Thunderstorm

For over an hour, we watched the distant storm on the horizon. It never seemed to come closer from sunset until almost 10 PM, when the winds kicked up and the lightning intensified. We then decided to put all the yard furniture and boats away just in case the storm was severe. As we packed everything away, the storm got closer and the winds picked up dramatically.



I enjoy watching storms approach, but usually they arrive rapidly, and there isn't much time to watch and enjoy the lightning.  This time, the storm seemed to sit in place and move left to right, giving us plenty of time to view the storm.

Miller Woods Ponds

Our hike through Miller Woods continued, as we encountered dozens of ponds and interdunal ponds. The ponds dotted the landscape, in the oak savanna, the woods, as well as the grassy fields. Many varieties of spring flowers were in bloom, adding plenty of color to the mostly green fields.

The trail to the beach was a bit over two miles long, and there was something new to be seen at every turn, and over every hill. I suspect this trail would be perfect for bird watching, judging by the variety of ecosystems and the birds we saw on this day.



Along the trail we noticed quite a few areas where there were dead standing trees.  Most were not near any standing water, so I could only guess at the cause. One possibility was that these trees were killed by insects or disease. Perhaps they were ash trees damaged by the emerald ash borer, or oak trees damaged by oak wilt.  Another possibility is intentional removal of damaged trees or non-native species - some of these trees had ribbons tied around them, suggesting a mark for removal, treatment, or study.

Larger lakes were encountered during the hike as well, not to mention Lake Michigan, which was our destination on this hike.

Oak Savanna Hike

A late spring hike through Miller Woods offered a wide range of landscapes to explore. Located within the Indiana Dunes National Park, Miller Woods includes trails ranging from a quarter mile to over two miles one-way from the trail head to the beach. Hundreds of plant species can be viewed in this area of the park, lots of wildlife, and quite a few ponds and lakes.



The first half mile or so of the beach trail includes some peaceful ponds and lakes, some of which are rather large, and surrounded by oak savanna. Unlike most wooded areas in the Midwestern United States, these woods are as they naturally were before invasive plants were introduced to the area. Commonly, the invasive plants litter the floor of the forests, and create an impenetrable mass of vegetation; often, one can't even see through it.

In a natural state, the oak savanna has large spaces between oak trees with only short plants covering the ground. These areas have the best preserved oak savanna in northern Indiana. I imagine the rolling dunes dotted with small ponds discouraged farming and industry in this area, so the landscape never really changed much.



Recent rainy weather for the past two months has filled up many of the small lakes and ponds in the Miller Woods. However, only a few small areas of the trail were slightly flooded. These ponds pepper the landscape, we encountered one after another as we hiked the rolling land.

Located right next to the Lake Michigan shore, and at the boundary of the city of Gary, Indiana, this portion of the park is a huge surprise to anyone driving through the area.

Disappearing Beach

Water levels on Lake Michigan have risen over the past few years, causing some erosion along the Indiana shoreline. Central Beach has been disappearing for some time, due in part to rising waters, but also because of the piers marking Michigan City's Trail Creek. These piers prevent the waves from carrying sand to the beaches down shore, and instead, deposit it on the windward side of the pier.

I remember reports of the dunes of Michigan and Indiana crumbling into Lake Michigan back in the 1980's, but have witnessed an accelerated erosion over the past five years or so.  The park service prevents people from walking along the dunes, saying they are contributing to the demise of the dunes. Anyone can easily see, the lake is the culprit- in fact, the paths that were once on top of the dunes are somewhere in Lake Michigan now. Many meters of the dunes are gone, including the trees which were completely uprooted and eventually washed away by waves. This wasn't caused by people walking on the dunes, but it is a convenient excuse for the Park Service to keep people off of the dunes. --See, we're doing something to save the dunes. I suppose someone will buy it - I don't.



Not long ago, Central Beach was a great destination for those looking to spend a day on the sand.  Now, even when the water is flat calm, there is barely any sand to walk on. Perhaps now that the Indiana Dunes has National Park status, something can be done about the disappearing beaches of Indiana. But that something needs to be the right thing, not just the appearance of conservation, or simply doing something to say something is being done.

Slowly Unfolding

With the quick and extreme changes in weather over the past few weeks, it's hard to believe plants are even able to emerge.  Temperatures have reached the high 70's and 24 hours later, they drop low enough for two inches of snow to accumulate.

Our hike through the wetlands of the Kemil Beach trail revealed thousands of ferns unfolding, getting ready for the warmer weather.  Two types of ferns could be found here, and these were smaller and few in number.



From what I remember during hikes over the last few years, these ferns will turn into tall, thin plants with three or four fronds at the top. They grow to a height of 18 inches or so, and litter the forest floor.

