13. Earth and Space Sciences Flashcards

1
Q

What is the difference between Earth science, Geology, and Meteorology?

A

The study of the physical makeup of Earth is often called Earth science. Geology describes Earth’s physical appearance, and meteorology deals with the atmosphere and weather.

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2
Q

What is the difference between the earth’s mesosphere, asthenosphere, and lithosphere?

A

Mesosphere is located in the lower mantle surrounding earth’s core. In the mesosphere, temperatures are high enough to melt rock, but a tremendous amount of pressure keeps all the material solid.

Asthenosphere is in the middle part of the mantle. The rocks there are solid, but they move like glaciers do. (It’s called plastic flow.) The temperatures in the asthenosphere are still very high, which can lead to some melting.

Lithosphere is the uppermost part of earth’s mantle, and it’s attached to the crust. The rocks in the lithosphere are solid, thick, and brittle, like the crust, but they’re not officially part of the crust because they’re made from different minerals than the crust is.

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3
Q

Geologists classify rocks into three major categories: sedimentary, metamorphic, and igneous. Differentiate all of them.

A

Sedimentary: Formed by sediment (such as particles of sand, seashells, and other materials, sedimentary rocks “grow” in layers. Over a long period of time, sediment hardens — but it is still considered soft, as far as rocks go. This type of rock most often contains the fossils.

Metamorphic: Metamorphic rocks form because of the heat and pressure below Earth’s surface. these rocks sometimes gave shiny crystals inside them and may form layers that look like ribbons, such as marble gneiss.

Igneous: Magma, the super-heated molten rocks simmering below Earth’s crust and above its mantle, collects in pockets called magma chambers beneath volcanoes that eventually erupt. (It’s ultra-hot — between 1,000 degrees Fahrenheit and 3,000 degrees Fahrenheit). When magma comes out through a volcano, it’s lava. Cooed lava form igneous rocks. Magma that cools quickly is shiny and glasslike; when it cools slowly, crystals can form. Obsidian and granite are types of igneous rock,

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4
Q

What are the three major types of faults in Earth’s crust?

A
  1. Reverse fault
  2. Normal fault
  3. Strike-slip fault
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5
Q

What is the Richter magnitude scale?

A

The Richter magnitude scale is a mathematical formula that scientists use to compare the size of earthquakes.

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6
Q

What are oceanographers?

A

Oceanographers study the physical and biological properties of the seas. They look at temperature, rising, and falling levels, sea creatures, and the geologic frameworks that make the oceans, well, the oceans.

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7
Q

Earth has only one global ocean, which covers 72 percent of the planet and holds 97 percent of the planet’s water, but scientists have divided it into five named oceans to make keeping track of regions easier, what are those?

A
  1. Atlantic
  2. Pacific
  3. Indian
  4. Arctic
  5. Southern
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8
Q

Earth itself is about ______ years old.

A

4.54-billion-year-old, which scientists determined by studying the oldest mineral grains on Earth (tiny zirconium silicate crystals that are at least 4.3 billion years old).

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9
Q

What are the layers of the Earth’s atmosphere? Differentiate

A
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10
Q

Different the percentages of how much nitrogen, oxygen, argon, and carbon dioxide within the atmosphere.

A
  1. Nitrogen = 78%
  2. Oxygen = 21%
  3. Argon = 0.93%
  4. Carbon dioxide = 0.04%
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11
Q

What is the magnetosphere?

A

Earth’s magnetosphere is a globe of space around the planet’ that is controlled by our magnetic field. It’s not part of the atmosphere, but it is important because it deflects solar wind. Earth’s magnetic field is invisible, but because Earth’s core is made from iron and other hot, liquid metals that create electrical currents, it’s there — and its protective forces come out of the Souther Hemisphere (where the south pole is) and travel back into the planet in the Northen Hemisphere (where the north pole is).

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12
Q

What are contrails?

A

Air is warmest near ground-level in the bottom of the troposphere, and it becomes colder at higher levels; that is why you can sometimes see snow on the peaks of big mountains in the summer and why jets leave white trails, called contrails, in the sky.

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13
Q

How does temperature affect density?

A

Temperature affects air density (how closely packed the air molecules are). Cold air is denser than warm air. Because it is denser, cold air has high pressure, compared to warm air’s low pressure. (A barometer measure atmospheric pressure). Air moves from areas of high pressure to areas of low pressure, creating wind. The angle of the sun also affects air density (the sun shines directly over the equator but not the poles).

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14
Q

Air masses have certain characteristics depending on where they form, can you elaborate?

A
  • If an air mass forms over land, it’s dry, and if it forms over water, it’s wet.
  • Air masses formed in Earth’s northern and southern regions are cold, and those formed at the equator are warm.
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15
Q

What happens when two different air masses meet?

