Discover the Leelanau Shoreline at Sleeping Bear Dunes
For years I visited the Pierce Stocking Overlook perched extreme over the seemingly countless horizon of Lake Michigan, and would typically see kayakers paddling Inside the watermethod down under. Wouldn’t It is nice, I’d say to myself, if I Might be down there wanting up On the people like me? Finally, I acquired that probability.
That is my all-time favourite Leelanau paddling location. The expertise of paddling on such An monumental physique of water with a wall of sand stretching for miles on one facet of your kayak is Almost as good As a Outcome of it ever will get. Do You’d like to’ll Have The power to go when circumstances are accommodating, You will have the paddle of a lifetime. We’ve been fortunate That Every one three of our paddles to “The Bear” have been in Definitely one of the Greater of circumstances.
Location: Simply north of Empire And growing to Glen Haven.
Entry: Cannery Boathouse Museum Parking lot in Glen Haven; Life-Saving Station Museum Parking lot (nearer to Sleeping Bear Level); Lake Michigan Seashore Park in Empire; North Bar Lake beach north of Empire.
Distance/Time: Empire to Glen Haven: 9miles, 3 hours (A method); Empire to Pierce Stocking Overlook: 2 miles, 1 hour (spherical journey); Glen Haven to Pierce Stocking Overlook: 5 miles, 4 hours (spherical journey).
Strategies: Ought to you’re using Simply one car To maneuver your kayaks, it’s important To imagine about wind course and wind speeds. The biggest circumstances Can be mild winds from the east. Ought to you’re placing in at Glen Haven and heading south to Empire, a southerly or easterly wind is preferable.
Highmild: The huge sand dune Throughout the Overlook is An unimaginable factor to see from a kayak. This wall of sand extends for a quantity of miles, from just south of the Overlook, All of the biggest Method to Sleeping Bear Level. These dunes are referred to as perched sand dunes, or dunes that develop on a pre-current hill or cliff. Right here, The prevailing cliff is the rock and residue left from the movement of the final glacier, about 10,000 years in the past. There are additionally many decrease sand dunes as you paddle nearer to Glen Haven.