acidic groundwater
Glacial ice is the most probable agent of erosion that deposited unsorted sediments in deposit B. Glaciers can transport a wide range of sediment sizes and mix them together as they move, resulting in unsorted sediments.
Water erosion, specifically through the dissolution of carbon dioxide in water to form weak carbonic acid, is the primary agent responsible for creating limestone caves through the process of chemical weathering. Over time, this acidic water dissolves the limestone, creating caves, sinkholes, and other karst topography features.
Acid rain, which is formed from the reaction of carbon dioxide and water in the atmosphere, can dissolve the calcium carbonate in limestone statues through a chemical process known as carbonation. This leads to the breakdown and erosion of the limestone over time.
The agent of erosion most likely responsible for the deposition of sandbars along ocean shorelines is wave action. Waves can move sediment along the coastline and deposit it in certain areas, forming sandbars.
Water is the most common agent of erosion on Earth. It is responsible for shaping the landscape through processes such as river erosion, coastal erosion, and weathering.
Glacial ice is the most probable agent of erosion that deposited unsorted sediments in deposit B. Glaciers can transport a wide range of sediment sizes and mix them together as they move, resulting in unsorted sediments.
Grikes in limestone primarily form due to water erosion rather than wind erosion. Water seeping into the limestone gradually dissolves and widens vertical joints and fractures, creating the grikes. Wind can contribute to weathering and desiccation of the limestone, but it is not the primary agent responsible for the formation of grikes.
Water erosion, specifically through the dissolution of carbon dioxide in water to form weak carbonic acid, is the primary agent responsible for creating limestone caves through the process of chemical weathering. Over time, this acidic water dissolves the limestone, creating caves, sinkholes, and other karst topography features.
Groundwater is most effective in eroding soluble rocks like limestone, where it dissolves and carries away materials easily. Areas with high concentrations of limestone, such as karst landscapes, are particularly prone to groundwater erosion. Additionally, areas with abundant underground water flow or heavy precipitation can also experience significant erosion from groundwater.
Wind is the weakest agent of erosion.
Glaciers are the agent of erosion that deposit irregular mounds of unsorted sediment with parallel scratches on rounded particles. This type of deposit is called a moraine, which is formed as the glacier moves and carries a mixture of different-sized sediments that get deposited when the glacier melts.
The agent of erosion on cliffs mostly is gravity.
Gravity induced moving water is the most effective agent of erosion.
Acid rain, which is formed from the reaction of carbon dioxide and water in the atmosphere, can dissolve the calcium carbonate in limestone statues through a chemical process known as carbonation. This leads to the breakdown and erosion of the limestone over time.
Water erosion, particularly through processes like rivers, streams, and rainfall, is generally considered to be the most significant agent of erosion on Earth.
The agent of erosion most likely responsible for the deposition of sandbars along ocean shorelines is wave action. Waves can move sediment along the coastline and deposit it in certain areas, forming sandbars.
Water is the most common agent of erosion on Earth. It is responsible for shaping the landscape through processes such as river erosion, coastal erosion, and weathering.