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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 Saturday was cold but clear with wall to wall sunshine. I decided to take a walk along the Ashuelot River in Keene to see if it had frozen over and was surprised to find that it had frozen over the whole length of the distance I walked.

It looked more like a pasture than a river.

I saw some strange animal tracks on the ice but I couldn’t get close enough to find out what animal they were from. They might have been from a rabbit or squirrel.

Wool grass (Scirpus cyperinus) likes wet places and grows here and there on the riverbank. Though its common name points to a grass this plant is actually in the sedge family. It is also called bulrush. Its seeds are eaten by waterfowl and muskrats will eat its roots. Native Americans used this plant to weave mats, bags and other utilitarian objects. I like its drooping habit.

Something that sets my blood racing at this time of year is bare ground, and I’m seeing more of it wherever I go. The sun gets stronger each day and no matter how many storms we have or how cold it is the snow will melt, starting on southern exposures. You can also see in this shot how the snow on the trail had been packed down by many feet. The going was easy as long as I stayed on the trail.

There were strange looking ice formations on the surface of the river.

There was some snow built up on the bent tree that lives out here. This tree never seems to get any larger.

I thought the beavers might have finished the job they started last fall on this huge oak tree but they’ve abandoned it. Girdling means that the bark has been removed around the entire tree and since the inner bark (cambium) is what carries nutrients and moisture to the crown, a tree cannot survive without it. Anything above the girdling will die.

It really is amazing what beavers can do with their sharp teeth. From what I’ve seen no wood is too hard for them.

I saw a girdled smaller tree and I can say for certain that this was not done by a beaver. I don’t know why anyone would do this unless it was the Keene Parks and Recreation Department wanting to remove trees along the trail. Girdling has been used to remove trees for thousands of years and the Native Americans who once lived and fished in this area surely used it to clear land. Once the trees died and fell on a piece of land the brush and trunks would be burned and the resulting wood ash and whatever rotting wood was left helped to fertilize the land for farming. Girdling is still used by foresters, horticulturalists and land owners today.

I saw many trees that had fallen naturally out here. In fact I see them wherever I go and most of them are white pines and red maples.

I was stopped by the bright, orange-brown color of a blueberry branch in the sunlight. I should have gotten a shot of its small red buds as well.

The sunlight was also caught in the trees and it was so beautifully golden against the deep blue of the sky.

I saw lots of oriental bittersweet berries (Celastrus orbiculatus) still on plants, and that’s a good thing. It means the birds aren’t spreading its seeds around.

Oriental bittersweet vines are as strong as wire and don’t expand as whatever they wrap themselves around grows larger. The alder with bittersweet wrapped around it in this photo will eventually be strangled to death unless something is done.

When it gets cold dark, almost black spots appear on the bark of trees. They are really there all the time but are kind of a lighter reddish color and not quite so noticeable at other times of year when there are so many other things to see. Those who think they’ve never seen a liverwort might want to stop and take a closer look at these dark, lacy blotches because they are Frullania liverworts, one of the few liverworts that can thrive in dry places.

There are about 800 species of Frullania liverworts and many grow as epiphytes on the bark of trees and shrubs where the humidity is high. Epiphytic plants take nothing from the host plants they grow on, so this liverwort does no harm to trees. Its leaves are very small and hard to get a good photo of.

Something not quite so pretty as the frullania liverwort is the beech scale (Cryptococcus fagisuga) seen here. Excessive feeding by this scale insect causes two different fungi, Neonectria faginata and Neonectria ditissima, to produce annual cankers or blisters on the bark of the tree. The continuous formation of lesions around the tree eventually girdles it, resulting in canopy death.

You know it’s cold when pine sap turns blue, and we’ve had a cold February. It was about 25° F. (-4° C) on this day.

