Hemisphere. ...
geogch01
... • degree- a unit of measure used to determine absolute location; on globes and maps, latitude and longitude are measured in degrees • equator- an imaginary line that circles the globe at its widest point (halfway between the North and South poles), dividing the Earth into two halves called hemispher ...
... • degree- a unit of measure used to determine absolute location; on globes and maps, latitude and longitude are measured in degrees • equator- an imaginary line that circles the globe at its widest point (halfway between the North and South poles), dividing the Earth into two halves called hemispher ...
Geolocating - Baylor School Moodle
... Using the pole as a point and the Prime Meridian as a base, all other meridians are place at 1° angle intervals to the East AND West of the Prime Meridian. Meridians run 0° to 180° West of the PM (towards the US) and 0° to 180° East of the Pm towards China. There is a single line of 180° longitude, ...
... Using the pole as a point and the Prime Meridian as a base, all other meridians are place at 1° angle intervals to the East AND West of the Prime Meridian. Meridians run 0° to 180° West of the PM (towards the US) and 0° to 180° East of the Pm towards China. There is a single line of 180° longitude, ...
Geolocating:
... Using the pole as a point and the Prime Meridian as a base, all other meridians are place at 1° angle intervals to the East AND West of the Prime Meridian. Meridians run 0° to 180° West of the PM (towards the US) and 0° to 180° East of the Pm towards China. There is a single line of 180° longitude, ...
... Using the pole as a point and the Prime Meridian as a base, all other meridians are place at 1° angle intervals to the East AND West of the Prime Meridian. Meridians run 0° to 180° West of the PM (towards the US) and 0° to 180° East of the Pm towards China. There is a single line of 180° longitude, ...
Equal Area World Maps: A Case Study
... Geological Survey. In this article, we will examine the step-by-step construction of another equal area map known as the Mollweide projection. First announced in 1805 by Karl Brandan Mollweide (1774–1825) and commonly used in atlases today, this map projection represents the whole world in an ellips ...
... Geological Survey. In this article, we will examine the step-by-step construction of another equal area map known as the Mollweide projection. First announced in 1805 by Karl Brandan Mollweide (1774–1825) and commonly used in atlases today, this map projection represents the whole world in an ellips ...
Thinking Geographically An Introduction to An
... One of the biggest cultural modifiers is globalization. Globalization includes all of the beliefs, material goods, and trends that aim to become global and mask the local customs that tend to define homogonous areas. Some people are very excepting to globalization and believe it is necessary to proc ...
... One of the biggest cultural modifiers is globalization. Globalization includes all of the beliefs, material goods, and trends that aim to become global and mask the local customs that tend to define homogonous areas. Some people are very excepting to globalization and believe it is necessary to proc ...
Geography Handbook - Boone County Schools
... because they represent the shortest distances from one city to another. The idea of a great circle shows one important difference between a globe and a map. Because a globe is round, it accurately shows great circles. On a flat map, however, the great circle route between two points may not appear t ...
... because they represent the shortest distances from one city to another. The idea of a great circle shows one important difference between a globe and a map. Because a globe is round, it accurately shows great circles. On a flat map, however, the great circle route between two points may not appear t ...
Geography - Bingham`s Place
... or parallels, circle the earth parallel to the Equator and measure the distance north or south of the Equator in degrees. The Equator is measured at 0° latitude, while the Poles lie at latitudes 90° N (north) and 90° S (south). Parallels north of the Equator are called north latitude, and parallels ...
... or parallels, circle the earth parallel to the Equator and measure the distance north or south of the Equator in degrees. The Equator is measured at 0° latitude, while the Poles lie at latitudes 90° N (north) and 90° S (south). Parallels north of the Equator are called north latitude, and parallels ...
WorldGeo_U5_C1_L1_p0..
... widening and has an average depth of 11,700 feet. The Atlantic Ocean is bordered by Europe and Africa on the east and by North America and South America on the west. The Indian Ocean is the third largest ocean and covers an area of about 28.3 million square miles or 73.3 billion square kilometers. A ...
... widening and has an average depth of 11,700 feet. The Atlantic Ocean is bordered by Europe and Africa on the east and by North America and South America on the west. The Indian Ocean is the third largest ocean and covers an area of about 28.3 million square miles or 73.3 billion square kilometers. A ...
5 Themes of Geography
... street address (local location). – Paris France is 48o North Latitude and 2o East Longitude. – The White House is located at 1600 Pennsylvania Ave. ...
... street address (local location). – Paris France is 48o North Latitude and 2o East Longitude. – The White House is located at 1600 Pennsylvania Ave. ...
FREE Sample Here
... Persons traveling west across the International Date Line must ____. a. turn their calendar back one day b. turn their calendar ahead one day c. turn their watch 12 hours ahead d. turn their watch 12 hours back ...
... Persons traveling west across the International Date Line must ____. a. turn their calendar back one day b. turn their calendar ahead one day c. turn their watch 12 hours ahead d. turn their watch 12 hours back ...
Latitude
In geography, latitude (φ) is a geographic coordinate that specifies the north-south position of a point on the Earth's surface. Latitude is an angle (defined below) which ranges from 0° at the Equator to 90° (North or South) at the poles. Lines of constant latitude, or parallels, run east-west as circles parallel to the equator. Latitude is used together with longitude to specify the precise location of features on the surface of the Earth. Two levels of abstraction are employed in the definition of these coordinates. In the first step the physical surface is modelled by the geoid, a surface which approximates the mean sea level over the oceans and its continuation under the land masses. The second step is to approximate the geoid by a mathematically simpler reference surface. The simplest choice for the reference surface is a sphere, but the geoid is more accurately modelled by an ellipsoid. The definitions of latitude and longitude on such reference surfaces are detailed in the following sections. Lines of constant latitude and longitude together constitute a graticule on the reference surface. The latitude of a point on the actual surface is that of the corresponding point on the reference surface, the correspondence being along the normal to the reference surface which passes through the point on the physical surface. Latitude and longitude together with some specification of height constitute a geographic coordinate system as defined in the specification of the ISO 19111 standard.Since there are many different reference ellipsoids the latitude of a feature on the surface is not unique: this is stressed in the ISO standard which states that ""without the full specification of the coordinate reference system, coordinates (that is latitude and longitude) are ambiguous at best and meaningless at worst"". This is of great importance in accurate applications, such as GPS, but in common usage, where high accuracy is not required, the reference ellipsoid is not usually stated.In English texts the latitude angle, defined below, is usually denoted by the Greek lower-case letter phi (φ or ɸ). It is measured in degrees, minutes and seconds or decimal degrees, north or south of the equator. Measurement of latitude requires an understanding of the gravitational field of the Earth, either for setting up theodolites or for determination of GPS satellite orbits. The study of the figure of the Earth together with its gravitational field is the science of geodesy. These topics are not discussed in this article. (See for example the textbooks by Torge and Hofmann-Wellenhof and Moritz.)This article relates to coordinate systems for the Earth: it may be extended to cover the Moon, planets and other celestial objects by a simple change of nomenclature.The following lists are available: List of cities by latitude List of countries by latitude