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Posts Tagged ‘Winter Ice Formations’

Last Saturday I woke up to not only the snow that fell on Friday but a temperature of 9 degrees F. That told me we wouldn’t be seeing any melting going on. By 11 am it was 22 degrees, but with the wind the feel-like temperature was more like 18 degrees, so I opted for a place where I knew I could be out of the wind. Beaver Brook and the abandoned road that follows it lie at the bottom of a natural canyon sheltered by hills on 3 sides, so there usually isn’t much wind there.

It was still cold though.

I have a friend in California who grew up here and is very fond of this place, so I like to come here at least once in each of the four seasons so he can see what it’s looking like. The place itself doesn’t change much but the weather sure does. I’ve seen waist deep snow on the old road.

There is a small cave here that I’ve always thought looked like a perfect spot for an animal den and sure enough I could see tracks in the snow that looked like they might have been bobcat tracks, but since we’d had a little more snow overnight it was hard to tell. The cave goes much further back into the hillside than what it looks like here.

Stair-step moss (Hylocomium splendens) is a pretty moss that I only find in this place. It’s very delicate looking but it can take a lot of winter ice and snow and grows as far north as the arctic tundra. It is also called glittering wood moss because it sparkles when the light is right. It grows on the stone that caps the cave and seems to like places where it can hang over an edge.

The seep hadn’t frozen, but it rarely does. When you see this frozen over you know it is extremely cold. Hydrologically speaking a seep is a wet place where water reaches the surface from an underground aquifer, and this one stays just like this winter and summer. I saw it freeze one winter but I’ve never seen it dry up. It’s a good place for birds and animals to come and drink.

Near the seep is a boulder fall, and on some of the stones in the boulder fall dog lichens grow. I hoped to see them on this day but they were covered by snow. The sky was a beautiful blue though, and that more than made up for their lack.

Also near the seep is a tree that I’ve been watching. It died at some point and has been sloughing off its bark for at least two years now. When you find a tree in the woods that is completely without bark, this is why. Sometimes you can even find a bunched-up pile of shed bark at a tree’s base. It is normal for live, healthy trees to lose some bark, but not like this.

A goldenrod held out its seeds for birds that didn’t seem interested. There seems to be a lot of that going on here. Many fruits and seeds are not being eaten like they were a few years ago.

I love to see the sunlight falling on golden birches. It shows how they come by their name. They are also called yellow birch (Betula alleghaniensis) but to me they’re golden. Swamp birch is another name for this tree that is the largest and most valuable birch. They can live to 100 years regularly but at least one was found that was over 200 years old.

I was lucky to find a fallen golden birch branch that had the female seed heads (strobili) attached. They are quite big on this birch; about the size of bush clover seed heads, or the tip of your thumb.

And here was a single fallen golden birch seed, which is about twice the size of the gray birch seed I showed in a recent post. I’ve read that redpolls, pine siskins, chickadees, and other songbirds eat these seeds. Ruffed grouse eat the seeds, catkins, and buds, and red squirrels like the seeds and sap.

Golden and paper birches both have bark that peels like this. As any camper knows, it’s great for starting a campfire. That’s because it contains betulin, which is highly flammable. It is also water repelling, and that’s probably why Native Americans used birch bark for their canoes.

There was lots of ice on the ledges. These ledges don’t see a lot of sunshine; I’d guess maybe two or three hours per day, so the ice grows slowly. It is clear and hard.

The sunshine that falls here in winter comes over the hillside to the right, out of this view. In winter it takes its time reaching the other hillside on the left, so much of the road is shaded. It can be a cold walk. The overhead electric wires just follow this handy corridor. There are no houses here.

I met and old timer up here once who told me that rock climbers used to practice on that erratic over on the other side of the brook. It is big; maybe twice the size of the 40-ton Tippin Rock in Swanzey.

I loved the way the reflected light fell on the water in this spot. So much beauty, everywhere you look.

In the place where the brook becomes wide and calm it had iced over. I’ve seen Beaver Brook with ice three or four feet thick on it, so thick that the brook lost its singing voice.  I’m hoping I don’t see that this year.

The icicles hanging from the stones in the brook have large “feet” and I think that is because they grew in length as far as the water surface and then, once they couldn’t grow any longer, they grew wider instead. I’ve watched the ice in the Westmoreland deep cut and when it reaches the surface of the drainage channels it widens, just like this. If that is what is happening here then the water level has dropped about a foot since the icicles grew.

Ice hung from every stone. Anywhere water splashes is a good place to look for ice formations.

The seed pods of Indian pipe plants (Monotropa uniflora) look like small, carved wooden melons. This one had split to release the tiny, winged seeds. They split into five parts and each segment will eventually fall off, leaving the hard, dried central style behind. I had to take my gloves off to get this shot so it is a bit rushed. I wanted to show more of the top so we could see the funnel shaped hole in the stigma, but it was cold. The wiry looking bits are what is left of its ten dried stamens which, when the plant is flowering are inside the petals. You can see one of the dried petals behind the seed pod there in the lower right. It really is fascinating how much of the flower’s structure is still there in the dead plants. I always like to stop and take a closer look when I see them.

I stopped to look at the chubby purple buds of red elderberry (Sambucus racemosa). Buds with many bud scales that overlap like shingles are called imbricate buds. A gummy resin often fills the spaces between the scales and makes the bud waterproof. If ice should form inside the bud scales it could kill the bud. I’ve seen these buds in the past with purple and green stipes and they were beautiful. The colors reminded me of drawings of court jesters that I’ve seen. I can’t say why some buds are striped and others are not but I have a feeling that temperature might have something to do with it. Many plants like American wintergreen, turn purple in winter and I’ve noticed that the color is darker when it is cold.

As is often the case these days I didn’t dare to climb down the embankment to get a good view of the falls, but this shot from 2015 is a good representation of what I saw by peeking through the brush on this day. There was a good roar but I’ve seen even the falls covered by ice in the past, quieted by the cold.

As I was leaving, I noticed that the sun was higher in the sky and its light had reached the brook. There wasn’t much warmth but there was light. This shot also shows how treacherous climbing down to the water would be, and this spot would be much easier than at the falls. You’ve got to be careful up here because you’d wait quite a little while for any help to come and in this cold that wouldn’t be good.

The sunshine had also reached the icicles on the ledges but I’d be surprised if it had enough time to do any real melting. It won’t be long though. There is a little more daylight each day and it will be March before we know it.

In the winter, the world gets sharp. Beautiful things happen. ~Peter Fiore

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We’ve had more ice than snow here so far this winter and if there is one thing that will strike fear into the most winter hardened New Englander, it is an ice storm. Trees, weighed down by ice, fall and take wires down with them, and there have been times here when the power has been out for weeks. No power when it’s cold means you move, unless you happen to have a non electric heat source or a generator. In any event I wanted to take a walk after a recent ice storm because though terrible, on a sunny day ice can also be beautiful.

The trouble was, there wasn’t much sunshine to make the ice sparkle like prisms, and instead of clear and beautiful some of the ice was kind of slushy, as the ice on this beaver cut tree shows.

This clear, hard ice covered every exposed twig and branch but luckily, I saw only a few that had fallen. There was no sunlight to make it sparkle.

