Practice Exam Flashcards

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1
Q

Explain why it’s important for anyone who wants to extract minerals from the ground to understand the geothermal gradient

A

The geothermal gradient is important for several reasons. The geothermal gradient helps to predict temperatures at a certain depth which is important for extracting minerals - it helps you to know which equipment and drilling techniques should be used. It affects the formation and stabilization of minerals as the temperature and pressure at different depths can cause minerals to either dissolve or precipitate out of a solution. The geothermal gradient can influence the concentration and distribution of minerals. Certain minerals are more likely to be found in certain depths or temperatures. It can help minimize the environmental disruption because it allows for more accurate predictions of surface concentrations

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2
Q

Explain how absorption lines allow us to know what the sun is compromised of

A

Absorption lines allow us to know what elements are present in a star. We know that the sun is compromised of the same elements as earth, but in different proportions - hydrogen (73%) and helium (25%). Absorption lines appear in a spectrum if an absorbing material is placed between the material (the sun) and us (the observers). This material could be the outer layers of a star, a cloud of interstellar gas, or a cloud of gas. By looking at the absorption line spectrum we are able to determine what elements the sun is compromised of

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3
Q

Where do earthquakes happen? What are the focus and epicenter? What are some consequences?

A

Earthquakes are caused when underground rocks suddenly break along a fault causing seismic waves, which cause the ground to shake. Earthquakes typically occur along oceanic and continental plates. The focus is the spot underground where rocks break. The epicenter is the place right above the focus. Earthquakes pose a risk to the health, safety, and economic viability of Canada and the rest of the world. A recent example is the earthquake that hit Turkey where it resulted in massive loss of life, huge financial instability, and the downfall of industrial societies.

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4
Q

What is Absolute Dating and it’s 3 methods?

A

Absolute Dating used different methods to chronologically estimate the age of certain geologic materials in fossils and the direct age of fossils. Radiometric dating uses the radioactive decay of certain materials such as potassium and carbon, as reliable clocks to date ancient events. Electron spin resonance and thermoluminescence assess the effects of radioactivity on the accumulation of electrons of the crystal structure of a mineral to determine its age. Radioactive decay is when an unstable isotope changes its number of protons or neutrons or both

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5
Q

What are the Saturnian satellites and what is so special about Enceladus?

A

Enceladus is a small ocean world covered in ice. It’s one of 60 confirmed moons that orbit Saturn. It’s young - less than 100 million years old. A global ocean flows under an ice shell 30-40 km thick. Life could exist

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6
Q

Choose 2 exoplanets and discuss their characteristics

A

Kepler 186f was the first rocky planet to be found within the habitable zone. It’s close in size to earth. It orbits its star once every 130 days. It resides in the Kepler 186 system. It receives 1/3 of the energy from its sun-like star that earth receives from our sun. Osiris was the first planet to be seen in transit and have its light directly detected. Scientists detected oxygen and carbon in its atmosphere. It has an evaporating hydrogen atmosphere. It’s 7 million miles away from its star and has a surface heated to 1000 degrees C. It’s classified as a Chthonian planet due to its completely dead core of evaporated gas giants

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7
Q

What is the importance of the lithosphere and the asthenosphere in moving plate tectonics?

A

Plate tectonics is the theory that the earth’s outer shell is divided into several plates that glide over the mantle, the rocky inner layer of the core. These plates act like rigid hardshell compared to earth’s mantle. The outer shell is the lithosphere which is 100 km thick. The lithosphere consists of the crust and outer part of the mantle. Below the lithosphere is the asthenosphere, which is malleable or partially malleable, allowing the lithosphere to move around a bit.

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8
Q

Explain why the Hubble Space Telescope is important and include some facts

A

The Hubble space telescope orbits our planet at an altitude of 547 km. The telescope is inclined at 28.5 degrees to the equator. At this vantage point, we are able to see crystal-clear images of our planet without the atmosphere getting in the way. The telescope takes about 95 minutes to complete one full orbit around the earth. The telescope was named after Edwin Hubble, who along with another astronomer, confirmed the universe is expanding.

