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Oxford Cambridge and RSA Monday 23 May 2016 Morning AS GCE GEOLOGY F792/01 Rocks Processes and Products *6008024131* Candidates answer on the Question Paper. OCR supplied materials: None Other materials required: Ruler (cm/mm) Protractor Electronic calculator Duration: 1 hour 45 minutes * F 7 9 2 0 1 * INSTRUCTIONS TO CANDIDATES Write your name, centre number and candidate number in the boxes above. Please write clearly and in capital letters. Use black ink. HB pencil may be used for graphs and diagrams only. Answer all the questions. Read each question carefully. Make sure you know what you have to do before starting your answer. Write your answer to each question in the space provided. If additional space is required, you should use the lined page(s) at the end of this booklet. The question number(s) must be clearly shown. Do not write in the bar codes. INFORMATION FOR CANDIDATES The number of marks is given in brackets [ ] at the end of each question or part question. Where you see this icon you will be awarded a mark for the quality of written communication in your answer. You may use an electronic calculator. You are advised to show all the steps in any calculations. The total number of marks for this paper is 100. This document consists of 20 pages. Any blank pages are indicated. [H/500/8417] DC (LK/SW) 125449/1 OCR is an exempt Charity Turn over

2 Answer all the questions. 1 (a) Sedimentary rocks are classified into clastic and non-clastic rocks. (i) Describe the term clastic.... [1] Non-clastic sedimentary rocks are divided into two types based on how they form. State the two types of non-clastic rocks. 1... 2... [1] (b) (i) Grain size coarse Complete the classification diagram below by entering the names of the correct clastic sedimentary rocks in boxes A, B, C and D. Composition Grain shape Rocks rock (lithic) fragments quartz cement or matrix angular rounded A B >90% quartz well-rounded orthoquartzite medium 25% K feldspar 50% quartz 25% rock (lithic) fragments sub-angular to sub-rounded C 25% clay matrix 50% rock (lithic) fragments and other minerals 25% quartz sub-angular to sub-rounded D fine 90% mineral E 10% quartz too fine to observe shale [4] State the range of sizes used to define medium grains in sedimentary rocks.... [1] (iii) Identify mineral E that is found in the fine-grained clastic rocks.... [1]

(iv) 3 Use labelled diagrams to show the difference between angular and rounded grains. angular rounded [1] (c) (i) Describe three characteristics of desert sandstone. 1... 2... 3... Describe three characteristics of sandstone formed in a fluvio-glacial environment. 1... 2... 3... (d) Complete the following sentences by writing the correct terms in the spaces. Choose terms from the list below. Each term should be used only once or not at all. bioclastic calcite coccoliths concentric crinoids quartz nucleus oolite In... limestone, 75% of the rock is composed of shell fragments and the rest of the rock is a mineral cement of.... Chalk is composed of.... A limestone formed in shallow seas where tidal action or currents have moved particles is called... limestone. It has... layers of calcium carbonate around a.... [4] [Total: 17] Turn over

2 The diagrams below show features of three types of volcanic eruptions F, G and H. 4 Volcanic eruptions Simplified cross-section of volcanoes Volcanic products Tick ( ) if present 0.5 km lava F tuff ignimbrite G 0.5 km lava tuff H 0.5 km ignimbrite lava tuff ignimbrite (a) (i) Complete the table using ticks ( ) to show which volcanic product or products are formed by each volcanic eruption type. [3] Identify the point on the VEI scale for each volcanic eruption type F, G and H. Use the information in the table below and the diagrams of the volcanic eruption types above. Write F, G and H once only in the correct boxes in the last column of the table. VEI scale Ejecta volume (km 3 ) Description Cloud column height (km) Frequency 0 < 0.0001 effusive effusive < 0.1 constant Volcanic eruption type 1 > 0.0001 effusive gentle 0.1 1 daily 2 > 0.001 explosive severe 1 5 weekly 3 > 0.01 explosive violent 3 15 few months 4 > 0.1 explosive cataclysmic 10 25 H 1 yr 5 > 1 explosive paroxysmal 20 35 H 10 yrs 6 > 10 explosive colossal > 30 H 100 yrs 7 > 100 explosive mega-colossal > 40 H 1000 yrs 8 > 1000 explosive apocalyptic > 50 H 10 000 yrs

(b) (i) Describe how an ignimbrite forms. 5... Describe how an agglomerate forms.... (c) Describe the stages of caldera formation during and after final eruption. You should use labelled diagrams. Labelled diagrams During final eruption Description After final eruption [4] [Total: 13] Turn over

3 The graph below shows the crystal size and silica percentage for three igneous rocks. 80 6 75 70 granite SiO 2 % 65 60 55 50 basalt gabbro 45 0 1 2 3 4 5 6 7 8 9 crystal size (mm) (a) (i) On the graph, clearly plot and label the rocks andesite and dolerite. State the minerals found in the rocks gabbro and granite that are used to classify them. gabbro... granite... (iii) Describe the relationship between the rock colour and mineral content of gabbro and of granite. gabbro... granite... (iv) Explain why silica composition is not used to identify igneous rocks in the field.... [1]

