Not exact matches
Most
of the ocean's salts were derived from gradual processes such the breaking up
of the cooled
igneous rocks of the Earth's crust by
weathering and erosion, the wearing down
of mountains, and the dissolving action
of rains and streams which transported their mineral washings to the sea.
Most
of Australia's landscape is covered in a blanket
of weathered rock, sediments and
igneous rocks, effectively «hiding» the surface where mineral deposits lie.
A further reduction by carbonate sediment dissolution, and reactions with
igneous rocks, such as silicate
weathering and sediment burial, will take anything from tens to hundreds
of thousands
of years, or even longer.