Yes it was cold but it was also a beautiful sunny day so I stood on the bridge for a while listening to the silence, which was broken only by birdsong and the occasional cracking of river ice. It would have been easy to lose myself and stand here for longer than I did but you have to watch that in winter because frostbite can be a possibility and once you stop moving you cool off fast.

On the way back I thought a contrail looked much like what smoke from a campfire might have looked like long ago. It wasn’t hard to imagine Native lodgings out there somewhere; archeological digs have shown Native Americans were here at least 12,000 years ago.

I decided to check on Ashuelot falls before leaving. They were all splash and foam and remained thawed for the most part.

There were some huge ice formations here and there though. This one looked like the arm and paw of a gigantic polar bear.

Above the falls I saw these strange tracks on the ice. They were big, easily as big as my hand, and I wondered if they might be moose tracks. Moose are occasionally seen in this area. They have even walked through Keene neighborhoods and down city streets. They also occasionally fall through the ice and it’s quite a job getting them back on dry land. An adult male moose can weigh over a thousand pounds.

The earth is rude, silent, incomprehensible at first; be not discouraged – keep on – there are divine things, well envelop’d; I swear to you there are divine things more beautiful than words can tell. ~Walt Whitman

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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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Sometimes when you walk a trail you come back with more questions than answers, and that’s what last Saturday was like.

I chose a rail trail in Swanzey because the snowmobile traffic had packed the snow down, and that made for easy walking. I saw a few riding the trail that day. There goes one now.

The snow in the woods wasn’t all that deep but if you strayed too far off the trail you’d get a shoe full.

The old stock fencing along the trail still looked as good as the day the railroad put it up.

An animal had come out of the woods on the other side of the trail. I couldn’t tell what it was but it wasn’t a deer. The prints looked more like a fox or coyote, but they weren’t clear.

A window had opened up into the drainage channel that ran along the trail.

A quarter size beard lichen floated in the channel. These interesting lichens fall from the trees regularly.

An evergreen fern had stood against the weight of the snow. These delicate looking ferns are anything but delicate.  

I was going to tell you that these lichens were common greenshield lichens (Flavoparmelia caperata) but something about them tells me they may not be that lichen. The branching and the lobes don’t seem quite right but it could be just because they were dry. I wish I had walked over to them instead of taking this photo from the trail but for now I’ll just say they are large round, green foliose lichens. Close to 20,00 species of lichens are said to cover 6% of the earth’s surface but few pay any attention to them, and that’s too bad.

The lichens will most likely be there when I get back; this land is protected.

I’ve taken photos of both alder and hazelnut catkins this winter and both have had a reddish cast to them that I’ve never seen. These American hazelnut catkins (Corylus americana) were a pinky-brown according to my color finding software, so it isn’t my imagination. They’re usually green and this was just one of a few mysteries that I came away from this particular trail with.

And here was another mystery. I found this strange growth on the same hazelnut that I showed in the previous photo. I believe that it must be some type of gall but I’ve never seen anything like it before on a hazelnut and I’ve looked at a lot of them.

It seemed to be a bunch of deformed leaves, which some galls are, but it was small; about the size of a grape. It was also quite furry.

This was not a mystery. Even in silhouette shagbark hickory trees (Carya ovata) are easy to identify because of their peeling, shaggy looking bark. These trees produce good crops of nuts each year and help feed many different birds and animals.

I looked at a hickory bud but I didn’t see any signs of swelling yet. It has still been quite cold but it won’t be long now before the sap starts to flow.

If you find what looks like a big clearing in the woods in winter you had better walk around it until you are sure, because this clearing is a river. When you can’t tell where the land stops and the water starts it’s easy to find yourself walking on ice. I’ll never forget walking down the middle of this very river as a boy and hearing the ice start cracking under me. I don’t think I have ever moved that fast since.

This would be a good indication that what you might think is a clearing isn’t a clearing.

It’s funny how in spots the river is clear of ice and in others it is frozen over. Another mystery. I’m guessing that the speed of the current has something to do with it.

