Geikie Inlet

From the water, you’re looking at classic glacial terrain: dark bedrock walls rising sharply from tidewater and a backdrop of named peaks like Fossil Peak and Mount Wood. The inlet sits among a cluster of side coves and inlets—Charpentier, Hugh Miller, Tidal, and more—so the scenery changes bend by bend. You’re also seeing the aftermath of big ice: the modern Geikie Glacier now lies inland from the head of the inlet, leaving a deep, quiet fjord where ice once filled the waterway.

This inlet tells one of Glacier Bay’s clearest glacier-change stories. John Muir wrote about the Geikie Glacier here in the late 1800s; by 1892, H. F. Reid found it split into two—keeping “Geikie” for the northern remnant and naming the southern one “Wood Glacier.” Wood Glacier has since vanished. That timeline makes Geikie Inlet a living exhibit of how fast this landscape has changed.

USGS work in this area documents substantial bedrock complexity, including thick sequences of limestone with fossil-bearing layers. Even if you’re not a geologist, you’ll notice the stark contrasts—layered rock, sharp ridgelines, and sheer walls shaped by ice.

Specific wildlife notes for this inlet are limited, but Glacier Bay’s inlets often host marine mammals and seabirds, with the possibility of bears along the shoreline. Keep distance and follow park guidance if you encounter wildlife.