A banked curve.
A river's current slow down and tend to meander across a flat valley floor. The river's current is faster on the outside of the bend, and slower on the inside.
The outside of a meandering stream erodes more than the inside bends due to the faster flow of water on the outside of the curve. The higher velocity of water on the outside causes more erosion through processes like hydraulic action and abrasion, wearing away the bank more quickly. Additionally, the outside bends experience more turbulence, leading to increased erosion compared to the inside bends.
Rivers "carry" their sediment load only as long as the velocity of the water remains high enough to create sufficient turbulence to keep the particles "stirred up". Once a river loses its velocity and the stirring effect of the turbulence subsides the sediment load can no longer remain suspended in the water. At this point gravity takes over and the river begins to "drop" its sediments in a process named deposition.Now a river going around a curve is like two tires at each end of an axle going around a curve. The tire on the outside of the curve has to move faster than the tire on the inside of the curve since it has a longer radius of travel. So too the water in the river moves faster at the outside of the curve than the water inside the curve. Between the two different water velocities the deposition is going to occur on the inside curve of the river where the water loses its velocity.Conversely, the opposite of deposition which is erosion will take place at the outside of the curve in the river.
A big curve of coastline is called a bay.
The path of Earth's orbit in the shape of an elongated closed curve is called an ellipse. An ellipse is a type of geometric shape that resembles an elongated circle, with two focal points inside the curve. This shape is a result of the gravitational forces between Earth and the Sun.
Since the outside curve has a higher velocity, it has more erosion meaning the inside curve has a slower velocity more deposition causing it to be shallower. The outside curve is deep.
No
the 'outside' of the elbow is also called the 'wenis', and the 'inside' can also be called the antecubital. Other synonyms can also include: joint, angle, curve
A river's current slow down and tend to meander across a flat valley floor. The river's current is faster on the outside of the bend, and slower on the inside.
The outside of a meandering stream erodes more than the inside bends due to the faster flow of water on the outside of the curve. The higher velocity of water on the outside causes more erosion through processes like hydraulic action and abrasion, wearing away the bank more quickly. Additionally, the outside bends experience more turbulence, leading to increased erosion compared to the inside bends.
A curve in a stream channel is called a meander. Meanders are caused by the flow of water eroding the outside of a bend and depositing sediment on the inside, leading to a winding pattern in the channel. Meanders are a natural feature of rivers and streams and play a vital role in shaping the landscape.
Rivers "carry" their sediment load only as long as the velocity of the water remains high enough to create sufficient turbulence to keep the particles "stirred up". Once a river loses its velocity and the stirring effect of the turbulence subsides the sediment load can no longer remain suspended in the water. At this point gravity takes over and the river begins to "drop" its sediments in a process named deposition.Now a river going around a curve is like two tires at each end of an axle going around a curve. The tire on the outside of the curve has to move faster than the tire on the inside of the curve since it has a longer radius of travel. So too the water in the river moves faster at the outside of the curve than the water inside the curve. Between the two different water velocities the deposition is going to occur on the inside curve of the river where the water loses its velocity.Conversely, the opposite of deposition which is erosion will take place at the outside of the curve in the river.
The PPF graph is a bowed out curve. The x-axis being quantity produced of one product/service and the y-axis being another quantity produced of a product/service. Any point on the curve is productive efficiency. Outside of the curve is unattainable and inside of the curve is inefficient.
A straight line that intersects a circle or curve at two points, but which has both end points outside the circle or curve is called a secant. A straight line that links two points on a circle or curve is called a chord. A straight line which touches a circle or curve at one point is called a tangent. A straight line that cuts a circle or curve at one point is a straight line.* For moving diagrams see Related links below this box.
A leftward shift in the supply curve would mean that some outside (Macro-economic) or inside (Micro-economic) event occurred that caused the supplier of the good to not be willing to make as many at a lower price. The price of the good/service will increase. The new price will be at the new (higher) intersect of the supply and demand curves (equilibrium).
explain what happens inside curve sample
The current is faster on the outside of a bend than on the inside. The outside bank will erode and the inside will fill in. Also depends on the rock make up. In this way, in a uniform soil/rock, a river will follow a sine-type curve along its flatland basin etched out over millions of years and the sine curve will advance down the current flow line.