Latitude is measured on a map or globe in degrees, with the equator being 0 degrees and the North and South Poles being 90 degrees north and south, respectively.
Some weaknesses of using a globe as a model of the Earth include its limited portability compared to flat maps, distortion of land masses near the poles, and difficulty in accurately representing the true size of continents and oceans. Additionally, globes can be bulky and less convenient for detailed or large-scale analysis.
The most accurate way to show Earth's continents is using a map projection that minimizes distortions, such as the Winkel Tripel projection or the Robinson projection. These projections aim to balance shape, area, distance, and direction, providing a more accurate representation of the continents compared to other types of projections.
A Map, in one one of these different types of projections: Mercator, Gnomonic, and Polyconic. Mercator - Shows the whole world except for the poles. Gnomonic - A circle projection showing, most often, the poles but sometimes other small places of the earth. Polyconic - Made as if a cone of paper had been wrapped around the earth, often used for places in the middle latitudes, such as the United States.
The best way to explore the Great Dividing Range mountains on a map is to use a detailed topographic map that shows the elevation and terrain features of the range. Look for specific trails, peaks, and landmarks to plan your route and get a better understanding of the geography of the area.
Longitude on Earth is measured in degrees east or west of the Prime Meridian, which is the imaginary line that runs from the North Pole to the South Pole through Greenwich, England.
Look for a colored line that goes straight north-south from the North Pole to the South Pole - latitudes. Longitudes are evenly spaced all the way around a globe. They will be equally spaced. The big one at the middle of the globe is the Equator. They have numbers on them. They start at 0 on the Equator.
A map projection drawn in such a way that an area on the map is proportional to the area on the globe is called an equal-area projection map.
Lines of latitude on a polar projection map radiate outward from the center towards the edges of the map. On a polar projection map, the North Pole is typically at the center, while lines of latitude move southward towards the map edges.
You would use map instead of a globe because on a globe you would barley see south Jersey.But if you use a map you would be able to find even EHT.
You would use map instead of a globe because on a globe you would barley see south Jersey.But if you use a map you would be able to find even EHT.
The lines don't measure anything, any more than the marks on a ruler do any measuring for you. Latitude is an angle on the Earth's surface. It's the angle, measured north or south, from the equator to whatever location you want to talk about. On a map or globe, there may be some lines printed along the way, to help estimate the angle.
There is no standard set of "lines". They may be printed at different intervals on different maps and globes. We have no way of knowing what the interval is on the map or globe that you're looking at, and it may be different on the next one you see.
If you mark a dot on the globe at every place that has the same latitude, the dots form a line all the way around the Earth. That line is sometimes called a 'parallel' of latitude.
The lines don't measure anything, any more than the marks on a ruler do any measuring for you. Latitude is an angle on the Earth's surface. It's the angle, measured north or south, from the equator to whatever location you want to talk about. On a map or globe, there may be some lines printed along the way, to help estimate the angle.
In the Mercator projection, the horizontal scale increases with latitude to preserve angles and maintain straight lines for navigation purposes. This distortion in scale towards the poles helps with navigation by allowing lines of constant bearing (rhumb lines) to appear as straight lines on the map.
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on a flat map