The leg of rail trail crosses a road several times. The tire tracks of one of the monster machines that plowed the road were fun to look at but not so much fur to walk in.

I expect to see beech and oak leaves falling at this time of year but not maple. We do have a couple of sugar maples where I work though that are still clinging to a few of their leaves.

I saw a single white pine seed scale, which is odd. I usually see piles of many hundreds of them, left by squirrels. White pine seeds grow two to a scale. It takes them around two years to mature, and they usually ripen in August and September. They are light brown, oval in shape and winged so the wind can disperse them. I’ve tried to get the seeds, with their thin wings intact, from a scale and I can tell you that it is all firmly attached together. Squirrels can do it all day but I have yet to get one in good enough condition to show you here.

At first this was a mystery but after I looked at it for a while I thought it might be the seed head of a white flowered turtlehead plant (Chelone glabra linifolia). When I got home and looked it up there was no doubt and I was happy that I finally found the seedpods for this plant after so many years of finding the flowers. They look a little like the flowers and that makes them relatively easy to identify.

In the end I went home with a pocket full of mysteries but that was fine because it was a beautiful day, with the sky that shade of blue that only happens in winter and puffy white clouds to keep it interesting. I hope everyone is still able to get outside and enjoy. There is such a lot of beauty out there to see.

Outdoors is where the great mystery lies, so going into nature should be a searching and humbling experience, like going to church. ~Skip Whitcomb

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Punxsutawney Phil the weather predicting Groundhog saw his shadow when he was removed from his burrow last Tuesday, the second of February. That means, as the tale goes, that there will be six more weeks of winter. This isn’t a photo of Phil, but it is an excellent shot of a groundhog taken by Peter Chen and found on Wikimedia Commons. Here in this part of the country we call them woodchucks and they’re all sleeping peacefully through winter. If you’ve never seen one, a groundhog is about as big as a big house cat or maybe a little bigger, with lots of fur. We have a big one where I work but I’ve never been able to get a shot of it.

Anyhow, while Phil was predicting six more weeks of winter we were having a good old fashioned nor’easter, as the road on my way to work showed.

One of my favorite winter quotes by William Sharp says that There is nothing in the world more beautiful than the forest clothed to its very hollows in snow. It is the still ecstasy of nature, wherein every spray, every blade of grass, every spire of reed, every intricacy of twig, is clad with radiance. That is just how it was on this day.

And for every day thereafter for a while, because a fine misty rain fell after the snowfall and froze all of the snow to the branches. A lot of forest still looks like this over a week later in fact, and that is unusual. Usually the wind comes up and blows all the snow off the branches in short order.

We had a meager 6 inches where I live but in Hancock where I work they had closer to 11 inches. Either way, I had to do some snow removal.

But while I was removing the snow I was able to admire its beauty up close. I love the color of beech leaves in winter.

Snow pasted on the tree trunks told me the wind had been out of the south east, blowing to the north at a pretty good clip.

The wind had sculpted the snow around some trees…

…and had tried to bury others.

I’m always surprised by how much snow eastern hemlocks (Tsuga canadensis) can take. This one must have had who knows how many pounds of snow on its branches, but they just flexed down and bore the weight. Once the snow falls away they’ll return to their more normal positions. Younger birch trees will bend almost double under the weight of snow but quite often they don’t spring back and they die bent like a bow.

If you walk through a forest that looks like this you’d better have a hat on and your collar up, because  the slightest breeze will send all that snow cascading down upon you. It has happened to me many times.

Spruce trees can also take a lot of snow weight. Actually most evergreens can.

This is a view across part of the 13 acre field where I work. I mow it in summer but in winter the snow stays where it falls. It’s like a huge white blanket.

The black, mirror finish of water against the white snow is very beautiful and I often stop here on my drive to work to see it.

Everything was still and silent on this morning. It was just me and the beauty all around me.

