Snowdonia Case Study Flashcards

1
Q

What is the Snowdonia or Eryri National Park?

A

The Snowdonia or Eryri National Park is the third National Park established in England and Wales, covering an area of 2,171 km2 (838 square miles) in North Wales. It includes the Carneddau and Glyderau mountain ranges and Mount Snowdon, the highest mountain in England and Wales.

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2
Q

When was the Snowdonia National Park established?

A

The Snowdonia National Park was established in 1951.

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3
Q

What is the purpose of classifying an area as a National Park?

A

The purpose of classifying an area as a National Park is to preserve and enhance places of outstanding natural beauty and provide public access for recreation and tourism while maintaining their natural beauty.

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4
Q

What are some economic activities in Snowdonia National Park?

A

Some economic activities in Snowdonia National Park include farming, forestry, quarrying, and the tourism industry.

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5
Q

Who oversees the activities in Snowdonia National Park?

A

The activities in Snowdonia National Park are overseen by The Nature Conservancy Council, which works in conjunction with the park’s inhabitants to preserve the unique environment and beauty of the area.

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6
Q

What makes Snowdonia attractive to tourists?

A

Snowdonia is attractive to tourists because of its spectacular upland environment, shaped by its geological past and the effects of the last Ice Age.

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7
Q

What geological events shaped the landscape of Snowdonia?

A

The landscape of Snowdonia was shaped by volcanic activity, folding, and sedimentary deposition during the Cambrian, Ordovician, and Silurian eras, which occurred between 500 and 395 million years ago.

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8
Q

What major uplift event transformed the landscape of Snowdonia?

A

The Caledonian earth movements, which occurred at the end of the Silurian period, caused major uplift and transformed the landscape of Snowdonia into the upland area seen today.

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9
Q

How have the mountains of Snowdonia changed over time?

A

The mountains of Snowdonia were once much higher but have since been eroded into a lower, yet still rugged, landscape through aerial (climatic) and fluvial (water) erosion. The effects of ice have also had a major impact on the land surface.

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10
Q

What is glaciation?

A

Glaciation refers to the formation and movement of glaciers and ice sheets during an ice age.

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11
Q

When was the most recent ice age in Snowdonia?

A

The most recent ice age in Snowdonia occurred as recently as 10,000 years ago.

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12
Q

What conditions are necessary for an ice age to develop?

A

For an ice age to develop, a small drop in temperature is needed, resulting in winter snowfall that does not fully melt during the following summer. This leads to the accumulation of snow, which eventually compresses into ice.

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13
Q

How did ice affect the landscape of Snowdonia?

A

During the ice age, ice accumulated on the higher, cooler slopes of Snowdonia and flowed down the former river valleys under gravity. This fundamentally altered the landscape of the area.

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14
Q

Where did the ice surrounding the Snowdonia ice cap originate from?

A

The ice surrounding the Snowdonia ice cap originated from the Irish Sea.

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15
Q

What led to conflict during the formation of the Snowdonia ice?

A

Some of the Snowdonia ice was blocked in its path to the lowlands while elsewhere it radiated outwards, leading to conflict.

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16
Q

Which directions did the Snowdonia ice flow?

A

The Snowdonia ice flowed eastwards to the Shropshire – Cheshire Plain, north into the Irish Sea, and westwards into Cardigan Bay.

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17
Q

What is the estimated maximum depth of the Snowdonia ice?

A

The maximum depth of the Snowdonia ice has been estimated at over 1,000 meters.

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18
Q

What happened when the Snowdonia ice met other ice sheets?

A

When the Snowdonia ice met other ice sheets that had accumulated and flowed away from the Lake District and southern Scotland, it caused major erosion.

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19
Q

What evidence supports deposition in the area of Llandudno?

A

The presence of erratics, which are rocks of a different geological origin from the area in which they are currently found, supports deposition in the area of Llandudno.

20
Q

What is an example of an erratic found in the Llandudno area?

A

Erratics in the Llandudno area have been identified as originating in the Lake District and the Firth of Clyde.

21
Q

What paths did the Snowdonia ice follow?

A

The Snowdonia ice followed the routes cut by rivers as the easiest path.

22
Q

How does the movement of ice affect the landscape?

A

The movement of ice can significantly alter the landscape over which it flows due to its solidity and bulkiness compared to water particles.

23
Q

What are some classic glacial features found in Snowdonia?

A

Some classic glacial features found in Snowdonia include pyramidal peak (Mount Snowdon), arête (Tryfan), Cwm (corrie or cirque) (Cwm Idwal), U-shaped valley/glacial trough (Nant Ffrancon), ribbon lake (Llyn Ogwen), hanging valley (Nant Ffrancon), truncated spurs (Nant Ffrancon), and Roche moutonnée (Nant Ffrancon).

