Grade 10 Science
Motion — Speed, Distance, Time
- L1Lesson 1Reading the Quantitiesspeed, distance or time — the units say which
Welcome to the exam room — this chapter is about things that move, and it stars exactly three characters. A distance is ground covered: it wears metres (m) or kilometres (km).
- L2Lesson 2The Speed FormulaSay it aloud and it's yours
Read aloud: v equals d over t. v is the speed, d the distance, t the time — and a formula you can SAY is a formula you own, so say it now (quietly is fine, nobody's looking).
The formula in this lesson - L3Lesson 3Calculate the Speedrunners, cyclists, cars — numbers into sockets
The working habit that earns full marks, here and in every science course after this one: set up before you solve.
- L4Lesson 4Solve for Distanced = v·t · the seconds cancel
Sometimes the speed is the given and the distance is the mystery. One formula, turned around: d = vt — read aloud, d equals v t.
- L5Lesson 5Solve for Timet = d/v · how long will it take
Every “are we there yet” ever asked is this formula, waiting to be written down. Run the units check again: m over m/s — the metres cancel and seconds remain.
- L6Lesson 6Speed in Real Unitsm/s ↔ km/h · the ×3.6 bridge
Physics thinks in m/s; the road signs outside think in km/h.
- L7Lesson 7Average Speed over a Whole Triptotal distance over total time — no shortcuts
Real trips change pace — highway, roadwork, back roads.
The formula in this lesson - ★Boss lessonThe Highway Runthe boss · no calculator · three legs, one average
No calculator — the numbers are picked to fit in your head, the way a good exam question always secretly is.
Light & Geometric Optics
- L9Lesson 9Light as a WaveEvery wave obeys it, light included
And here is the wonderful part: light plays by the same rule.
The formulas in this lesson, - L10Lesson 10The Index of RefractionHow much a medium slows light
But push light INTO glass or water and it genuinely slows down.
The formula in this lesson - L11Lesson 11Snell's LawLight bends at the border
A straw in a glass of water looks broken at the surface because light changes direction the instant it changes speed.
The formula in this lesson - L12Lesson 12The Critical Angletotal internal reflection · the angle of no escape
Light leaving water for air bends AWAY from the normal — the exit angle is always wider than the angle inside.
- L13Lesson 13Curved MirrorsThe focus sits at half the radius
A concave mirror is a polished slice of a sphere, and that sphere has a radius R — the radius of curvature. Shine parallel rays at the mirror (sunlight does nicely) and they all bounce through one bright point: the focus.
The formula in this lesson - L14Lesson 14The Thin Lens EquationThe chapter's first full ladder
It is this chapter's first full ladder: pick the formula, rearrange it, place the givens, then compute. The one rule of reciprocal land: never add the plain distances.
The formula in this lesson - L15Lesson 15MagnificationMinus means upside down
Magnification answers the honest question: how many times bigger is the image than the thing itself?
The formulas in this lesson, - L16Lesson 16Lens Power in DioptersP = 1/f · metres only — mind the cm
A SHORT focal length means a strong lens that bends light hard, so flipping f makes bigger mean stronger — which is exactly how a label should behave.
- ★Boss lessonBoss — The Optics Benchthe boss · no calculator · candle, lens, screen
One candle, one lens, one screen, and every answer feeds the next: the focal length, then the image's new position when the candle moves, then the magnification, then the height of the flame on the screen.
Heat & Temperature
- L18Lesson 18Heat Is Not Temperaturejoules move, degrees describe
Dip a spoon in your hot chocolate and dip a spoon in a hot bath. The hot chocolate is hotter — but the bath could melt a whole snowman, and the mug could not.
- L19Lesson 19Specific Heat CapacityThe price tag on a degree
Warming things up costs energy, and every material posts its price: the specific heat capacity c, in joules per kilogram per degree.
The formula in this lesson - L20Lesson 20Rearranging Q = mcΔTmass, price tag or climb — the mystery metal
Detectives with thermometers. Your safety rail when rearranging is the units. Whatever you solve for, push the units through: if they refuse to cancel down to the answer's units, the rearrangement is wrong — no appeal.
- L21Lesson 21Latent Heat of Phase ChangeEnergy in, temperature flat
Drop a thermometer into a glass of melting ice and watch closely: heat pours in from the warm room, and the reading parks at 0 °C until the last sliver of ice is gone.
The formula in this lesson - L22Lesson 22Climbing the Heating Curvesensible plus latent · add every leg
The rule is simply to price every leg and add them. Ice from the deep freeze climbs to 0 °C, crosses the melting plateau, and climbs again as water — three legs, three lines, one total.
- L23Lesson 23Thermal ExpansionWhy the rail has gaps
Warm a solid and it grows — every metre of it, by a tiny fixed fraction, for every degree.
