ESS 101 B Laboratory 6 Quiz Metamorphic
Rocks Actual Exam 2026/2027 | Complete Exam-
Style Questions | 100% Verified – Detailed
Rationales – Pass Guaranteed – A+ Graded
TABLE OF CONTENTS
Section 1 | Metamorphic Processes and Conditions | Q1 – Q13
Section 2 | Metamorphic Rock Types and Identification | Q14 – Q25
Section 3 | Metamorphic Textures and Structures | Q26 – Q37
Section 4 | Metamorphic Grade, Facies, and Applications | Q38 – Q50
Instructions: Choose the single best answer. Pass: 75% in 60 minutes.
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SECTION 1: METAMORPHIC PROCESSES AND CONDITIONS Q1 – Q13
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Question 1 of 50
During a field mapping project in the contact aureole of a granite intrusion, you observe a shale
unit that has been baked but retains its original bedding. The rock is hard, fine-grained, and
breaks with a conchoidal fracture. Which metamorphic process is primarily responsible for this
specific texture?
A. Differential stress
B. Hydrothermal alteration
C. Thermal metamorphism
D. Dynamic metamorphism ✓ Correct Answer
Correct Answer: C
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Rationale: Thermal metamorphism, driven by the heat from the magma intrusion, causes
recrystallization without significant directed pressure, preserving the original bedding while
hardening the rock. Differential stress would have created foliation, destroying the original
sedimentary structures, while hydrothermal alteration usually involves significant fluid changes.
This process creates the "baked zone" or hornfels often found surrounding igneous intrusions.
Question 2 of 50
A geologist is studying a deep-sea subduction zone where oceanic crust is being dragged under a
continental plate. The rocks here are undergoing metamorphism under extremely high pressure
but relatively low temperatures compared to their depth. What specific type of metamorphism is
occurring in this setting?
A. Burial metamorphism
B. Impact metamorphism
C. Blueschist facies metamorphism
D. Contact metamorphism ✓ Correct Answer
Correct Answer: C
Rationale: The low geothermal gradient in subduction zones creates high-pressure, low-
temperature conditions characteristic of blueschist facies metamorphism. Burial metamorphism
occurs with higher geothermal gradients, while impact metamorphism is caused by meteorite
strikes. These unique conditions produce minerals like glaucophane that define the blueschist
facies.
Question 3 of 50
In the laboratory, you examine a metamorphic rock sample that contains garnet crystals but no
sillimanite. Based on the stability fields of these index minerals, what can you infer about the
pressure and temperature conditions relative to the sillimanite zone?
, 3
A. Lower temperature and lower pressure
B. Higher temperature but similar pressure
C. Lower temperature or lower pressure
D. Higher pressure but variable temperature ✓ Correct Answer
Correct Answer: C
Rationale: Garnet typically forms at lower grades than sillimanite, so the absence of sillimanite
suggests the rock either did not reach the high temperatures required or the specific pressure
conditions for sillimanite stability. Assuming the rock is not retrograde, it simply exited the
stability field before forming sillimanite. This helps geologists map isograds in regional
metamorphic terrains.
Question 4 of 50
While conducting a geothermal gradient study, you note that fluids act as a catalyst for
metamorphic reactions. How chemically active fluids primarily facilitate the recrystallization of
minerals during metamorphism?
A. By increasing the lithostatic pressure
B. By dissolving ions and enhancing ion mobility
C. By removing the source of heat
D. By increasing the differential stress ✓ Correct Answer
Correct Answer: B
Rationale: Fluids facilitate metamorphism by dissolving mineral ions in areas of high stress and
transporting them to areas of low stress, effectively enhancing ion mobility and reaction rates.
They do not increase lithostatic pressure or differential stress, nor do they remove the heat
source. This process is essential for creating larger crystal sizes during metamorphism.
Question 5 of 50