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9
Q

Explain the 5 basic characteristics of a star

A

Luminosity is the amount of light a star radiates. We can determine a star’s luminosity by its size and surface temperature. Apparent Magnitude is a star’s perceived brightness factoring in size and distance. Absolut Magnitude is a star’s true brightness that is determined by its distance from earth. A star’s color is determined by its surface temperature. Cooler stars tend to be redder while hotter stars tend to be bluer. Stars that are yellow have an average temperature like our sun. A star’s surface temperature is measured using the Kelvin scale. Zero degrees on the kelvin scale is theoretically absolute zero and equal to -273 degrees C. We can measure a star’s size by comparing it to our own sun. Our sun has a radius of 1 solar radii, meaning a star with that same measurement is the same size as our sun. We can also determine a star’s mass by comparing it to our own sun

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10
Q

How do volcanoes form?

A

Volcanoes usually form at the boundaries of the earth’s tectonic plates. These plates are huge slabs of the earth’s crust and upper mantle that fit together like puzzle pieces. Although the plates are not fixed in one place, they move at an extremely slow rate; only a few cm every year. The plates either collide together or move apart. Volcanoes are common in geologically active boundaries. Principle types of volcanoes include stratovolcanoes, shield volcanoes, lava domes, and pyroclastic cones.

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11
Q

What methods are used to detect planets?

A

Radial Velocity, aka Doppler Spectroscopy, was the only known method capable of detecting extrasolar planets. It relies on the fact that a star does not remain completely stationary when it is orbited by another planet. As a star moves away from us, the light waves leaving the star are stretched and move toward the red end of the spectrum. As a star moves toward us the light waves are compressed and move toward the blue end of the spectrum. Transit photometry measures the minute dimming of a star as an orbiting planet passes between it and the earth. If dimming changes, a planet is orbiting around it and passing in front of it once every orbital period. Microlensing is the only method capable of discovering planets at a truly great distance. This is an astronomical effect predicted by Einstein’s General Theory of Relativity. When the light emanating from a star passes close to another star, the gravity of the lensing star will bend the light-years of the source star causing them to appear farther apart than they actually are. If a source star passes behind an intermediary star, light rings will appear known as Einstein’s rings.

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12
Q

Describe the String Theory

A

The string theory is the best contender for a quantum theory of gravitation. It states that everything in the universe is made up of open strings with two separate ends to form a type of loop. Spatial curvature describes the way spacetime is curved due to gravity

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13
Q

What happened during the Pleistocene Epoch?

A

The Pleistocene Epoch is defined as the time period that began 2.6 million years ago until 11,700 years ago. This epoch was the most recent ice age where glaciers covered huge parts of the heart. Large sheets of ice covered all of Antarctica, large parts of Europe, North, and South America, and small parts of Asia. This epoch was the first in which Homo Sapiens evolved, and in the end, humans could be found all over the world. This epoch was followed by the current stage called the Holocene Epoch.

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14
Q

Who was J. Tuzo Wilson and why was he so significant?

A

J. Tuzo Wilson, a Canadian geophysicist, had a theory on why some volcanoes appear thousands of km away from tectonic plate boundaries which is where they usually occur, In 1963, he stated that these volcanoes are created by exceptionally hot areas fixed deep below the mantle. These hot spots can independently melt the plate directly above them, creating magma, which erupts onto the top of the plate. Hot spots beneath the ocean create volcanic mounds. These mounds, over millions of years, grow until they reach sea level and creates volcanic islands.

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15
Q

What is Hubble Law? What are some objectives of the Hubble Space Telescope?

A

Hubble’s Law states that the redshifts in the spectra of distant galaxies are proportional to their distance. Hubble’s objectives are to study the history and evolution of the universe, confirm the universe’s physical laws, investigate the constitution, physical characteristics, and dynamics of celestial bodies, and provide a long-term space research facility for optical astronomy.

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16
Q

Explain what Precambrian Time was like and the features of that time.