The sun was in the trees but it had no real warmth.

What the sun lacked in warmth it made up for in beauty. I hope these snowy, icy posts haven’t made all of you shiver. If there is one thing a nature blogger knows it is that you take what nature gives, and when everything is covered in snow you take photos of the snow. It won’t last; it’s February already and before long the sap will start to flow and the smell maple syrup will be in the air. The syrup makers are already tapping the trees.

By walking in a snowy forest you can 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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I didn’t realize, until I started cleaning it up, how much stuff falls from trees. There must be tons of it raining down; it falls 24 hours per day seven days per week. Eastern forest broadleaf trees alone, it is estimated, can drop 2 to 3 tons of leaves per acre in the fall. And then there are the branches, seed cones, acorns and everything else that falls. If it wasn’t for the animals, bacteria and fungi that process it we would surely be buried under it all.

The tiny black specks you see here are seeds of the gray birch (Betula populifolia). Tiny yes, but there must have been millions of them in this small birch grove. Pine siskins, chickadees, and other songbirds eat them. Deer, moose and rabbits eat gray birch twigs.

I thought the brown on the snow in this shot must be dust like seeds but I suspect it was just dust.

Eastern white pines (Pinus strobus) drop an incredible amount of material each year; large branches, needles, cones and bark all end up on the forest floor.

Whenever I see a fallen pine branch I check it for lichens and probably 8 out of 10 times there are lichens on it. I believe this foliose example is in the Tuckermanopsis family, possibly Tuckermanopsis americana. It was quite dry even though it was on the snow, so I’d guess that its color had lightened.

After branches pine cones are probably the things that fall out of pine trees the most. They are everywhere, but they don’t always fall end first into the snow like this one had. The heavy end falls first sometimes like this one did but I’ve also seen them turned 180 degrees with the lighter end in the snow.

Usually when you see a fallen pine cone they look like this, but this one has done something special; the sun had heated it enough for it to melt its way into the snow. I’ve seen oak leaves melt into the snow in the same way.

When I see good size fallen pine limbs I always look for bark beetle damage. Bark beetles usually attack weak or dying trees but they can also kill healthy trees by girdling them.  Adults bore small holes in the bark and lay eggs in a cavity. Once the larvae emerge from the eggs they make tunnels in the inner bark, like those seen here. Once they stop feeding they will pupate at the end of these tunnels. The pupae then become young adults and fly off to find another tree. These beetles carry spores of various fungi which can grow on the outer sapwood and stop the upward flow of water to the crown. Bark Beetles include over 100 species and it is said that their work is like a fingerprint for the species. They can create such beautiful patterns in wood that it looks as if a calligrapher has taken up a chisel instead of a pen.

Mosses of course, are also common on fallen branches. These were very dry but the shield lichen next to them didn’t look too bad. I think it was a common greenshield (Flavoparmelia caperata) , which is indeed very common. They often have patches of granular soredia on them as this one did in its center.

If white pine branches are the most common on the forest floor then eastern hemlock (Tsuga canadensis) branches are the second most common. The difference about hemlock branches though, is how they are almost always small enough to decompose quickly.

Both pines and hemlocks catch much of the snow on their branches, and underneath them the ground is often bare or nearly so in all but the snowiest winters. These bare spots are often full of small birds like juncos scratching around for seeds.

Honey locust (Gleditsia triacanthos) seed pods are pretty things. When the seed pods are green the pulp on the inside is edible and very sweet, while the pulp of the very similar black locust (Robinia pseudoacacia) is toxic. One good way to tell the two trees apart is by the length of their seed pods; honey locust pods are much longer and may reach a foot in length, while black locust pods only grow to about 4-5 inches long. Honey locust seed pods look a lot like giant flat string beans about 9-12 inches long and often curled. Some of them look like polished mahogany and others can be purple. Beautiful white, fragrant flowers cover these trees in late spring. Locusts are legumes, in the pea family. Deer love the seed pods, which often fall in such abundance they cover the ground under the trees.

