Rashid's Blog: A Place for Inquisitive Souls

An unusually extended interglacial has happened before: MIS 11 represents the longest and warmest interglacial interval of the last 500 kyr. In theory at least a repeat due to natural variation can’t be ruled out. Blaming humans now can only be an opinion, not a statement of fact. Note the curious case of the Arctic’s

Did ‘Climate change stop the next ice age’, as these researchers claim?

Finlands Approach to Housing

Love of Maps

Terrain classification is the systematic grouping of the Earth’s surface into different categories based on its elevation, slope, relief, landforms, geological structure and geomorphological characteristics.

In physical geography, terrain refers to the physical characteristics of an area of land, including its shape, height, steepness and surface features.

1. Classification based on elevation and relief

1. Plains

Extensive areas of relatively flat or gently undulating land with low local relief. They are often formed by river deposition, marine processes or erosion.

Examples: Indo-Gangetic Plain, Mississippi Plain.

2. Plateaus

Elevated areas with relatively flat or gently rolling surfaces, often bounded by steep slopes or escarpments.

Examples: Deccan Plateau, Tibetan Plateau.

3. Mountains

High-relief terrain characterised by steep slopes, significant elevation differences and prominent peaks or ridges.

Examples: Himalayas, Alps, Andes.

4. Hills

Moderately elevated terrain, generally lower and less rugged than mountains, with rounded or irregular summits and slopes.

Examples: Aravalli Hills, Shivalik Hills.

Elevation thresholds used to distinguish hills, mountains and plateaus vary across geographical classification systems. Relative relief and slope are often more important than absolute elevation.

2. Classification based on slope

Terrain type	Characteristics
Flat	Very low slope; suitable for agriculture, settlements and transport
Gently sloping	Gradual elevation change; relatively easy to develop
Moderately sloping	Noticeable gradients; development requires careful planning
Steep	High gradients; greater erosion and landslide risks
Very steep or rugged	Sharp relief, cliffs and difficult accessibility

Slope classification is particularly important in geomorphology, civil engineering and urban planning.

3. Classification based on geomorphological origin

Terrain can also be classified according to the processes responsible for its formation.

• Structural terrain: Formed or controlled by geological structures, such as folded mountains, fault-block mountains and structural plateaus.
• Fluvial terrain: Shaped by rivers, including floodplains, valleys, natural levees and deltas.
• Glacial terrain: Formed by glaciers, including cirques, arêtes, U-shaped valleys and moraines.
• Aeolian terrain: Formed by wind action, including sand dunes, loess plains and deflation hollows.
• Coastal terrain: Shaped by waves, tides and coastal currents, including beaches, cliffs and coastal plains.
• Volcanic terrain: Formed by volcanic activity, including lava plateaus, volcanic cones and calderas.

4. Terrain classification in GIS and remote sensing

In modern geographical studies, terrain is classified using Digital Elevation Models (DEMs), satellite imagery and GIS techniques.

Terrain parameter	What it indicates
Elevation	Height above a reference level, usually mean sea level
Slope	Steepness of the land surface
Aspect	Direction a slope faces
Relief	Difference in elevation within an area
Curvature	Whether the surface is convex, concave or relatively flat
Terrain ruggedness	Degree of irregularity of the surface

These parameters help identify terrain units and assess their suitability for agriculture, urban expansion, road construction, watershed management and hazard mapping.

Readings:

Basic Idea of Terrain Classification

Concept and Applications of Digital Elevation Model