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Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer? for Humanities/Arts 2024 is part of Humanities/Arts preparation. The Question and answers have been prepared according to the Humanities/Arts exam syllabus. Information about Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer? covers all topics & solutions for Humanities/Arts 2024 Exam. Find important definitions, questions, meanings, examples, exercises and tests below for Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer?.

Solutions for Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer? in English & in Hindi are available as part of our courses for Humanities/Arts. Download more important topics, notes, lectures and mock test series for Humanities/Arts Exam by signing up for free.

Here you can find the meaning of Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer? defined & explained in the simplest way possible. Besides giving the explanation of Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer?, a detailed solution for Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer? has been provided alongside types of Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer? theory, EduRev gives you an ample number of questions to practice Direction: Read the case study given below and answer any three of the questions that follow.Small- to medium-sized round to sub-rounded shallow depressions called swallow holes form on the surface of limestones through solution. Sink holes are very common in limestone/karst areas. A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom with sizes varying in area from a few sq. m. to a hectare and with depth from a less than half a metre to thirty metres or more. Some of these forms solely through solution action (solution sinks) and others might start as solution forms first and if the bottom of a sinkhole forms the roof of a void or cave underground, it might collapse leaving a large hole opening into a cave or a void below (collapse sinks). Quite often, sinkholes are covered up with soil mantle and appear as shallow water pools. Anybody stepping over such pools would go down like it happens in quick sands in deserts. The term doline is sometimes used to refer the collapse sinks. Solution sinks are more common than collapse sinks. Quite often the surface runoff simply goes down swallow and sink hole sand flow as underground streams and re-emerge at a distance downstream through a cave opening. When sinkholes and do lines join together because of slumping of materials along their margins or due to roof collapse of caves, long, narrow to wide trenches called valley sinks or Uvalas form. Gradually, most of the surface of the limestone is eaten away by these pits and trenches, leaving it extremely irregular with a maze of points, grooves and ridges or lapies. Especially, these ridges or lapies form due to differential solution activity along parallel to sub-parallel joints. The lapie field may eventually turn into somewhat smooth limestone pavements.Q. Quite often, sinkholes are covered up with soil mantle and appear as shallow_________.a)water poolsb)river poolsc)oasisd)swimming poolCorrect answer is option 'A'. Can you explain this answer? tests, examples and also practice Humanities/Arts tests.