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Earth Science (Quiz#3)
50問 • 1年前
  • Paula Tapnio
  • 通報

    問題一覧

  • 1

    are naturally occurring solid aggregates composed of one or more minerals or mineraloids. They form the Earth's crust and are classified based on their origin, formation process, and mineral composition

    rocks

  • 2

    are the solid substances which may have a combination of more than one mineral.

    rocks

  • 3

    do not have a definite chemical composition

    rocks

  • 4

    are mainly classified as igneous, sedimentary and metamorphic rocks

    rocks

  • 5

    These are inorganic substances that occur naturally.

    minerals

  • 6

    have a definite chemical composition

    minerals

  • 7

    are mainly classified into four groups namely silicates, carbonates, sulphides and metallic minerals.

    minerals

  • 8

    Types of rocks

    Igneous Sedimentary Metamorphic

  • 9

    is formed through the cooling and solidification of magma or lava. This can happen beneath the Earth's surface, or at the surface. The cooling speed affects the size of the crystals in the rock.

    igneous rocks

  • 10

    These form when molten rock, called magma, cools and solidifies beneath the Earth's surface. Because the cooling process is slow, these rocks typically have larger crystals. Ex.: Granite

    intrusive (plutonic) igneous rocks

  • 11

    These form when molten rock, called lava, erupts from a volcano and cools quickly on the Earth's surface. This rapid cooling results in smaller crystals. Ex.: Basalt.

    extrusive (volcanic) igneous rocks

  • 12

    light in color; feldspar & silicates

    felsic

  • 13

    dark in color; made up of Mg & Fe

    mafic

  • 14

    between mafic & felsic

    intermediate

  • 15

    very dark color

    ultramafic

  • 16

    overall appearance

    texture

  • 17

    fine grained

    aphanistic

  • 18

    coarse grained

    phaneritic

  • 19

    large crystals with small crystals

    porphyritic

  • 20

    non-ordered solid from rapid quenching

    glassy

  • 21

    composite of ejected fragments

    pyroclastic

  • 22

    form the foundation of many landscapes & are a key component of the Earth's crust. They contribute to soil formation when they break down over time, providing essential nutrients for plant growth

    igneous rocks

  • 23

    Ex.: tuff & basalt (Moai statues of Easter Island) & granite are widely used in construction, helping to build our cities and infrastructures

    igneous rock

  • 24

    are the most common rocks found on Earth's surface. They form from bits of other Frocks, minerals, and organic materials that get pressed and cemented together over time.

    sedimentary rocks

  • 25

    The process involves the accumulation of sediments over a long period, followed by compaction and cementation, which gradually turn them into solid rock

    sedimentary rocks

  • 26

    Eroded sediments end up in water and begin to settle down

    erosion and transportation

  • 27

    The release of moisture from the sedimentary layers makes layers compact

    composition

  • 28

    Salt crystals glue the layers to the la to form form more compact sedimentary rocks

    cementation

  • 29

    With time, more sediments are added newly formed sedimentary layers

    deposition

  • 30

    formed from the fragments of other rocks that have been compacted and cemented

    clastic sedimentary rocks

  • 31

    formed from the precipitation of minerals from water

    chemical sedimentary rocks

  • 32

    formed from the accumulation of plant or animal debris.

    organic sedimentary rocks

  • 33

    Ex.: Sandstone, Shale, Conglomerate

    clastic sedimentary rock

  • 34

    Ex.: Lim estone & Halite

    chemical sedimentary rocks

  • 35

    Ex.: Coal & Chalk

    organic sedimentary rocks

  • 36

    often contain fossils, which are crucial for understanding Earth's history and past life forms. They are also important sources of natural resources like oil, natural gas, and coal

    sedimentary rocks

  • 37

    are rocks that have been transformed from pre-existing rocks due to intense heat, pressure, or chemical processes deep within the Earth. This transformation changes the rock's structure, texture, and mineral composition without melting it.

    metamorphic rocks

  • 38

    These rocks exhibit a layered or banded appearance due to the alignment of minerals under directed pressure

    foliated metamorphic rocks

  • 39

    Ex.: Schist & Gneiss

    foliated metamorphic rocks

  • 40

    These rocks do not have a layered texture and usually form under uniform pressure.

    non foliated metamorphic rocks

  • 41

    Ex.: Marble & Quartzite

    non foliated metamorphic rocks

  • 42

    Classification of metamorphic rocks

    foliated metamorphic rocks and non foliated metamorphic rocks

  • 43

    are often harder and more durable than their precursor rocks, making them valuable for construction and artistic purposes Ex.: marble in sculpture and architecture.

    metamorphic rocks

  • 44

    the process that describes the gradual transformation between the three main types of rocks. It is occurring continuously in nature through geologic time.

    rock cycle

  • 45

    fundamental to understanding Earth's dynamic nature and the interconnectedness of geological processes. It also explains the distribution of different types of rocks across the Earth's surface.

    rock cycle

  • 46

    play a critical role in Earth's geology, influencing landscapes, supporting ecosystems, and providing valuable resources for human use. They are essential for understanding Earth's history, structure, and dynamic processes.

    rocks

  • 47

    crystalline, dark or light, no layers

    igneous rocks

  • 48

    grainy, layered, varying colors, fossils may be present

    sedimentary rocks

  • 49

    crystalline or banded, foliated or non-foliated, colors with streaks or bands.

