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<title>KidzTalk - Recent questions tagged reverse</title>
<link>https://www.kidzsearch.com/questions/tag/reverse</link>
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<title>dont look at this. not using reverse psychology</title>
<link>https://www.kidzsearch.com/questions/799940/dont-look-at-this-not-using-reverse-psychology</link>
<description>Dont read this. i answered these questions for school on my phone accidentally and my school computer is stupid and this is the only way i can transfer it.&lt;br /&gt;
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1. **&amp;quot;Drift&amp;quot;** means the continents slowly move or shift over time.&lt;br /&gt;
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2. **Alexander du Toit** proposed two supercontinents: Laurasia (north) and Gondwana (south).&lt;br /&gt;
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3. **Ortelius** suggested continents once fit together like puzzle pieces—supporting continental drift.&lt;br /&gt;
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4. **Rocks and fossils** show continents were once connected in similar environments.&lt;br /&gt;
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5. **Coal deposits** in cold regions suggest those lands were once near the equator.&lt;br /&gt;
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6. **Glacial evidence** shows glaciers once spread across now-warm continents, meaning they moved.&lt;br /&gt;
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7. **Continental drift** describes movement; **plate tectonics** explains how and why it happens.&lt;br /&gt;
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8. The **theory of plate tectonics** says Earth’s lithosphere is broken into plates that move on the mantle.&lt;br /&gt;
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9. The **lithosphere** is Earth’s rigid outer shell (crust + upper mantle).&lt;br /&gt;
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10. The **asthenosphere** is the soft, flowing layer beneath the lithosphere.&lt;br /&gt;
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11. **Heat and convection currents** in the mantle cause material to move.&lt;br /&gt;
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12. A **hypothesis becomes a theory** when supported by repeated evidence and observation.&lt;br /&gt;
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13. **Plate tectonics** explains earthquakes, volcanoes, mountains, and sea-floor spreading.&lt;br /&gt;
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14. **Evidence:** fossils, rock types, magnetic patterns, and satellite data.&lt;br /&gt;
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15. At **mid-ocean ridges**, new crust forms as magma rises—called **sea-floor spreading**.&lt;br /&gt;
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16. **Older crust** moves away from the ridge as **new crust** forms.&lt;br /&gt;
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17. **Far edges** of the sea floor are forced under continents—**subduction**.&lt;br /&gt;
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18. **Subduction:** one plate sinks beneath another into the mantle.&lt;br /&gt;
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19. Earth’s **magnetic field** has reversed direction many times.&lt;br /&gt;
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20. **Magnetic reversals** leave mirrored patterns in sea-floor rocks.&lt;br /&gt;
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21. **Sea-floor dating** shows newer rock near ridges, older farther away—proving spreading.&lt;br /&gt;
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22. **Earthquakes and volcanoes** occur where plates move—evidence of active spreading.&lt;br /&gt;
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23. The **map** showed matching patterns across oceans, proving continents move.&lt;br /&gt;
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24. Developed from **Wegener’s drift idea** → **sea-floor spreading** → full **plate tectonics theory**.&lt;br /&gt;
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25. **Causes:** mantle convection, ridge push, and slab pull.&lt;br /&gt;
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26. **Convection current:** flow of heated, less dense material rising and cooler material sinking.&lt;br /&gt;
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27. **Lower velocity waves** show hotter, softer regions in the mantle.&lt;br /&gt;
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28. **Higher velocity waves** show cooler, denser rock.&lt;br /&gt;
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29. **Mantle plumes** form from hot material rising from deep within the mantle.&lt;br /&gt;
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30. **Ridge push:** gravity slides new crust away from mid-ocean ridges.&lt;br /&gt;
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31. Helps **predict earthquakes, locate resources**, and understand natural hazards.&lt;br /&gt;
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32. Guides **safe construction**, avoiding fault lines or volcanic zones.&lt;br /&gt;
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33. **Wegener’s evidence:** fit of continents, fossils, rock layers, and climate clues.&lt;br /&gt;
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34. **Continental drift** describes movement; **plate tectonics** explains the mechanism.&lt;br /&gt;
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35. **Oldest sea-floor** is near the **edges** of the Atlantic, farthest from the ridge.&lt;br /&gt;
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36. The **mid-ocean ridge** is where the youngest rocks are and magnetic stripes mirror outward.</description>
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<pubDate>Sun, 19 Oct 2025 18:00:28 +0000</pubDate>
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