September 1, 2015
Monument to the Dean of Michigan’s Tourism Activity on Roadside America says:
If someone asked, “Who has had a rock pyramid built in their honor?” you might think of an Egyptian pharaoh or an Aztec king. You would probably not think of a bespectacled, middle-aged, mid-western man named Hugh J. Gray. Nevertheless, Hugh has one — on a smaller scale compared to the ones in Egypt and Mexico, but a rock pyramid nevertheless.
Hugh was, according to the plaque on his pyramid, the “Dean of Michigan’s Tourist Activity.” The pyramid, erected in 1938, stands on Cairn Highway, named apparently in reference to Hugh’s pile of rocks. Cairn Highway is an obscure back road today, which says something about the transient nature of fame.
Hugh’s pyramid is built of rocks from each of Michigan’s 83 counties.
Ragnar suggests that you plug the coordinates 44.948227, -85.352708 into Google Maps to find your way there. View his photo background big and see more in his slideshow.
More roadside attractions on Michigan in Pictures!
August 31, 2015
Confession: I probably don’t give Silver Lake Dunes State Park enough love. What an incredible place.
In Scientific American Robert S. Anderson, associate professor of earth sciences at the University of California at Santa Cruz explains why regular, wavelike shapes form when the wind blows over the sand on the beach for a long time:
Ripples in sand, found on both beaches and dunes, are one of nature’s most ubiquitous and spectacular examples of self-organization. They do not result from some predetermined pattern in the wind that is somehow impressed on the surface, but rather from the dynamics of individual grains in motion across the surface. They arise whenever wind blows strongly enough over a sand surface to entrain grains into the wind. The subsequent hopping and leaping of these grains is called saltation. Saltating grains travel elongated, asymmetric trajectories: Rising relatively steeply off the bed, their path is then stretched downwind as they are accelerated by drag forces. They impact the sand surface centimeters to tens of centimeters downwind, typically at a low angle, around 10 degrees. It is this beam of wind-accelerated grains impacting the sand surface at a low angle that is responsible for ripples.
“An artificially flattened sand surface will not remain flat for long. (Try it on the beach or on the upwind side of a dune and see for yourself.) Small irregular mottles in the sand surface, perhaps a couple centimeters in wavelength, rapidly arise and grow once the wind starts to blow hard enough to initiate saltation. They then slowly organize themselves into more regular waves whose low crests are aligned perpendicular to the wind direction and begin to march slowly downwind. Typical ripple spacing is about 10 centimeters, whereas the typical height of the crests above the troughs is a few millimeters. The pattern is never perfect, but instead the ripple crests occasionally split or terminate, generating a pattern that looks remarkably like one’s fingerprint.
Read on for a whole lot more including Michigan Sea Grant educator Walt Hoagman explaining how the speed of wind (and water) over sand influences the waves.
August 29, 2015
Van’s is the most popular public beach in my hometown of Leland for reasons that are probably made obvious by this photo. When Traverse City Tourism shared the picture, I figured I should too!
The Leelanau Conservancy has this to say about Hall Beach, also known as Van’s Beach:
The beach is Leland’s first public beach on Lake Michigan since the harbor was constructed in 1970. It lies at the base of the south breakwall of the harbor and was originally owned by the Hall family. The beach area was made possible by the Hall Family and the Michigan Natural Resources Trust Fund.
It lies at the base of the breakwall and connects Fishtown to the rest of the public beach to the south which was gifted by the Miller Taylor families. Linked together, these areas create an uninterrupted protected area from Fishtown to where the trail comes down to the water from the parking area at the road end of Cedar street – for both wildlife and public to enjoy. A favorite place for watching Lake Michigan sunsets, Hall Beach also protects historic Fishtown from future commercial development.
Click through for a map and to see more beaches and preserves on the Leelanau Peninsula.
I will add that Van’s beach got its name from Van’s Garage, owned by the Van Raalte family. Also, when the wind is from the north or northwest this is one of the area’s best surf spots. The point you can see in the distance is Whaleback, also preserved by the Leelanau Conservancy.
View the photo bigger on Facebook, see several more in the Traverse City Tourism feature and definitely follow Northern Way of Life on Facebook for lots more from the Leelanau Peninsula & Northern Michigan.
More Michigan beaches on Michigan in Pictures.
August 28, 2015
August 27, 2015
Here’s a fun pair of pics. Tom went back to where this family photo was taken in the early 30s and got a picture of the scene. You can see the one above background big, the one below right here and see more including another shot from the Belle Isle Conservatory in his Wonderful Michigan slideshow.
August 26, 2015
GoWaterfalling’s page on Gorge Falls says:
A very scenic waterfall set in a very scenic gorge. An added plus is the close proximity of the equally impressive Potawatomi Falls. These are two of the most impressive falls on the Black River and are also the two easiest to access.
Gorge falls is named for the deep and narrow gorge above and below the falls. This was my personal favorite of Black River Scenic Byway waterfalls. It is also one of the easier waterfalls to visit, being only a short distance from the parking area. There are a fair number of stairs to the falls overlook. It is only a short walk upstream to see Potawatomi Falls.
Read on for more including directions to this and other nearby waterfalls along the Black River.
Tons more Michigan waterfalls (including some by Eric!) on Michigan in Pictures.