3. Film with subtitles and pauses. Listen and repeat after the speaker.
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4. Film with subtitles and narration.
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classicmobile
Exercise 1
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Exercise 1
classicmobile
Exercise 2
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Solve the exercise. Rozwiąż ćwiczenie.
Solve the exercise. Rozwiąż ćwiczenie.
After familiarizing yourself with the film “Drilling holes”, match the Polish words/phrases with their English equivalents. Po zapoznaniu się z filmem „Wiercenie otworów”, połącz polskie słowa/zwroty z ich angielskimi odpowiednikami.
Source: Fundacja na Rzecz Rozwoju Polskiego Rolnictwa / Eduexpert Sp. z o.o., licencja: CC BY 3.0.
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Exercise 2
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Classification of rocks and their uses
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classicmobile
Exercise 3
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Solve the exercise. Rozwiąż ćwiczenie.
Solve the exercise. Rozwiąż ćwiczenie.
After watching the animation “Classification of rocks and their uses”, decide whether the sentences are true or false. Po obejrzeniu animacji „Klasyfikacja skał”, zdecyduj, czy twierdzenia są prawdziwe, czy fałszywe.
Prawda
Fałsz
Magma rocks are formed as a result of the solidification of the silicate melt in the depths of the Earth, or on its surface.
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Granite and gabbro crystallize on the surface of the Earth.
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Rhyolite and basalt crystallize on the surface of the Earth.
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Volcanic rocks are characterized by holocrystalline structures, in other words full- rystalline structures, where the minerals are in the form of crystals.
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Plutonic rocks have hypocrystalline structures, which means they are partially crystalline, and partly made of enamel.
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Weathering, transport and sedimentation are not processes that result in the formation of sedimentary rocks.
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Organogenic rocks are formed as a result of the accumulation of animal remains.
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Chemogenic rocks are formed as a result of the precipitation of substances from a glacier.
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Metamorphic rocks are formed as a result transformation of older magma and sedimentary rocks due to high temperatures and pressure in the lithosphere.
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Marbles and sandstones can be used to build fireplaces.
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Source: Fundacja na Rzecz Rozwoju Polskiego Rolnictwa / Eduexpert Sp. z o.o., licencja: CC BY 3.0.
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Exercise 3
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Stages of the creation of geological maps
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classicmobile
Exercise 4
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Exercise 4
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Identifying minerals
The hypertext material is a conversation between a mineralogist and a photographer. Its topic is the way of identifying minerals. The mineralogist talks about physical features of minerals: their hardness, color, streak and lustre. The conversation takes place in a mineralogical museum.
Hipertekst stanowi rozmowę mineraloga z panią fotograf. Jej tematem jest sposób rozpoznawania minerałów. Mineralog opowiada o cechach fizycznych: twardości, barwie, rysie, połysku. Rozmowa odbywa się w muzeum mineralogicznym.
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Photographer: Good morning, mister Christopher.
Mineralogist: Hello, miss. The minerals are ready, just as you asked.
Photographer: They’re beautiful. Please, tell me how you distinguish them. I’d like to write about it in the guide.
Mineralogist: Minerals have physical properties, such as hardness determined by theMohs scalem2dd36574f7a71c1b_1497279637332_0Mohs scale, wheretalcm2dd36574f7a71c1b_1497279718401_0talcis the softest, anddiamondm2dd36574f7a71c1b_1497279733582_0diamondthe hardest.
Photographer: This one has a beautiful green color.
Mineralogist: That’smalachitem2dd36574f7a71c1b_1497279738479_0malachite. It also has a greenstreakm2dd36574f7a71c1b_1497279743621_0streak.
Photographer: And what about the mineral grouping over here?
Mineralogist: That’s adrusem2dd36574f7a71c1b_1497279748379_0druseof purpleamethystm2dd36574f7a71c1b_1497279753543_0amethystcrystals, of thequartzm2dd36574f7a71c1b_1497279762480_0quartzvariety.
Photographer: Quartz is a very common mineral, commonly known as the mountain crystal. Is every mineral a crystalm2dd36574f7a71c1b_1497279767416_0crystal?
Mineralogist: No, this term is reserved for well‑formed minerals withwallsm2dd36574f7a71c1b_1497279772536_0walls,edgesm2dd36574f7a71c1b_1497279782995_0edges, andtopsm2dd36574f7a71c1b_1497279777622_0tops.
Photographer: Some minerals are more shiny, others less.
Mineralogist: That’s their next feature - lustre. It depends on the degree to which light is reflected by the surface of the crystal.
Photographer: I’ve heard that some minerals have unique properties.
Mineralogist: Yes,magnetitem2dd36574f7a71c1b_1497279787842_0magnetitehas magnetic properties,sulphurm2dd36574f7a71c1b_1497279793098_0sulphuris flammable, andhalitem2dd36574f7a71c1b_1497279799633_0halitehas a salty taste.
Photographer: Is halite our table salt?
Mineralogist: Yes, it is. Minerals are everywhere.
classicmobile
Exercise 5
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Exercise 5
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skala Mohsa
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talk
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diament
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malachit
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rysa
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szczotka
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ametyst
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kwarc
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kryształ
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ściana
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wierzchołek
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krawędź
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magnetyt
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siarka
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halit
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Ordering fossils based on their occurence in geological eras
The hypertext material is a conversation between a guide of a museum of Earth history and the museum’s visitors. Its topic is the occurrence of variousindex fossilsm2dd36574f7a71c1b_1497292330786_0index fossilsin particular geological eras.
Hipertekst stanowi dialog przewodnika ze zwiedzającymi muzeum historii Ziemi. Jego tematem jest opis występowania skamieniałości przewodnich w poszczególnych erach geologicznych.