Even the beech leaves had a coating of ice, and that made them even more beautiful. Simple, everyday natural beauty is available to everyone at any time but we can’t just look. We need to see.

That’s ice, not a water droplet. Sometimes it seemed like every living thing must be coated in ice on this day.

This puddle ice was unusual. I’m not sure I’ve ever seen a puddle do that.

The sun and clouds just couldn’t decide who would win out and I found that trying to time my shutter clicks to when the sun did shine was fighting a losing battle so I just enjoyed the day, sun or clouds.

Pretty little goldthread (Coptis groenlandicum) leaves grew in a crook made by pine roots. You wouldn’t think such a tender looking plant would be evergreen but they are. In spring the leaves are a bright, glossy lime green but darken as they age and by winter will often be very dark green. They’ll hold their color under the snow all winter and look similar to wild strawberries until late April or early May when new leaves and small white flowers will appear. Goldthread gets its common name from its thread like, bright yellow roots.

I saw a single small jelly crep growing on a log. Jelly creps (Crepidotus mollis) are small, quarter sized “winter mushrooms” that like to grow on hardwood logs. They are also called soft slipper mushrooms and feel kind of spongy and flabby, much like your ear lobe. When they grow in groups, they grow with an overlapping shelving habit like shingles.

Here are the jelly crep’s gills. This mushroom was only about half an inch across so this was a tough shot to get.

A small bracken fern (Pteridium aquilinum) somehow remained ice free. Determination, I thought.

There was sunlight at the end of this tree tunnel.

If you follow the trail long enough you find the closeness of the forest opens up into quite a large expanse of wetland, which is home to fish, frogs, beavers, herons and other critters. I’ve seen some beautiful sunsets right here in this spot as well. I’m glad there are laws that prevent the filling in of wetlands now. When I was a boy, I saw load after load of concrete rubble and just about anything else you can think of dumped into wetlands to fill them so they could be built on.

The stream in the previous photo goes under a road and though it looked like spring on that side of the road I found winter on this side. It seemed odd to have such a change happen over such a short distance.

This is the only gray birch I’ve ever seen with inner bark that color. It is beautiful and so bright, the first time I saw it I thought it was a plastic marker. I was glad that it wasn’t.

There was quite a large clear spot under some pine trees and I knew what that meant.

The pine’s branches had taken on the weight of the ice. This is why limbs break off and take down power lines. Ice can be very destructive.

I looked at the gray birches (Betula alba var. populifolia) in a small grove to see if all the seeds had been eaten yet.

There were quite a few left but they were being eaten. Ripe female catkin-like strobiles like the one seen here resemble small cones. Fruit (seeds) are blown about by the wind in late fall and winter. Unless that is, birds get to them. Many songbirds love them. You can often find the snow under a gray birch littered with hundreds of tiny winged seeds. Seeds can persist for years in the soil and will grow if the soil is disturbed.

I wanted to show you a gray birch seed so I brought home a strobile and put a single seed on a white background. They are very small and I couldn’t think of anything to compare them to, so I put a period on the paper with a blue pen. Each tree must produce hundreds of thousands of these seeds, which are technically called nutlets.

This is a gray birch catkin. A true catkin is really just a long string of small flowers spiraling around a central stem, and these will open in May.

I saw what looked like a stream through the woods but it was actually a giant puddle. Quite a beautiful reflecting pool, I thought.

Their deep warm color, the shine of their icy coating, and the the way that the soft light falling on them seemed to caress them made these oak leaves a thing of great beauty. As I’ve said before; if you can find joy in the simple things in life, joy will follow you wherever you go. These beautiful leaves certainly put a smile on my face on such an icy day.

By walking in a snowy forest you can really forget about this world, and every time you forget about this world you leave this world, and every time you leave this world you gain a very special wisdom that does not exist in this world. ~Mehmet Murat ildan

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It seems that these “looking back” posts get harder every year. Choosing a handful of photos is never easy but this year it seemed daunting at first. But then I sat down and remembered what this blog was all about, which is showing you the beauty of nature. I dangle a carrot and entice you into going out and seeing nature for yourself, and when you do you fall in love with what you see, just as I did. That’s the plan, anyway. So as you look at what I’ve chosen remember that these photos are about the beauty of this world and nothing else. Of course, beauty is in the eye of the beholder and you might not think the stream ice in the above shot is beautiful at all. Hopefully though, as you wade through this post, you’ll find something that catches your eye. And remember, if I saw it, you can too.

This is more stream ice, this time with leaves trapped in it. This reminded me of putting a leaf between 2 sheets of waxed paper and then ironing the paper so it sealed around the leaf. It’s always slightly fuzzy, never clear like glass.

The first two photos were taken last January. In February I was at the North Pole, or so it seemed when I was looking at this wind sculpted snow. I love to see the designs the wind can make in snow, but it has to be the right kind of snow with the right consistency or it doesn’t seem to work.

This shot, taken later in February, makes me want to say “whew,” because it shows the first sign of warm colors and melting ice after a long white winter. I’ve always believed that once we’ve made it through February winter’s back is broken. Sure, we can get more snow and even cold, but it doesn’t usually last for weeks like it can in January and February.

In early March there was still snow on the ground but the willows burned brightly and this scene reminded me of an impressionist painting. Vincent van Gogh, maybe?

March is when the first flowers appear but I doubt many people notice the beautiful male alder catkins dangling from the bushes like strings of jewels. A catkin is really just a string of flowers and there are probably hundreds of tiny male blossoms in this shot.

April is when things really get going and large willow shrubs full of bright yellow flowers appear at wood edges and out in the fields. They’re a breath of spring that I look forward to each year and their blossoming usually signals the return of red winged blackbirds.

Bloodroot is one of our most beautiful wildflowers which don’t often appear until early May, but last spring they came along in April. I’m not sure how a flower could be more perfect than this. Its simplicity is what makes it so beautiful, I think. It isn’t busy and there’s nothing to deduce or discover; it’s all right there so all you need to do is just admire its beauty. If you happen to find bloodroot growing in the wild you should remember the spot because this plant will come up in the same spot for many years if undisturbed.

May is when I start looking at buds and though there were many to choose from, I chose this velvety soft, pink and orange, striped maple bud. They seem to glow, and seeing a tree full of them is a sight not soon forgotten. This is a smallish tree and common in this region, so the next time you’re walking along a trail in early May, look out for it.

By mid to late May some of our most beautiful wildflowers are just coming into bloom, like the wild columbine seen here. The columbines grow on stone ledges off in the woods where few people ever see them, but some like me consider them very special and make it a point to go to see them each year. They’re quite a rare find; this spot in Westmoreland is the only place I’ve ever found them. It’s a bit of a hike but it isn’t any work at all to go and see them on a beautiful spring day in May when the leaves are just coming out on the trees and the air is full of sunshine and birdsong. In five short months it will be time to take that walk again, and I’m already looking forward to it.

In this area nothing says June like our native blue flag irises. I watch the roadside ditches because that’s where I find a lot of them blooming beautifully in large clumps. I also see them on pond and river edges. They like a lot of water and can sometimes even be found in standing water. They’re a beautiful flower that always says summer to me and you don’t have to hunt for them, because they’re everywhere.