A

Precambrian time began 4.6 million years ago and until 541 million years, known as the beginning of the Cambrian period. Several rock types indicated the type of environments that could have existed during this time. Precambrian rocks contained evidence of the very beginnings of life on earth, nearly 3.5 million years ago. This time is known for the explosion of life forms without skeletons and the development of sexual reproduction. It’s divided into the Archean and Proterozoic Eons.

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17
Q

What are the 6-8 qualities of water that make it unique? Explain how it fully functions on Earth

A

Our earth is the only known planet with huge bodies of liquid water. Water is unique in that it can absorb enormous amounts of water without a large alteration in its temperature. During the day, water absorbs enormous amounts of heat in order for the earth to stay cool. During the night, water releases the heat it absorbed during the day in order to keep the surface from freezing solid. Compared to virtually all other materials, water contracts when it is cooled and then expands until it freezes. The Coriolis effect which produces ocean currents, keeps the ocean in liquid form so the myriad of creatures can thrive.

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18
Q

What are the Galilean Satellites and what is so special about Europa?

A

Europa’s surface is mostly water and ice, but beneath the ice, the crust is liquid water. Europa’s ice crust is 15-25 km thick. Europa orbits Jupiter every 3.5 days. There is a potential for life such as cells and microbes - but not humans because the atmosphere is too thin.

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19
Q

What are Relative Dating and its 4 principles?

A

Relative Dating is the geological age of fossil organisms, rocks, features, or events that is defined relative to other organisms, rocks, features, or events rather than in terms of years. The principle of Superposition states that in an undeformed sequence of sedimentary rocks, each layer of rocks is older than the one above it and younger than the one below it. The principle of Cross-cutting relationships states that any geologic features that cut across strata must have formed after the rocks were deposited. The principle of original horizontally states that strata have to be deposited horizontally and then tilted vertically after they’re deposited. The principle of faunal succession states that different fossil species always appear and disappear in the same order.

20
Q

Compare the Paleozoic era to the Cenozoic era

A

The Paleozoic era was known as a time of great change on earth. During this era, the climate was warm worldwide but was soon followed by an ice age that caused glaciers to form. The Cenozoic era was the most recent era - from 65 million years ago until today. The climate was overall more consistent and much warmer than it is today. All sorts of animals become common. The Cenozoic era was divided into 3 periods: Neogene, Paleogene, and quaternary periods. During the Paleogene period, rats and small horses were common. During the Neogene period, early primates such as early humans, cattle, sheep, goats, antelopes, and gazelle were flourishing. During the Quaternary period, cave lions, giant deers, woolly rhinos, and woolly mammoths were the prevailing species.

21
Q

What is the difference between a V-shaped valley and a U-shaped valley? What is a hanging valley?

A

Mountain glaciers typically leave behind unique erosional features. A glacier pucks rocks from the side and bottom when it cuts through a V-shaped valley. When this happens, the glacier widens the valley and steeps the walls efefctviely creating a U-shaped valley. A hanging valley is when two tributary glaciers flow into a main glacier in their U-shaped valley, where the main glacier cuts off the tributary glacier creating a cliff. When streams flow over the cliff, it creates a waterfall, such as Niagara Falls

22
Q

Explain what the Cenozoic Era was like and the features of that time

A

The Cenozoic era began 65 million years ago and contineus into the present. The era is divided ito 3 periods known as the Paleogene period, Neogene period, and Quaternary period. During the paleogene period, rats and small horses were common. During the neogene period, there was the rise of early primates such asearly humans, cattle, sheep, goats, antelopes, gazelles were flourishig. During the Quaternary period, cave lions, giant deers, woolly rhinos, woolly mammoths were prevailing species. The current locations of the continents and their modern-day inhabitants can be traced to this period. The era began at the end of the cretaceous-paleogene extinction event that wiped out the remaining non-avian dinosaurs.

23
Q

How do mountains form?

