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Quiz about Metamorphism  The Story of a Changed Rock
Quiz about Metamorphism  The Story of a Changed Rock

Metamorphism: The Story of a Changed Rock Quiz


These rocks are as pathetic a lot as ever you'll find. They can't take the heat. They buckle under pressure. After a while, you can't even discern their former selves! Take this quiz to learn the story of a Changed Rock...

A multiple-choice quiz by pu2-ke-qi-ri. Estimated time: 7 mins.
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Author
pu2-ke-qi-ri
Time
7 mins
Type
Multiple Choice
Quiz #
233,031
Updated
Dec 03 21
# Qns
10
Difficulty
Very Difficult
Avg Score
4 / 10
Plays
1627
Awards
Top 35% Quiz
Last 3 plays: PurpleComet (7/10), Guest 197 (3/10), Guest 64 (2/10).
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Question 1 of 10
1. Our story begins a long time ago on a tectonic plate far, far away. Our rock, let's just call him Bob the Basalt, solidifies from basaltic lava pouring out of a volcano at a midoceanic ridge. At the moment of his birth, is Bob a metamorphic rock?


Question 2 of 10
2. Bob the Basalt spends his short happy life as a part of the top layer of the ocean crust. All good things must come to an end, however, and Bob's plate begins subducting beneath another plate, this one made out of continental crust. Bob and all his friends start on their journey into the upper mantle. What kind of rock does Bob become? Hint


Question 3 of 10
3. As Bob goes deeper and deeper into the mantle, he becomes yet another different kind of rock. What rock does Bob-the-former-Basalt turn into at conditions above 500 degrees C and 1.2 gigapascals? Hint


Question 4 of 10
4. Maybe Bob meets his end in the mantle. Maybe Bob bobs up to the surface if the lower, denser part of the plate de-laminates from the downgoing slab and sinks. In any case, let's turn our attention to his sister, Hillary Tuff. Hillary Tuff formed when a volcano in an island chain coughed up a lot of volcanic ash, which settled in a layer on the flank of the volcano. Hillary Tuff has the same bulk composition as Bob the Basalt. When this island chain runs into the continent and things start to heat up just a little bit, what kind of minerals form in Hillary? Hint


Question 5 of 10
5. As the Hillary Tuff formation rams into the continent at full steam, Hillary goes through the mid-T, mid-P greenschist and amphibolite facies. Remember, Hillary has a mafic bulk composition. If Hillary is mostly consists of plagioclase and amphibole in the greenschist facies, what will happen to her in the amphibolite facies? Hint


Question 6 of 10
6. Let's shift our attention from Hillary Tuff to the excitement on the continent that was unlucky enough to run into an island arc. The island arc is pretty well stuck. It's just too darn big and bulky to subduct. The continent ain't moving, either. They're gradually getting smushed together. What sort of geologic event do we have here? Hint


Question 7 of 10
7. A great big wedge of muddy sediment lay of the edge of this continent. We'll call it Pete the Pelite. Pete became several different kinds of rock on his way to fame-- the lower temperature metamorphosed parts of him are now covering the floors and roofs of the homes of the rich and famous. What is the order, from lowest temperature and pressure to highest, of the kinds of rocks that Pete the Pelite became? Hint


Question 8 of 10
8. It just so happens that at the moment, Pete the Pelite is equilibrating to conditions in the lowest temperature portion of the amphibolite facies. Which mineral is just now forming in Pete? Hint


Question 9 of 10
9. Next to Pete the Pelite we have Cici the Siliceous Limestone. Before metamorphism occurred, Cici consisted of calcite with a little bit of quartz. What mineral will most likely form in Cici? Hint


Question 10 of 10
10. Finally, we come to Bryce the Gneiss. Would Bryce be more likely to melt in the presence or absence of water?

Answer: (One word, "presence" or "absence.")

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Quiz Answer Key and Fun Facts
1. Our story begins a long time ago on a tectonic plate far, far away. Our rock, let's just call him Bob the Basalt, solidifies from basaltic lava pouring out of a volcano at a midoceanic ridge. At the moment of his birth, is Bob a metamorphic rock?

Answer: No

Bob the Basalt is an igneous rock. Igneous rocks solidify from some sort of molten rock, whether quickly at the surface (extrusive/volcanic) or slowly in magma chambers at depth (intrusive/plutonic). Metamorphic rocks, to give a rather posh definition from the IUGS, form as a result of "subsolidus processes leading to changes in mineralogy and/or texture (for example grain size) and often in chemical composition of a rock." In other words, metamorphism comes from changes in the size and type of minerals present in a rock under conditions that don't lead to the rock melting completely.
2. Bob the Basalt spends his short happy life as a part of the top layer of the ocean crust. All good things must come to an end, however, and Bob's plate begins subducting beneath another plate, this one made out of continental crust. Bob and all his friends start on their journey into the upper mantle. What kind of rock does Bob become?

