- •Preface
- •Content
- •Unit 5- igneous rocks 96
- •Part 2 - continental crust 172
- •Unit 1 geology
- •1. Comprehension
- •Fig. 1. James Hutton (1726-1797)
- •2. Reading comprehension Read the text «What is Geology?»
- •2. 1 Vocabulary
- •Text: What is Geology?
- •2.2 Exercises
- •2.2.2 Translate into Russian:
- •2.2.3 Complete the sentences:
- •2.2.6 Match the word phrases in right column with the word phrases in the left one and compile your own sentences.
- •2.2.7 Give the English equivalents to the Russian words:
- •2.2.8 Read the text and find the English equivalents to the following terms and phrases.
- •2.2.9 Match the science with the description of what it studies:
- •2.2.10 Choose the correct variant.
- •3. Discussion
- •4. Wordlist
- •4.1 Pronunciation
- •4.2 Terms
- •Unit 2 fossils
- •1. Comprehension
- •1.1 Vocabulary
- •3. Pay attention to the underlined terms and expressions in the text:
- •Channel канал
- •2. Exercises
- •2.1 Mark the stressed syllable on the following words from the text:
- •2.3. Give the Russian equivalents to the following word combinations and phrases:
- •2.4 Read the text below and think of the word that best fits each space. Use only one word in each space. There is an example at the beginning.
- •2.5 Form nouns from the following verbs and find the sentences in the text with these new words.
- •2.6 Put a preposition in each of the numbered spaces:
- •2.7 What are the corresponding words?
- •2.8 Choose between the alternatives to complete these sentences:
- •(1) Petrify (2) organ (3) decompose (4) effect (5) cover (6) compact (7) lithify (8) reduce (9) react (10) fossil
- •3. Reading comprehension
- •3.1. Detailed reading: Relative Dating: Using Rocks
- •3.2.1 How to Treat a Fossil in Geological Fieldwork
- •4.1 Read the following text and pay special attention to the pronunciation of the geological periods. The Geological Column
- •Geologic Time Scale
- •History of the time scale
- •Terminology
- •Table 1. Geologic Time Scale
- •4.2 Read the texts “Geological Time Scale» in self-study booklet, pg. 58) Choose one period and using the following plan, make a short report.
- •5. Listening comprehension
- •5.1. You will hear a radio report about fossils. Answer statements 1-10 by writing t (for True) and f (for False):
- •5.2. Listen to the report once more. Then, for statements 11-20, complete the notes that summarize what the speaker says. You will need to write a word or a short phrase in each box.
- •6. Discussion (r.P – 2.1)
- •Communicative formulas
- •7. Wordlist
- •7.1. Pronunciation
- •7.2 Terms
- •7.3 Words and phrases
- •Unit 3 sizing up the earth
- •1. Comprehension
- •1.1 Vocabulary
- •1.2 Read the text «Our layered planet» and pay attention to the terms in bold (r.P – 3.4, 3.5) our layered planet
- •Fig. 7. Differentiation of early Earth
- •2.4 State whether the following statements are true or false.
- •3.1.2 Read the text once more and fill in the chart with the necessary information. Then label the diagram and give an explanation what each item means.
- •3.2 Detailed reading - Earth’s size and shape
- •Isostasy
- •Fig. 10. Relative abundance of elements in whole Earth
- •Fig. 11. Relative abundance of elements in Earth’s crust
- •4. Listening comprehension
- •4.3. You will hear a lecture on the Earth’s origin. For statements 16-20, choose the best answer a, b, c, d.
- •5. Discussion: (r.P – 3.1, 3.3)
- •1. Situational game-
- •2. The earth
- •6. Wordlist
- •6.1 Pronunciation
- •6.2 Terms
- •Unit 4 rocks and minerals
- •1. Comprehension
- •Definitions
- •Fig. 12. Rock cycle
- •1.3 Read the following text and fulfill the after task exercises the rock cycle
- •Vocabulary
- •2. Exercises
- •2.3 Spelling dictation
- •2.4 Read the following definition and fill in the gaps with the missing words and then give a short outline of this definition. (r.P – 8.2.12)
- •Fig. 13. Rock cycle
- •3. Reading comprehension
- •3.1 Scanning: Earth’s building blocks (r.P – 4.2)
- •3.1.1 Pay attention to the pronunciation of the following minerals:
- •3.1.2 Find the information you need to complete the following diagram from the text below.
