Tides occur mainly in oceans because that is basically one huge body of water that is free to move all over the earth. Lakes and rivers do not cover enough area to have their water be moved significantly by gravity, or in other words, to have tides.
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The smallest body of water in which lunar tides have been measured is Loch Ness in the UK, which is 37 kilometres long. Here, the tides have an amplitude of about 1.5 millimetres. Tides result from the small differences in the moon's gravitational attraction from place to place on Earth.
Geology of Lake InferiorLake Inferior is an underground lake that is located beneath Lake Superior. It is believed to be formed by a process known as karstification, which is the dissolution of limestone and dolomite rock. This process creates sinkholes, caves, and underground rivers and lakes.
Exorheic, or open lakes drain into a river, or other body of water that ultimately drains into the ocean. Endorheic basins fall into the category of endorheic or closed lakes, wherein waters do not drain into the ocean, but are reduced by evaporation, and/or drain into the ground.
The greatest differences between a sea and a lake are their formation, boundaries, and size. Seas are vast naturally occurring bodies of saltwater that are partially enclosed by landmasses that are anywhere from 100,000 square feet and larger.