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Lost River - Karst Information Portal

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This five-stage model may have implications<br />

about the geomorphic development of the<br />

adjacent Mitchell Plain, in that its present<br />

low relief might be due to the lack of basin<br />

Geology Field Trip<br />

rejuvenation and extensive erosion of interfluve<br />

areas by fluvial and karst processes during static<br />

base level (valley floor) conditions which have<br />

existed throughout the Pleistocene.<br />

Figure 14. Tower Quarry is located within the Crawford Upland with the quarried limestones<br />

exposed along Dry Run and its tributaries. Wyandotte Cave is located just to the east.<br />

107

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