- •Table 2. Chemical Grouping and Composition of Some Common Minerals
- •3.1.3 Complete the following chart. Give examples of each type of rock forming mineral.
- •3.2 Informative reading- Minerals and their physical properties.
- •Part 1 Minerals
- •3.2.2 Read the text and fulfill the after-reading exercises. (r.P – 4.3, 4.6) Physical Properties
- •Table 3 Mohs Hardness Scale
- •Fig. 18. Pyrite cube showing metallic luster (Photo by John Bett) Fig. 19. Vitreous luster on quartz crystal faces (Photo by John Bett)
- •3.2.2.3 Give examples of the following physical properties of minerals
- •Fig. 24. Conglomerate – sedimentary rock
- •4. Listening comprehension
- •5. Discussion
- •5.1 Complete the mind map. Discuss the following questions:
- •5.2 Exploratory speaking (short talk)
- •Use the mind-maps and the table below. Don’t forget communicative formulas. Communicative formulas
- •Table 4. Rocks and minerals
- •6. Wordlist
- •6.1 Pronunciation
- •6.2 Terms
- •6.3 Words and phrases
- •Igneous rocks
- •1. Comprehension Read the following text «Anatomy of a volcano»
- •1.1 Vocabulary
- •1.2 Anatomy of a volcano Pay attention to the following terms in bold. (r.P. – 5.3)
- •2. Exercises
- •2.1 Read the text (once) more carefully and choose the correct alternative for these words:
- •Round-formed opening
- •2.2 Use two words from the corresponding line to complete each sentence.
- •2.3. Give the Russian equivalent the following phrases:
- •2.4 Match the words in the right column with the words in the left one.
- •2.5 Use the terms and fill in the gaps
- •3. Reading comprehension
- •3.1 Scanning - Igneous rocks (r.P. -5.5)
- •Fig. 26. Classification of igneous rocks
- •3.1.1. Correct the following statements where necessary (Igneous rocks)
- •3.1.2. You have one minute to read this part of the text -Classification and chemical differentiation of igneous rocks
- •3.2 Informative reading – Igneous Rocks (r.P.-5.4)
- •Fig. 27. Various modes of occurrence of igneous rocks
- •3.2.2 Can these terms and phrases be understood without translating? Why?
- •3.2.3 State, which sentences, is t (true) or f (false) according to the text.
- •3.2.6 Complete the following sentences, using words and phrases from the text.
- •3.2.7 Answer the following questions and give more / extra information.
- •4. Listening comprehension
- •4.1 You will hear a radio report about volcanic rocks. Answer statements 1-10 by writing t (for True) and f (for False):
- •4.3 Listen to the lecture in geology at the Aberdeen University. The topic of the lecture is intrusive igneous rocks. Complete the following chart with the missing information.
- •Igneous Rocks- Intrusive
- •4.4. Listen to the lecture once more. Look at the diagram and describe the features produced by intrusive rocks, using the given definitions:
- •5. Discussion
- •Fig. 28. Shapes of volcanoes
- •6. Wordlist
- •6.1 Pronunciation
- •6.2 Terms
- •Unit 6 sedimentary rocks
- •Comprehension
- •1.1 Vocabulary
- •1.2 Read the text and fulfill the after reading exercises (r.P – 6.1)
- •Fig. 29. Breccia
- •Exercises
- •2. 2 Read the following phrases, write down the word. Read the word and find sentences with this word.
- •2.3 Match the verb with the noun. (Add the preposition where necessary)
- •2.4 Complete the following sentences, by unscrambling the bolded words. Spell the word. Give its definition.
- •2.5 There is a spelling mistake in each line. Write the correct word in the space provided. Prepare for a spelling dictation.
- •2.6 Fill in the space with the appropriate word or phrase.