    metamorphic rocks

  • 50

    3 types of sedimentary rocks

    clastic chemical organic sedimentary rocks

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    問題一覧

  • 1

    are naturally occurring solid aggregates composed of one or more minerals or mineraloids. They form the Earth's crust and are classified based on their origin, formation process, and mineral composition

    rocks

  • 2

    are the solid substances which may have a combination of more than one mineral.

    rocks

  • 3

    do not have a definite chemical composition

    rocks

  • 4

    are mainly classified as igneous, sedimentary and metamorphic rocks

    rocks

  • 5

    These are inorganic substances that occur naturally.

    minerals

  • 6

    have a definite chemical composition

    minerals

  • 7

    are mainly classified into four groups namely silicates, carbonates, sulphides and metallic minerals.

    minerals

  • 8

    Types of rocks

    Igneous Sedimentary Metamorphic

  • 9

    is formed through the cooling and solidification of magma or lava. This can happen beneath the Earth's surface, or at the surface. The cooling speed affects the size of the crystals in the rock.

    igneous rocks

  • 10

    These form when molten rock, called magma, cools and solidifies beneath the Earth's surface. Because the cooling process is slow, these rocks typically have larger crystals. Ex.: Granite

    intrusive (plutonic) igneous rocks

  • 11

    These form when molten rock, called lava, erupts from a volcano and cools quickly on the Earth's surface. This rapid cooling results in smaller crystals. Ex.: Basalt.

    extrusive (volcanic) igneous rocks

  • 12

    light in color; feldspar & silicates

    felsic

  • 13

    dark in color; made up of Mg & Fe

    mafic

  • 14

    between mafic & felsic

    intermediate

  • 15

    very dark color

    ultramafic

  • 16

    overall appearance

    texture

  • 17

    fine grained

    aphanistic

  • 18

    coarse grained

    phaneritic

  • 19

    large crystals with small crystals

    porphyritic

  • 20

    non-ordered solid from rapid quenching

    glassy

  • 21

    composite of ejected fragments

    pyroclastic

  • 22

    form the foundation of many landscapes & are a key component of the Earth's crust. They contribute to soil formation when they break down over time, providing essential nutrients for plant growth

    igneous rocks

  • 23

    Ex.: tuff & basalt (Moai statues of Easter Island) & granite are widely used in construction, helping to build our cities and infrastructures

    igneous rock

  • 24

    are the most common rocks found on Earth's surface. They form from bits of other Frocks, minerals, and organic materials that get pressed and cemented together over time.

    sedimentary rocks

  • 25

    The process involves the accumulation of sediments over a long period, followed by compaction and cementation, which gradually turn them into solid rock

    sedimentary rocks

  • 26

    Eroded sediments end up in water and begin to settle down

    erosion and transportation

  • 27

    The release of moisture from the sedimentary layers makes layers compact

    composition

  • 28

    Salt crystals glue the layers to the la to form form more compact sedimentary rocks

    cementation

  • 29

    With time, more sediments are added newly formed sedimentary layers

    deposition

  • 30

    formed from the fragments of other rocks that have been compacted and cemented

    clastic sedimentary rocks

  • 31

    formed from the precipitation of minerals from water

    chemical sedimentary rocks

  • 32

    formed from the accumulation of plant or animal debris.

    organic sedimentary rocks

  • 33

    Ex.: Sandstone, Shale, Conglomerate

    clastic sedimentary rock

  • 34

    Ex.: Lim estone & Halite

    chemical sedimentary rocks

  • 35

    Ex.: Coal & Chalk

    organic sedimentary rocks

  • 36

    often contain fossils, which are crucial for understanding Earth's history and past life forms. They are also important sources of natural resources like oil, natural gas, and coal

    sedimentary rocks

  • 37

    are rocks that have been transformed from pre-existing rocks due to intense heat, pressure, or chemical processes deep within the Earth. This transformation changes the rock's structure, texture, and mineral composition without melting it.

    metamorphic rocks

  • 38

    These rocks exhibit a layered or banded appearance due to the alignment of minerals under directed pressure

    foliated metamorphic rocks

  • 39

    Ex.: Schist & Gneiss

    foliated metamorphic rocks

  • 40

    These rocks do not have a layered texture and usually form under uniform pressure.

    non foliated metamorphic rocks

  • 41

    Ex.: Marble & Quartzite

    non foliated metamorphic rocks

  • 42

    Classification of metamorphic rocks

    foliated metamorphic rocks and non foliated metamorphic rocks

  • 43

    are often harder and more durable than their precursor rocks, making them valuable for construction and artistic purposes Ex.: marble in sculpture and architecture.

    metamorphic rocks

  • 44

    the process that describes the gradual transformation between the three main types of rocks. It is occurring continuously in nature through geologic time.

    rock cycle

  • 45

    fundamental to understanding Earth's dynamic nature and the interconnectedness of geological processes. It also explains the distribution of different types of rocks across the Earth's surface.

    rock cycle

  • 46

    play a critical role in Earth's geology, influencing landscapes, supporting ecosystems, and providing valuable resources for human use. They are essential for understanding Earth's history, structure, and dynamic processes.

    rocks

  • 47

    crystalline, dark or light, no layers

    igneous rocks

  • 48

    grainy, layered, varying colors, fossils may be present

    sedimentary rocks

  • 49

    crystalline or banded, foliated or non-foliated, colors with streaks or bands.

    metamorphic rocks

  • 50

    3 types of sedimentary rocks

    clastic chemical organic sedimentary rocks