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Humanities/Arts Exam  >  Humanities/Arts Questions  >  An archaeological site, which was used for qu... Start Learning for Free
An archaeological site, which was used for quarrying limestone was:
  • a)
    Chesowanja, Kenya.
  • b)
    Schoningen, Germany.
  • c)
    Dolni Vestonice, Czech Republic.
  • d)
    Neander Valley, Germany.
Correct answer is option 'D'. Can you explain this answer?
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An archaeological site, which was used for quarrying limestone was:a)C...
Neander Valley is a gorge in Germany. It is popular for the quarrying of limestone. Here, the evidence of early man was discovered by workers who were quarrying for limestone in August 1856.
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An archaeological site, which was used for quarrying limestone was:a)C...
Neander Valley, Germany

Neander Valley, also known as Neanderthal Valley, is an archaeological site located in Germany. It is famous for being the place where the first Neanderthal fossil was discovered in 1856. The site is situated near the town of Mettmann, in the western part of the country.

Quarrying Limestone

The Neander Valley was not primarily used for quarrying limestone. In fact, it is well-known for its significance in paleoanthropology as it provided valuable evidence about the existence of Neanderthals, an extinct species of hominids closely related to modern humans. The discovery of the Neanderthal fossil in this valley revolutionized our understanding of human evolution.

Other Archaeological Sites

While the Neander Valley is not associated with limestone quarrying, let's briefly explore the other options mentioned:

- Chesowanja, Kenya: This archaeological site is located in Kenya and is known for its stone tools, which date back to the Early Stone Age. It does not have a connection to limestone quarrying.

- Schoningen, Germany: This archaeological site, also located in Germany, gained fame for the discovery of remarkably well-preserved wooden spears and other artifacts. It is not linked to limestone quarrying.

- Dolni Vestonice, Czech Republic: This site is situated in the Czech Republic and is renowned for its Upper Paleolithic artifacts, including ceramic figurines and dwellings. It does not pertain to limestone quarrying.

Conclusion

In conclusion, the correct answer is option D, Neander Valley, Germany. The Neander Valley is an archaeological site that played a crucial role in the study of human evolution, particularly the discovery of Neanderthals. It is not associated with limestone quarrying.
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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. Where are sinkholes commonly found?

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. ________ form on the surface of limestones through solution.

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. ________ form on the surface of limestones through solution.

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. Where are sinkholes commonly found?

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_________.

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An archaeological site, which was used for quarrying limestone was:a)Chesowanja, Kenya.b)Schoningen, Germany.c)Dolni Vestonice, Czech Republic.d)Neander Valley, Germany.Correct answer is option 'D'. Can you explain this answer?
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