⚛️ 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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Use these targets, vocabulary, rubrics, examples, and score sheet with the instructor's approved lesson and procedure. This is an assessment companion, not a complete lesson or safety authorization.

Student lessons, data, and worked answers: Unit 04 learning pathway.

Unit learning targets

The student demonstrates the following:

How this unit is assessed

Mastery rubric

Five science criteria plus separately reported integration (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 Developing, Proficient, or Mastery — 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. Each student has three tokens per term; each token retries one rubric criterion. Approved accommodations, equipment failures, and approved absences are handled separately and do not consume these tokens.

▲ Page 2 — Key terms
Metamorphic Rocks · Vocabulary
Key Terms — What Counts as Correct
Vocabulary
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Accept listed synonyms; use the distinction column to resolve near-matches.

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 — Developing / Proficient / Mastery
Rubric
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CriterionDevelopingProficientMastery
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 & physical modelsConfuses grade, depth, and texture.Uses one texture as an exact pressure-temperature gauge.Interprets the common pelitic grade sequence and assigned pressure/temperature calculations, accounting for composition and model limitations.
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 cycle (lab)Treats 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)Makes no supported connection between the source and the science.Uses the source but needs help connecting evidence, writing, or limitations to the science.Independently connects History, Reading, and Writing using a cited source, appropriate evidence, a limitation, and a scientific explanation.
What “Mastery” 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 Developing on criterion 1 — recrystallization happens in the solid state, short of melting.
Grading it at home

The split between Proficient and Mastery 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 Mastery and Developing actually sound like, plus the edge cases where you should coach rather than decide on the spot.

Protolith & grade reasoning

▶ Mastery
“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.”
▶ Developing
“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

▶ Mastery
“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.”
▶ Developing
“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 meltingDev / Prof / Mast
2Foliated vs non-foliatedDev / Prof / Mast
3Metamorphic grade & physical modelsDev / Prof / Mast
4Protolith reasoningDev / Prof / Mast
5The rock cycle (lab)Dev / Prof / Mast
6Integration (cross-domain)Dev / Prof / Mast

Bench & rock-cycle routing — technique check

Used a token this session?

☐ No    ☐ Yes — for criterion: __________
Tokens left this term after this session (choose one): ☐ 3   ☐ 2   ☐ 1   ☐ None left

Dev = Developing · Prof = Proficient · Mast = Mastery · Unsure between two levels? Circle the lower one and note what a re-do would need.