The Blue Hole: Difference between revisions
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'''The Blue Hole''' represents the initial of two significant springs situated within [[McConnell Springs]]. Its source can be traced back to a broad region in the southwest of [[Lexington, Kentucky|Lexington]], where the waters travel underground through the limestone bedrock. | |||
The distinct blueness of this water is a result of prismatic effects generated by its exceptional depth of 15 feet. This exposed water body was formed when water discharged from a crevice in the bedrock with enough force to remove the topsoil and sediment. As a result, it currently forms a cone-shaped basin that remains filled by the springs underneath.</ref> | |||
==References== | |||
* [https://www.lexingtonky.gov/mcconnell-springs-park McConnell Springs Park: Sites. Lexington-Fayette Urban County Government] | |||
Revision as of 17:02, 3 January 2024
The Blue Hole represents the initial of two significant springs situated within McConnell Springs. Its source can be traced back to a broad region in the southwest of Lexington, where the waters travel underground through the limestone bedrock.
The distinct blueness of this water is a result of prismatic effects generated by its exceptional depth of 15 feet. This exposed water body was formed when water discharged from a crevice in the bedrock with enough force to remove the topsoil and sediment. As a result, it currently forms a cone-shaped basin that remains filled by the springs underneath.</ref>