- •3. Reading comprehension
- •3.1 Scanning
- •3.1.1 Rocks from living things
- •3.1.2 Rocks from chemicals
- •1. Match the words with the Russian equivalent.
- •2. Translate the following word combinations and phrases.
- •3. Compose questions to the text, using the following Wh-words: what, which, where, when, how
- •3.2 Informative reading- Rocks from fragments
- •3.2.1 Read the text (Part 1, Part 2) and for statements 1-12, choose the best answer: a, b, c or d. Then explain the words in bold. Part 1
- •Fig.33. Ferruginous sandstone Part 2
- •B. No bigger than sand grain
- •A. Medium-grained
- •B. Greywacke
- •3.2.2 Read the text once more and fill in the charts with the necessary information from part 1 and part 2. Sedimentary rocks
- •Types of sedimentary rocks
- •3.2.3 Give detailed information to the following questions.
- •3.2.4 Use the following, so as to write a description of sedimentary rocks. Label each description (conglomerate / breccia / rudite)
- •3.3 Detailed reading
- •Text 1 - Sedimentary Rocks
- •Table 5. Classification of Common Sedimentary Rocks
- •3.3.2. Match the English terms with the Russian ones in the right column
- •3.3.3. Match the words from column a with the words in column b.
- •3.3.4. Fill in the blanks with the correct word.
- •3.3. 5. Compile sentences using the following phrases.
- •3.3.6. State whether the following statements are true or false.
- •3.3.7. Answer the following questions.
- •Fig. 36. Sedimentary stages in the rock cycle
- •Fig. 37. Continental, shoreline and marine sedimentary environments
- •Read the following text and fill in the missing words.
- •3.3.9. Complete the following sentences.
- •4. Listening comprehension
- •4.2 You will hear a lecture. You will hear it twice. For questions 6-10 choose the best answer a, b or c.
- •B. Destruction of sedimentary rocks
- •5.2 You have to give a lecture on sedimentary rocks. Use the following diagram.
- •5.3 Group discussion
- •6. Wordlist
- •6.1 Pronunciation
- •6.2 Terms
- •Unit 7 metamorphic rocks
- •1. Comprehension
- •1.1 Vocabulary
- •3. Read the following word formations and remember their pronunciation:
- •1.2 Read the text and fulfill the after reading exercises. (r.P – 7.2, 7.3) metamorphic rocks
- •Fig. 38. Gneiss Fig. 39. Marble
- •Fig. 40. Grade and facies describe metamorphism
- •Table 6. Classification of Common Metamorphic Rocks
- •2. Exercises
- •2.1 Define the following terms with their similar meaning in Russian
- •2.2 Match the English equivalents to the Russian terms.
- •2.4 Fill in the gaps using the word formations.
- •2.7 State whether the following statements are true or false.
- •3. Readng comprehension
- •3.1 Detailed reading: Occurrence and classification of metamorphic rocks
- •3.1.1. State whether the following sentences are t (true) or f (false), according to the information from the text
- •3.2 Informative reading: Metamorphic rocks
- •Fig. 41. Metamorphic facies
- •4. Revision
- •4.1 Choose the correct variant
- •5. Listening comprehension
- •5.1 You will hear part of a lecture. For statements 1- 10, complete the notes, which summarize what the speaker says. You will need to write a word or short phrase in each box.
- •5.2 You will hear a conversation between a student and a teacher in Geology at Aberdeen University. For statements 1-10, choose the best answer a, b, or c.
- •6. Discussion: task 1
- •Communicative formulas
- •7. Wordlist
- •7.2 Terms
- •7.3 Words and phrases
- •Unit 8 the restless crust part 1: oceanic crust
- •1. Comprehension
- •1.1 Vocabulary
- •1.2 Read the text «The Ocean Floor». Pay attention to the diagram. Fulfill the exercises after the text. (r.P – 8.1.1)
- •Fig. 42. Ocean floor
- •2. Exercises
- •2.1 Look at the geographical map and point out the oceans. Name them.
- •2.2 Look at the diagram below and answer the following questions (r.P.- 8.2.1)
- •Fig. 43. Ocean areas and depths
- •2.3 Match the English term with the Russian one.
