Skip to main content

UGC NET Geography UPSC

Indus and Brahmaputra are examples of—
 (A) Subsequent drainage 
(B) Superimposed drainage 
(C) Antecedent drainage 
(D) Consequent drainage

The correct answer is (C) Antecedent drainage.

Let's explain all the options:

(A) Subsequent drainage: Subsequent drainage refers to a river system that develops and follows the slope of the land that has been formed by tectonic forces or other geomorphic processes. It occurs after the formation of the land and is not related to the initial development of the landscape. It is not applicable to the Indus and Brahmaputra rivers.

(B) Superimposed drainage: Superimposed drainage occurs when a river cuts through existing rock structures and maintains its course regardless of the underlying geological features. This type of drainage develops over previously formed landscapes and is often influenced by erosion-resistant rock layers. It is not applicable to the Indus and Brahmaputra rivers.

(C) Antecedent drainage: Antecedent drainage occurs when a river system develops in a region before the surrounding landmass undergoes uplift or tectonic changes. The river maintains its course despite the subsequent changes in the landscape caused by geological forces. This is the correct option for the Indus and Brahmaputra rivers. These rivers existed before the Himalayan mountain range was uplifted and have maintained their courses by eroding through the rising mountains.

(D) Consequent drainage: Consequent drainage develops in response to the existing topography or landform patterns. It occurs as a result of the initial structure and relief of the area. This option is not applicable to the Indus and Brahmaputra rivers because their courses were established before the formation of the Himalayas.

Therefore, the correct answer is (C) Antecedent drainage, as the Indus and Brahmaputra rivers existed before the formation of the Himalayas and have maintained their courses by eroding through the rising mountains.



Comments

Popular posts from this blog

Energy Interaction with Atmosphere and Earth Surface

In Remote Sensing , satellites record electromagnetic radiation (EMR) that is reflected or emitted from the Earth. Before reaching the sensor, radiation interacts with: The Atmosphere The Earth's Surface These interactions control how satellite images look and how we interpret them. I. Interaction of EMR with the Atmosphere When solar radiation travels from the Sun to the Earth, four main processes occur: 1. Absorption Definition: Absorption occurs when atmospheric gases absorb radiation at specific wavelengths and convert it into heat. Main absorbing gases: Ozone (O₃) → absorbs Ultraviolet (UV) Carbon dioxide (CO₂) → absorbs Thermal Infrared Water vapour (H₂O) → absorbs Infrared Concept: Atmospheric Windows These are wavelength regions where absorption is very low, allowing radiation to pass through the atmosphere. Remote sensing depends on these windows. For example, satellites like Landsat 8 use visible, near-infrared, and thermal bands located in atmospheric windows. 2. Trans...

Atmospheric Window

The atmospheric window in remote sensing refers to specific wavelength ranges within the electromagnetic spectrum that can pass through the Earth's atmosphere relatively unimpeded. These windows are crucial for remote sensing applications because they allow us to observe the Earth's surface and atmosphere without significant interference from the atmosphere's constituents. Key facts and concepts about atmospheric windows: Visible and Near-Infrared (VNIR) window: This window encompasses wavelengths from approximately 0. 4 to 1. 0 micrometers. It is ideal for observing vegetation, water bodies, and land cover types. Shortwave Infrared (SWIR) window: This window covers wavelengths from approximately 1. 0 to 3. 0 micrometers. It is particularly useful for detecting minerals, water content, and vegetation health. Mid-Infrared (MIR) window: This window spans wavelengths from approximately 3. 0 to 8. 0 micrometers. It is valuable for identifying various materials, incl...

Scattering

Scattering 

Platforms in Remote Sensing

In remote sensing, a platform is the physical structure or vehicle that carries a sensor (camera, scanner, radar, etc.) to observe and collect information about the Earth's surface. Platforms are classified mainly by their altitude and mobility : Ground-Based Platforms Definition : Sensors mounted on the Earth's surface or very close to it. Examples : Tripods, towers, ground vehicles, handheld instruments. Applications : Calibration and validation of satellite data Detailed local studies (e.g., soil properties, vegetation health, air quality) Strength : High spatial detail but limited coverage. Airborne Platforms Definition : Sensors carried by aircraft, balloons, or drones (UAVs). Altitude : A few hundred meters to ~20 km. Examples : Airplanes with multispectral scanners UAVs with high-resolution cameras or LiDAR High-altitude balloons (stratospheric platforms) Applications : Local-to-regional mapping ...

History of GIS

1. 1832 - Early Spatial Analysis in Epidemiology:    - Charles Picquet creates a map in Paris detailing cholera deaths per 1,000 inhabitants.    - Utilizes halftone color gradients for visual representation. 2. 1854 - John Snow's Cholera Outbreak Analysis:    - Epidemiologist John Snow identifies cholera outbreak source in London using spatial analysis.    - Maps casualties' residences and nearby water sources to pinpoint the outbreak's origin. 3. Early 20th Century - Photozincography and Layered Mapping:    - Photozincography development allows maps to be split into layers for vegetation, water, etc.    - Introduction of layers, later a key feature in GIS, for separate printing plates. 4. Mid-20th Century - Computer Facilitation of Cartography:    - Waldo Tobler's 1959 publication details using computers for cartography.    - Computer hardware development, driven by nuclear weapon research, leads to broader mapping applications by early 1960s. 5. 1960 - Canada Geograph...