Sandhill Crane

A magnificent, large gray bird with a long neck, long legs, and a distinctive red forehead. In flight, they keep their necks extended. Their feathers are primarily gray, though can be stained rusty brown by iron-rich mud.

Uniform pale-to-medium slate gray. Lacks banding or spots. No iridescence. Melanin-based coloration typical of adult plumage. Shaft is translucent to white at the base, turning gray-tan upward.

Densely interlocked pennaceous barbs on the upper 80% of the vane for aerodynamic efficiency; loose plumulaceous (downy) barbs near the superior umbilicus at the base.

Smooth and firm texture with a slightly matte finish. The surface feels dry and somewhat stiff, characteristic of water-associated birds that require durable flight surfaces.

Uniform slate-gray color, broad rounded tip, robust rachis, and the presence of a substantial downy section at the base.

Open wetlands, marshes, wet meadows, and grain fields. Prefers areas with standing water for roosting and open land for foraging.

Broadly distributed across North America. Breeds in Canada, Alaska, and the northern US; winters in the southern US, Mexico, and Cuba. Notable migratory stopovers in Nebraska.

Omnivorous foragers that stir up soil and consume insects, seeds, and small vertebrates; they serve as important symbols of wetland conservation.

Great Blue Heron (feathers are usually longer/narrower with more blue-gray), Canada Goose (darker brown-gray with different barb density).

Sandhill Cranes are known for their spectacular dancing displays and their prehistoric-sounding, rolling 'garoo-a-a-a' calls produced by a long, coiled trachea.

Good condition with minor wear on the trailing edge. The calamus is intact, suggesting a natural molt. No significant fault bars or parasitic damage visible.