The formula in this lesson - L24Lesson 24Heat Flowing Through a WallA rate, not a total
So far every answer has been a lump sum of joules. But heat through a window never finishes — it runs as a steady rate, joules every second, and a joule per second has a name you know from light bulbs: the watt.
The formula in this lesson - ★Boss lessonThe Kettle Problemthe boss · no calculator · tap to steam
No calculator — the numbers are chosen to carry in your head, the way a kind examiner sets them: the tap runs at 20 °C so the climb is a clean 80 degrees, and 4.2 × 80 is just 4 × 80 plus a fifth of 80 — 336.
The formula in this lesson
Electricity — Circuits & Power
- L26Lesson 26Charge and CurrentAmps are coulombs on the move
Electricity is stuff on the move. The stuff is charge, measured in coulombs (C) — one coulomb is about six billion billion electrons, a crowd far too big to count one by one.
The formula in this lesson - L27Lesson 27Ohm's LawThe chapter's anchor formula
Meet the most famous formula in electricity: V = IR — read aloud: V equals I R. V is voltage in volts, the push. I is current in amperes, the flow. R is resistance in ohms (Ω — the Greek letter omega), how much the path squeezes.
The formula in this lesson - L28Lesson 28Rearranging Ohm's Lawone law, three outfits
V = IR is one fact in three outfits.
- L29Lesson 29Series Circuitsend to end · resistances stack
Put two resistors end to end — a single loop, no branches — and you have a series circuit. The same current threads through both, like one line of people passing through two doorways.
- L30Lesson 30Parallel Circuitsside by side · the total drops
Now give the current a choice: two resistors side by side, each on its own branch, make a parallel circuit. More paths make the trip EASIER, so the total resistance drops below the smallest branch — always.
The formula in this lesson - L31Lesson 31Electrical PowerThe I²R detour
Power is how fast a device spends energy, measured in watts (W) — one watt is one joule spent per second. The main road: P = VI — read aloud: P equals V I — the push times the flow.
The formulas in this lesson, - L32Lesson 32The Hydro Billkilowatt-hours, and what they cost
Your hydro bill never mentions joules — the joule is too small a coin for a month of electricity. The bill's unit is the kilowatt-hour (kWh): what a 1000 W device spends in one hour of running.
- ★Boss lessonThe Circuit Boardthe boss · no calculator · one board, every line
No calculator — the values are chosen to fit in your head. One circuit board: a battery, two resistors in series, and a clock on the wall.
The formula in this lesson
Weather, Climate & the Atmosphere
- L34Lesson 34Pressure Is Force over AreaWhy snowshoes work
The unit is the pascal: one newton spread over one square metre. A pascal is tiny — a single sheet of paper lying flat presses on the table with about 1 Pa.
The formula in this lesson - L35Lesson 35Pressure Under WaterP = ρgh · every metre costs 9.8 kPa
Here is the nugget that ties the chapter together: ten metres of water costs about 98 kPa — almost exactly one whole atmosphere.
- L36Lesson 36Thin Air — Pressure with Altitudeestimate first · halvings every 5,500 m
You live at the bottom of an ocean of air. At sea level it presses with about 100 kPa — the weight of everything overhead.
- L37Lesson 37Relative HumidityWarm air is a bigger sponge
Air holds water as invisible vapour, and how much it CAN hold depends on temperature: warm air is a bigger sponge.
The formula in this lesson - L38Lesson 38The Dew Pointcool to the line, fog appears
Take today's air, with today's water in it, and COOL it. The sponge shrinks around the same water, RH climbs, and at some exact temperature it hits 100 %.
- L39Lesson 39Feels-Like Temperatureshumidex or wind chill · pick the day's index
The thermometer reports the air; your skin reports the EXPERIENCE, and two things drive them apart. In summer, moisture: sweat cools you by evaporating, and near-full air won't take the water, so heat piles up.
- L40Lesson 40Sunlight, Albedo and the Lapse RateAir cools as you climb
The scores tell a climate story in one line: fresh snow reflects about 0.9 of its sunlight; grass about 0.25; open water a mere 0.06.
The formulas in this lesson,, - L41Lesson 41Counting the Stormflash to bang · sound does the travelling
Lightning hands you a free measuring tape. The flash reaches your eyes essentially instantly; the thunder plods along at the speed of sound, so the count between them IS the distance, in disguise.
- ★Boss lessonBoss — The Weather Stationthe boss · no calculator · one stormy afternoon
No calculator — every number is chosen to fit in your head, and the whole chapter reports for duty: force over area for the instrument plate, the vapour ratio for the humidity, the forecaster's dew-point rule (1 C° below air temperature…
The formula in this lesson
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