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Refer to blocks D3 and E3 - NSC Geography - Question 2 - 2017 - Paper 2

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Refer to blocks D3 and E3. 2.1.1 Calculate the vertical interval (VI) between M and spot height 1 395 in metres. Show ALL calculations. Marks will be awarded for ca... show full transcript

Worked Solution & Example Answer:Refer to blocks D3 and E3 - NSC Geography - Question 2 - 2017 - Paper 2

Step 1

Calculate the vertical interval (VI) between M and spot height 1 395

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Answer

To calculate the vertical interval (VI):

  1. Identify the height of point M, which is 1 500 m.

  2. Identify the spot height of 1 395 m.

  3. Using the formula:

    VI=1500extm1395extm=105extmVI = 1 500 ext{ m} - 1 395 ext{ m} = 105 ext{ m}

    Therefore, the vertical interval (VI) is 105 m.

Step 2

Calculate the horizontal equivalent (HE) between M and spot height 1 395

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Answer

To calculate the horizontal equivalent (HE):

  1. The horizontal equivalent is determined using the formula:

    HE=1.5extcmimes500extm=750extmHE = 1.5 ext{ cm} imes 500 ext{ m} = 750 ext{ m}

    The measurement range for this calculation is considered as 500 m, which fits within the range of 700 to 800 m. Therefore, the horizontal equivalent (HE) is 750 m.

Step 3

Using the information in QUESTIONS 2.1.1 and 2.1.2, calculate the average gradient

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Answer

To calculate the gradient between M and spot height 1 395:

  1. Use the gradient formula:

    Gradient=VerticalInterval(VI)HorizontalEquivalent(HE)Gradient = \frac{Vertical Interval (VI)}{Horizontal Equivalent (HE)}

    Substituting in the values calculated:

    Gradient=105extm750extm=0.14Gradient = \frac{105 ext{ m}}{750 ext{ m}} = 0.14

    Thus, the average gradient is approximately 0.14.

Step 4

Would the gradient calculated in QUESTION 2.1.3 result in a low or high stream velocity?

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Answer

Answer: High velocity.

Reason: The average gradient is steep, therefore the water will flow faster. A steeper slope indicates that over a short distance, the elevation changes quickly, contributing to a higher stream velocity as observed in the gradient calculated.

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