Sea-level change refers to temporal variations in the height of the global or regional ocean surface relative to a reference datum, driven by combined effects of eustatic, isostatic, and steric ...

The Holocene epoch has witnessed profound transformations in coastal environments driven by a combination of melting ice sheets, thermal expansion of the oceans and ongoing tectonic and isostatic ...

Snowball Earth defines periods of our planet's history when ice spanned the globe, even reaching the equator. The planetary-scale freeze is thought to have been driven by ice sheet expansion ...