no
the angkle of projection is an angle and the projection
Parallel projection does not produces realistic views whereas perspective projection produces realistic viewin parallel projection lines of projection are parallel whereas in perspective projection lines are not parallel and the point where these lines meets is called ceter of projection in case of perspective projection
Rectangle area = (rectangle width) x (rectangle height)
Isometric projection is another way of saying 3D. With isometric projection things are drawn on a two dimensional surface to show how they would look in 3D.
A = lw Area of a rectangle = length times width
a gnomonic map makes countries look longer, distorted, and hard to understand
Compare: Both Mercator and Gnomonic projections are commonly used for nautical purposes, such as routes for ships to take.Contrast: Gnomonic projections usually display a small area of the Earth, whereas a Mercator projection displays the entire Earth, but with distortions at the poles.
a parallel is two line that never cross each other
Land masses are distorted towards the edges of a gnomonic projection, with the distortion increasing as you move away from the center point. The distortion is most noticeable at the outer edges of the map, particularly near the poles.
A map projection that is used for sea travel includes the gnomonic projection. This was most often used to find the shortest routes between points on a sphere.
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Advantages: pinpoint accuracy, air traffic, and the only way to get the north and south pole. Disadvantages: Makes countries look longer, distorted, and hard to understand.
The Mercator projection is commonly used for navigation and general-purpose world maps due to its ability to accurately represent directions. The Gnomonic projection, on the other hand, is often used for navigational purposes like plotting great circle routes or representing shortest paths between two points on a globe.
jk lol
The type of projection formed by placing a sheet of paper so that it touches the globe at only one point is called an azimuthal projection. This projection preserves direction accurately from the central point of contact, making it useful for navigational purposes. Examples include the polar azimuthal and gnomonic projections.
A Mercator projection map is the most familiar and common to usage in primary education systems. Mercator projections model the continents and oceans into a flattened and rolled cylindrical format. In comparison a Gnomonic projection is also two dimensional and flat but it uses lines which are actual representation of point-to-point s indicating true distance. Another significant difference is scale as Mercator's can represent the entire earth whereas Gnomonics represent a geographical limited area. Lastly Mercator's have the difference of distortion and under representing the actual sizes of Greenland and Continental Africa.