A

When two different air masses meet, they don’t mix. They form a boundary called a front. When cold air meets warm air, cold front develops. The warm air may be pushed up to form clouds, causing heavy rain. When a warm air mass meets a cold air mass, a warm front develops. The war air passes over the cold air, forming a different kind of cloud, which causes light rain.

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16
Q

What is evapotranspiration?

A

Evapotranspiration is the measure of the rate at which plants and the land release moisture into the air.

17
Q

What is the difference between weather and climate?

A

Weather is different from climate. The term weather refers to daily atmospheric conditions, while climate refers to patterns in weather over time (usually 30 years or more). Weather fluctuates sometimes it’s 30 degrees Fahrenheit and sometimes it’s 110 degrees Fahrenheit — and the term only refers to the weather you can see, feel, and remember in the recent past. Climate is an average pattern of weather you can see, feel, and remember in the recent past. Climate is an average pattern of weather across the whole Earth or in a specific region. For example, Alaska has a colder climate than Florida does, and Earth’s overall climate is warmer now than it was a hundred years ago.

18
Q

What are the three main types of clouds?

A
19
Q

Differentiate the following prefixes: Cirro-, Alto-, and Nimbo-

A
  • Cirro- is the prefix given to high clouds (base above 20,000 feet.)
  • Alto- is the prefix given to the midlevel clouds (base between 6,000 adn 20,000 feet)
  • Nimbo- added to the beginning of a cloud name or -nimbus added to the end means the cloud is producing precipitation.
20
Q

What are the equations for the following temperatures?

Fahrenheit

Celsius

Kelvins

A

F = 9/5C + 32

C = 5/9F - 32

K = C + 273.15

21
Q

What are paleontologists?

A

Paleontologists are scientists who, in general, study fossil animals and plants.

22
Q

What are the 9 variety of subdisciplines in being a paleontologist?

A
  1. Invertebrate paleontology: These paleontology study invertebrate animal fossils, such as mollusk, brachiopods, and arthropods (like crabs, shrimps, and barnacles).
  2. Vertebrate paleontology: Is that a wooly mammoth or a tyrannosaurus rex? Vertebrate paleontologists can tell you. These scientists study vertebrate fossils, including fish and mammals.
  3. Paleobotany: These not-quite-garden-variety paleontologists deal with fossil plants to study their evolutionary history.
  4. Micropaleontology: Armed with microscopes and other tools, micropaleontologists study microscopic fossils from the ocean floor and all over land. Micropaleontology is the largest discipline within paleontology because the microorganism these scientists study are so abundant.
  5. Palynology: Sifting through archeological and geological deposits to study pollen grains and other spores is just another day at the office for a paleontologists who focuses on palynology.
  6. Taphonomy: Scientists who study taphonomy are looking at the process of how organisms decay and become fossils.
  7. Ichnology: Ichnology is a branch in several scientific disciplines (including biology and geology), but paleontologists who focus on it study fossil tracks, footprints, and trails.
  8. Paleoecology: Paleontologists who study paleoecology investigate the relationships between ancient organisms and their responses to changing environments.
23
Q

Scientists use dozens of methods to determine the ages of fossils, but some of the most important are…

A
  1. Radiometric dating: This technique involves observing the natural decay of radioactive elements.
  2. Relative dating: This technique involves evaluating the layers of sediments and rock in which the fossil was found; some layers and types of rock are older than the others are, so scientists compare what they already know to what they find.
  3. Paleomagnetism: This method compares magnetic particles in sediment layers, which can be used for relative dating, to known worldwide shifts in the Earth’s magnetic field.
  4. Biochronology: Animal fossils can often be dated by comparing them to other, well-dated species.
24
Q

What is vernal equinox, summer solstice, autumnal equinox, and winter solstice?

A
  1. Vernal equinox: The first day of spring — the vernal equinox — is the day the sun crosses from south to the equator to north of it.
  2. Summer solstice: Summer solstice is the day the sun reaches the farthest point north on the ecliptic (the path the sun takes each year).
  3. Autumnal equinox: The sun crosses the equator toward the south and kicks off fall un the autumnal equinox.
  4. Winter solstice: Winter solstice is the day the sun is as far as south as possible on the ecliptic.
25
Q

What are the phases of the moon?

A
26
Q

What are the number of moons on each planet in the solar system?

A
  1. Mercury = 0
  2. Venus = 0
  3. Earth = 1
  4. Mars = 2
  5. Jupiter = 63
  6. Saturn = 61
  7. Uranus = 27
  8. Neptune = 13
27
Q

What is the difference between long-period comet and short-period comet?

A

Long-period comets, which takes 200 years or more to orbit the sun and originate in the Oort Cloud.

Short-period comets, which complete their orbits in fewer than 200 years and most likely originate in the Kulper Belt.