You want to watch where you walk under a honey locust because fallen branches can be very thorny. Honey locust thorns grow singly and can be 3 to 6 inches long. They will sometimes branch like the example in the photo. These thorns are big and as hard as iron. They can reach 6 inches in length and poke right out of the bark of the tree along its branches and sometimes even the main trunk. They are tough enough to puncture shoe soles and can cause a nasty wound. In the past the hard thorns of the younger trees were used as nails. Confederate soldiers once used them to pin their uniforms together and survivalists still use them as fish hooks, spear heads, nails, sewing needles and even small game traps. Native Americans used the wood to make bows, and medicines were made from various parts of the plant.

The orangey color of these leaves caught my eye. I think they may have been American hornbeam leaves (Carpinus caroliniana). This tree is also know n as muscle wood, ironwood, hornbeam and blue beech, and younger trees will often hang onto their leaves quite late into the year.

In the fall shortening day length tells most deciduous trees that it’s time to stop growing, so the tree forms a layer of waxy, corky cells at the base of each leaf. This is called an abscission layer, and it slows and finally stops the flow of sap to the leaf. In some trees like oak (Quercus), beech (Fagus), and hornbeam (Carpinus), this abscission layer forms much later, so even though the leaves might freeze dead and turn completely brown they still cling to the branches. Pin oaks (Quercus palustris) don’t form an abscission layer until spring, so their leaves stay on the tree all winter. This retention of dead leaves is known as marcescence. When I start seeing lots of beech leaves blowing around in late winter I get excited, because that means spring isn’t far off.

I think this pile of beech leaves, blown by the wind, was fairly recent.

I see a lot of woodchips around dead and dying trees, almost always left there by woodpeckers. These small bits of wood disappear quickly.

Trees losing their bark isn’t anything strange but there were a lot of animal tracks around this tree and it looked like an animal might have pulled this piece of bark off. Porcupine maybe?

This white pine had lost some of its bark but it wasn’t lying on the ground anywhere near the tree that I could see. Wounds like this are how fungi can get into a tree and start things like heart rot.

I was surprised to see a virgin’s bower vine (Clematis virginiana) on the ground. This vine can climb high enough to make it into the trees occasionally but usually it just drapes itself over shrubs and hangs on tight. It’s more likely to decompose right there on the shrub than to fall on the forest floor. Those long feathery filaments called styles are on its seeds (fruits) so the wind can carry them, but that can’t happen if they’re on the ground.

This switch grass did most certainly not fall from a tree but its delicate beauty caught my eye so I’ve put it here. I hope you enjoy seeing it as much as I did.

Anyone who thinks fallen leaves are dead has never watched them dancing on a windy day. ~Shira Tamir

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Since the last time I did one of these posts it has gotten colder; cold enough to freeze over our ponds and lakes in fact, as this morning scene from Half Moon Pond in Hancock shows. Many ice fishermen and skaters have been enjoying the ice this year. The ice has also been very vocal, and the pinging and twanging sounds I hear daily signal cracking of the ice. If you’ve never heard it the ice can sound eerie, but some people hear it as music. There is a good video with accurate reproduction of these sounds here: https://www.youtube.com/watch?v=chxn2szgEAg
Nature just never ceases to amaze.

Pressure ridges have been building in the ice on the shore of the pond. It’s easy to think of ice as hard and rigid but it can be quite plastic and it moves around a lot.

Here was a window through the ice; a window into spring.

But it will be a while before spring arrives. We still have to get through February which, though it is the shortest month, can sometimes seem like the longest.

Of course cold doesn’t let snow melt so what looks like a lot of snow in this photo is what has built up over the course of two or three storms that have carried only three or four inches. “Nuisance storms” are what they’re called because, though the amount of snowfall is minimal and hardly worth shoveling or plowing, you never know what the next storm will bring so you’d better get out there and clean it up. It might be a nuisance but you feel better about having done it.

