Angle of elevation: tangent angle = opposite/adjacent and by rearranging the given formula will help to solve the problem
It is some kind of chemical, or it can also stand for the popular online multiplayer game "Transformice".
the further the angle down the faster it will burn, but the wax of the furthest down one drips on the flame so it goes out. But it is still the fastest
"Tromandas" does not appear to be a widely recognized term in English or any specific context. It might be a misspelling, a niche term, or a word from a different language. If you provide additional context or clarification, I’d be happy to help you further!
The term "cotaxme turnturn" does not appear to have a widely recognized meaning in English or any specific context. It may be a misspelling, a phrase from a niche area, or a reference to a specific cultural or artistic work. If you provide more context or clarify its origin, I may be able to help further!
When your Odysseyware answer turns blue, it typically indicates that the answer has been submitted or recorded successfully. This color change often signifies that the system has recognized the input, allowing you to proceed with further questions or tasks. If you're unsure, you can usually check for any confirmation messages or feedback from the platform.
When contour lines are farther apart, it indicates a gentle slope or gradual change in elevation in the terrain. This means the change in elevation over a given distance is more gradual.
It can be shown that:height = (d tan α tan β)/(tan α - tan β)where: α is the angle closest to the objectβ is the angle further away from the objectd is the distance from the point of angle α to the point of angle βThus: height = (80 ft × tan 45° × tan 34°)/(tan 45° - tan 34°) ≈ 165.78 ft
The Texas Rule of Thumb is: The further you travel Northwest, the higher the elevation and lower the precipitation, the further you travel Southeast, the lower the elevation, and higher the precipitation.
When the crust thickens, the elevation typically increases due to the isostatic response of the Earth's lithosphere. As the crust becomes more buoyant, it can rise to maintain equilibrium with the underlying mantle. This process is often associated with tectonic activity, such as mountain building or volcanic activity, which can further contribute to increased elevation. Overall, thicker crust generally leads to higher elevations.
No, if you can measure no parallax, the star is far away - further than a certain distance.
It can be shown that:height = (d tan α tan β)/(tan α - tan β)where: α is the angle closest to the objectβ is the angle further away from the objectd is the distance from the point of angle α to the point of angle βThus: height = (53 ft × tan 31.4° × tan 26.4°)/(tan 31.4° - tan 26.4°) ≈ 140.87 ft
From what I remember in two geology classes, scientists measure the distance between a star and Earth by comparing "red shift," a shifting of certain bands of light toward the "red" end of the spectrum. The further the shifting, the greater the distance.
To determine the dip of formation from a geological map, first identify the strike direction of the rock layers, which is indicated by the orientation of the geological symbols. Next, look for contour lines or symbols that represent the elevation of the formations; the difference in elevation across a horizontal distance indicates the dip. Finally, use the formula for calculating dip, which involves the change in elevation divided by the horizontal distance, typically expressed in degrees. Additionally, any cross-sections included in the map can provide further insight into the dip of the formations.
The comparative degree of "far" is "farther" when referring to physical distance or "further" when referring to metaphorical distance or degree.
The land elevation along the coastal plain varies but generally ranges from sea level to a few hundred feet above sea level. The elevation gradually increases as you move further inland from the coast.
Pressure decreases with increasing elevation, so pressure is higher at lower elevations and vice versa. This is because the density of the atmosphere decreases as you move further away from the Earth's surface.
In order to "map" a terrain a cartographer needs to know how high or how low the soil is (land) from sea level. The physical makeup of earth, the physical map of places shows you land formations through the use of color which codes the particular place as being a certain distance above sea level. If the map was coded so that low elevation numbers (valleys) are dark and high elevations (mountains, peaks, plataues) are light, what you end up with is an image (likely shaded) which represents the "relief" of the place. Relief means 3 dimensional or sculptured in art. You can think of a map as a kind of art of the 3 dimensional physical world.