The larger, more robust ferns were abundant and still in tight, round fiddleheads. Of course, just an hour after this photo was taken, it began to snow again.

Lonely Sunset

A red sky over Lake Michigan a few minutes after sunset mark the end of a windy day at the Indiana Dunes National Park. The wind blowing over the cold waters of the lake made the 55 degree air temperature feel like the mid 30's. In fact, the cold water often reduces the actual temperature near the lake.

The high winds and cooler air seemed to keep a lot of people away from the beaches, even though the day was clear and sunny. Earlier in the day, as we hiked from the beach to the rolling dunes inland, we had to remove our jackets because the temperature was much warmer just a quarter mile away from the water.

As we left the National Park, these benches seemed so lonely; in the summer, this beach is often overrun with people until after 9 pm. On this day, we had it to ourselves.

The Trail to the Cave

After hiking through the narrow passage next to Steamboat Rock, the landscape opens up a bit, and the trail leads to a nearby cave. The cave is quite a bit above the trail, and requires a bit of climbing just to see inside.



Here again, we were surrounded by names and initials carved into the soft sandstone, some dating back to the early 1900's. Looking around, it's interesting to think about who passed through this area, and why. The Mississippi River is only a mile or two away, perhaps some of the visitors making their way down the river ventured through these cliffs.

Steamboat Rock

One of the rock features of Iowa's Wild Cat Den State Park is Steamboat Rock. This large rock was separated from the rock cliff some time ago, and one of the pieces resembles the prow of a ship. The trail splits here, one part takes hikers between the rocks, and the other takes them around the outside of the "steamboat."

Evidence of visitors to this place is everywhere. Names and initials carved into the soft sandstone are everywhere, including some rather difficult to access places. Some date back to the 1800's if you can believe them, but they do appear old and worn, and written in a typeface not too common anymore.



Steamboat Rock isn't too tall, perhaps 30 feet, but it does seem like people like to climb up to the top for the view or the challenge. Here, one person takes in the surroundings after the climb up.



The easy way up was to climb along a diagonal rock process until some fingerholds were found toward the top of the rock. The carved initials are well defined on this particular rockface, these being in a place relatively easy to reach.

Wild Cat Den State Park, while not overwhelmingly large, offers some interesting trails and formations through a variety of terrain. Visitors can hike all of the trails in a single day.

The Hike to the Ridge

Fresh out of the Devil's Punch Bowl- the name of the previous canyon- we hiked along the foot of the sandstone cliffs toward Steamboat Rock. People can't resist climbing up the rockface for a better view of the surrounding area. "Real" rock climbing is not allowed, and is not a good idea on sandstone anyway, but these places seemed quite safe and worn from previous adventure seekers.



One of the best things about photography for me is the chance to get outdoors and enjoy nature. Every so often, you just need to stop and notice your surroundings, taking in the sights, the sounds, and the smells. It would be a shame to simply capture images without enjoying what nature really is.



One of the benefits of hiking and exploring this area in early spring is the lack of leaves on the trees. You can see more of the rock formations when the trees are bare. Of course it's a bit less lush and green, but more of the distant features can be seen, and once found, they may deserve a closer investigation.

Wild Cat Den State Park's Undercut Canyon Wall

Located 12 miles outside of Muscatine, Iowa, and about a mile west of the Mississippi River, lies Wild Cat Den State Park. This park is home to several small sandstone canyons, ravines, and some historic structures including a schoolhouse and a mill.

We began our morning hike on one of the five miles of trails, the one we thought would have the most interesting rock formations. Hiking the Punch Bowl Trail would take us through wooded ravines and canyons to a waterfall called the Devil's Punch Bowl. Before we explored the punch bowl, we headed to another interesting looking canyon with round, undercut walls. The undercut was most likely cut into the 300 million year old sandstone by rushing water.



The shady canyon still showed signs of winter, with a frozen waterfall still intact. The bright sun and warm air was a big contrast to this winter water feature.



Hearing this park could be quite crowded in the warm months, and knowing some of these parks offer better views of the canyons when the trees are bare, we decided to visit in early spring. While the immediate landscape can appear a bit dull at this time of year, the surrounding landscape is visible without the foliage in the way.

This small canyon was just the beginning of our hike, and the rock features only got better and better as the day went on.

Sandhill Cranes

Each spring, thousands of Sandhill Cranes migrate through Indiana, and many make stops in rural LaPorte County. Hearing the calls late at night, I figured the cranes were spending the night on the frozen lake, and sure enough, in the dim light of the morning, I saw hundreds of cranes in two groups.

As the morning went on, the birds began leaving the ice, taking flight in small groups. Several flew directly overhead, so I couldn't resist capturing a few photographs.



