I think you might be referring to what is called textural maturity. It is assumed that a rock with high textural maturity has traveled a longer distance, as high maturity corresponds to more processes acting on the sediment and a longer time between erosion and deposition. Features to look for to determine maturity are grain size sorting, angularity/roundedness, and composition purity. Same-sized grains, round grains, and a single mineral type all indicate high textural maturity (this sediment forming this rock traveled far). A wide range of grain sizes, grains that are jagged, and a lot of different mineral grain types, all point to low textural maturity (this rock formed near it's source). And you can have combinations inbetween.
You would use the arrival time of the seismic waves at the station and knowledge of the wave velocities in various materials. By measuring the time it takes for the waves to reach the station and knowing how fast they travel through different types of rock, you can calculate the distance they have traveled from the origin.
Different clastic sediments have different textures based on the size, shape, and sorting of the grains they are composed of. The composition of a clastic sedimentary rock will vary depending on the mineralogy of the grains present in the rock. Factors such as the source rock, transportation distance, and depositional environment can all contribute to the differences in texture and composition between clastic sedimentary rocks.
A travel time graph shows the relationship between the distance traveled and the time taken for a journey. It helps to visualize how travel time changes as distance increases, and can be useful for planning routes and estimating arrival times. The slope of the graph represents the speed of travel.
the distance to the earthquake's epicenter. P waves, or primary waves, travel faster than S waves, or secondary waves, so the interval between their arrival times can be used to calculate the distance the seismic waves have traveled. By measuring this time difference at different seismograph stations, geologists can triangulate the epicenter of the earthquake.
The change in elevation divided by the distance traveled is known as the gradient or slope. It is commonly used to measure the steepness of inclines or declines along a route or terrain. The gradient is calculated by dividing the difference in elevation by the horizontal distance covered.
measure
No, you cannot.
To determine the distance traveled by an object based on its acceleration, you can use the formula: distance 0.5 acceleration time2. This formula calculates the distance traveled by an object with a constant acceleration over a certain period of time.
To determine the speed of an object, you would need to know the distance it has traveled and the time it took to cover that distance. Speed is calculated by dividing the distance traveled by the time taken to cover that distance.
To determine the distance traveled from a position-time graph, calculate the area under the curve. This can be done by finding the area of each individual section and adding them together. The total area represents the total distance traveled.
An odometer is commonly used to measure the distance traveled by a vehicle. It calculates the distance based on the rotations of the vehicle's wheels. GPS devices can also be used to determine distance traveled by tracking the device's movement.
no, you need to know its initial velocity to determine this; if initial velocity is zero then distance is 1/2 acceleration x time squared
To calculate the distance traveled by an object, you can use the formula: distance 0.5 acceleration time2. This formula takes into account the acceleration of the object and the time it has been moving to determine the distance traveled.
To determine the distance traveled by an object using its velocity and acceleration, you can use the equation: distance initial velocity time 0.5 acceleration time2. This formula takes into account the initial velocity of the object, the time it has been traveling, and the acceleration it is experiencing. By plugging in these values, you can calculate the distance traveled by the object.
You divide the distance by the time.You divide the distance by the time.You divide the distance by the time.You divide the distance by the time.
You can determine the rate of motion. For example mph (miles per hour) is found by multiplying miles traveled by the time (hours) in motion.this formula isRate * Time = Distance
Distance traveled can be calculated using the formula: distance = speed × time. This equation is used to determine how far an object has moved over a certain period of time at a specific speed.