Flowers come fast and furious in June and you can find many newly opened species each day. For this post though, I chose Robin’s plantain, a fleabane that’s considered a lowly weed. It comes up in lawns everywhere but even though it’s a weed, nobody mows it until it’s done blooming. I think this photo shows why. It’s such a beautiful weed.

There are times in the woods when I see something I can hardly believe I’m seeing, and that’s how it was the first time I saw this fringed bog orchid. I know I’ve found something special when all thoughts leave my mind and I just want to be quiet. I know I’m in the presence of something rare and very special, and I imagine that I feel as I would if I were walking into one of the world’s great cathedrals. It’s hard to explain, but you just know that this is a special moment and it deserves all of your attention, and your gratitude as well. You are humbled, I suppose is the best way to explain it, and it happens the same way each July when I go into the swamp where this magnificent orchid grows.

Also in July, this past July at least, because of all the rain, fungi and slime molds began to appear. I learned a lot by paying attention and watching closely this past summer. I saw a huge variety of fungi and slime molds appear that I had never seen before and as far as I can tell it was all on account of the steady rains we had. After two years of drought it was an amazing show of what nature can do under the right conditions.

In August I found the tiny flowers of the field forget-me-not growing in a lawn and that seemed appropriate, because August was the month that I lost a sister to lung cancer. Though nature has shown me that there is a deep well of peace within us all we have to find it before we can drink from it, and it isn’t something that one of us can give to another; each of us has to find it for ourselves. This was the unfortunate truth that I realized there alongside the forget-me-nots in August.

The concentric circles in tiger’s eye fungi also seemed appropriate for August. To me life is like a song, with a beginning, a middle, and an end. When one song ends a new one begins to take its place, and on and on it goes in a never-ending circle, through all of eternity.

In September I saw one of the prettiest displays of mushrooms I’ve seen when I found these Jack O’ lanterns growing on and around this old red maple. There were hundreds of them and they grew in a ring on all sides of the old tree. A day or two later and I would have missed this beautiful display, and that’s a good reason to get into the woods each day if you can.

This shot is a bit ironic with a monarch butterfly on a purple loosestrife because we wish we’d see more of the butterflies and less of the very invasive purple loosestrife. I didn’t count but I saw a fair number of monarchs, mostly in August and September of last year. I wish I knew why there were so many more, and I wonder if the weather had anything to do with it. I wouldn’t think a butterfly would want to be rained on but there were so many flowers blooming because of it.

This shot from October shows what I mean about having so many flowers blooming. This is just a roadside meadow of sorts that I pass each day on my way to and from work. It’s there every year but this past summer was the best I’ve seen it look. Because of this spot I discovered that New England asters like an awful lot of water. Seeing them in such a wet spot made me take note of soil conditions in other places they grew and each one was quite wet, or at least more than just moist.

You certainly receive plenty of hints in September and even in August of summer’s passing but October is when it really hits you. At least, that’s when it hit me one October morning when I stood on the shore of Half Moon Pond and saw how all the trees had colored. It was a beautiful way to end our summer and it went on and on, and again I think that was because of all the rain we had.

Very late October and early November is the time to visit Willard Pond in Hancock if you want to experience all the majesty of a New England hardwood forest in the fall. The oaks and beeches put on what is easily the most beautiful autumn spectacle that I’ve seen. It’s a quiet, peaceful place with well placed benches where you can sit and listen to the calls of loons and enjoy the beauty of the pond and surrounding forest.

I took a hike down a rail trail in November and just before I left, I snapped this shot of a distant hillside. I could see color on the hillside from where I was but it was like a smudge, with no real detail. I was surprised when I looked at the photo and saw that it was a hillside full of oaks. Everyone seemed to like this one so I’ll show it again.

We had our fist snowfall in December, barely an inch here, so I went out and got some photos of it. It was a nuisance storm and we’ve had two or three since, but no real snowstorms. People who have to shovel it are counting their blessings, but people who make money plowing it don’t feel quite so lucky. I think we all need to face the fact that winter has changed. Just over the course of this blog’s 11 years I’ve watched it go from cold and snowy to rather mild on average in comparison. Spring starts earlier and fall lasts longer now.  

It did get cold enough in December for me to get a shot of this frost crystal on my car windshield one morning. Everyone seemed to like seeing it, so here it is again.

And that’s 2021 in New Hampshire in a nutshell. I hope yours was even more beautiful, and I hope everyone has a safe, healthy and happy 2022!

The only time you should ever look back is to see how far you’ve come. ~Mick Kremling

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Finding ice baubles along the shore of the Ashuelot River last week made me wonder if the ice was growing at the deep railroad cut called the “icebox” up in Westmoreland, so last Saturday I decided to go and have a look. There was ice on the man-made canyon walls but it was too early for the ice climbers who named the place to be here.

Broken ice at the base of the ice falls told me that the icicles had formed and melted a few times. It takes a good cold period to get them going but once they start growing in earnest, they can reach the size of tree trunks in just a few weeks.

The groundwater that seeps through the fractures in the stone never stops. Winter or summer, it still flows. The reason the ice grows so well is because, the walls are shaded in this part of the canyon. The canyon rim is 50 feet high in some places, so sunshine might kiss the canyon floor for an hour each day. That’s also why you find no plants growing here.

In this photo from a few years ago you can see the scale of the place and you can also see that the ice climbers don’t wait long to start climbing. These are very focused, intent people and I don’t like to bother them when they’re up there.

In places water pours from the walls in streams but in most places it just seeps slowly, drip by drip.

Never was moss so green as it was on this day.

As you can imagine it is cold here, usually made colder by the breeze that blows through, so the 28 degrees F. I started with was probably more like 18 or 20 when I finally turned south to find some sunshine.

The railroad engineers had a lot of stone to get rid of once the canyon had been blasted through the hillside and one of the ways they got rid of it was to build massive retaining walls along sections of railbed. For the most part they’re still in perfect shape after 150 years.

The southern canyon’s walls aren’t quite so high so more sunshine pours in, and that means more plants grow here on the southern end. At this time of year it seems kind of empty but in summer the growth here is lush, with every vertical and horizontal surface covered by growing things, and it always reminds me of the Shangri-La that James Hilton described in Lost Horizon.

Last summer I discovered ostrich ferns (Matteuccia struthiopteris) growing here and here was the evidence; their feather like fertile fronds, covered with spore capsules. There will most likely be more of them here in the future. They’re a beautiful fern so I hope so.

There are lots of blackberries growing here as well and most still had leaves to show off.

But just because the sun shines brighter here in the southern canyon, that doesn’t mean that ice doesn’t grow here. The cold wins out over the weak winter sunshine and these walls are often trapped under ice that is feet thick until spring.

To give you a sense of what I’m talking about, here is the southern canyon in March of 2015. The ice columns, stained various colors by minerals in the groundwater, were thicker than tree trunks. It’s a good idea to wear warm clothes if you come here in winter.

Until and unless the drainage channels freeze over the ice, no matter how big it might get, is cutoff by the flowing water.

You can see how easily the groundwater can flow through the cracks and fissures in the stone. That’s what makes this place so special. I’ve been in other deep cuts but none have had ice like I find here. Everything has come together perfectly to create a land of water, stone and ice.

