Unit 11 · Earth Science arc · 7th grade

Solid,
not still.

The ground under your chair is moving right now — slower than your fingernails grow, and unstoppably. Continents drift, oceans open, mountains rise. One small freshwater reptile left the proof on two different coasts.

a cracked shell 6 manipulatives 12 flashcards 1 reptile
the atlantic mesosaurus ×2 same freshwater reptile. two coasts. one ocean between.

it couldn't swim salt water. so where was the ocean?

The phenomenon · scrub 270 million years

The Reptile That Couldn't Swim an Ocean

Mesosaurus: a small freshwater reptile, 270 million years dead. Its fossils turn up in exactly two places — eastern South America and southern Africa. Freshwater animals don't cross salt oceans, and it had no wings. So either it broke the rules… or the ocean wasn't there. Scrub the years and watch the Atlantic open.

the atlantic opens 270 million years ago · pangaea
270 Ma · joinedtoday · 3,000 km apart

Alfred Wegener read the map like this in 1912 and said the unsayable: the continents move. The fossils agreed. The rocks agreed. The coastlines agreed. Geologists said he was a crank — until WWII submarines mapped the seafloor and found the smoking gun lying in the middle of the ocean. The data was right before the theory was allowed.

Watch · Khan Academy

The theory, and the smoking gun

The case file · four independent witnesses

The evidence never met itself

Four separate lines of proof, gathered by different people with different tools over a century — all pointing the same direction. That's how you know it's not a coincidence.

01

Fossil twins

Mesosaurus in Brazil AND South Africa. Cynognathus and Lystrosaurus on three continents each. Identical land animals, separated by salt water — unless there was no water between them.

02

Matching rocks

The same rock layers, same ages, same mountain belts line up across the Atlantic — Brazil to Ghana, Appalachians to Scotland. The mountains were one range, split mid-slope.

03

The jigsaw coastlines

Everyone notices it on their first globe: South America's bulge fits Africa's bite. Wegener's starting point — and still the class favorite.

04

The smoking gun

Seafloor mapping after WWII: the youngest rock sits at the mid-ocean ridge, getting older symmetrically away from it. The ocean floor is being made at the middle and spread outward.

Manipulative · the conveyor

The shell is cracked — and it rides

Earth's rigid outer shell — the lithosphere — is broken into about 15 major plates, floating on a softer, slowly-flowing mantle (the asthenosphere). Heat from the core rises, cools, sinks: convection, the planet's conveyor belt. Watch it turn.

hot rises cool sinks new crust here

the conveyor never stops — it just moves at fingernail speed

Fingernail speed

Your fingernails grow about 3.5 cm a year. The Atlantic widens about 2.5 cm a year. Continents move at literally fingernail speed — and given a hundred million years, that's an ocean.

Scale check

Plate tectonics is the champion of Scale, Proportion, and Quantity: centimeters per year × millions of years = oceans opening, mountains rising, and a map that never sits still.

Manipulative · three moves

Where the action is: the edges

Plates barely change in the middle — everything interesting happens at the boundaries. Apart, together, or sideways: pick a move and run it.

the mantle conveyor

divergent: the blocks drift apart and new crust wells up between them — Iceland is splitting down the middle this way (you can SCUBA in the crack).

Standards: MS-ESS2-2 — geoscience processes change Earth's surface at varying time and spatial scales · MS-ESS2-3 — fossil, rock, coastline, and seafloor evidence of past plate motions (NGSS Lead States, 2013). DCIs: ESS2.A Earth's Materials and Systems, ESS2.B Plate Tectonics and Large-Scale System Interactions. CCCs: Scale, Proportion, and Quantity (fingernail speed × deep time), Patterns (the evidence agrees).

Myth-busters · tap to flip

Unlearn these three things

Manipulative · Spaced repetition

Say it like a scientist

Twelve words. Flip the card, grade yourself honestly, and the deck schedules your next review — hard words come back sooner. Come back tomorrow and it remembers you. (It lives in your browser, no account.)

due now
locked in
seen so far

flip the card, then grade yourself

Sketch · sketchnotes

Map the plates before you explain the drift

The exact page videos are identified. Printable sheets stay pending until transcript and analysis packages pass the sketchnote source gate.

Introduction to plate tectonics · 7jbwX1Uvd18 · 4:35

Sketchnote in the works

status page/video ID saved · analysis package pending

Plate tectonics and the ocean floor · A98wPKiPMJw · 4:00

Sketchnote in the works

status page/video ID saved · analysis package pending

Investigate · evidence first

Make the boundary move

The plate and seafloor models remain usable now; a print-first prediction record is queued after source review.

MS-ESS2-1 · plate evidence

Investigation in the works

Use the existing page models now. The exact transcript package and classroom record are still pending.

in the works

Exit ticket · 5 questions

Before you leave the ridge

No grade, no stakes — just proof the drift stuck. Answer all five to earn the stamp.

question 1 of 5

The ground is a conveyor.
Stand anywhere — you're moving.

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