7 (b) Indicate whether the following statements apply to lava flows or sills or both. Use ticks ( ) in the correct column(s). The first statement has been completed for you. Feature seen lava flow sill forms a concordant feature crystal size is 1 to 5 mm crystallisation has taken place more than 1 km below the surface has two baked margins may have a weathered surface the rate of cooling is measured in days or weeks [4] (c) (i) Draw a fully labelled diagram to show vesicular texture in basalt. Show an appropriate scale in mm. Describe how porphyritic texture forms in granite.... [Total: 15] Turn over

4 (a) The diagrams below show cross-sections of two sedimentary structures J and K. 8 sedimentary structure J sedimentary structure K 0 5 cm 0 5 cm (i) Identify structure J and explain how it forms. identification... formation... Identify structure K and explain how it forms. identification... formation... (b) In the space below, draw a labelled cross-section to show imbricate structure. Draw an arrow to show the direction of the current that formed the imbricate structure that you have drawn. imbricate structure

9 (c) The cross-section diagram below shows sedimentary structures that were formed by turbidity currents on the deep sea floor. rock L rock M 0 10 cm (i) Identify these sedimentary structures.... [1] Describe how these sedimentary structures form.... (iii) Name the two rocks L and M that are shown on the diagram. rock L... rock M... (d) Explain how an alternating sequence of rocks L and M forms................... [3] (e) Calcareous ooze forms on the deep sea floor. Describe how it forms............. [Total: 16] Turn over

10 5 (a) State the meaning of the term polymorph....... [1] (b) The graph below shows the stability fields of the Al 2 SiO 5 polymorphs. temperature ( C) 0 100 200 300 400 500 0 600 700 800 0 1 2 andalusite 5 3 pressure (kb) 4 5 kyanite sillimanite 10 depth (km) 6 15 7 8 20 (i) Plot the kyanite / sillimanite boundary line using the data that at 8 kb pressure the temperature will be 600 C. [1] State which of the minerals will be found in high-grade regional metamorphic rocks.... [1] (iii) State the polymorph that will form at 15 km depth if the geothermal gradient is 30 C / km.... [1] (c) Explain how paired metamorphic belts form by regional metamorphism at a convergent plate boundary where subduction is taking place.............

11 (d) The thin section diagrams below show rocks N and P produced by regional metamorphism. (i) Identify and describe the texture of rock N and explain how this texture formed. Rock N quartz garnet muscovite 0 5 mm texture identification... texture description... texture formation... [3] Rock P Identify and describe the texture of rock P and explain how this texture formed. quartz K feldspar biotite hornblende 0 5 mm texture identification... texture description... texture formation... [3] [Total: 12] Turn over

12 BLANK PAGE PLEASE DO NOT WRITE ON THIS PAGE

6 (a) (i) Describe the division of the geological column into eras and systems. You may use examples in your answer. 13 era... system... State the two principles of dating that are used to construct the geological column. 1... 2... [1] (b) The table below shows historic eruption data from the Icelandic volcano Hekla. Date of historic eruption Silica % of lava Time from previous eruption (years) 1510 63 121 1597 61 87 1636 58 39 1693 58 57 1766 60 73 1845 60 79 1947 63 102 1970 55 23 1991 54 21 2000 9 (i) Estimate a possible silica % value for the eruption in 2000.... [1] Calculate the average silica % of all the lavas erupted from 1510 to 1991.... [1] (iii) Use data from the table and your knowledge of the process of magmatic differentiation to explain why eruptions of Hekla vary in silica % over time.... [Total: 7] Turn over

14 7 Describe the main processes of the rock cycle operating at and just below the surface to a maximum depth of 500 m. Diagrams are not required in your answer. In your answer you must describe the effects of named processes of the rock cycle and use technical terms where appropriate.

15... [10] [Total: 10] Turn over

16 8 Describe the effects of contact metamorphism produced by a granite batholith on surrounding beds of shale and limestone. You may use diagrams to illustrate your answer. In your answer you should describe the characteristics and distribution of the rocks around the granite batholith formed by contact metamorphism at different grades.

17... [10] [Total: 10] END OF QUESTION PAPER

18 ADDITIONAL ANSWER SPACE If additional space is required, you should use the following lined page(s). The question number(s) must be clearly shown in the margin(s).

19

20 Oxford Cambridge and RSA Copyright Information OCR is committed to seeking permission to reproduce all third-party content that it uses in its assessment materials. OCR has attempted to identify and contact all copyright holders whose work is used in this paper. To avoid the issue of disclosure of answer-related information to candidates, all copyright acknowledgements are reproduced in the OCR Copyright Acknowledgements Booklet. This is produced for each series of examinations and is freely available to download from our public website (www.ocr.org.uk) after the live examination series. If OCR has unwittingly failed to correctly acknowledge or clear any third-party content in this assessment material, OCR will be happy to correct its mistake at the earliest possible opportunity. For queries or further information please contact the Copyright Team, First Floor, 9 Hills Road, Cambridge CB2 1GE. OCR is part of the Cambridge Assessment Group; Cambridge Assessment is the brand name of University of Cambridge Local Examinations Syndicate (UCLES), which is itself a department of the University of Cambridge.