0
The Okefenokee Swamp is not technically a swamp. It is a type of sphagnum bog that sits in a layer of peat. It was formed by a basin that was shaped like a saucer in the ocean floor filling with water from the rain. This caused plant and moss growth that eventually died and layered up to create the modern 'swamp.'
What else can I help you with?
Is the Okefenokee Swamp a constructive force?
Swamps like the Okefenokee are valuable resources. They are carbon dumps and provide cover and habitation for many different kinds of wildlife.
How was the okefenokee basin formed?
The Okefenokee Basin may have been formed when a bay of the Atlantic Ocean was cut off from the ocean by a barrier island.
How the Okefenokee Basin may have been formed?
The Okefenokee Basin may have been formed when a bay of the Atlantic Ocean was cut off from the ocean by a barrier island.
How was Okefenokee swamp?
It was formed when the Atlantic Ocean flooded.
Why is the Okefenokee swamp is destructive?
It was formed by rain so it is a destructive.
What landforms in Georgia are formed by destructive forces?
Okefenokee swamp
Where do swamps came from?
formed from the decaying organic matter in swamps
How was Okefenokee swamp form?
It was formed when the Atlantic Ocean flooded.
What are the 3 largest swamps in the world?
There are several large swamps all over the world. The three largest are the Sudd Swamp in Sudan, the Okefenokee Swamp in the United States, and the Sundarbans Swamp Delta in Bangladesh.
Why is the okefenokee swamp a destructive forces?
It was formed by rain so it is a destructive.
Where are many swamps located in the US?
Many swamps in the US are located in the southeastern region, particularly in states like Florida, Louisiana, and Georgia. The Everglades in Florida is one of the most well-known swamps in the country. Other notable swamps include the Okefenokee Swamp in Georgia and the Atchafalaya Basin in Louisiana.
Is okefenokee a constructive or a destructive force?
It were formed by destructive force it was made by weathering