A

Mountains form as a result of the movement of plates around earth’s surface, which exerts powerful lateral forces on rocks. The crust’s response to those rocks gives rise to a deformation on a large scale, particularly along plate boundaries. A lot of geologic processes can result in mountain building including volcanism, crustal shortening, crustal extension, heating or cooling of lithosphere, continental collision. Mountains are usually located along plate boundaries or former plate boundaries

24
Q

Explain the life cycle of a star

A

Stars form when a dense cloud of gas collapses until nuclear reactions can begin within the interir of the cloud providing enough energy to stop the collapse. The lifecycle of high mass stars differs from low mass stars after the stage of carbon fusion. In low mass stars, after helium fusin, the core will never get hot or dense enough to fuse any additional elements causig the star to die. In high mass stars, the temperature ad pressure in the core reach high enough values that after carbon fusion takes place, oxygen fusion can begin and heavier elements such as neon, magneisum, and silicon can undergo fusion continuing to power the star

25
Q

Why is earth unique? What would happen if earths orbit sped up or slowed down?

A

The earth is unique because it has liquid water, plate tectonics, and an atmisphere that protects it from the worst of the suns rays. The earth is the only planet circling our sun on which life exists. Earth is covered with green vegetation and enormous blue-green oceans containing thousands of islands. The earth is 93 million miles away from the sun. If the earths orbit sped or slowed down, the temperature would result in high/lows to extreme for life.

26
Q

Explain how a particle accelerator works

A

A particle accelerator produces a beam of charged particles that is made up of particles and/or electrons. The beam of charged particles creates a sort of vaccum. The accelerator takes the particles and consistently propels them through a circular pipe and with each pass the strength of the electric field increases. The detector observes the collision of one particle colliding with another.

27
Q

What is the difference between an idiochromatic, allochromatic, and pseudochromatic mineral?

A

Idiochromatic minerals are self-colored due to their composition. The color is a constant and predictable component of the mineral. Examples: blue Azurite and red Cinnabar. Allochromatic minerals are colorless in their pure forms, however can occur in different colors due to trace elements. Examples: quartz, spinel, beryl. Pseudochromatic minerals are “false-colored” due to tricks in light diffraction. The color is variable but a unique property. Exampels: the colors produced by precious Opal and the blue in Amazonite

28
Q

What is tectonic stress and what causes it? What are the physical processes that exert stresses on rocks?

A

Tectonic stress is stress that tectonic plates are subjected to that causes rocks to change their shape/volume. Often these stresses are caused by forces that are exerted on the edges or interior of a material. A wide variety of physical processes exert stress on rocks. Gravity is one of the physical processes. Gravity is constantly exerting downwards stress on all rocks.

29
Q

What are 5 of the 8 steps to identifying minerals?

A

Before identifying a mineral, we examine it for properties such as color, hardness, streak, luster, and crystal habit. Color is one of the easiest properties to observe, however you can rarely identify a mineral solely by its color. There are 3 main groups: idiochromatic, allochromatic, and pseudochromatic. Hardness is a mineral’s ability to resist being scratched. Mohs Scale is a reference for mineral hardness. Streak is the color of the powder of the mineral. Luster is the way light reflects off of the surface of a mineral. Scientists group minerals into 2 groups: metallic luster and non-metallic luster. Crystal habit describes the favored growth patterns of the imperfections of a crystal of a mineral species, whether individually or inaggregate.

30
Q

Explain how glaciers move. How can glaciers appear to move uphill?

A

Glaciers move as a combination of two things: deformation of ice and motion at the glacier base. The ice flow direction is determined by the glaciers surface, meanign a glacier will always flow in the direction the ice is sloping. A glacier can appear to move uphill beneeath ice, only if the ice’s surface is sloping downwards. Glaciers can flow out of “bowl-like” cirques and over deepenings in the land.

31
Q

What are the 5 characteristics of mineral?

A

Naturally Occuring - people did not make it in any way, its not ‘man-made’. Inorganic - the substance is not made by an organism. Solid - its not a liquid or gas at standard temperature and pressure. Definite chemical composition - every time we encounter the mineral, we will know what elements compose it. Ordered internal structure - the atoms in a mineral are arranged in a systematic and repeating pattern

32
Q

What are some facts about Earths moon? What would happen if it was larger or closer to us?