Their interactions are interesting to watch. In the photo above, the crane on the left looks over his shoulder to see another crane landing nearby. This was comical to me, as the groups of birds seem to communicate with each other on their way to the empty farm fields nearby to forage for food during the day.

Thousands of Sandhill Cranes pass through the area each year, and the Jasper-Pulaski Fish and Wildlife Area is a prime location to see them. The small lake in LaPorte County is about 45 miles northeast of that wildlife area, so that may be an indication of just how widespread the cranes are during the migration.

The cranes will linger in this area each spring for about three weeks or so, then the fields will be quiet again until next spring.

The Beginning of the Warm Up

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A little over a week before spring, the frozen canyons of Illinois receive a day of sunshine, the beginning of the warm up that would quickly melt the remaining ice and snow. Temperatures began to climb into the 40s while hiking through Tonty Canyon, in Starved Rock State Park. Crackling sounds were echoing off the rock walls, from the ice moving, cracking, and falling as it warmed up.

A few more hours of sunshine, and the creek would soon be a hazardous place to walk, the ice would soften enough for someone to fall through. This would most likely be the last time for walking on the frozen stream that cuts through the narrow canyon.



The stream in Matthiessen Park's upper dells was also frozen on this day. Evidence of times with higher water could be seen along the bank of the stream. Large blocks of ice litter the area, once the top layer of ice on the water when the stream was flooded. Once the water level lowered, the ice lost support, cracked and fell to the canyon floor. These blocks of ice were around five inches thick, and some as long as 10 feet.

Climbing Wildcat Canyon

Each winter, the waterfalls in Starved Rock State Park freeze, creating beautiful ice formations that are fantastic to view, and when conditions are right, a lot of fun to climb. One of the most popular waterfall to climb is found in Wildcat Canyon. The 80 foot waterfall is a challenge many ice climbers can't resist.



This year, there were two frozen waterfalls in Wildcat Canyon, but the second looks a bit fragile, and probably was not strong enough to safely climb.

The waterfalls attract visitors all season, and the visitors are treated to an additional spectacle of people attempting to climb the slippery ice formations. Certainly not for the casual climber, ice climbing must be done using crampons, and ice tools similar to the ice ax used in mountaineering, but specialized for climbing. The difficulty of the vertical climb is increased by the cold air, the cold surface, and the constant running water around the ice. Keeping your arms over your head for long periods of time keeps the blood flow to them lower than normal, and this makes the hands colder and colder the longer you climb.



That said, ice climbing is certainly an appealing sport for those who crave adventure. The short ice climbing season in Illinois doesn't allow for much practice or time on the ice, but it does keep the passion alive and flowing all year long in anticipation of the next hard freeze.

Melting Lake Falls

Winter is finally loosing it's grip on the frozen waterfalls of Illinois. Matthiessen's Lake Falls was running free on this morning, and the last of the ice remained clinging to the canyon walls, along the side of the rushing water.

The canyon here is natural, however the waterfall was created when a dam was built between this narrow passage. The canyon floor is riddled with potholes and textures formed by rushing water of the centuries, so it helps to know where you're walking in winter - where are the shallow spots, where are the deeper pools. Stay to the right for the most part.



This waterfall attracts plenty of visitors, and is a beautiful place to visit in any season, but Fall and Winter are the most picturesque.

On this day, I had the canyon to myself, in fact, I had the entire park to myself for about two hours when a few hikers showed up. Winter seems to keep people away because of the cold, but even when the weather warms up a bit, the packed snow trails of these canyons makes walking difficult and sometimes dangerous. A good pair of ice cleats is a necessity.

I would guess most if not all of the ice around this waterfall is gone by now, and while I enjoy visiting and photographing the canyons in winter, I'm looking forward to warmer weather and some life appearing outdoors once again.

Climbing Tonti

Tonti Canyon is an out of the way canyon within Starved Rock State Park. Out of the way because it's quite a hike from any parking area, and a broken bridge and closed trail makes the hike about a mile longer. Traffic is a bit lighter here, it seems people don't want to walk too far from the comforts of their cars, but they're the ones who are missing out. If you look closely in all the photos here, you'll see ice climbers, and if you look carefully in the photo above, the climber at the base of the distant ice fall gives an idea of just how tall these ice features really are. The photo was taken from behind one of the waterfalls, and under the overhang of the canyon wall. This is the ice fall in this canyon that climbers trust and attempt, while the distant one may be a bit too weak to support climbing. The climbers on the ice fall have almost made it to the top of the fall; once there, they will rappel down to the canyon floor and give the next climber a hand with the safety line. Ice climbing is much more difficult than it seems. The surfaces are very slick, usually wet with flowing water, and the cold temperatures of the air and the ice quickly take a toll on the climber. In addition, the arms of the climber are being used above their head, forcing the warm blood away from the extremities, quickly fatiguing the hands, and making them cold very fast. The ice climbing season in Illinois is quite short, and a good number of climbers take advantage of the brief window by climbing the impressive ice falls of Starved Rock State Park.