Here was new mineral staining that I hadn’t seen before. If an ice column grows in this spot, it will most likely be orange.

An evergreen fern grows in a grotto, set back from the face of the wall and each year icicles, like prison bars, surround it until spring.

But I’m getting a bit ahead of nature, because in other places the ice was rotten. Ice becomes rotten when water, air bubbles, and/or dirt get in between the grains of ice and cause it to honeycomb and lose its strength. Instead of a sharp ringing crack when it is struck it produces more of a dull thud. The grayish white color and matte finish are a sure sign that you should stay away from it when it’s hanging over your head. Compare the ice in this shot with that in the previous shot and the difference will be obvious.

There was puddle ice to see. Do you see the fish?

In one spot on the wall of the southern canyon a green alga called Trentepohlia aurea grows. Though it is considered green algae the same pigment that colors carrots orange makes green algae orange. It’s is very hairy, but with the drainage channels filled with water I couldn’t get close enough to show you.

Reptilian great scented liverworts (Conocephalum conicum) also grow on the southern canyon walls. This beautiful liverwort gets its common name from its fresh, clean scent. It will only grow near water that is very clean and it grows here just above the drainage ditches. Groundwater constantly splashes them and keeps them wet in warm months. In winter they are often encased in ice, and they will stay that way until spring. It doesn’t seem to hurt them any because there are thousands of them growing here.

The saddest thing I saw on this day was how the trail had flooded over half the length of the southern end. Nobody has maintained the drainage channels enough to keep them fully open and with all the rain we had over last summer they failed and flooded the trail. Snowmobile clubs try to keep up but there is only so much they can do with hand tools. To fix this properly now you’d have to bring in truck loads of gravel and heavy equipment to restore the drainage channels to the condition they once were in. It won’t be easy or cheap but I hope someone will do it because it would be a shame to lose this one-of-a-kind place. There is simply nothing else like it in this area.

All of the water in the drainage channels becomes a stream that runs off into the woods under that old bridge, and I was shocked to see how much soil had washed away from its banks. What was once a little surface stream is now about two feet below the surface.

I don’t know what this old bridge was used for but there was a lot of stone to be moved out of the canyons and I’m guessing that it was wheeled across this bridge and dumped in the woods. The railroad did that a lot and you can find piles of blasted stone all over this area. If I could find a way out there I’d go and see, but nobody is crossing this bridge unless they’re a tightrope walker.

And then there was the old lineman’s shack which, with its ridge beam broken, can no longer support its own weight. It now tilts at about 30 degrees, and if we have any mentionable amount of snow this winter I think it will surely come down.

It looks to me like the heavy slate roof is actually pulling what’s left of the building apart. It’s a shame that something so well built has to give itself up in this way but with absolutely no maintenance over a century or more, it has put up a good fight.

Though the old shack is beyond repair I hope the townspeople will somehow vote to find the funds to repair the damage to the trail itself one day. Other parts of the rail trails that surround Keene have had extensive work done to them, but they’re closer to town so more people use them. Meanwhile I’ll continue enjoying the place for as long as I’m able. I hope you enjoy seeing it as well. It’s a rare and special place that should be appreciated more than it is.

It’s amazing how quickly nature consumes human places after we turn our backs on them. Life is a hungry thing. ~Scott Westerfeld

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The weather people were saying that it was going to warm up so I thought I’d better to get into the man-made canyon on the rail trail up in Westmoreland before the ice started melting. Once the stone starts warming up the ice releases its grip and starts to fall, and I sure don’t want to be here when that starts happening.

Ice here grows as big as tree trunks and when it lets go it often falls all the way across the trail. I’ve never seen the big ones fall but I’ve come here right after they have, and I’ve seen enough to know that I’d rather not be here when it happens.

This isn’t a great year for colored ice but I did see some here and there. This formation was huge.

A few ice climbers were here but most of them had gone by the time I got here. They like to be here quite early in the morning I think, but since it was only 17 ˚ F. when I got up I thought I’d wait a while.

That icicle was longer than I am tall.

Evergreen ferns are still hanging on, even under the ice.

I saw a few snowmobilers. A lot of people complain about them but the arguments for them using the rail trails far outweighs the arguments against them in my opinion because they put a lot of time, money and effort into maintaining the trails. In fact without them many of our trails would no longer exist and thanks to them walking this trail in winter is like walking down a sidewalk. The ice climbers have posted rules to follow and one of them says that snowmobiles always have the right of way. I simply stand to the side and return their waves.

The southern canyon usually has the most colored ice. Blue is the most dense ice and I thought I saw blue in this group. It doesn’t look like the camera saw blue but it still saw plenty of beauty.

My color finding software tells me that the color of this ice is “lemon chiffon.” Pale yellow, I’d guess. You can look these names up and relate them to a specific color but I haven’t bothered.

It also sees orange and tan. I might see tan but I’m not sure about orange.

I thought this ice was green but the software sees pale orange and “wheat”.

I thought we’d agree that this was blue but no, the software sees slate gray.

I couldn’t even guess what color this ice was but the software says “papaya whip,” whatever that is. By the way, if you or someone you know is colorblind just search for “What Color?” color finding software and you’ll find it. It’s free and has no ads.

This shows that the color in the ice doesn’t color it completely sometimes. I still believe that it has to be minerals in the groundwater that color it. I don’t know what else could.

I hoped I might see some red ice stained by iron but there was none. Just lots of staining on the stone.

This ice looked just plain dirty. I’m sure a lot of soil must be washed out of the cracks in the stones by all the groundwater that seeps through them.

I was a little disappointed that there wasn’t much ice on the drainage channels. That’s where you often see the laciest ice.

I needn’t have been disappointed though because just a little further down the trail ice had formed on the channels.

All the variations in ice forms are an endless source of amazement and wonder for me. It’s quite beautiful.

This one that had formed on a stone just above the water surface looked like a fish, I thought.

A young skier was headed for the old lineman’s shack and I thought I’d follow him because that’s where all the sunshine was. He stopped to talk for a bit and said he was trying to do ten miles for the first time. He also said he hoped he’d make it. I hoped so too and wished him well.  

The old lineman’s shack still stands so it looks like it will somehow make it through another winter. When I see it I think of the way things once were and how things were built to last. It continues to surprise me.

I saw what was left of another small bird’s nest near the old shack. It might have been just big enough to hold a hen’s egg with no room to spare. I’d guess that it started life in the V of those two branches.

As I left I looked up and hoped it was warmer out there.

It had just reached freezing (32 ˚F) when I came in here so allowing for the usual 10 degree difference meant that with the breeze it was probably about 20 degrees inside the canyon. After two hours I was ready to leave and I had taken about three times the photos that I could use anyway. There is an awful lot to see in this place, all of it beautiful, but I think the next time I come here the ice will have fallen and it will be more green than white. Thousands of violets bloom here in spring and I want to be here to see them.

The splendor of Silence—of snow-jeweled hills and of ice. ~Ingram Crockett

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Last week I had some back pain that was uncomfortable enough to keep me home from work one day. But if there is one thing I’ve learned over 50 years of back pain it is that sitting around is the worst thing you can do, so as soon as it was warm enough I decided to try walking off the pain. Walking, I’ve discovered, is the best thing for my kind of back pain. The above photo is of the woods in part of my neighborhood that I walked past. Black bear, deer, rabbits, turkeys, hawks and blue herons are some of the larger birds and animals I’ve seen in the area.

