Three types of maps other than topographic, geologic, and soil maps include political maps, which show governmental boundaries and divisions; climate maps, which illustrate regions based on climate patterns and temperature; and thematic maps, which focus on specific themes or data, such as population density or economic indicators, providing insights into various geographic phenomena.
A topographic map legend typically includes symbols and colors that represent natural and cultural features such as elevation, water bodies, roads, and buildings. On the other hand, a geologic map legend includes symbols and colors that represent different rock types, faults, and geological formations present in an area. The key difference is that a topographic map focuses on the physical landscape, while a geologic map focuses on the underlying geological structure and rock types of the area.
Energy,metallic, and nonmetallic.
Topographic map
ElevationReliefSlope
A geologic map shows rock types making up earths surface.
There are a variety of types of maps. Some include political maps, physical maps, topographic maps, as well as climate maps.
A topographical map shows elevations. They are more useful than other types of maps when looking for information about landforms, their locations, and their heights.
A topographic map would show elevations and contours.
Airplane pilots typically use topographic maps, which show elevation and physical features of the Earth's surface, to navigate during flights. These maps provide information on terrain, airports, restricted areas, and other important features that help pilots plan routes and ensure a safe journey. Geologic maps, on the other hand, focus on the distribution of rock types and geological formations and are not commonly used for aviation navigation.
Geologic maps use color to represent various types of geologic features or units (a particular type of rock with a known age range).
The three types of stresses found at plate boundaries are compression (pushing together), tension (pulling apart), and shear (sliding past each other). These stresses occur due to the movement of tectonic plates and can result in various geologic phenomena such as earthquakes and mountain formation.
There are three main types of unconformities: angular unconformity, disconformity, and nonconformity. These unconformities represent gaps in the geologic record where erosion and non-deposition have occurred.