The course map.
Eight units — four per semester — the labs that anchor them, and the two-day rhythm that runs every week of the year. This is the planner’s view — the whole course on one page.
Two days a week, and the work between them.
Every unit runs on the same rhythm: Concept Day → [student works at home] → Field & Lab Day → [student synthesizes at home] → next Concept Day. One day forces a choice between depth and breadth; two days allow both. More than two crowds out the at-home work where integration actually happens.
Concept Day
- Arrival & warm-up — reconnect with the prior session
- Pre-lecture discussion — surface what the at-home reading raised
- Direct instruction — micro-lectures, worked problems, demonstrations
- Problem set / model work — apply the concept, solo or in pairs
- Misconception sweep & wrap-up — correct common errors, preview the lab
Guide's role: Socratic and diagnostic. Student's role: active participation; pre-reading required.
Field & Lab Day
- Pre-lab briefing — the question, the procedure, the safety
- Safety check — goggles, dust control, careful handling of specimens & the rock hammer; explicit, every time
- Setup — hand lenses, streak plates, Mohs kit, rock & mineral sets, partner assignment
- Execution — the lab itself; the guide circulates and coaches
- Debrief & lab notebook — completed before the student leaves
- Cleanup & specimen return — sets re-sorted and shelved to standard; non-negotiable
Guide's role: safety officer first, teacher second. Student's role: the lab notebook is THE artifact — predictions before results.
From the first mineral to deep time.
The sequence is deliberate: each unit assumes the one before it. Click any unit to open its mastery rubric — the standard a student demonstrates against to advance.
| Unit | Big ideas | Anchor lab(s) | Integrates with |
|---|---|---|---|
| 01 · Minerals | Mineral evidence, density and uncertainty, property keys, resource grade and recovery | Mineral ID by streak, hardness & acid test, worked through a dichotomous key | Foundation unit; the naturalists who first classified minerals (history, reading); applied math: Mohs ordering & density |
| 02 · Igneous Rocks & Volcanism | Magma vs. lava, intrusive vs. extrusive, crystal size vs. cooling rate, Bowen's reaction series, felsic→mafic, volcano types & eruption style | Igneous rock & crystal-size analysis | Builds on 01 — the minerals that crystallize from a melt; famous eruptions (history, geography); applied math: cooling rate vs. crystal size |
| 03 · Sedimentary Rocks & Stratigraphy | Sediment → clastic, chemical & organic rocks, cementation, superposition, original horizontality, lateral continuity, cross-cutting, unconformities | Sedimentary layering & stratigraphy | Builds on 01 — the minerals that survive weathering; Steno's principles of layering (history, reading); applied math: bed thickness & sequence logic |
| 04 · Metamorphic Rocks & the Rock Cycle | Heat + pressure, foliated vs. non-foliated, protoliths (shale→slate→schist→gneiss; limestone→marble), the full rock cycle | Metamorphic rock & rock-cycle sorting | Builds on 02 + 03 — closes the rock cycle; Hutton's endlessly recycled Earth (history, reading); applied math: pressure–temperature grids |
| 05 · Plate Tectonics & Mountain Building | Divergent, convergent & transform boundaries, seafloor spreading, subduction, orogeny (folding, faulting, uplift) | Plate-boundary & seismic-map modeling | Builds on 04 — where rock is forged and destroyed; the mapping of the ocean floor (history, geography); applied math: plate-motion rates |
| 06 · Earthquakes & Earth's Interior | Elastic rebound, P, S & surface waves, locating epicenters by triangulation, seismic evidence for the crust, mantle, outer & inner core | Approved seismic records or a labeled location model; magnitude, intensity and hazard probability | Builds on 05 — why and where the crust ruptures; the seismologists who read Earth's interior (history); applied math: travel-time curves & triangulation |
| 07 · Weathering, Erosion & Landforms | Weathering, transport, groundwater storage and flow, hydraulic head, karst and landscape hazards | Non-destructive observation or approved images; Darcy-flow and time-integrated sediment datasets | Builds on 01 + 03 — the front of the rock cycle; landscapes that shaped settlement (geography, history); applied math: rates of erosion & sediment yield |
| 08 · Geologic Time & Earth History | Relative relationships, conditional isotope clocks, deposition brackets, uncertainty and deep time | Radiometric-dating / half-life simulation | Builds on 03 — relative order before absolute age; Hutton → Lyell & the discovery of deep time (history, reading); applied math: half-life decay curves |
Every unit carries the core spokes — History, Reading, and Writing — anchored to the story in the integration guide. The column above names each unit’s distinctive spokes; geography and soft social studies run where they fit, and students pick from elective spokes (data, ethics, economics, technology, art). An applied-math lane runs through every unit too — math used in service of the science, never as a separate program.
Where mastery gets proven in person.
Three times across the year, the student steps up to a demonstration that cannot be faked, outsourced, or generated. These are the AI-proof core of the course — understanding, shown in real time, against a rubric, in front of a guide.
The rock & mineral ID defense
Identify unknown specimens by streak, hardness, cleavage, luster, and the dilute-acid test — then defend each call out loud, under questions.
Timed map & cross-section reading
Read a geologic map, cross-section, and seismogram under time — then justify the story the rocks tell.
Oral lab-notebook defense
Walk a guide through your own notebook: the question, the method, the data, the anomalies, the interpretation.
Assigned student learning
Open the eight learning pathways for specific reading sections, explanations, datasets, leveled practice, public practice answers (not assessment keys), and transfer evidence. Print the student unit pages alongside the separate assessment packets. Broad book recommendations do not replace the assigned sections.