- •2.6 Look at the (r.P – 8.1.1) cross section of an imaginary ocean. The vertical scale is exaggerated for effect. Name the 10 major features of an ocean floor. Point them out.
- •3. Reading comprehension
- •3.1 After-reading tasks.
- •3.1.1. Look through the text and pick out the terms, which have the following definition.
- •3.1.3. Spreading ridge evolves several stages. Put the words according to the stages. Compose sentences to describe the process. (r.P – 8.1.2, 8.1.3)
- •3.1.4. Put the facts in the correct order which shows how sea floor spreading develops.
- •4. Listening comprehension
- •6. Discussion (r.P – 8.1.5)
- •Earth’s changing surface
- •Fig. 45. Three types of plate boundaries
- •1. Comprehension
- •1.1 Vocabulary
- •1.2 Mountain building (r.P – 8.2.7, 8.2.8, 8.2.9)
- •Fig. 46. Mountain building
- •Fig. 47. Ocean-ocean subduction zone
- •Fig. 48. Ocean-continent boundary
- •Fig. 49. Continent-continent collision
- •2.3 Complete the following short description of mountain building. Scan the text once more.
- •3. Reading comprehension
- •Informative reading: How continents evolve
- •4. Listening comprehension
- •5. Discussion
- •3.1 Comprehension: faults
- •3.1.2 Fault terminology (r.P – 8.3.1.3, 8.3.1.2)
- •Fig. 50. Fault anatomy
- •Fig. 51. Three types of fault motion
- •3.1.3 Exercises
- •1. Match the English term with the Russian variant. (text: Fault terminology)
- •3. Match the term with its definition and then find its translation.
- •4 Fill in the gaps with the missing words.
- •5 Read the following fault types. The look at the diagrams and then try to draw them by heart. And draw a diagram. (r.P – 8.3.1.3, 8.3.1.4)
- •Fig. 52. Fault types
- •6. Here are six definitions. Read the definition, then name the term and give its translation (r.P – 8.3.1.3, 8.3.1.4)
- •3.1.4 Listening comprehension
- •3.2 Comprehension: folds
- •3.2.1 Vocabulary
- •Word formation
- •Fold terminology (r.P. - 8.3.2.1, 8.3.2.3)
- •Fig. 54. Folding structure
- •4. Discussion
- •5. Wordlist
- •5.1 Pronunciation
- •5.2 Terms
- •Appendix test 1 (unit 1- Geology)
- •B. Isaac Newton d. James Hutton
- •Test 2 (unit 2-Fossils)
- •B. Found in
- •Permeation
- •A. How old the rocks are
- •A. Crust rock
- •Test 3 (unit 3-Earth)
- •Test 4 (unit 4 - Rocks and Minerals)
- •Test 5 (unit 5-Igneous Rocks)
- •B. Central
- •A. Circular
- •A. Mafic lava
- •C. Felsic lava
- •Test 6 (unit 6- Sedimentary Rocks)
- •Test 7 (unit 7- Metamorphic Rocks)
- •C. Burial metamorphism
- •Test 8-1 (unit 8- Restless Crust)
- •Test 8-2 (unit 8- Restless Crust)
- •A. Faults
- •References
2. Reading comprehension Read the text «What is Geology?»
2. 1 Vocabulary
1.Pay attention to the pronunciation of the following terms:
geology |
Earth |
palaeoclimatology |
Mesozoic Era |
knowledge |
structure |
microscopic |
palaeonotology |
geochemical |
discipline |
mammoth |
technological |
geophysical |
stratigraphy |
dinosaur |
uniformitarianism |
2. Read the following word formations and remember their pronunciation:
apply-applicable-application |
transport-transportive-transportation |
destroy-destructive-destruction |
develop-development |
literally- дословно |
principally- принципиально |
relatively- относительно |
essentially- существенно |
primarily- главный, основной |
completely- полностью, совершенно |
particularly- особенно |
firstly- во-первых |
especially- особенно |
daily- постоянно |
constantly- постоянно |
considerably- значительно |
reconstruct- восстанавливать |
irregularity- неровность |
predominant- преобладающий |
|
3. Pay attention to the underlined terms and expressions in the text:
crust (Earth) |
кора (земная) |
force (s) |
сила |
endogenous |
эндогенный |
exogenous |
экзогенный |
weathering |
выветривание |
erosion |
эрозия |
transport (of rock material) |
перенос |
to level (v) / level (n) |
выравнивать; уровень, горизонт |
sedimentary rock |
осадочная порода |
geological time |
геологическое время |
remain ( trace) |
остаток, след |
geological process |
геологический процесс |
horizontal movement |
горизонтальное движение |
vertical movement |
вертикальное движение |
earthquake |
землетрясение |
agent |
агент |
alga |
водоросль |
in terms of |
in particular |
it is possible (to+V) |
only recently |
summing up |
by contrast |
Text: What is Geology?
