- •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
- •Test yourself
- •Unit 2 The Rock Cycle
- •Energy for the Earth system
- •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
- •Test yourself
- •Density and Specific Gravity
- •Individual work
- •Other Properties of Minerals
- •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
Grammar focus The Adverb in English
Task 1. Translate the sentences into Ukrainian paying special attention to the underlined adverbs.
Deeply buried “wet” rock has a much lower melting temperature than “dry” rock of the same composition.
Volatiles (principally water) can lower the melting temperature of hot mantle rock sufficiently to generate magma.
The mineral makeup of diorite is primarily sodium-rich plagioclase feldspar and amphibole.
The terms tuff and volcanic breccia are frequently used with a modifier, as, for example, rhyolite tuff.
Pyroclastic rocks composed mainly of particles larger than ash are called volcanic breccia.
The classification of igneous rocks is based largely on two criteria.
Workers in underground mines know that temperatures get higher as they go deeper.
Although the rate of temperature change varies considerably from place to place, it averages about 25 °C per kilometre in the upper crust.
During the crystallization process, the composition of the remaining liquid portion of the magma also continually changes.
Task 2. Look at the adverbs from Task 1. Can all of them form the degrees of comparison? Form the degrees of comparison where it is possible.
Task 3. Form degrees of comparison of the following adverbs. Mind that not all of them can do that.
Carefully, ever, soon, often, usually, fast, early, loud, well, happily, quickly, much, here, yesterday, lately, beneath.
Discussion
Task 1. Read and memorize the following words:
floor – дно (океану) |
prominent – відомий, видатний, помітний |
linear - вузький, довгий, витягнутий |
adjacent to – бути прилеглим, який примикає, суміжним, сусіднім |
margin – шельф, край |
gently sloping – похилий, пологий |
ridge - гірський кряж, гірський хребет; пасмо гір; вододіл |
plain - рівнина |
scenery – ландшафт, вид |
boundary – кордон, межа |
trench – океанська западина, каньйон |
fraction - частина; частка |
Task 2. Read the text. Talk about the major features of the ocean basins. Pay special attention to the pronunciation of the following words and word-combinations, transcribe them: boundary, canyons, plateaus, oceanographers, continental shelf, adjacent, abyssal plains. What are the three major regions of the ocean floor and some features associated with each?
If all water were drained from the ocean basins, a great variety of features would be seen, including linear chains of volcanoes, deep canyons, extensive plateaus, and flat plains. In fact, the scenery would be nearly as diverse as that on the continents. Oceanographers have gradually mapped significant portions of the ocean floor. From these studies they have defined three major regions: continental margins, deep-ocean basins, and oceanic (mid-ocean) ridges.
The continental margin is that portion of the seafloor adjacent to major landmasses. It may include the continental shelf, the continental slope, and the continental rise. Although land and sea meet at the shoreline, this is not the boundary between the continents and the ocean basins. Rather, along most coasts a gently sloping platform, called the continental shelf, extends seaward from the shore. The boundary between the continents and the deep-ocean basins lies along the continental slope, which is a relatively steep drop off that extends from the outer edge of the continental shelf to the floor of the deep ocean.
Between the continental margins and oceanic ridges lie the deep-ocean basins. Parts of these regions consist of incredibly flat features called abyssal plains. The ocean floor also contains extremely deep depressions that are occasionally more than 11,000 m deep. Although these deep ocean trenches are relatively narrow and represent only a small fraction of the ocean floor, they are nevertheless very significant features. Other trenches parallel linear island chains called volcanic island arcs. Dotting the ocean floor are submerged volcanic structures called seamounts, which sometimes form long narrow chains. Volcanic activity has also produced several large lava plateaus.
The most prominent feature on the ocean floor is the oceanic or mid-ocean ridge. This broad elevated feature forms a continuous belt that winds for more than 70,000 km around the globe. The oceanic ridge system consists of layer upon layer of igneous rock that has been fractured and uplifted.
Task 3. Look at Figure 3.1. Try to analyze major surface features of the geosphere using the information from Task 1.
Task 4. Fill in the gaps with on from the suitable words:
