Mass Movement: Shaping Earth’s Surface

Mass movements, a category of geomorphic processes, play a significant role in shaping the Earth’s surface. These dynamic events involve the downslope movement of materials, often as a result of gravitational forces, and they contribute to the formation of diverse landforms. Understanding the causes and consequences of mass movements is crucial in assessing geological hazards and landscape development.

Mass movements involve the transfer of rock debris down the slope under the direct influence of  gravity that influences all matter, from bedrock to weathering products.

• Factors favoring mass movements include weak materials, steep slopes, rainfall, and lack of vegetation.
• Mass movements can be slow (creep, heave) or rapid (flow, slide), categorized by their speed.

Slow Shifts: The Gradual Formation of Earth through Mass Movement

• Meaning: Slow movement is a movement occurring on moderately steep, soil-covered slopes.
  • It involves extremely gradual and imperceptible material displacement, such as soil or rock debris.
• Creep Varieties: Creep has important effects that can be observed in slow movement. 
  • It includes soil creep, talus creep, rock creep, and rock-glacier creep.
• Solifluction: Another form of creep, consists of slow downslope flow of saturated soil or fine-grained rock debris.
  • It  occurs in moist temperate areas due to surface melting of frozen ground and prolonged rainfall.

Rapid Movements: Mass Movement Dynamics and Environmental Impact

• It is the downslope movement of water-saturated clay or silt along a hill such as earthflows, mudflows and debris avalanche.
• Earthflow is the movement of water-saturated clayey or silty materials down low-angle terraces or hillsides.
• Mudflows occur when heavy rainfall saturates thick layers of weathered materials, flowing slowly or rapidly down channels like a stream of mud.
  • Mudflow can be destructive when they reach piedmonts or plains, engulfing roads, bridges, and houses, and are common around erupting volcanoes.
• Debris avalanches are fast-moving mass movements, occurring in narrow tracks on steep slopes, resembling snow avalanches.
• These all phenomena are more prevalent in humid regions and can have significant geological and environmental impacts.

Landslide: Exploring Mass Movements and Geological Impact

• Landslide refers to rapid and perceptible movements. 
  • The materials involved are relatively dry. 
  • The size and shape of the detached mass depends on the nature of discontinuities in the rock, the degree of weathering and the steepness of the slope.
• Depending upon the type of movement of materials, several types are identified in this category. These are following:
  • Slump  is the slipping of one or several units of rock debris with a backward rotation with respect to the slope over which the movement takes place. 
  • Rapid rolling or sliding  of earth debris without backward rotation of mass is known as debris slide. 

• Sliding of individual rock masses down bedding, joint or fault surfaces is rockslide.

• Rockslide is the sliding of individual rock masses along bedding, joint, or fault surfaces, especially over steep slopes.

• Rockfall is free falling of rock blocks over steep slopes while maintaining some distance from the slope’s surface.

Erosion And Deposition: Forces of Change Through Erosion and Deposition

Erosion: Forces Shaping Landscapes

• Erosion involves the acquisition and transportation of rock debris by various geomorphic agents.
  • When massive rocks break into smaller fragments through weathering and other processes, erosional geomorphic agents like running water, groundwater, glaciers, wind and waves remove and transport it to other places.
• Abrasion by rock debris carried by these geomorphic agents also aids greatly in erosion.
• Erosion is responsible for continuous changes in the Earth’s surface and is controlled by kinetic energy.
• Geomorphic agents of erosion include wind, running water, glaciers, waves, and groundwater.

Deposition: Role in Earth’s Landscape Formation

• Meaning: Deposition is a consequence of erosion when erosional agents lose velocity on gentler slopes, causing materials to settle.
  • Deposition occurs in the reverse order of particle size, with coarser materials depositing first.
• Landscape Aggradation: Deposition fills depressions and leads to landscape aggradation.
• Agents of Erosion and Deposition: The same agents of erosion, such as running water, glaciers, wind, waves, and groundwater, can also act as depositional agents.
  • Erosion and deposition processes significantly shape the Earth’s surface, leading to various landforms.

Major Landforms Formed by Exogenic Forces: Mass Movement’s Role in Crafting Earth’s Landforms

The landscape undergoes continuous transformation through two fundamental processes: 

weathering and erosion, giving rise to various landforms, as listed below:

Landform by River: Majestic Waterfalls to Delta Deltas

• Waterfall: Weathering of steep terrain or hard rocks can lead to the formation of waterfalls.
• Meanders: Upon entering plains, rivers form large meanders or bends.
• Oxbow lake: Continuous erosion and deposition at meander sides bring the loops closer, eventually forming cut-off lakes or oxbow lakes.
• Levees : Occasional riverbank overflows result in flooding, depositing fertile sediments, and forming flat floodplains with raised banks, known as levees.
• Delta :When the river’s speed diminishes near the sea, causing it to split into distributaries, each creating its own mouth. 
• The sediments collected by all distributary mouths accumulate to form a delta.

Landforms by Sea: Sea Caves to Majestic Stacks

• Sea Caves: It formed when wave action strikes rocks, causing cracks to form and expand over time. 
• This process results in the creation of hollow sea caves. 
  • Continued erosion enlarges these caves, forming sea arches.
  • Further erosion breaks the roof, leaving behind wall-like features called stacks.

Landforms by Ice: Glaciers and the Formation of Moraines

• Glaciers: Often referred to as “rivers of ice,” contribute to landscape erosion. 
• The debris carried by glaciers, including rocks and sediments, form glacial moraines.

Landforms by Wind: The Beauty of Wind-Formed Landscapes

• Wind Landforms : significant erosion and deposition in deserts formed wind landforms. It includes:
  • Mushroom rocks, with a narrower base and wider top, are common desert formations due to wind erosion.
  • Sand dunes form when  wind  carries and deposits sand, forming low hill-like structures called.
  • Loess formed when fine, light sand can be carried over extensive distances by strong winds, leading to the formation of large areas of loess.