The total surface area (TSA) is determined by the sum of areas of its 6 faces - TSA = 2 (lw + wh + hl)
Geometric configurations that do not conform to standardized shapes (squares, triangles, circles, etc.) can still have their areas determined. They can be calculated by dividing the given parcel into known shapes (and thus formulae) and then calculating the areas of each, and combining their values.
It depends completely on the type of map and the scale of the map. Look several contour lines above and below the area of interest. Often, the elevation is printed on every 5th contour line. Divide the difference by the number of spaces between the two lines. Example, one contour line says "1000" and the next one with an elevation says "1500". If there are 4 lines in between these two, it is 100 ft per contour line. In some areas, you will need to follow a contour line around the map to track down the elevation of that line. Easier still, check the legend on the side or bottom of the map. The example showing the colors or symbols used may also tell the contour interval if it is consistent for the entire map.
Your question is very broad, but I will attempt to answer it. If I don't give you the answer you are looking for, then perhaps you can resubmit it, with a more specifics. Please see the related link Generally, we obtain information from a contour map (a map with contour lines). The most common map is an elevation map, showing the height of a surface above a common datum (usually sea level). However, many types of data can be measured and contour maps developed from the data. Temperature and atmospheric pressure data can be contoured. Of course, it changes from day to day, so our map may be good for only one specific time period. See the related link for more on the different contour map. Contour maps are a means of understanding our data, and obtaining relavent information quickly. We can see regions of high and low values. If we are looking at an elevation map, these are the highest and lowest areas of a given region. If the countour lines are close together, this shows a high gradient or slope. For example, if our elevation map shows contours close together, this is area where the ground is sloping up or down. We can make calculations of areas and volumes. For example, we can estimate the area where the elevation is between two numbers, say 50 to 60 ft above sea level. Sometimes, to obtain accurate estimates of areas and volumes, we need to input the contour map into the computer, and let it make the calculations.
Your question is very broad, but I will attempt to answer it. If I don't give you the answer you are looking for, then perhaps you can resubmit it, with a more specifics. Please see the related link Generally, we obtain information from a contour map (a map with contour lines). The most common map is an elevation map, showing the height of a surface above a common datum (usually sea level). However, many types of data can be measured and contour maps developed from the data. Temperature and atmospheric pressure data can be contoured. Of course, it changes from day to day, so our map may be good for only one specific time period. See the related link for more on the different contour map. Contour maps are a means of understanding our data, and obtaining relavent information quickly. We can see regions of high and low values. If we are looking at an elevation map, these are the highest and lowest areas of a given region. If the countour lines are close together, this shows a high gradient or slope. For example, if our elevation map shows contours close together, this is area where the ground is sloping up or down. We can make calculations of areas and volumes. For example, we can estimate the area where the elevation is between two numbers, say 50 to 60 ft above sea level. Sometimes, to obtain accurate estimates of areas and volumes, we need to input the contour map into the computer, and let it make the calculations.
Due to gravity, ocean water is attracted to areas of high topography and away from areas of low topography on the sea floor, causing bulges and depressions on the ocean surface. Satellite radar can detect these changes in elevation.
in topographic maps we find local areas in relief map we find things like mountain valley etc, well, the answer above is wrong the difference between the two is that a topography map has lines on it to show elevation and releif maps have colors to show elevation.
Hikers find contour maps most useful in mountainous or hilly terrain where elevation changes are frequent and steep. Contour maps help hikers to visualize the topography, identify elevation gains and losses, locate ridges and valleys, and plan their routes accordingly.
Topography is the shape of the land.Answerto·pog·ra·phyn., pl. -phies.Detailed, precise description of a place or region.Graphic representation of the surface features of a place or region on a map, indicating their relative positions and elevations.A description or an analysis of a structured entity, showing the relations among its components: In the topography of the economy, several depressed areas are revealed.The surface features of a place or region.The surface features of an object: The topography of a crystal.The surveying of the features of a place or region.The study or description of an anatomical region or part.
Mangrove swamps are typically found in coastal areas and estuaries with low elevation, often close to sea level. The elevation can vary depending on the location and topography of the region, but mangrove swamps are generally characterized by their presence in low-lying coastal areas.
The area of topography include mountains, valleys, plains, and bodies of water.
high elevation areas that get more rain than the surrounding low elevation areas
The 2011 tsunami reached inland up to 10 kilometers in some areas of Japan. The extent of inland penetration varied based on factors such as topography and elevation.
Limestone
Areas of higher elevation are colder compared to areas of lower elevation because the air pressure is lower at higher elevations, causing the air to expand and cool. Additionally, as you move higher in elevation, the atmosphere becomes thinner and contains less heat-absorbing gases, leading to lower temperatures.
Topography influences soil characteristics by affecting factors such as drainage, erosion, and nutrient availability. Steep slopes can lead to poor drainage and increased erosion, while flat areas may retain more water. Differences in elevation can also impact the distribution of nutrients and organic matter within the soil.
Actually, a plain is a flat, low-lying area of land, usually with minimal elevation changes and relatively open vegetation. It is typically contrasted with areas that have more rugged terrain or varied topography.