Bogs can be miles deep, often only reaching bottom until they hit bedrock.
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Bogs can vary in depth from a few inches to several feet, depending on factors such as vegetation cover, water levels, and underlying substrate. On average, bogs are typically a few feet deep.
they eat the food off the bottom of the bog
Bog iron forms when iron compounds in water react with organic matter and oxygen in a bog environment. Over time, iron precipitates out of the water as solid particles or layers, creating bog iron deposits. These deposits can be harvested and smelted to extract iron for use in various applications.
The Tollund Man's body was well-preserved in the bog due to the unique conditions of the acidic, oxygen-poor environment, which slowed decomposition and preserved soft tissues. The peat bog acted as a natural preservative, protecting the body from bacteria and fungi that would typically break down organic material. The cold temperature of the bog also played a role in the preservation of the Tollund Man.
rocks
Bog Woodland Sphagnum