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In Class 9 Geography, this topic from the chapter “Drainage” explains how rivers shape the land through erosion, transportation and deposition. Students learn how river systems and drainage patterns influence plains, valleys, agriculture, settlements, transport and the availability of water. The topic also highlights the importance of rivers in human life, along with challenges such as pollution, floods and the need for careful conservation and management of river resources.
TOPIC PRACTICE
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Up to 20 questions from this page. Select your focus, then start.
Rivers are important to industries because they can provide useful water and, in some situations, support energy production. Many industrial processes need water for processing, cooling, cleaning, or other operations. Rivers may also support hydropower where suitable conditions exist. In addition, river locations can help transport materials, although the given answer focuses on water supply and energy.
Option A is correct because it states two genuine ways rivers can support industry. The word “can” is important: not every river supplies every industry, and industrial use depends on location, water availability, technology, and environmental rules. The other options are incorrect because rivers do not always close industries, do not completely destroy raw materials, and do not stop the use of electricity. Their statements are absolute and contrary to the usual industrial role of rivers.
A delta forms near the mouth of a river when the river loses speed and deposits the sediment it has been carrying. The deposited silt, sand, and clay can gradually build land that often has branching distributary channels. Therefore, option A is correct: a river forms a delta when it deposits silt near the sea or another standing body of water. Deltas are depositional landforms, not features made by the river drying or flowing backward.
At the river mouth, the current may slow because the channel enters relatively still water. As carrying power decreases, heavier and then finer sediments settle. Repeated deposition expands the sedimentary area and may create a roughly triangular or fan-like shape. The other options do not describe this process: ice on mountains, complete drying, and reverse flow are unrelated. Thus the key connection is river mouth plus sediment deposition, leading to answer A.
The governing hydrological concept is groundwater recharge, the replenishment of underground water when surface water infiltrates through soil and permeable rock. Water flowing in a river or stored along its channel may seep downward, especially where the riverbed contains sand, gravel or other permeable sediments. Some of that infiltrated water reaches the saturated zone and adds to groundwater. The amount depends on soil, rock, vegetation, rainfall, river flow and human changes such as paving or excessive pumping. Rivers do not always send water into the sky, make all ground impermeable or produce only salt. Therefore option A is correct.
During floods, a river may deposit the fine silt it carries over floodplains and fields. This silt contains mineral nutrients and can increase soil fertility. A reduction in soil fertility is a possible harmful effect of floods, not a positive one. Exam tip: Remember fertile silt deposition as a benefit of floods, and damage to crops and property as harmful effects.
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