A

The moon is earths only natural satellite. It’s the 5-th largest satellite in our solar system/ If the moon was larger or closer to us, huge tides would result from the close moon that would overflow into the lowlands and erode the mountains. Basically, a tiny change to the way things run could cause unpleasant events.

33
Q

Explain the difference between metamorphic foliated and metamorphic nonfoilated

A

Metamorphic rocks have two classes: nonfoliated and foliated. Foliated: when a rock with flat or elongated minerals is put under immense pressure, the minerals line up in layers, creating foliatin. Examples: gneiss, slate, phylitte, schist; all have a layered appearance that is produced by exposure to heat and directed pressure. Nonfoliated rocks: do not contain the minerals that tend to line up under pressure and therefore do not have the layered appearance of foliated rocks. They can also form via metamorphism which happens when magma comes into contact with the surrounding rock. Examples: quartzite, marble, hornfels, novaculite

34
Q

Describe what atmospheric circulation is and how it causes the directions of the winds.

A

Atmospheric circulation is any air flow that refers to the general circulation of the earth and regional movements of air around areas of high and low pressure. In subtropical high pressure belts at 30 degrees N and 30 degrees S, air desceds causing the winds to blow westwards and towards the equator at earths surface. These winds merge and rise in the intertropical convergence, blowing eastwards and polewards. Atmospheric circulation creates winds across the planet as air moves from areas of high pressure to areas of low pressure.

35
Q

Explain how the Oscillating theory is different from the Big Bang Theory

A

The Oscillating theory, or the “big crunch”, is the idea that the universe is expanding now, but later it will syop turn around and collapse again to a point - ‘the crunch’. This comes from the fact that although we know that the universe is expanding, we also know that the gravity of all the matter in the universe is slowing that expansion. If there is enough matter in the universe, it would then have strong enough gravity to stop the expansion and cause a collapse. The Big Bang theory; the most important concept about the big bang is expansion not explosion. It explains the expansion of space itself, which in turn means everything contained within space is spreading apart from everything else. The universe was extremely hot and dense at first. there was so much energy that matter as we know it couldn’t form. But the universe expanded rapidly which meant the universe cooled down. As it expanded, matter began to form and radiation began to lose energy. In a few seconds, our niverse formed out of a sinularity that strctehed across space. One result of the big bang was the formation of the four basic forces in the universe: electromagnetism, strong nuclear force, weak nuclear force, and gravity.

36
Q

What are moraines? Why do we study them? Explain the different types

A

Moraines are linear rock deposits - basically any material left behind from a glacier. We study moraines in order to figure out how far glaciers have extended and how long it took to melt them away. There are 5 types of morianes: Lateral, Medial, Ground, Terminal, and End moraines. Lateral moraines typically form at the edges of the glacier as material drops onto a glacier from the erosion of valley walls. Medial moraines typically form where the lateral moraines of 2 tributary glaciers come together in the middle of a larger glacier. Ground moraines form when sediment undeneath a glacier melts. ground moraines contribute to the fertile-transported soils in numerous regions. Terminal moraines are described as long ridges of till that are left at the furthest point the glacier reached. End moraines are typically deposited where the glacier stopped for a long period of time, enough to create a rocky ridge, while it retreated

37
Q

Compare any 2 astronomers discussing their similarities and differences

A

Galileo Galilei invented the optical telescope that culd magnify objects 20x. He discovered the four primary moons of Jupiter, known as the Galilean moons, as well as the rings of Saturn. He saw the Venus revolved around the sun and agreed with Copernicus about planetary motion. Galileo stated that the earth and the planets must orbit around the sun. His discovery of Jupites moons was evidence that objects can orbit around other objects. Helen Hogg pioneered research into globular clusters and variable stars. She was the first female president of several astronomical organizations. She was a notable woman of science in a time when many universities would not award scientific degrees to women. Helen was an American-Canadian astronomer. She received numerous rewards for er work in astronomy.