24
Q

What processes led to the formation of a classic glaciated upland landscape?

A

The four erosional processes that led to the formation of a classic glaciated upland landscape are listed in Figure 4.

25
Q

What is a cwm and how is it formed?

A

A cwm is an armchair-shaped hollow that is usually found on sheltered north-facing slopes, at angles between 310 and 120 degrees. It is formed where ice accumulated and freeze-thaw and possibly chemical weathering acted at the base of the ice. Rotational movement and frost shattering aided this process and scoured out a deeper floor.

26
Q

What is an arête and how is it formed?

A

An arête occurs where two corries form, one on each side of a mountain or ridge.

27
Q

What is a pyramidal peak and how is it formed?

A

A pyramidal peak forms where three corries form on all sides of one mountain and are separated by three ridges.

28
Q

Which valley perfectly displays the classic U-shaped valley associated with upland glaciated areas?

A

The Nant Ffrancon Valley (GR 6460 to 6363) perfectly displays the classic U-shaped valley associated with upland glaciated areas.

29
Q

What are truncated spurs and what do they represent?

A

Truncated spurs (GR 640611) are the remnants of the interlocking spurs of the original river valley. They were eroded as the ice forced a straighter, more efficient path to the Irish Sea.

30
Q

What are hanging valleys and what do they indicate?

A

Hanging valleys (e.g., GR 637627) mark the old upper courses of rivers which were either not affected by ice or only affected by smaller glaciers. They indicate that these rivers did not erode to the depth of the main glacial valley or trough.

31
Q

What is a roche moutonnée and how is it formed?

A

A roche moutonnée is formed where a hard volcanic dike protrudes from the floor of the valley. It is smoothed on the upstream side but made rugged by plucking and abrasion of the rock on the downstream side. It displays the area’s varied geology and the effects of ice both plucking and abrading the rock.

32
Q

What type of lake is Llyn Ogwen?

A

Llyn Ogwen is a ribbon lake.

33
Q

How did Llyn Ogwen form?

A

Llyn Ogwen occupies a glacial valley floor and follows the shape of the valley. It extends from the lip of the Ogwen Falls in the glacial hollow created by the Irish Sea ice sheet. The lake itself is a post-glacial feature but indicates the effect the ice had in creating a hollow as it flowed over the landscape.

34
Q

What resource would be useful in locating these features using grid references?

A

Referring to a copy of the OS 1:50,000 map sheet 115 of Snowdonia would be useful in locating these features using grid references.

35
Q

What marks the watershed or division between two river basins, linking Cwm Idwal with the Nant Ffrancon valley?

A

The Ogwen Falls (Figures 8 and 9) mark the watershed or division between two river basins, linking Cwm Idwal with the Nant Ffrancon valley.

36
Q

Why did the ice flow divert towards the north-west and enter the Ffrancon Valley instead of flowing down the Ogwen valley?

A

The ice’s route down the Ogwen valley was blocked by the Irish Sea ice sheet, so it diverted towards the north-west and flowed over the Ogwen watershed, entering the Ffrancon Valley instead.

37
Q

What marks the breach from one former river system into another at the Ogwen Falls?

A

The breach from one former river system into another is marked by a steep waterfall at the Ogwen Falls.

38
Q

What are some features of deposition seen in Snowdonia?

A

Features of deposition seen in Snowdonia include glacial till and moraines.

39
Q

What is till?

A

Till refers to the unsorted mix of rocks, stones, and boulders found on most valley floors.

40
Q

What has largely washed away the glacial till remnants on the lower slopes in Snowdonia?

A

Post-glacial river activity has largely washed away the glacial till remnants on the lower slopes in Snowdonia.

41
Q

What do the remnants of glacial till contain?

A

The remnants of glacial till contain a mixture of unsorted materials, both angular and rounded in shape, indicating the effects of both ice and water.

42
Q

What does Figure 10 on page 4 show in Snowdonia?

A

Figure 10 on page 4 shows the Mount Snowdon area and displays the features associated with a glacial landscape.

43
Q

How can you match the features on the sketch in Figure 10 with the features on the OS map in Snowdonia?

A

You can match the features on the sketch in Figure 10 with the features on the OS map in Snowdonia by comparing the shapes of the features.

44
Q

What type of landscape is Snowdonia?

A

Snowdonia is a dynamic landscape that is constantly changing.

45
Q

What climatic conditions could cause the whole landscape of Snowdonia to be covered with ice once again?

A

Climatic conditions may return, which could cause the whole landscape of Snowdonia to be covered with ice once again.