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Guide: Welcome to the Museum of Earth History. My name is John and I’ll be your guide today.
Visitors: There are a lot of specimens here.
Guide: The exhibition includes more than three thousand exhibits. On the right, you can see a model showing the living conditions on Earth in particular geological periods.
Visitors: When was life created on Earth?
Guide: The origins of life date back to 3.8 billion years ago. In the Cambrian periodm2dd36574f7a71c1b_1497292341857_0Cambrian period, about 541 million years ago, the so‑called explosion of living things took place.
Visitors: Which animals were the most common then?
Guide: Representatives of the Paleozoic eram2dd36574f7a71c1b_1497292338305_0Paleozoic era, which constituted trilobitesm2dd36574f7a71c1b_1497292326285_0trilobites. Most of them were benthic organismsm2dd36574f7a71c1b_1497292312053_0benthic organisms.
Visitors: How big were they?
Guide: From showcase no. 2, all our visitors are greeted by our largest specimen, trilobite Henry which measures over 70cm. It consists of a cephalon, thorax, and a pygidium.
Visitors: When did the trilobites die out?
Guide: The greatest extinction in the history of life on Earth occurred at the end of the Paleozoic era. It also affected the trilobites. Now, I present to you the heroes of the Mesozoicm2dd36574f7a71c1b_1497292307534_0Mesozoiceram2dd36574f7a71c1b_1497292307534_0era, which began around 252 million years ago.
Visitors: Those are dinosaurs and the first mammals.
Guide: Yes, as well as the ammonitesm2dd36574f7a71c1b_1497292302003_0ammonites, which evolved in warm seas. Do you have any more questions?
Visitors: How were the ammonites built?
Guide: Their shell, usually spirally twisted, was made of aragonitem2dd36574f7a71c1b_1497292294450_0aragonite. It was divided into a residential part, and a gas‑filled phragmoconem2dd36574f7a71c1b_1497292283746_0phragmocone.
Visitors: When did birds appear on Earth?
Guide: In the next era. Only later did the evolution of man take place, in the Cenozoic eram2dd36574f7a71c1b_1497292278430_0Cenozoic era. It began about 66 million years ago and continues to this day.
Visitors: What's in the next room?
Guide: Dinosaur skeletons. You can see them until 5 PM. In the meantime, let me thank you for your attention.
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kambr
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era paleozoiczna
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classicmobile
Exercise 6
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Solve the exercise. Rozwiąż ćwiczenie.
Solve the exercise. Rozwiąż ćwiczenie.
After familiarizing yourself with the hypertext “Ordering fossils based on their occurrence in geological eras”, match the Polish words/phrases with their English equivalents. Po zapoznaniu się z hipertekstem „Uporządkowanie skamieniałości pod względem ich występowania w okresach geologicznych”, połącz polskie słowa/zwroty z ich angielskimi odpowiednikami.
ammonites, benthic organisms, phragmocone, trilobites, Mesozoic era, Cenozoic era, index fossils, Paleozoic era, argonite, Cambrian period
kambr
era paleozoiczna
skamieniałości przewodnie
trylobity
organizmy bentoniczne
era mezozoiczna
amonity
aragonit
fragmokon
kenozoik
Source: Fundacja na Rzecz Rozwoju Polskiego Rolnictwa / Eduexpert Sp. z o.o., licencja: CC BY 3.0.
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Exercise 6
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skamieniałość przewodnia
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trylobite
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organizm bentoniczny
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era mezozoiczna
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amonit
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aragonit
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fragmokon
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kenozoik
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Defining the subject of a public procurement for a publication on the development of Earth's crust
The hypertext material is a description of a procurement for a popular science publication which should focus on the development of Earth’s crust.
Hipertekst przedstawia opis zamówienia na publikację popularnonaukową, która ma dotyczyć rozwoju skorupy ziemskiej.
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The editors of the popular science magazine „Earth” announce a competition for the preparation of a scientific publication on the development of Earth's crust.
The content of the commissioned texts needs to include information on:
● the formation of cratonsm2dd36574f7a71c1b_1497302764422_0cratons, as the initial form of the continents, ● the boundaries of Earth's crustm2dd36574f7a71c1b_1497302754287_0Earth's crust, external - in the form of the atmospherem2dd36574f7a71c1b_1497302748645_0atmosphere and hydrospherem2dd36574f7a71c1b_1497302736917_0hydrosphere, and internal - developed as Earth’s mantlem2dd36574f7a71c1b_1497302733680_0Earth’s mantle, ● weatheringm2dd36574f7a71c1b_1497302728712_0weathering processes, ● the composition of the continental crustm2dd36574f7a71c1b_1497302618223_0continental crust, which includes silicon, clay, iron, calcium, magnesium and potassium compounds, ● paleocontinentsm2dd36574f7a71c1b_1497302614191_0paleocontinents: Gondwanam2dd36574f7a71c1b_1497302609415_0Gondwana and Rodiniam2dd36574f7a71c1b_1497302603612_0Rodinia.
The material must be prepared within two months from the date of signing the contract.
The contractor will provide a person with at least 5 years of experience as a lecturer, or as a researcher in the field of dynamic geologym2dd36574f7a71c1b_1497302598187_0dynamic geology and geochemistrym2dd36574f7a71c1b_1497302589553_0geochemistry.
The Contractor must attach an initial outline of the work, two pages long, in the A4 format, to the offer.
The evaluation criterion will be price and project evaluation, each constituting 50% of the evaluation.
Offers should be submitted in person, or via e‑mail at editorialboard@editorialboard.eu until March 31 this year.