Answer: Blueschist

The amphibole mineral "glaucophane" gives blueschist its distinctive blue color. Glaucophane only forms in relatively high pressure, low temperature conditions. These are the pressure- temperature conditions of a subduction zone! The pressure increases relatively rapidly as the plate subducts, but rocks are poor conductors of heat, so the subducting plate stays rather cool. Of course, this still means anything up to 500 degrees C!
3. As Bob goes deeper and deeper into the mantle, he becomes yet another different kind of rock. What rock does Bob-the-former-Basalt turn into at conditions above 500 degrees C and 1.2 gigapascals?

Answer: Eclogite

I call eclogite "the Christmas rock" because it is green with red spots! The green is the mineral omphacite, a clinopyroxene, and the red is pyropic (= high Mg) garnet. At such high pressures and temperatures, all the elements present in the rock can be crammed into just two minerals.
4. Maybe Bob meets his end in the mantle. Maybe Bob bobs up to the surface if the lower, denser part of the plate de-laminates from the downgoing slab and sinks. In any case, let's turn our attention to his sister, Hillary Tuff. Hillary Tuff formed when a volcano in an island chain coughed up a lot of volcanic ash, which settled in a layer on the flank of the volcano. Hillary Tuff has the same bulk composition as Bob the Basalt. When this island chain runs into the continent and things start to heat up just a little bit, what kind of minerals form in Hillary?

Answer: Zeolites

These very low temperature and pressure conditions are known as the "zeolite facies," after the zeolite minerals that form in them. The zeolite facies, to quote my TA, is the "easy-bake oven version of metamorphism." Zeolite minerals are very hydrous and low density. If you're only going to remember two zeolite minerals, make it laumontite and analcite...Nah, just remember "zeolite"!
5. As the Hillary Tuff formation rams into the continent at full steam, Hillary goes through the mid-T, mid-P greenschist and amphibolite facies. Remember, Hillary has a mafic bulk composition. If Hillary is mostly consists of plagioclase and amphibole in the greenschist facies, what will happen to her in the amphibolite facies?

Answer: She'll still be mostly plagioclase and amphibole.

Metamorphism of mafic rocks isn't all that spectacular. At the amphibolite facies, the minerals epidote and chlorite disappear. That's it for reliable, obvious changes in mineralogy! Whoop-dee-do. The chemical composition of the plagioclase and amphibole does change, and it is possible to sorta work out these changes in a petrographic microscope (or, better, an electron microprobe!)
6. Let's shift our attention from Hillary Tuff to the excitement on the continent that was unlucky enough to run into an island arc. The island arc is pretty well stuck. It's just too darn big and bulky to subduct. The continent ain't moving, either. They're gradually getting smushed together. What sort of geologic event do we have here?

Answer: Orogeny (mountain-building episode)

Mountain building produces some of the most extreme examples of metamorphism. Just think of the Himalayas or the Alps, and how much heated and deformed rock would be needed to make mountains that high!
7. A great big wedge of muddy sediment lay of the edge of this continent. We'll call it Pete the Pelite. Pete became several different kinds of rock on his way to fame-- the lower temperature metamorphosed parts of him are now covering the floors and roofs of the homes of the rich and famous. What is the order, from lowest temperature and pressure to highest, of the kinds of rocks that Pete the Pelite became?

Answer: Shale, slate, phyllite, schist

Shale isn't even a metamorphic rock. Slate has a slight sheen and splits into perfectly flat sheets. Phyllite is like slate, but the mineral grains are big enough to be seen in a hand lens. In schist, the minerals are big enough to be seen with the naked eye. Why do all of these rocks split into flat sheets so cleanly? They contain minerals, like biotite and muscovite mica, that form flat sheets all aligned in the same direction.
8. It just so happens that at the moment, Pete the Pelite is equilibrating to conditions in the lowest temperature portion of the amphibolite facies. Which mineral is just now forming in Pete?

Answer: Staurolite

You may have seen staurolite-- it's the mineral that forms those interesting cross shapes. Quite a while ago, a fellow named George Barrow recorded a series of minerals that appeared in rocks of pelitic composition under increasing pressure-temperature conditions.

They are: chlorite, biotite, garnet, staurolite, kyanite, sillimanite. Pelites are nice because they go through such obvious changes in mineralogy when the pressure and temperature change!
9. Next to Pete the Pelite we have Cici the Siliceous Limestone. Before metamorphism occurred, Cici consisted of calcite with a little bit of quartz. What mineral will most likely form in Cici?

Answer: Wollastonite

To give the chemical formulas, CaCO3 (calcite) + SiO2 (quartz) = Ca2SiO3 (wollastonite) + CO2 Temperature, pressure, and the mole fraction of CO2 in any fluids present determine when this reaction occurs. High temperature, high pressure, and low mole fraction of CO2 favor the formation of wollastonite. And you thought limestone just turned into marble, huh?
10. Finally, we come to Bryce the Gneiss. Would Bryce be more likely to melt in the presence or absence of water?

Answer: Presence

Water can lower the melting temperature of a rock by a couple hundred degrees! It is possible to find metamorphic rocks that have been partially melted-- they're called migmatites. Total melting, and, well, that's it for metamorphism!

Many thanks to benniebenbenny for suggesting the title for this quiz!
Source: Author pu2-ke-qi-ri

This quiz was reviewed by FunTrivia editor crisw before going online.
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