⚛️ Metamorphic Rocks & the Rock Cycle — printable rubric packet (Geology Unit 04). Print 8.5×11 portrait. Every page is designed for clipboard use while you grade at the bench.
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▲ Page 1 — Unit overview
Bright Minds Geology · Course Pack
Metamorphic Rocks & the Rock Cycle — Unit Packet
Overview
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This packet is everything a parent or guide needs to assess Unit 04 at home — learning targets, the answers that count as correct, the mastery rubric, calibration examples, and a clipboard score sheet. No multiple-choice test: the student shows mastery by identifying metamorphic rocks, inferring each one’s protolith, and routing a grain around the rock cycle aloud.

Unit learning targets

By the end of the Metamorphic Rocks & the Rock Cycle unit, a student should be able to:

How this unit is assessed

Mastery rubric

Six criteria, each judged Not yet / Approaching / Mastered (Page 3).

Bench & rock-cycle routing

Identify metamorphic rocks and route a grain through the cycle.

Oral check

The student defends the protolith and cycle path each rock records (Page 4).

Lab notebook

Rock ID, inferred protolith, and the traced cycle path kept distinct.

How to read a Bright Minds rubric

You are making a decision, not adding up points. For each criterion, decide whether the work is Not yet, Approaching, or Mastered — the column language tells you which. A criterion counts as mastered only when the student can both name the rock and defend the protolith and cycle path it records. A student carries three tokens per term; one token buys a re-do of one criterion on another day, so a single bad afternoon never sinks the unit.

▲ Page 2 — Key terms
Metamorphic Rocks · Vocabulary
Key Terms — What Counts as Correct
Vocabulary
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Accept any answer in the synonyms column — they are pre-approved as equivalent. The third column flags the confusions that look close but are not yet, so you can coach precisely.

Canonical answerAccepted synonymsCommon confusion / discriminator
Metamorphism
Metamorphismchange by heat & pressureThe rock stays solid — it recrystallizes, it does not melt
Recrystallizationsolid-state regrowthMinerals regrow larger or realign without the rock melting
Directed pressuredifferential stressSqueezing from one direction; aligns minerals into bands
Texture & grade
Foliationbanding / layeringMineral alignment under directed pressure — not sedimentary layers
Non-foliatedunbandedNo alignment; e.g. marble, quartzite
Metamorphic gradeintensity of changeRises with heat & pressure: slate → phyllite → schist → gneiss
Protolithparent rockWhat the rock was before metamorphism — limestone → marble
The rock cycle
Rock cyclerock-forming loopAny rock can become any other; not a one-way path
Marblemetamorphosed limestoneNon-foliated; protolith is limestone (a carbonate)
Quartzitemetamorphosed sandstoneNon-foliated; protolith is quartz sandstone
Gneisshigh-grade banded rockCoarse light/dark bands; highest grade in the slate–gneiss series
▲ Page 3 — Mastery rubric
Metamorphic Rocks · Mastery Rubric
Six Criteria — Not yet / Approaching / Mastered
Rubric
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CriterionNot yetApproachingMastered
Heat & pressure without meltingThinks metamorphism means the rock melted.Names heat and pressure but not that the rock stayed solid.Explains how heat and pressure recrystallize a rock in the solid state, short of melting.
Foliated vs non-foliatedCannot tell banded from unbanded rock.Labels foliation but cannot say what causes it.Distinguishes foliated from non-foliated rock and explains foliation as mineral alignment under directed pressure.
Metamorphic grade (slate → gneiss)Treats all foliated rock as the same.Orders part of the sequence but misplaces phyllite or schist.Orders slate, phyllite, schist, and gneiss by rising grade and reads increasing heat and pressure.
Protolith reasoningCannot say what a metamorphic rock started as.Guesses a protolith without evidence.Infers the protolith — limestone to marble, sandstone to quartzite, shale to slate — from texture and composition.
The rock cycleTreats the three rock families as unrelated.Names the rock cycle but cannot route a grain through it.Traces a mineral grain around the full rock cycle, linking igneous, sedimentary, and metamorphic paths.
Integration (cross-domain)Treats the science as isolated facts.Names a link to history, reading, or writing but cannot defend it.Connects the unit across History · Reading · Writing and defends why it matters.
What “Mastered” requires
The student identifies the rock and infers its protolith from texture and composition, then routes a grain through the rock cycle — unprompted.
What does not pass
Saying metamorphism “melted” the rock is Not yet on criterion 1 — recrystallization happens in the solid state, short of melting.
Grading it at home

The split between Approaching and Mastered is the rock’s history: not just naming marble, but inferring it came from limestone and placing it in the cycle. Ask “what was this rock before, and where does it go next?”

▲ Page 4 — Anchor exemplars
Metamorphic Rocks · Calibration
Anchor Exemplars — To Calibrate Your Ear
Anchors
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Read these before you grade. They show what Mastered and Not yet actually sound like, plus the edge cases where you should coach rather than decide on the spot.

Protolith & grade reasoning

▶ Mastered
“This is schist — shiny, wavy foliation with visible mica, so it’s higher grade than slate. It started as shale, and with more heat and pressure it would band into gneiss. The rock never melted; the minerals just realigned in the solid state.”
▶ Not yet
“It’s a shiny rock. It got hot so it must have melted and hardened again. I don’t know what it used to be.”

Integration — Hutton & the rock cycle

▶ Mastered
“Hutton saw rock as a cycle with ‘no vestige of a beginning’ — this marble was once limestone made of sea shells, buried and cooked into stone, and one day it will weather back into sediment. Every rock is mid-journey.”
▶ Not yet
“Hutton had a theory about rocks.” (A name, with no link to the cycle or deep time.)

Edge cases — coach, don’t fail

▶ Metamorphism read as melting
Says the rock “melted and re-formed.” Coach: metamorphism is solid-state — recrystallization short of melting. Melting would make it igneous. Common, fixable.
▶ Foliation vs sedimentary layers
Calls foliation “sediment layers.” Coach: foliation is mineral alignment under directed pressure, not beds laid down by water.
▲ Page 5 — Score sheet (clipboard)
Metamorphic Rocks · Score Sheet
Unit Score Sheet — One per student
Score Sheet
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Student: ______________________________________    Date: _______________    Guide: _________________________

Mastery criteria — circle one per row

#CriterionDecisionNotes
1Heat & pressure without meltingNY / Appr / Mast
2Foliated vs non-foliatedNY / Appr / Mast
3Metamorphic grade (slate → gneiss)NY / Appr / Mast
4Protolith reasoningNY / Appr / Mast
5The rock cycleNY / Appr / Mast
6Integration (cross-domain)NY / Appr / Mast

Bench & rock-cycle routing — technique check

Token used this session?

☐ No    ☐ Yes — for criterion: __________    Tokens remaining: ☐ 3   ☐ 2   ☐ 1   ☐ 0

NY = Not yet · Appr = Approaching · Mast = Mastered · Unsure between two levels? Circle the lower one and note what a re-do would need.