key idea 3a: how do coastal landforms evolve over time as climate changes?

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emergent landscapes are shaped significantly by falling sea levels, often linked to cooling climates. these landscapes provide valuable insight into past and present geomorphic processes.

7 Terms

1

what happened in the quaternary period?

  • experience glaciations/ice ages → substantial cooling of global climate

  • large water volumes were trapped in ice sheets/glaciers → drop in sea level. 20,000 years ago sea level was approx. 120m lower than present levels

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2

what happens when sea levels fall?

  • submerged land areas are exposed → emergent landforms

  • primary geomorphic processes: erosion, weathering, deposition.

  • form raised beaches, marine terraces and abandoned cliffs

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3

how do raised beaches form?

  • former shorelines are elevated above sea levels due to sea level fall + isostatic rebound

  • consist of wave-cut platforms and beach deposits that are located inland + higher elevation

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4

how are marine terraces formed?

  • step-like landforms created by sea-level change + tectonic uplift

  • sea level fall, waves erode bedrock → create flat, bench-like platform. sea level stabilise temporarily, terrace is formed.

  • fall in sea levels/tectonic uplift → series of terraces at different elevations, each representing a former sea level.

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5

how are abandoned cliffs formed?

  • steep slopes/escarpments that mark former position of the coastline

  • actively eroded by wave action when sea levels were higher. sea level fell → wave action shifted eastward → leaves cliffs abandoned inland

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6

present climate change

  • e.g global warming → sea level rise → thermal expansion of seawater + melting of ice caps + glaciers

  • lead to re-submergence of emergent landforms → alters structure via wave action, erosion

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7

future climate and sea level changes

  • continue sea level rise → submerge raised beaches + marine terraces → back to active coastal system

  • abandoned cliffs → renewed erosion is wave action reaches base → slope instability + increased landslides

  • ongoing tectonic acticity, isostatic adjustments + sea level change → modify emergent landscapes

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