Summer vs Winter in LaSalle Canyon

LaSalle Canyon is a treat to visit in all weather, and during all seasons. Last week's frozen waterfall images strongly contrast the photos I captured in the summer. The angles aren't exactly identical, but close enough to show the contrast between the warm months and the cold. The photos below are views from under the stone overhang, behind the LaSalle Canyon waterfall.

Double Waterfalls in The Canyon Beyond Cedar Point

The canyon just across the stream from Matthiessen's Cedar Point has two waterfalls, and you can usually explore behind both of them. But this time of year, so much ice has formed, it's become too thick to allow anyone inside. I generally view this waterfall from ground level, but getting up on an old trail allowed me to see the canyon above, and the path the water takes to create this 12 foot tall waterfall. There are quite a few more waterfalls in the canyon above, but they would be a bit too dangerous to explore in winter. From the center of the canyon, both waterfalls can be viewed at once. While a relatively small state park, Matthiessen has six waterfalls to view in a relatively short hike. Be prepared to get wet feet most of the year if you wish to see them all. From the head of the canyon, the first waterfall can be seen in the distance. This waterfall has a free-fall of about 16 feet, but begins quite a bit higher, with a cascade of around 20 more feet. These waterfalls don't flow too fast, but in winter, the small amount of water builds up over time, creating some interesting frozen waterfalls. Warm weather is approaching, so these falls won't be around for much longer.

The Dual Icefalls of Kaskaskia Canyon

After another week of very cold weather, the temperatures are set to climb above 40 for the next few days, so the icefalls of Illinois' Starved Rock State Park won't be here for much longer. I figured after the single digit temperatures this week, the falls would be frozen solid, and they were. Ever changing, they're never the same twice, even though this was my forth trip to the frozen falls this winter, it's still exciting to enter each canyon to see the ice formations. On my last trip, I wasn't able to get to Kaskaskia Canyon because water from the melting snow filled the canyon floor. This time, the creek was still frozen solid, providing a good surface to walk on. "Good" meaning solid, but pretty much solid ice all the way. The pathways at the park were once packed snow, but that turned to very slick ice. Hiking some trails today without ice cleats was not only impossible, but very dangerous. At this time of the morning, I was the only person in these canyons, so it's difficult to see how tall the waterfalls are because there are not people in the image for scale. The waterfall engulfing the logs is about 12 to 15 feet high. Nowhere near the tallest in the park, but certainly an interesting combination of ice, rock, and logs. The warm weather will certainly take it's toll on the icefalls over the next few days, but first, the creeks will begin to melt and flow, making it difficult to access some of these winter sculptures.

Ice Volcanoes

The ice mounds along the shore of Lake Michigan form as the waves push the drift ice up on shore, or onto the shelf ice. The action of the water and waves creates mounds in a conical shape, where the splashing water comes from the center, and the ice is deposited around the center. This is the same action as a volcano basically, so these mounds are often called "ice volcanoes." These are interesting to view, but very dangerous to get near, or climb upon. The center of the ice volcano is empty, and leads directly to the freezing water below. These are especially interesting to watch when the water is still splashing up through the center. Depending upon the weather, wind, waves, temperature, and even the shape of the beach, the ice forms in sheets or mounds. Here, the lake is mostly drift ice frozen together making something that looks like a solid sheet of ice, with only a few mounds along the shore where the waves once reached. Those mounds on the shore are magnets for visitors taking photos of themselves and their friends. The mound this person is standing on is actually on the shore and quite safe, however, it was very slippery, and slipping off the edge toward the lake would result in a very cold plunge.

The Difficult Path Ahead

While walking along the frozen shore, we came upon a rift in the drift ice on Lake Michigan. The ice looks static, but if you visit the beach in winter, you'll realize it's almost always moving, and here is a place where forces pushed the ice apart. If you look closely, you'll notice the right side of the ice rift fits perfectly into the left side. This is sort of like a fault in geology, where the plates are pulling apart. What I found interesting is the path through the dunes to the beach seemed to lead directly to the rift, making the two appear to connect, and lead right to the horizon. Of course this is not the case, but from the top of the dune, the beach below can't be seen, and the rift looks as if it touches the dune. Over time this break in the drift ice will change. It will most likely get wider for a time, then the open spaces will ice over or fill with other drift ice pushed in by the winds over the lake.