CurriculumGrade 6Science

Weathering, Erosion, and Deposition

Aligned to MS-ESS2-2 — Next Generation Science Standards.

What this lesson teaches

Earth's surface is reshaped by three linked processes: weathering breaks rock into pieces, erosion carries those pieces away by water, wind, or ice, and deposition drops them somewhere new. Tiny changes each year add up over huge spans of time to carve canyons and build beaches.

Worked example

A river bend shows all three at once: the fast-moving outer bank is eroded and undercut, the sediment travels downstream, and on the slow inner bank it is deposited to form a sandbar. Over centuries this makes the river snake into wide S-shaped meanders.

Practice questions

  1. Pour water down a tray of sand at different slopes and observe where material is picked up and where it piles up.
  2. Explain the difference between weathering and erosion in your own words with an example of each.
  3. Find a spot near your home showing deposition (like sand or gravel) and describe what likely carried it there.

Watch the lesson

Every lesson comes with a video taught in English and Spanish — the same video the QR code in the printed workbook opens.

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En español

Meteorización, erosión y depósito

La superficie de la Tierra se remodela mediante tres procesos ligados: la meteorización rompe la roca en fragmentos, la erosión los transporta mediante agua, viento o hielo, y el depósito los deja en un lugar nuevo. Cambios diminutos cada año se acumulan durante enormes lapsos de tiempo para tallar cañones y formar playas.

Ejemplo: Una curva de río muestra los tres a la vez: la orilla exterior de agua rápida se erosiona y se socava, el sedimento viaja río abajo, y en la orilla interior lenta se deposita y forma un banco de arena. Durante siglos esto hace que el río serpentee en amplios meandros en forma de S.

More Earth & Space Science lessons

Earth in the Solar SystemMS-ESS1Why the Moon Has PhasesMS-ESS1-1The Solar System to ScaleMS-ESS1-3Reading Earth's History in Rock LayersMS-ESS1-4The Rock CycleMS-ESS2-1Plate Tectonics: Evidence the Continents MovedMS-ESS2-3

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