description Chalky Inlet Overview
Chalky Inlet is a large, remote fjord located in New Zealand's Fiordland region on the southwestern coast of the South Island. It is characterized by its steep sides and deep waters, typical of the glacially carved sounds in the area. The inlet is adjacent to Chalky Island, known for its prominent white limestone cliffs that gave the area its name. Historically, these sheltered waters served as a seasonal base for early 19th-century maritime sealers operating in the Southern Ocean.
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Where is Chalky Inlet?
Chalky Inlet is a large remote fjord in Fiordland on New Zealand’s southwestern South Island. It is adjacent to Chalky Island and is surrounded by steep, glacially carved terrain.
Why is Chalky Island associated with Chalky Inlet?
Chalky Island lies beside the inlet and gives the surrounding coastal area its recognizable geographic reference. The island and fjord form part of Fiordland’s remote southwestern coastline.
How deep is Chalky Inlet?
Chalky Inlet has deep marine waters, but a single depth figure is not necessary to identify its character. Its steep sides and flooded glacial valley are typical of New Zealand’s Fiordland inlets.
How was Chalky Inlet formed?
The inlet was shaped by glacial erosion during the last ice age. When the glacial valley flooded, it became the steep-sided marine fjord seen today in Fiordland.
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