What type of formations can visitors primarily see in Niagara Cave?

Get prepared for the Niagara Cave Tour Guide Test. Utilize flashcards and multiple-choice questions to ensure a comprehensive understanding of key concepts. Arm yourself with explanations and hints for each question and face your exam with confidence!

Visitors to Niagara Cave primarily see stalactites and stalagmites, which are mineral formations created by the deposition of minerals from dripping water over time. Stalactites hang from the ceiling of the cave, formed as mineral-rich water drips and leaves behind tiny deposits. Stalagmites grow from the ground up as the dripping water lands and deposits minerals there. This characteristic feature of caves provides stunning visual displays and serves as an indicator of the cave's mineral content and the environmental conditions over thousands of years.

Other formations like glacial formations are related to past ice movements and are not the primary types seen inside the cave. Cave paintings do occur in some locations and provide historical insight into human activity, but they are not a feature of Niagara Cave itself. Volcanic formations, while fascinating, are not relevant to the geology of Niagara Cave, as it is not formed from volcanic activity. Thus, the presence of stalactites and stalagmites is what primarily defines the cave’s interior and makes it visually striking for visitors.

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