Uplifted Lowland Coast

An uplifted lowland coast is a type of coastal landform that occurs when a low-lying area of land is raised up above sea level due to tectonic uplift or isostatic rebound. This type of coast is characterized by a wide, flat plain that rises gently from the sea, with a series of low hills and mountains in the background. Examples of uplifted lowland coasts include:

1. South-eastern U.S.A.: The Atlantic coastal plain of the south-eastern United States, stretching from New Jersey to Florida, is an example of an uplifted lowland coast. This region was formed by the gradual uplift of a low-lying coastal plain over millions of years.

2. Western Finland and Eastern Sweden: The Gulf of Bothnia, which separates the two countries, is an example of an uplifted lowland coast. The land in this region has been rising slowly since the last ice age, resulting in a wide coastal plain that is now several meters above sea level.

3. Coastal Argentina: The coast of Argentina south of the Rio de la Plata is also an example of an uplifted lowland coast. The region was uplifted over millions of years and is now characterized by a wide coastal plain that extends for hundreds of kilometers.

Features of Uplifted Lowland Coasts

1. Wide coastal plain: The most distinctive feature of an uplifted lowland coast is the wide coastal plain that extends for many kilometers inland from the shoreline.

2. Low-lying areas: Despite being uplifted, these coasts are still relatively low-lying, often only a few meters above sea level.

3. Gentle topography: The topography of an uplifted lowland coast is generally quite gentle, with low hills and mountains in the background.

4. Estuaries and deltas: Uplifted lowland coasts are often characterized by large estuaries and deltas where rivers meet the sea.

5. Good harbors: The wide, shallow bays created by these coasts make excellent natural harbors for shipping and fishing.