Question map
Which one of the following is the best example of repeated falls in sea level, giving rise to present-day extensive marshland?
Explanation
The correct answer is option D - Rann of Kutch.
The satellite imagery, as well as detailed mapping, have revealed a network of distributaries and extensive graded deposits, products of Holocene marine regression[1] in the Rann of Kutch region. Marine regression refers to the retreat or fall of sea levels, which explains the geological formation of this area. Stretching over an area of 20,720 sq km, the Rann of Kutch consists of salt flats, brackish ponds, and marsh interrupted by a few rocky elevations[2], confirming its extensive marshland character. The topography of the Great Rann of Kachchh is typically deltaic, developing usually at the mouth of rivers, confirming entry of a few rivers in the sea in this region[1], which indicates its past connection with the sea. The repeated marine regressions (sea level falls) during the Holocene period transformed what was once a shallow gulf or arm of the sea into the present-day extensive marshland. The other options (Bhitarkanika Mangroves, Marakkanam Salt Pans, and Naupada Swamp) do not have this distinctive geological history of marine regression creating extensive marshlands.
Sources- [1] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > SARASWATI-THE MYSTERY OF A LOST RIVER > p. 27
- [2] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 16: India–Political Aspects > The Rann of Kutch Dispute > p. 36
PROVENANCE & STUDY PATTERN
Guest previewThis is a classic 'Process-based Geography' question. It moves beyond simple mapping ('Where is Rann?') to geomorphology ('How did Rann form?'). It is directly solvable from standard texts like Majid Husain which explicitly link the Rann to 'Holocene marine regression' and the drying up of the paleo-Saraswati.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: Is Bhitarkanika Mangroves an example of an area where repeated falls in sea level produced the present-day extensive marshland?
- Statement 2: Are the Marakkanam Salt Pans an example of an area where repeated falls in sea level produced the present-day extensive marshland?
- Statement 3: Is Naupada Swamp an example of an area where repeated falls in sea level produced the present-day extensive marshland?
- Statement 4: Is the Rann of Kutch an example of an area where repeated falls in sea level produced the present-day extensive marshland?
Defines mangroves as occurring in tidal flats, estuaries and muddy coasts — environments strongly influenced by sea-level change.
A student could check whether Bhitarkanika sits on a former tidal flat/estuary plain that would be exposed during sea-level falls, supporting marsh development.
Notes coastal mangroves occur along eastern coastal shallow seas and are productive ecosystems tied to coastal dynamics.
Using a map of the eastern coast (Odisha) and basic coastal-process knowledge, one could assess whether past sea-level fluctuation plausibly shaped local marsh extent.
Lists Bhitarkanika explicitly as a major wetland/mangrove area, confirming the site type to which general rules about tidal flats and marsh formation apply.
Knowing the site is a large wetland, a student could look for published palaeo-shoreline or sediment records for this named location to test sea-level fall hypotheses.
Mentions mudflats and salt marshes as coastal geomorphological features of ecological importance in CRZ context.
A student could relate the presence of mudflats/salt marshes to past sea-level lowstands that expose sediments and favour marsh development, then seek local geomorphic evidence.
States Bhitarkanika is the second largest mangrove in India located along the Odisha coast, implying significant coastal sedimentary/geomorphic setting.
Combining this site identification with general coastal sedimentation knowledge, one could investigate whether the Odisha coast has records of regressive (falling sea-level) phases relevant to marsh formation.
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