physical fieldwork Flashcards

1
Q

title of geographical enquiry

A

how are coastal processes shaping the beach at Porlock Bay?

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1
Q

where is Porlock bay

A

In south-west England, in west Somerset

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2
Q

why was this location suitable for our enquiry

A
  • a site of longshore drift
  • coastal processes made an impact at the beaches on either side of bay
  • clear difference to compare
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3
Q

what are the steps of a geographical enquiry

A
  • introduction and planning
  • methods and data collection
  • data presentation and analysis
  • conclusion and evaluation
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4
Q

what is longshore drift

A

the process where waves transport eroded material along a beach in a zigzag motion, and deposit it further down the coast

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5
Q

meaning of tenuous

A

lacking sound reasoning, weak (a tenuous argument)

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6
Q

name some risks and ways to avoid

A

Drowning - maintain a 3m distance from the water at all times
Slipping/ twisted ankles - wear appropriate footwear and don’t run
Hypothermia - wear appropriate clothing (thermals, hats), and have an extra layer at all times
Illness from rain - bring a waterproof layer

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7
Q

how does secondary data help plan a coastal fieldwork enquiry

A

Provides a time-efficient source of information on the wave and wind direction, the geology and the coastal processes of the area. We can use these to choose a location where there will be a clear change in results, dependant on where we are measuring (in this case, a difference in average sediment size and beach profile at the headlands)

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8
Q

what direction is longshore drift going in porlock bay

A

eastward

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9
Q

name of the headlands at porlock bay

A

Gore point (west one), Hurlstone point (east one)

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10
Q

How did we measure beach profile

A

Did stratified for location, and systematic for beach profile itself. We set up a reference point on a reference person for the clinometer. We stationed the reference person 5m up the slope. Measured the angle with the clinometer and wrote it down. Moved the clinometer up 5m, and the reference person up 5m and repeated measuring process. Did this until we reached the top of the slope.

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11
Q

What was our justification for beach profile method

A
  • systematic distancing between measurements eradicated bias
  • enabled us to cover the whole slope
  • we could compare the beach profiles at either end of bay with same measurements
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12
Q

how did we ensure accurate results for beach profile method

A
  • kept tape measure taut
  • used the same person as reference
  • used the same person measuring
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13
Q

what were limitations of beach profile method

A
  • would not have gotten minor changes in gradient (no changes within 5m)
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14
Q

how did we measure sediment size

A

We selected a random rock at regular, systematic intervals and measured the A-axis (longest side) with a calliper. We wrote down the measurements and repeated this process every 5m

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15
Q

justification for sediment size method

A

allowed us to cover whole slope
reduced bias (random selection)

16
Q

how did we ensure accuracy for sediment size method

A
  • callipers increase accuracy of measurement (more than a ruler)
  • had same person measuring
  • used different people to pick rock so it was more random and reduces bias
  • measured multiple rocks so there’s a large sample size
17
Q

what were the limitations of the sediment size method

A
  • only measured one side/axis
  • some bias in the fact that people picking rock (instead of computer)
18
Q

how did we measure sediment shape

A

We selected a random rock at regular, systematic intervals and used the power’s index of roundness to decided how rounded/ angular. We wrote down the score and repeated this process every 5m

19
Q

justification for sediment shape method

A
  • allowed us to cover whole slope
  • reduces bias (random selection)
  • tried to quantify something quite subjective
20
Q

how did we ensure accuracy/reliability in sediment shape method

A
  • same person judging roundness of rock
  • measured multiple pebbles (large sample size)
  • different ppl randomly selected pebbles, so less bias
21
Q

limitations of sediment shape method

A

subjective (not a clear scale, based on opinion)

22
Q

Advantages of random sampling

A
  • can cover larger area
  • eradicates bias
23
Q

disadvantages of random sampling

A
  • can lead to poor representation of population
  • may not be time efficient
24
advantages of systematic sampling
- good coverage of study area - simplest method than others
25
disadvantages of systematic sampling
- slightly more biased (not all points have even chance of being chosen) - could lead to over or under representation - time consuming
26
advantages of stratified sampling
- can be used along the others - if supported by secondary data, can be more representative of the population - time efficient
27
disadvantages of stratified sampling
- need secondary data to have accurate representation
28
how can sample size affect results
often, the larger the sample size, the less reliable the results, because it's harder to collect data that represents the population
29
Give advantages and disadvantages of beach profile sketches
Good visual representation, so easy to compare There's no axis so hard to compare actual, numerical data
30
Give advantages and disadvantages of geolocated proportional circles
GIS is very quick to produce graphic. Easy, visual comparison. Data is associated with specific location. Difficult to calculate actual value of circle. Size of circle may obscure location, or mean less accurate location. If there' a lot of data collected, circles may overlap, and be hard to read
31
Give advantages and disadvantages of radar graphs
Easy to visually compare data, it's on the same scale. Scale is not clear to read all the way around the graph, the points aren't labelled with values, making it harder to read.
32
Give advantages and disadvantages of box and whisker dispersion graphs
Easy to visually compare sediment size at each beach. Clearly shows min and max. Lack of x-axis may be confusing.