I didn’t walk through the woods though; I stuck to the road. Back pain calls for easy walking, not breaking trails. This shot of beech leaves in the sunshine and every other photo in this post is from the road.

There are some old black cherry trees out here and most have some type of noticeable changes caused by black knot disease. This one looked like a burl but no, it is a swelling caused by a fungus called Apiosporina morbosa. Infected stems swell up and produce hard black knots which will eventually become serious wounds, and eventually the tree will die.

Witch hazels (Hamamelis virginiana) grew right at the edge of the road so I was able to get a shot of the little cup shaped bracts that the petals come out of. This is a fall blooming witch hazel but the spring blooming Hamamelis vernalis witch hazels will be blooming soon.

I’m seeing what seems like an awful lot of fallen trees everywhere I go.  

I saw plenty of signs that it had been snowing. I haven’t kept close track but we’ve gotten at least some snow almost every day for the past two weeks.

There is quite a large wet area along the road where red maples grow. Some people call them swamp maples but if you look up “swamp maple” you find Acer rubrum, the red maple. They are also called water or soft maple. They don’t mind occasional wet feet.

Overhead I could see red maple buds that seemed to be swelling up, preparing to blossom in March. It’ll still be a while before the flowers unfurl, but they’re on the way and they’re beautiful to see in spring. Seeing the hillsides awash in a red haze from hundreds of thousands of red maple flowers is a treat that I always look forward to.

I looked at a sugar maple (Acer saccharum) and saw that it had a broken branch. And where the broken branch met another there was a single drop of pure maple sap, so the sap is flowing and that means buds are indeed swelling.

Cattails (Typha latifolia) decorated the edge of a small pond. I have a feeling that muskrats or other critters are eating the roots of this particular patch of cattails because it has actually been getting smaller over the years. That’s unusual for cattails because they can grow faster than fertilized corn. Scientists have recorded cattail marshes travel up to 17 feet in a year in prime conditions just by sending out new shoots. They are very beneficial to many animals and birds and even help the ponds and lakes they grow in by filtering runoff water and helping reduce the amount of silt and nutrients that flow into them.

The fluffy cattail seed heads are all ready for the return of red winged blackbirds, which will use them in their nests. I’ve also watched female red winged blackbirds pick grubs out of the previous year’s stems. Cattails were an important food for Native Americans. Their roots contain more starch than potatoes and more protein than rice, and native peoples made flour from them.  They also ate the new shoots in spring, which must have been especially welcome after a long winter of eating dried foods. They had uses for every part of this plant; even the pollen was harvested and used in bread.

I got lost for a bit in the beautiful bark of an old white pine. We have some very old, very big white pines in this area but many of the tallest, straightest trees were taken by England in colonial days to be used as ship masts. In 1722, a pine tree law decreed settlers couldn’t cut any white pines bigger than a foot in diameter and then later on the colonists had to pay for a royal license to cut white pine trees on their own land. In 1736, one of the king’s surveyors seized white pine logs in Exeter, New Hampshire. This act so enraged residents they disguised themselves as Indians, beat up the surveying party, sank their boat and chased them into the woods, where they hid all night. All of this led eventually to what is known as the Pine Tree Riot. In an open act of rebellion New Hampshire colonists cut down and hauled off many marked mast pines in what was just a taste of what would come later in the American Revolution.

An oak that stood next to the pine in the previous photo had Trentepohlia algae growing on it. Trees have vertical grooves in their bark that help channel water away in a rain and many mosses, lichens and even algae grow on the “banks” of these vertical streams. You can see that happening in this photo. Apparently these are the places that stay wettest longest after a rain.

Even in silhouette I knew I was under a northern catalpa tree (Catalpa speciosa) because of the string bean like seed pods that can be two feet long. In fact when I was a boy we called them string bean trees. Catalpa wood is very rot resistant and railroads once grew great plantations of them to be used as railroad ties. They are still used for utility poles today. Midwestern Native American tribes hollowed out the trunks of catalpa trees and used them as canoes, and the name Catalpa comes from the Cherokee tribe’s word for the tree. Natives made tea from the bark and used it as an antiseptic and sedative. Parts of the tree are said to be mildly narcotic.

I’m guessing that this hole in a maple is an animal’s home. There are scratch and / or bite marks all around it. It was big enough for a squirrel and they will live in hollow trees given the chance.

It’s hard to go anywhere in New Hampshire without seeing a stone wall so I wasn’t surprised by this one. You can tell by the smaller stones supporting larger stones that some thought and care went into this wall, and that means it is a laid wall. Most of our walls are “tossed” or “dumped” walls, built only to get rid of the stones in the pasture with no thought taken for looks. Laid walls took longer and were usually built along road frontage where they could be seen by passers by, just as this one was.  New Hampshire has an estimated 50,000 miles of stone walls but I doubt anyone will ever know for sure. The woods are full of them.

More expensive walls were built of cut stone like the piece of granite seen here. illustrates perfectly how feathers and wedges were used to split stone. The finger size half holes seen at the top are about 3-4 inches deep holes and were drilled (by hand) in a line where the split was to take place. Then curved pieces called feathers were put into each hole and wedges were driven in between them. As happens in splitting wood, the force from the wedges being driven ever deeper splits the stone. I have a feeling this piece of granite was found and placed here because most of this wall was simple field stone. Building stone walls is one of the most satisfying things I’ve done but unfortunately it’s very hard on the body.

After walking for a while I came to the Thompson covered bridge, named after playwright Denmon Thompson who was a native son, and built in 1832. This bridge is a truss style bridge with two spans that meet on a center support. One span covers 64 feet and the other 63.5 feet, making the total length 136 feet 10 inches long. It once had two covered walkways, but now has only one on the upriver side. It can be seen on the left in the photo. Town records indicate that there has been a bridge in this spot since at least 1789.

This view shows the stone center support for the two spans. The bridge design is known as “Town lattice,” patented by Connecticut architect Ithiel Town in the early 1800s. The open lattice work lets a lot of light into the bridge and this is unusual because many covered bridges were and are dark and cave like. In the 1800s being able to see daylight inside a covered bridge would have been the talk of the town. The Thompson Bridge is considered by many to be the most beautiful covered bridge in New England.

The Ashuelot River, which the Thompson Bridge crosses, was partially frozen over in this spot. I thought I might see some Canada geese but they don’t seem to winter over here anymore. This photo does show what a beautiful day it was, geese or not.

I hope this post shows that you can find a lot of interesting and beautiful things right in your own neighborhood without even leaving the road. My favorite photo from this walk is of an ice covered stone in the river. It was like alabaster on silk and I thought the colors and textures of the water were beautiful.

Though my back hadn’t returned to 100 percent the two hour walk did it a world of good and I returned to work the following day. Not only does walking exercise muscles; what you see in nature takes your mind off the pain and lets tense muscles relax.

My wish is to stay always like this, living quietly in a corner of nature. ~Claude Monet

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I hope you’re in a nice warm place while reading this because this post is full of ice like that in the photo above, and you might feel a little chilly by the time you’ve reached the end.