The word geology comes from the Greek language and means literally “science or knowledge of the Earth”. Only recently, this term has been applicable to the Earth as a whole because it is only recently that geochemical and geophysical work has yielded information about the interior of our planet. Geology has to do with the nature and development of the Earth’s crust and particularly with those parts that are accessible or exposed. The structure of the crust is not simple and in the mountain ranges can even be very complex. Events, which happened hundreds of millions of years ago, have to be reconstructed from evidence-direct or indirect- is available.
Geology has been subdivided into several specialized disciplines and only drawing on information from several disciplines can often solve problems.
Classical geology seeks to interpret the events of the past in terms of processes, which occur at present, and thereby it is possible to attempt to reconstruct the forces that were at work in the past.
The uppermost part of the crust is affected by two different kinds of forces. Firstly, there are endogenous forces that originate within the Earth. The crust is never completely at rest because of movements resulting from these endogenous forces. Everything is in motion. Volcanic activity, earthquakes and the fact that the crust is constantly subjected to vertical and horizontal movements that can be observed from satellites are among the more obvious expressions of these endogenous forces.
The form of the Earth’s surface is the result of a balance between the endogenous forces and exogenous forces that act at the Earth’s surface and do not derive from within it. The most obvious effects of such forces are the destructive effects of the weathering, erosion and transport of rock material that tends to level the landscape and even out the irregularities of the surface. The principal agents of this process are water, wind and in the polar and mountain ranges, ice.
Although endogenous forces can result in the formation of new rocks (for example, in volcanoes), the exogenous forces, by contrast, are predominantly destructive and transportive. The study of the Earth’s geological history, as revealed principally by the succession of sedimentary rocks, is called stratigraphy. It is possible to trace changes in the distribution of land and sea, different climates and even changes in the constitution of the atmosphere during geological time; further the origin and development of past mountain belts can be determined.
People have long been fascinated by the almost daily discovery in rocks of the remains of past plants and animals. The oldest known traces of life are microscopic structures (predecessors of algae) about 4000 million years old. These lowly organisms stand in stark contrast to the giant dinosaurs of the Mesozoic Era or the ice age mammoths. The observation and classification of the organic remains that occur in rocks and the reconstruction of their evolution is the subject of paleontology (which is subdivided into paleobotany and paleozoology).
Regional geology aims at the integration of all the geological information pertaining to a particular area and this is expressed in the form of geological map. Such maps are the essential basis of all kinds of practical geological work.
Applied geology is concerned with the practical use of geological knowledge (discovery of mineral resources, oil and water, etc.). Applied geology finds further important applications in nature conservation. The study of present day processes is basic of all geological work – the principle of uniformitarianism is often expressed in the form “the present is the key to the past”. The natural laws controlling geological processes have remained essentially the same for thousands of millions of years.
Summing up, geology is the study of the Earth’s history and draws on all the technological resources of modern science in deciphering the record of the rocks as documents of Earth history. The geologists use his experience to correlate sequences of geological events established in separate areas into a general temporal sequence.
The present state of geology has been attained as a result of much work spread over many years and even now, views on the Earth’s evolution and Man’s ideas of his own development are far from complete. In particular, the concept of geological time has changed considerably over the past 2300 years and it is necessary now to trace the development of the geological sciences.
(Robert Lauterbach “The World of Geology -The Earth then and now” 1983 Leipzig)