Bedrock river

Some rivers flow over hard rock.

These are called bedrock rivers. They are often in high mountains. The water moves very fast down the hills.

Fast water has a lot of energy. This energy hits the rock. It can wear the rock away slowly.

Small bits of sand and dirt help. They rub against the rock like sandpaper. This can make deep holes.

Sometimes, the water even pulls big chunks away. This makes the river bed change. It is amazing to see!

Most rivers flow over loose sand or dirt. But some rivers flow over hard rock. These are called bedrock rivers. They are often found in high mountains.

These rivers change the rock in many ways. One way is through stream power. As water flows down a steep slope, it gains energy. This energy hits the rock and wears it down. This is called incision.

Another way is called abrasion. This happens when the water carries small bits of sand or silt. These bits rub against the rock. This can make deep holes or troughs.

Sometimes, the river moves big chunks of rock. This is called quarrying, or plucking. A crack might form in the rock first. Then, the water forces the piece out. The river then pushes the heavy block along the bed.

Small grains can also cause wedging. These grains get stuck in tiny cracks. As more grains enter, the cracks grow wider. Finally, large blocks can break off. In some rocks, the water can even dissolve the stone. This is called dissolution. It is a slow way to change the river.

Most rivers flow over loose sand or dirt. But some rivers flow over hard rock. These are called bedrock rivers. They are often found in high mountains.

A bedrock river has very little sediment covering the stone. Most of these rivers are a mix of rock and loose material. You can tell them apart by how much sediment covers the bottom. This depends on how much material the water brings in. It also depends on how much the water can carry. These rivers are special because they help us study how water cuts into rock. This is called incision.

Water uses energy to change the shape of the river. One way is through stream power. This happens when water moves down a steep slope. The water turns its stored energy into kinetic energy. This is the energy of motion. The water uses this energy to beat against the bedrock. Another way is called abrasion. This is when small grains like silt or clay rub against the rock. These tiny grains are part of the suspended load. They float in the water and hit bumps in the river bed. This can wear away the rock and make potholes.

Rivers can also move much larger pieces of stone. This process is called quarrying, or plucking. It is very much like how glaciers move rock. First, a crack or a flex appears in the bedrock. Then, things like frost-cracking or water pressure force a block out. If the rock has many joints or cracks, it is easier to move. Once the block is loose, the river must push it along. The river's force must be stronger than the friction holding the rock down. This can cause the river to grow backward through headward erosion.

Other small actions can lead to big changes. Wedging happens when tiny grains get stuck in small cracks. These cracks might form during heavy storms or big movements. When the bedrock flexes, the grains stay in the crack. This makes the crack wider and deeper over time. Eventually, this can lead to the quarrying process. Some rocks can even undergo dissolution. This is when the water dissolves the stone. It happens most in rocks like sandstone or carbonate rocks. This is often how caves are made.

Even bedrock rivers can carry and drop sediment. Most of the time, the river carries material downstream. It might drop grains in patches where the water is slower. These patches happen where the rock is rough. This increases the stability of the grains. You might see these as alluvial bars. These are shapes made of sand or gravel on the river bed. The river will carry these bits until it reaches an alluvial section. This is where the river is deeper and wider.

A bedrock river is a unique type of river system. In these rivers, there is little to no alluvium covering the solid rock. Alluvium is the layer of loose sediment, like sand or silt, that usually sits on a riverbed. Most bedrock rivers are not perfectly pure. Instead, they are a combination of a bedrock channel and an alluvial channel. You can tell them apart by looking at the extent of the sediment cover. This coverage depends on the sediment flux, or the amount of material supplied to the channel. It also depends on the channel's transport capacity. These rivers are usually found in mountainous or upland regions. They are important because they allow scientists to study incision. Incision is the process of a river cutting into solid bedrock without the influence of glaciers.

Bedrock incision often begins with tectonic plate movement. As the land is uplifted by these movements, the river is forced to cut downward to keep flowing. This process uses several different erosional mechanisms. One primary factor is stream power. Stream power is the process where the energy from moving water is converted into kinetic energy. This happens because of the steepening of the river's slope. As water travels downstream, it loses gravitational potential energy. According to the laws of conservation of energy, this energy must transform into another form. It becomes the kinetic energy of the water beating against the bedrock. Scientists calculate the rate of this energy loss using a specific equation. This equation includes water density, the gravitational constant, the hydraulic discharge, and the slope of the channel. Stream power may be the most important factor in how a river cuts into rock.

Another major process is abrasion. Abrasion occurs when sediments are transported within the river flow to wear down the bed. The rate of erosion depends on the strength of the bedrock and the amount of sediment load. If there is too much sediment, the particles lack the energy to erode the rock. If there is too little, they do not contact the bed enough. Abrasion can erode individual grains or small flakes from the rock surface. This often creates potholes or trough-like shapes in the riverbed. There are three types of sediment transport: dissolved load, suspended load, and bed load. The suspended load is very important for bedrock rivers. This load consists of fine grains like clay and silt that float in the water. These particles have high kinetic energy. When they hit an obstruction in the bed, they can cause significant damage.

Bedload erosion also plays a large role in shaping the river. This involves grains that are heavier and move differently. Some grains move through saltation, where the water lifts them up and tosses them back down. This usually happens with gravel or pebbles if the stream power is high enough. However, very fine clays and silts have too much cohesion to move this way. Other bedload moves through traction. Traction is when sediment is too large to be lifted but is pushed or rolled along the bottom. As these particles hit the bedrock, they wear it away. They can create or expand tiny micro-cracks in the stone. The physics shows that the mass of rock worn away is proportional to the kinetic energy of the particle.

Quarrying, also called plucking, is a more aggressive form of erosion. In this process, a large chunk of bedrock is removed and forced along the riverbed. This is very similar to how glaciers erode the land. It works best in rivers where the rock has close jointing, which means it has many cracks. A crack or a flex in the rock can create a disconnected piece. Then, factors like hydraulic wedging or frost-cracking force the block out. If the rock is already fractured or has a bedding plane, it is easier to remove. Once the block is loose, the river's shear stress must exceed the friction on the bottom to move it. This process can cause headward erosion, where the river cuts backward into the landscape.

Wedging is a process that often leads to quarrying. It starts when small cracks appear in the riverbed due to rapid pressure variations. These variations can be caused by heavy storms or mass movements of earth. Once a crack forms, a small amount of sediment can settle inside it. When the bedrock flexes back to its original position, the sediment stays trapped. This acts as a wedge that keeps the crack open. Over time, more sediment accumulates, making the crack wider and deeper. This is most common in riverbeds that are already heavily jointed. Additionally, some rocks undergo dissolution. This is a chemical process where the water dissolves the rock. This typically affects rocks like sandstone or carbonate rocks, which are prone to dissolving. This process is how many caves are formed.

Even though these are bedrock rivers, they can still transport and deposit sediment. You might see patches of sediment where the bedrock is rough. Roughness increases grain stability and reduces the kinetic energy of the water. These deposits are known as alluvial bed forms or bars. Most sediment is eventually carried downstream to more alluvial sections of the river. In those sections, the river is often deeper and wider. The likelihood of deposition depends on the slope and the amount of water flowing in.