Last Sunday, about a month since my last visit, I decided to visit the deep cut rail trail up in Westmoreland where the “big ice” grows each winter. The walls of the manmade canyon are 50 feet high in places and groundwater running through the stone creates ice columns as big as tree trunks. I wanted to see how much the ice had grown in a month.

It had grown quite a lot; enough to climb, in fact and by chance the Appalachian Mountain Club were training here today. They come here as soon as the ice is safe to train people in ice climbing. On this day the 25 degree temperature and 10 mile per hour wind made this place feel like an icebox, and that’s exactly what the climbers call it.

I was here for ice too; not to climb but to photograph, and I saw plenty.

There was an entire canyon full of it.

Some of the ice is colored various colors, I believe according to the minerals that happen to be in the groundwater.

There are plenty of mineral stains to be seen on the stones where groundwater has seeped out of cracks and it makes sense that mineral rich water would color the ice.

This slab of ice is huge and if it ever lets go of the rock it grows on I hope I’m nowhere near it.

I speak about “rotten ice” a lot when I come here so I thought I’d show you the difference between good, solid ice like that in the above photo and the rotten ice in the following photo. This ice is clear and very hard and will ring sharply if you tap on it. It has very few air bubbles and other impurities trapped inside it.

Rotten ice on the other hand is opaque, weak and full of impurities. Ice becomes rotten when water, air bubbles, and/or dirt get in between the grains of ice and cause it to honeycomb and lose its strength. When you tap on ice that looks like this you hear a dull thud. The grayish white color and matte finish are a sure sign that you should stay away from it when it’s hanging over your head like it can do here.  

Falling ice is a real danger here; most of these pieces were big enough to have killed someone. This doesn’t usually happen until the weather warms in March though, so I was surprised to see it.

Then there are the falling stones. These fell very recently because they were on the ice of the frozen drainage channel. This always concerns me because I walk in or over the drainage channels to get to the canyon walls. That’s where interesting mosses and liverworts grow. If I had been hit by any one of those stones it would have been all over.

But speaking of the drainage channels, the ice growing on them was beautiful.

The opening photo of this post also shows ice that formed on the drainage channel, just like that in the above shot.

Here was something I’ve never seen; an icicle fell and stabbed through the ice on the drainage channel, and then froze standing up.

Last year’s leaves were trapped under the ice in places.

In other places the drainage channel hadn’t frozen at all. Here the sun was reflected in the water of the channel. I thought the colors were very beautiful. Like molten sunshine.

This spirogyra algae dripping off the stones was something I’ve seen but have never seen here. Spirogyra has common names that include water silk and mermaid’s tresses. It is described as a “filamentous charophyte green algae of the order Zygnematales.” I’ve read that they grow in nutrient rich places. They’re always interesting and I wanted to take a closer look but I didn’t have my rubber boots on so I couldn’t walk through the drainage channel.

Here is some spirogyra algae that I found last year. The strange thing that looks like a vacuum cleaner hose is a chloroplast, and its spiral growth habit is what gives these algae their name. There are more than 400 species of Spirogyra in the world, almost always found in fresh water situations. According to what I’ve read, when used medicinally spirogyra are known as an important source of “natural bioactive compounds for antibiotic, antiviral, antioxidant, anti-inflammatory, and cytotoxic purposes.” As I said; they’re always interesting.

NOTE: A botanist friend has written in to say that chloroplasts are microscopic so the hose like thing is not one of those, but neither one of us can figure out exactly what it is. It’s a very strange thing to be seen under algae, that’s for sure. I wish we had studied algae in the botany classes that I had!

The orange red color in this shot is iron oxide, washed from the soil by groundwater. I thought the colors in this scene were amazing; otherworldly and beautiful. There was much beauty to be seen here on this day and it reminded me why I come here again and again.

As I always do I stopped at what is left of the old lineman’s shack. It was easy to imagine a group of workers huddled around an old potbellied stove in there on a day like this, but it would have had walls and a roof then. It was very well built and simply refuses to fall. They actually used railroad ties for the sills.

Here is a look at the inside of the shack. It’s too bad people feel the need to tear things apart, but it has probably been abandoned for close to 50 years now, since the Boston and Maine Railroad stopped running in the 1970s.

If you aren’t cold yet you must be a real trooper, but I thought I’d end with a warm shot of sunshine and blue sky just in case. With the wind chill the temperature was about 10 degrees F, and I was thankful that my cameras hadn’t stopped working. I was also thankful to be back in a warm car again even though I discovered that wearing a cloth mask is a good way to keep your face warm. Hopefully spring isn’t too far off.

It’s getting cold. Some of you will put on jackets from the last season. Check your pockets. You might  well find a forgotten, unfulfilled wish.
~ Ljupka Cvetanova

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There is a little stream that I pass each day that I like to visit up close every now and then, just to see what changes have taken place and to see all the things I missed on my previous visits.

It was cold enough for there to be ice.

Here an ice bauble had formed around a stick that was sticking up out of the water.

This stream is called a meandering stream because of its sinuous, snake like curves. This shot shows how gravel has built up on the inside, slower part of the curve (left) which is called a point bar, and how this forces the water to eat away at the embankment on the faster outside part of the curve (right). In this way the stream swings from side to side over the length of its course and this is known as a meander belt. According to what I’ve read the length of the meander belt is typically from 15 to 18 times the width of the stream or river. But wait a minute I say, because this is a view of the stream when it is calm. After we’ve had a lot of rain I’ve seen it swell to 10 times this width, enough to cover all of the ground in these photos and more, so I wonder how that affects its meander.

A squirrel had a fine meal of white pine seeds if I am to judge by this large pile of scales at the base of the tree. Squirrels like to sit on something when they eat and I’ve seen these piles at the base of stumps, rocks, and even fence posts. They don’t like to eat while on the ground and I’ve always thought it was because they could spot predators better up a little higher.

I spotted a fine crop of what I believe were mock or orange oyster (Phyllotopsis nidulans) mushrooms. Since they were frozen solid and I couldn’t get above them I can’t really be sure but they were a touch of woodland beauty nevertheless. I didn’t see it at the time but you can see how the underside of the large example just above center has been gnawed on. I’ve seen squirrels eat mushrooms but I can’t say for sure what animal did it.

One of the bracket fungi that sort of mimic the common turkey tail (Trametes versicolor) is the thin-maze flat polypore (Daedaleopsis confragosa). (There are a few others) Since turkey tails have pores and these have what appear to be gills they are hard to confuse. Thin maze flat polypores start life very white but turn gray as they age. They have some zoning like turkey tails and are often covered with green algae.

The pores on this bracket fungus are elongated and can resemble gills but in any event they are very different than the “pin hole” pores found on the underside of turkey tails.

I did see some turkey tails but there were only two or three and they were so beautiful I couldn’t bear to pick one and show you its pores. Turkey tails are sabprobic fungi, meaning they decompose dead or decaying organic material. Though they do occasionally grow on live trees, if you find them on a standing tree it is most likely dead. Turkey tails cause white rot of the sapwood. They also show great promise in cancer research.

