- •Contents
- •Introduction
- •Unit 1 The Science of Geology
- •Different Areas of Geologic Study
- •Grammar focus The Noun in English
- •Discussion
- •Individual work
- •The Earth system
- •Energy for the Earth system
- •Test yourself
- •Unit 2 The Rock Cycle
- •The rock cycle
- •Grammar focus The Degrees of comparison of adjectives
- •Discussion
- •Lithosphere, mantle, layers, core, crust
- •Individual work
- •Earth’s Mantle
- •Earth’s Core
- •Test yourself
- •Unit 3 The Face of Earth
- •Grammar focus The Adverb in English
- •Discussion
- •Oceanic (mid-ocean) ridges, mountain belts, ocean basins, continental margins, continents, stable interior
- •Individual work
- •Test yourself
- •Unit 4 magma Part 1
- •Origin of Magma
- •Grammar focus Prepositions in English
- •Discussion
- •How Magmas Evolve
- •Individual work
- •Assimilation and Magma Mixing
- •Partial Melting and Magma Composition
- •Test yourself
- •Unit 5 magma Part 2
- •Intrusive Igneous Activity
- •Grammar focus The Present Indefinite and the Past Indefinite Tenses
- •Discussion
- •Massive Intrusive Bodies: Batholiths, Stocks, and Laccoliths
- •Individual work
- •Mineral Resources and Igneous Processes
- •Magmatic, igneous, vein deposits, metal-rich, hydrothermal solutions, disseminated deposit
- •Test yourself
- •Volcanic eruptions
- •The Nature of Volcanic Eruptions
- •Grammar focus The Past Indefinite Tense
- •Discussion
- •Why Do Volcanoes Erupt?
- •Individual work
- •Materials Extruded during an Eruption: lava
- •Test yourself
- •Volcanic structures and eruptive styles Part 1
- •Anatomy of a Volcano
- •Grammar focus The Present Indefinite versus the Future Indefinite tenses in complex sentences
- •Discussion
- •Types of volcanoes
- •1. Shield Volcanoes
- •2. Cinder Cones
- •3. Composite Cones
- •Individual work
- •Materials Extruded during an Eruption: gases and pyroclastic materials
- •Test yourself
- •Other Volcanic Landforms
- •Grammar focus The Continuous tenses
- •Discussion
- •Plate Tectonics and Volcanic Activity
- •Individual work
- •Test yourself
- •Weathering and Soil
- •Weathering
- •Grammar focus Perfect Tenses
- •Discussion
- •Mechanical Weathering
- •Individual work
- •Chemical Weathering
- •Test yourself
- •Internal processes, mass wasting, external processes, erosion, weathering
- •Grammar focus The Passive Voice (1)
- •Discussion
- •Controls of Soil Formation
- •Individual work
- •Soil Erosion
- •Test yourself
- •Sediment, type of vegetation, rock cycle, rate of soil, soil erosion
- •Unit 11 mineralogy Part 1
- •Grammar focus The Passive Voice (2)
- •Discussion
- •Characteristics of minerals
- •Individual work
- •Physical Properties of Minerals Optical Properties
- •Test yourself
- •Unit 12 mineralogy Part 2
- •Mineral Strength
- •Grammar focus
- •Indirect Speech
- •Discussion
- •Density and Specific Gravity
- •Individual work
- •Other Properties of Minerals
- •Test yourself
- •Unit 13 mineral groups
- •Grammar focus Modals in English
- •Discussion
- •Common silicate minerals
- •Individual work
- •Important nonsilicate minerals
- •Mineral resources
- •Test yourself
- •Unit 14
- •Igneous rocks Part 1
- •Magma: The Parent Material of Igneous Rock
- •The Nature of Magma
- •Grammar focus
- •Infinitive
- •Discussion
- •Igneous Processes
- •Igneous Compositions
- •Individual work
- •Other Compositional Groups
- •Test yourself
- •Unit 15
- •Igneous rocks Part 2
- •Igneous Textures: What Can They Tell Us?
- •Types of Igneous Textures
- •Grammar focus Gerund
- •Discussion
- •Felsic (Granitic) Igneous Rocks
- •Intermediate (Andesitic) Igneous Rocks
- •Individual work
- •Mafic (Basaltic) Igneous Rocks
- •Pyroclastic Rocks
- •Test yourself
- •Unit 16 metamorphism and metamorphic rocks
- •What Is Metamorphism?
- •Grammar focus Participle
- •Individual reading
- •Common Metamorphic Rocks Foliated Rocks
- •Nonfoliated Rocks
- •Test yourself
- •Sedimentary, pressure, mineralogical, metamorphism
- •Vocabulary
- •Glossary
- •List of reference books
Test yourself
Task 1. Tell whether the sentences are true or false. Correct the false ones.
Rock-forming minerals and economic minerals are mutually exclusive groups.
Only eighty elements make up the vast majority of the rock-forming minerals and represent more than 98 percent (by weight) of the continental crust.
Silicon and oxygen are by far the most common elements in Earth’s crust.
Silicon and oxygen readily combine to form the silicates.
It is impossible to indicate the conditions under which each silicate mineral is formed.
The most common silicate minerals can be divided into two major groups on the basis of their chemical makeup: the light silicates and the dark ones.
The dark silicates contain some amounts of aluminum, potassium, calcium, and sodium rather than iron and magnesium.
The most common member of the pyroxenes group is augite.
Biotite has a shiny light appearance that helps distinguish it from the other dark ferromagnesian minerals.
Both olivine and garnet have a glassy luster.
When calcite is the dominant mineral, the rock is called limestone.
Gypsum is the mineral name for common table salt.
Task 2. Using the geologic definition of mineral as your guide, determine which of the items on the list are minerals and which are not. If not a mineral, explain.
a. gold nugget d. cubic zirconia |
b. sea water e. obsidian |
c. quartz f. ruby
|
g. glacial ice |
h. amber
|
|
Unit 14
Igneous rocks Part 1
Task 1. Read and memorize the following words:
cool - охолоджувати |
emit - випускати, випромінювати, викидати (дим, лаву) |
eject - викидати, вивергати |
outpourings – розлив, вилив |
propel - рухати, виштовхувати |
melt - розплавлена речовина, розплав |
ash - попіл |
chamber – проруб, отвір |
mush - м'яке, кашоподібне; кашка |
volatile - летюча речовина; той, що швидко випаровується |
vent - вхідний або вихідний отвір; вентиляційний отвір; віддушина; повітряний клапан |
exert - викликати, спричиняти |
confine by - обмежуватись |
immense - величезний, колосальний |
surrounding - оточуючий |
to increase - збільшуватись |
Task 2. Read the following text, translate it into Ukrainian.
Magma: The Parent Material of Igneous Rock
Igneous rocks (ignis=fire) are formed as molten rock cools and solidifies. Some scientists believe that the parent material for igneous rocks, called magma, is formed by melting that occurs at various levels within Earth’s crust. Once formed, a magma body rises toward the surface because it is less dense than the surrounding rocks.
Occasionally molten rock reaches Earth’s surface where it is called lava. Sometimes lava is emitted as fountains that are produced when escaping gases propel it from a magma chamber. On other occasions, magma is explosively ejected, producing dramatic steam and ash eruptions. However, not all eruptions are violent; many volcanoes emit quiet outpourings of very fluid lava.
