Study Photograph A, which shows part of Mount Pinatubo, a volcano in the Philippines, ten years after the 1991 eruption.

Describe the features of Mount Pinatubo shown in Photograph A.   [4]

Study Photograph C and Fig. 4, which show scences of Aguas Calientes.

Using Photograph C and Fig. 4, explain how the local people might benefit from tourism.  [5]

Study Figs. 3 and 4, which show Anak Krakatoa, a volcanic island between Sumatra and Java.

Use the information on Figs. 3 and 4 to describe the shape and characteristics of Anak Krakatoa.  [4]

Study Fig. 5, which shows the changing pattern of world tourist arrivals in 1990  and 2013.

Compare the increases in international tourist arrivals in the five areas shown on Fig. 5 between 1990 and 2013.  [5]

Study Fig. 4, which shows the contributions to global carbon dioxide emissions by selected countries from 1800 to 2015.

Describe how the contributions to global carbon dioxide emissions by selected countries have changed over time. Use Fig. 4 to support your answer.  [4]

Study Fig. 3, which shows the shape and height of land before and after a landslide caused by an earthquake.

Use Fig. 3 to describe how the landslide changed the shape and height of the land.   [4]

Study Fig. 2, which shows selected world climate zones.

Use Fig. 2, describe the global distribution of the equatorial (also try cool temperate climate if you can).  [4]

Study Figs. 4 and 5. Fig. 4 shows tectonic plates and plates boundaries. Fig. 5 shows the distribution of fold mountains and volcanoes.

Using Figs. 4 and 5, describe how similarities and differences in the distribution of fold mountains and volcanoes are influenced by different types of plate boundaries.  [4]

Study Fig. 3, which shows the degree of shaking during an earthquake in Christchurch in New Zealand in 2011.

Describe the pattern of shaking shown in Fig. 3.  [4]

Study Fig. 3, which shows average winter temperature in China.

Describe and explain the difference in average winter temperatures along the line AB on Fig. 3.  [5]

It has steep sides and has a narrow summit,forming a cone shape

The magma is more viscous in stratovolcanoes than shield volcanoes as it has more silica content

It has violent eruptions due to dissolved gases not being able to escape the magma and building up over time.

• locals are provided with income from tourist spending on consumer goods and services.

•This boost in the local economy provides an incentive for locals and planning authorities to preserve culture.

•also enhanced cultural ecosystem services.

•As seen in photograph C where the locals in peru are selling their locally made goods with traditional designs

Most of the severe shaking is more localised and is concentrated primarily in the epicentre which is in the main built-up area.

Most of the minor shaking is spread out outside of the main built up area as far as 25km away from epicentre.

However, there are a few locations that experience severe shaking more than 100km from the epicentre.

Before the landslide occured , the upslope of the land was gentle and the downslope was steeper.

The upslope was 2950m at a distance of 500m while downslope was 1800m at a distance of 3450m.

compared to after the landslide, the upslope of the land was steeper and the downslope was gentle.

The upslope was 2950m at a distance of 525m while downslope was 1950m at a distance of 4000m.

• Ash and rocks settle on the sides of Mount Pinatubo.

• There are small magma alternating through layes of ash and lava.

Could describe shape first before moving onto characteristics

Did not refer to Fig 3 or 4

•eg locals can earn money through employment as seen in photograph c

• locals are provided with income from tourist spending on consumer goods and services.

•This boost in the local economy provides an incentive for locals and planning authorities to preserve culture.

•also enhanced cultural ecosystem services.

•As seen in photograph C where the locals in peru are selling their locally made goods with traditional designs

Before the landslide occured , the upslope of the land was gentle and the downslope was steeper.

The upslope was 2950m at a distance of 500m while downslope was 1800m at a distance of 3450m.

compared to after the landslide, the upslope of the land was steeper and the downslope was gentle.

The upslope was 2950m at a distance of 525m while downslope was 1950m at a distance of 4000m.

By comparison, the upslope changes by 25m in distance and the downslope changes by 150m in height and 550m in distance

-The biggest decrease in contribution to global carbon dioxide emissions is from UK, drastically decreasing from 98% to 5%, from 1800 to 2015.

-The smallest increase in contribution to global carbon dioxide emissions is India, which increased from 0% to 2%, from 1925 to 2015, in comparison to United States which had the biggest increase, from 0% to 26%.

-Although both United States and China have an overall increasing change in contributions to global carbon dioxide emissions, China has a constant increase, whereas United States had an even higher contribution in 1950 with a percentage of 40%, before dropping to 26% in 2015.

-Additionally, China increased faster than India, even though both started increasing from 1925, China increased to 12% while India increased to only 2%.

It has steep sides and has a narrow summit,forming a cone shape

The magma is more viscous in stratovolcanoes than shield volcanoes as it has more silica content

It has violent eruptions due to dissolved gases not being able to escape the magma and building up over time.

There is also a forest located on the far eastern side of the island, a rock face located on the east side of the volcano

The contours increases going down the volcano from a steep slope at 200 contours to a gentler slop at 100 contours