500 to 1000 meters
The greatest factor that determines climate in any given location is its distance from the equator, which affects the amount of sunlight and heat received. Other factors include proximity to large bodies of water, elevation, and prevailing winds.
Absolute Location is the specific location of a place with latitude and longitude.
The amount of solute that can dissolve in a given amount of solvent is determined by the solubility of the solute in that solvent at a specific temperature. Solubility is expressed as grams of solute per 100 grams of solvent. By knowing the solubility, you can calculate how much solute can dissolve in the specified amount of solvent.
Concentration
volume
The amount of shaking produced by an earthquake at a given location is called "intensity".
Benthic Realm
The amount of shaking produced by an earthquake at a given location is called the intensity. It is measured on the Modified Mercalli Intensity (MMI) scale, which quantifies the level of shaking experienced by people and structures during an earthquake.
It measures he amount of sunlight at a given location.
The thicker the slab of seafloor, the more material it contains, leading to a greater weight. This weight is influenced by the density of the rock forming the seafloor. Thicker slabs of seafloor would have more mass and therefore weigh more than thinner slabs.
Time of day and atmospheric conditions (like cloud cover) are the two biggies. Also, location laditude, however, the question specified "in a given location"
is a measure of the amount of matter in a given amount of space
is a measure of the amount of matter in a given amount of space
is a measure of the amount of matter in a given amount of space
The greatest factor that determines climate in any given location is its distance from the equator, which affects the amount of sunlight and heat received. Other factors include proximity to large bodies of water, elevation, and prevailing winds.
The amount of matter is given space is mass.
Weathering and erosion are the steps that occur immediately before sediments are laid down in the rock cycle. Weathering breaks down rocks into smaller particles, while erosion transports these particles to a new location where they can accumulate and form sedimentary rocks.