38
Q

Identify and explain the 5 of the 6 changes in matter

A

Phase changes happen when you reach certain special points. Freezing is when a liquid turns into a solid. Condensation is when a gas turns into a liquid. Boiling is when liquid turns into a gas. Fusion/Melting is when a solid turns into a liquid. Sublimation is when a solid turns into a gas. It’s an endothermic process that requires/absorobs energy from its surroundings. Example: dry ice can turn into a gas when left in a room. Deposition is when a gas turns into a solid without going through the liquid state of matter. Example: frost on winter mornings; when water vapor turns into a solid.

39
Q

What is the difference between a physical change and a chemical change? Give examples

A

Physical changes are related to changes in the immediate environment. The basic chemical structure does not change when it is a physical change. Different ways to create a physical change includetemperature, pressure, other physical forces. Chemical changes is when something new is created. If the formula of water were to change, that wuld be a chemical change. If you add a secod oxygen atom to a water molecule, it becomes hydrogen peroxide. The molecules would not be water anymore. Different ways to create a chemical change include rotting, burning, exploding, and reactions to something added.

40
Q

Explain how normal magnetic polarity and reversed magnetic polarity appear on the ocean floor. How does it help prove the plate tectoics theory?

A

The youngest rocks at the ridge crest have present-day normal magnetic polarity meaning it points towards the north pole. Stripes of rock that are parallel to the ridge crest, alternate in magnetic polarity. Example: normal-reversed-normal, etc. This suggests that they were formed during different epochs and documented the nrmal and reversal episodes of the earths magnetic field. The magma that erupts from deep within the earth creates new oceanic crust, showing that the crust created from the magma shows the magnetic field at the time. This process is called seafloor spreading. Seafloor spreading is a geologic process in which tectonic plates - large slabs of earth’s lithosphere - split apart from each other.

41
Q

What is the difference between Convergent Boundaries and Transform Margins?

A

Convergent boundaries, also known as subduction zones, are located where the lithosphere mantle slides over an overiding plate. Deep sea trenches, destructin of seafloor crust, subduction. Transform margins are slip-sliding plates suhc as California’s San Andreas fault, here the North American and Pacific plates grind past each other with a mostly horizontal motion.

42
Q

Explain the difference between Igneous Extrusive and Igneous Intrusive

A

Igneous rocks are classified in two different ways: Intrusive and Extrusive. Igneous intrusive rocks are formed inside the earth and crystallize below the earths surface. The slow cooling that occurs allows for large crystals to form. Examples: granite - has a coarse texture with large mineral grains indicating that it spent thousands or millions of years cooling down inside the earth allowing large crystals to form. obsidian - has very small grains and a relatively fine texture, this happens when magma erutps into lava and then cools more quickly than it would have if it stayed inside the earth, giving crystals less time to form. Igenous extrusive rocks form outside or on top of the earth’s crust. Etxrusive rocks typically have a vesicular or holey texture.This happens when the ejected magma still has gases inside as it cools, resulting in the gases trapped and giving the rock a bubbly texture such as the rock pumice.

43
Q

Explain the difference between sedimentary clastic and sedimentary chemical. Give examples

A

Sedimentary clastic form from clasts or pieces of rocks. They form from the weathering o rbeaking down of the exposed rock into small fragments. Throughout the process of erosion, these fragments are removed from their source and transported by water, wind, ice, or any biological activity to a new location. Once the sediment settles somewhere, and enough of it collects, the lowest layers become so compacted and tight they form solid rock. Examples: conglomerate, sandstone, shale. Chemical sedimentary rocks form from chemical precipitation. A chemical precipitate is a chemical compound that forms when the solution it is dissolved in, usually water, evaporates and leaves the compound behind. Examples: limestone and salt

44
Q

List 5 out of the 6 geologic processes that can result in mountain building.

A

crustal shortening, crustal extension, continental collision, volcanism, heating or cooling of the lithosphere.

45
Q

Explain what hdyraulic fracturing is and the pros and cons of using this method of mineral extraction

A