Last year at work I was lucky enough to find some chicken of the woods mushrooms (Laetiporus sulphureus) that I could watch every day, and toward the end of their time they looked exactly like the dead, white examples seen here. Too bad I didn’t see them when they were alive; they’re a big beautiful, very colorful mushroom.

One of the reasons I wanted to come here was to visit my friends the tree mosses (Climacium dendroides). This is the only spot I’ve ever found them so they aren’t common in this area, but they are spreading here along the little stream. On this day some of them looked a little brown but I hope they’ll come back. They must not mind being under water for a time because when the stream floods they get very drenched, growing as they do right on its bank.

They are cheery mosses that remind me of little palm trees, and they always glow with a beautiful inner light.

I’ve spoken about frost cracks many times on this blog but I read recently in the excellent book Woods Whys by Michael Snyder that though frost cracks are indeed caused by cold that isn’t all of the story. Frost cracks usually appear where there is previous damage to the tree, such as the scar on this young maple. I have a feeling that this was caused by a male white tail deer rubbing its antlers on the tree.

I can’t guess what other animal would peel bark in strips like this. Porcupines eat bark but to my knowledge they don’t peel it and leave it like this. And I didn’t see any teeth marks.

By the way; though the book Woods Whys would be a great addition to any nature library I was told that it was out of print. Luckily though my local bookstore was able to find a copy after two weeks of searching, so if you’d like a copy don’t give up because they are out there.

This tree stand told me that my thoughts about buck rubs might be accurate. It’s a simple thing; a hunter would climb the ladder and sit at the top, waiting for a deer. But sitting up there in November waiting all day for a deer to wander by would take something that I apparently don’t have in me.

This natural trail leads into a swamp that the stream feeds into. I believe this trail was made by beavers. When the stream floods this entire area is under water.

There were animal tracks leading into the swamp.

This shows that even animals slip on the ice. I think there are the tracks of two animals here; the one in the upper left has nails like a fox or a small dog and the others look more like a cat, possibly a bobcat. In any event there was a lot of traffic going into the swamp.

This stump and quite a few others showed plenty of fairly recent beaver activity. By the way that stump is iron wood, which isn’t called that for nothing. I’ve also seen beavers chew through elm, which is another very tough species.

By looking at the black knot damage on this old cherry it was easy to see where the stories of ogres living in the woods came from. Black knot disease is caused by the fungus Apiosporina morbosa which can also attack plums, peaches, and apricots. If not pruned off and burned as soon as possible when the tree is young it will kill the tree, and I don’t think this one has far to go.

Even in what appears to be a dry area these fertile, spore bearing fronds of sensitive fern (Onoclea sensibilis) tell a different story. Sensitive fern is an indicator species and it indicates that you’re in a wetland, so you had better have your boots on.

Sensitive fern fertile fronds are pretty things to stop and admire in winter. In this case the typically round spore capsules had opened, and this is something few people see. It isn’t a rare sight though in my experience; I think people simply don’t look.

I hope you’ve enjoyed this little meander by a meandering stream. I had a great time and as is often the case, I had to pull myself away.

The waters of the stream played the part of the orchestra, and the sunlight provided the dancers. Every now and then a crescendo of wind highlighted the symphony in the clearing by the creek.
~Edward Mooney Jr.

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I’ve seen some really stunning photos coming from smartphones lately so since it was time for me to get a new one I spent quite a lot of time researching which one had the best camera for the money. By the end of this post I hope you’ll agree that I made a good choice; the tiny mushroom in the photo above was hardly bigger than a pea. Yes this phone does macro photography, and it does it well.

Tiny bird’s nest fungi weren’t much of a challenge for the phone but depth of field was slightly off. I think that was my fault more than the phone’s though.

I was splitting wood at work and there, deep inside a piece of oak, was this mushroom mycelium. I was lucky I had a phone with me that could see it and get a half way decent photo of it. I always love finding mycelium because I never know what my imagination will have me see in it. You might see a river delta. Or a tree. Or bird feathers. Or you might see the vast one-ness from which all life arises. Whatever you see in it let it be beautiful; let it reflect the beauty that is inside you.

One of the haircap mosses, either mountain or juniper haircap moss I believe, peeked out from under a dome of paper thin ice. This is a male moss and you can tell that by its color and by the tiny male reproductive structures called antheridia, which look like tiny flowers scattered here and there.

And here was a female haircap moss with its spore capsules almost ready to release their spores. There was a breeze this day and the phone camera didn’t freeze the movement of the capsules as much as I would have hoped but something about this photo grabs me so I’ve added it here, slightly blurred capsules and all. It’s a mouse eye view of the landscape with a certain minimalistic Japanese feel to it, and maybe that’s why I like it.

This bristly beard lichen growing on a white pine is another photo where the depth of field was slightly off and I think it’s happening because I’m getting too close. In fact the phone has told me to “back up for better focus”. But I’ll learn; I’m used to taking photos with my Olympus macro camera, where I can be almost touching the subject. A bristly beard lichen has isidia, which appear as little bumps along its branches. An isidium is a reproductive structure common to some lichens and their presence is a good identifier.

This liverwort, called flat-leaved scalewort (Radula complanata) was about 3/4 of an inch across and grew on a tree, and I thought the phone handled it well. I’ve read that this liverwort is common on trees and shrubs but I rarely see it. Plants are usually flattened, either forming patches like the one seen above or single stems creeping among mosses. It has round, flattened, overlapping leaves which are quite small. Each one is no more than 1/16  of an inch across. This liverwort is said to like sunny, sheltered, moist conditions and will sometimes grow on streamside rocks. Liverworts are epiphytes that take nothing from the trees and shrubs they grow on. ­­They simply perch on them, like birds.

Color reproduction seems to be quite accurate with this phone but beware that this is coming from one who is colorblind. Still, even someone colorblind can see the difference between the hemlock in the foreground and the one beside it, because the one in the foreground is “artificially” colored by Trentepohlia algae. I don’t think I’ve seen this much algae on a single tree before. I wonder how it chooses which trees to grow on and I wonder why, in this case, it hasn’t spread to other trees.

Here is a phone camera macro look at algae on a different tree.

Tiny lichens are a big part of the content on this blog so of course I had to see what the phone could do with them. Again, I think I was a bit too close to this one but I was impressed with the camera. This lichen was only about a half inch across.

In this photo I backed the phone away from the subject lichen and the shot came out much better. This lichen was about half the size of the previous one but it came out much sharper so I’ve got to watch out for getting too close.

Compared to the lichens these alder catkins were huge but the phone camera handled them well, even in a breeze.

I wanted to show something that everyone reading this would know the size of, so for that I chose lilac buds. This is an excellent example of what this phone can do.

The bud of a Norway maple is not something everyone will recognize but they are slightly smaller than the lilac buds.

If you’ve ever wondered why woodpeckers spend so much time drilling into trees, this is why. This yellow insect larva was deep inside a red oak log, seen only when I split it. The tiny creature was about the diameter of a piece of spaghetti and maybe an inch long.

This is just simple stream ice but it was beautiful, I thought.

Of course I had to try plants with the phone camera and it did well on this trailing arbutus. I didn’t want to kneel in the snow so I just bent down and clicked. This phone is said to use a kind of artificial intelligence chip that I don’t fully understand, and it said to be able to compute very fast. In fact I’ve read that some phones can do 5 trillion operations per second.  Speed is one thing, but this phone seems to know or sense what you want before you tell it what you want and I find that a bit odd, if not unsettling. It’s almost like having an assistant who does all the work for you.

Here were the dried flower heads of sweet everlasting. There was a breeze on this day and once again the phone handled it well.

The color red is a challenge for any camera so I thought I’d try some holly berries. The phone camera once again did well, I thought. I like the detail that came through on the leaves as well.

Boston ivy berries (Parthenocissus tricuspidata) are about as big as a small pea, so while I was walking past them while going in for a haircut I thought I’d see what the phone could do with them. I was happy with the shot. Boston ivy isn’t a true ivy and it isn’t from Boston but it is pretty on buildings, especially in the fall when its leaves turn bright red. True ivy belongs to the genus Hedera but Boston ivy is the ivy that lends its name to ivy league universities.

The phone camera seems to do well on landscapes as well. It also has a “night vision mode” but I didn’t use it for this shot of a stream I pass on my way to work early each morning.

The phone tells me I was 11 meters (36 feet) from this tree when I took it’s photo. Why it thinks I need to know that is a mystery. I would have fumbled around with my camera settings for several minutes for this shot, trying to keep the trees light and the clouds dark, but the camera phone did it in two shots without my changing any settings.

This shot looking up a pine tree was taken in almost full darkness, well after sundown and with twilight almost gone. When you push the shutter button on the phone you can hear the shutter click twice when it’s in night vision mode and the photo comes out like this. How it does this is unknown to me as yet. I wanted to show you a dark sky full of bright stars but it has been cloudy every night since I bought the phone.

This shot, taken before sunup early in the morning, was the first shot I ever took with the new phone. I suppose I should give you the name of this phone after putting you through all of this, shouldn’t I? It’s a Google Pixel 4A, 5G and for the same money, according to the reviews I’ve read, no other phone camera can touch it. I find that it is especially useful in low light situations but I also find it a bit awkward to hold a phone while taking photos. I’m certainly happy with it but I think I need more practice. I’m guessing that when the newness wears off it will become just another tool in my tool kit; a camera I can speak into.

We become what we behold. We shape our tools and then our tools shape us.
~Marshall McLuhan

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It was cloudy but finally warm at 38 degrees F. last Sunday so I decided to see how the ice had grown in the deep cut rail trail that ice climbers call the icebox. Since we have had plenty of below zero nights I expected the ice to be big, and I wasn’t disappointed.


Though I’ve seen as many as thirty at a time, on this day there were only two ice climbers here. It was dark in this part of the canyon on such a cloudy day so I had to really increase the ISO on my camera. Sunshine is limited on this part of the trail even on a sunny day because it’s about 50 feet below the surrounding hill that the railroad cut through.


The ice climbers said this was their third time here but they were climbing on a skimpy little ice column that didn’t look like it would support much weight. I pointed out the huge ice column on the other side of the canyon and told them that was where most people climbed, but they stayed where they were and I bid them good luck. You could fit what I know about ice climbing in a thimble anyway.

This massive pile of ice is where most ice climbers climb but on this day you could hear water dripping behind it, and that was odd.


There was a large pool of water at its base as well, and that probably would have given me second thoughts about climbing it. If groundwater was dripping between the ice and the stone of the canyon the whole thing could come tumbling down, and you don’t want to be here when that happens.


But I decided not to think of such things and instead focused on the beauty of the ice. After all, it was why I had come. All of the water that drips from the stone walls of the canyon collects in drainage ditches originally built by the railroad 150 years ago. The water is carried by the ditches out into the woods where it must eventually find its way to a swamp or pond. Meanwhile beautiful patterns form in the ice covered ditches.

Ice can be very beautiful, especially on a warm day when you have time to linger and appreciate it. I often catch myself lost in the photos I’ve taken of it as well, wondering what I might see. I’ve seen birds flying, eyes staring, waves and rivulets caught in mid flow and entire galaxies, all frozen into the ice. I love what it did here; it’s much like a topographic map because if you look closely you see that the ripples formed around peaks, and the peaks are stones in the stream. It’s a beautiful scene, and there are thousands upon thousands of others much like it out there, just waiting to be discovered.


I saw that someone had put up a sign to warn snowmobilers that there were people on the trail. That’s a good idea because the trail curves in the canyon and I’m sure a snowmobiler could be just about on top of the climbers before he sees them, depending on how fast he was moving. I hear people complaining about snowmobilers but I don’t agree, because if it wasn’t for them many of these rail trails would have become impassable long ago. Many snowmobile clubs donate their time and tools and work hard all summer long to keep these trails open and we who use them owe them a real debt of gratitude.


When you come into the canyon you can go north where the ice climbers climb or you can go south where the most colorful ice grows. I usually do both. The walls don’t soar quite as high in this section but the ice comes in many colors and grows as thick as tree trunks.

There was lots of blue ice here this day and I wasn’t surprised because it has been so cold. I’ve heard that blue ice is the hardest and most dense, and its color comes from the way the dense ice reflects light, rather than any imperfections in the water.


Other colors come from the minerals in the groundwater, I believe. Some years you see lots of orange ice like this and in other years you hardly find any. You can see at the base of the column how the snow is stained by the dripping, mineral colored water.


Though I see green when I see this ice my color finding software sees tan. Since I’m colorblind the software gets the call. Whatever the color, this formation was big. This also illustrates why I don’t come here much after the end of February, because when large ice columns like this one release from the stone they often fall like trees, right across the trail. I’d rather not be here when that happens because a person could easily be crushed.

Here is some mineral staining on the stone walls of the canyon. I believe this is what colors the ice but the strange thing is how these colors all but disappear in warmer months. Cold brings out the colors in many things like tree sap, and apparently mineral staining on stone.


It was the texture of this ice column that caught my eye. It was like ten thousand icicles had all frozen together. Quite often you see these ice columns with a smooth, shiny surface but this one was rough.


Here is a better example of how the snow stains at the base of these columns.


Frost flowers bloomed on the ice covering the drainage ditches.


I don’t see these very often so conditions must have to be just right. I’m guessing it has a lot to do with humidity. I see birds flying above Saturn’s rings, and the universe beyond.


This takes the prize as the biggest mass of ice I’ve ever seen off a pond. It’s so big I don’t know how to explain just how big it is. Tons and tons of ice, I’d guess.


Somehow a beech leaf stuck itself to an icicle. I’ve noticed that many beech and oak leaves are falling, and I hope that’s a sign that spring isn’t far away.

A small animal came out of its den for a drink and found the well frozen over. Its tracks made the snow look as if it had been zipped together.


My walk through the canyon ends at the old lineman’s shack, because that’s where the big ice ends. It looks like the old building will make it through another winter, though I don’t know how. It’s the very definition of well built. I picture it full men sitting around a potbellied, coal fired stove, wishing they didn’t have to shovel all the snow out of that canyon. But that chore must have fallen to someone.

Ice burns, and it is hard for the warm-skinned to distinguish one sensation, fire, from the other, frost. ~A.S. Byatt

Thanks for stopping in.

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