When the snow is light and powdery the wind can sculpt it into all kinds of shapes. That’s how these ripples were made.

I wonder if anyone knows what made these marks in the snow?

The marks were made by a pine cone, blown by the wind and rolling through the snow. I see this a lot.

Animals have started digging through the snow to find acorns and other seeds. I’m guessing these dig marks were made by a squirrel. They have a rough time in the extreme below zero cold we’ve seen lately.

Skunk cabbages (Symplocarpus foetidus) are patiently waiting in their swamp for the weather to be right before showing their mottled spathes, but it won’t be long. Once the modified leaves called spathes have unfurled and the flowers on the spadix have produced pollen the shoot you see here will grow and unfurl and become the large green, cabbage like leaves that the plant gets its name from. Skunk cabbage, through a process called thermogenesis, can produce its own heat and melt its way through ice and snow. They are a sure sign that spring has arrived.

I’m seeing lots of blackberries hanging onto their leaves this winter, and I’m always happy to see them. These were a pleasing shade of maroon. To see actual leaves in January is a great gift, in my opinion.

When a sunbeam lights up a single bit of nature in a given area I pay attention, and on this day one fell on a golden birch. Golden sunshine on a golden birch; a gift of gold that warmed my spirit on a cold blue winter day.

Blue is a color I see a lot of in winter. Here the normally white or greenish white stripes on a striped maple trunk (Acer pensylvanicum) have turned blue. Since I’ve only seen this happen in winter I assume that it is the cold that does it. This native tree is also called goosefoot maple due to the shape of its leaves, and moosewood maple because moose eat its leaves. Another name that I haven’t heard much of is snake bark maple. Native Americans are said to have used the wood to make arrows, which would make sense because these trees grow very straight. They also used it medicinally to treat coughs and colds.

My favorite part of the striped maple at this time of year is its pink buds at the tip of orange branches. From this point until they leaf out they will get even more beautiful.

This photo taken previously what those striped maple buds will look like in late April or early May, just before they break and the leaves come out. A tree full of them is very beautiful.

A young striped maple’s bark is smooth and green or greenish brown with long white or whitish green vertical lines. As the tree ages the bark turns reddish-brown with darker vertical lines, as can be seen in this photo. It’s a tree that goes through many very visible changes and I like to watch them over time.

I saw an old river grape vine that was as big around as my arm. The bark on grape vines peels naturally and birds use it for nest building. North America has about 20 native species of wild grape and Native Americans used them all. The fruit is usually too acidic to eat from the vine so the grapes were used for juice and jelly or cooked and used in various recipes. Grapes were also used to dye baskets with a gray violet dye.

There is a disease of grapes called black spot disease, also known as anthracnose of grapes, but this isn’t it. This was like a thin black film on the vine that could be peeled off. I’ve searched grape diseases online for a while now and have found nothing like it. I’d hate to think there was a disease spreading among our wild grapes.

I believe that I do know what these black spots I saw on an oak log are; hypoxylon canker, which is a fungal disease of oaks. It appears as black, dead lesions on limbs, branches, and trunks and can kill the tree by causing white rot of the sapwood. The disease usually affects trees that are under stress or which have been damaged in some way. Signs are smaller leaves which are yellowing, along with a thinning canopy and falling twigs and branches.

I can remember when I was surprised to find a single maple dust lichen (Lecanora thysanophora), the only one I had ever seen, but now I’m seeing them everywhere. I don’t know if they were always there and I didn’t see them or if they are spreading, but I’m always happy to find them. They grow usually on smooth barked trees like beech and young maples. Most that I see are an inch or so across but they can get larger.  I like their stark simplicity.

The white / gray fringe around the outside of a maple dust lichen is called the prothallus and using it is a great way to identify it, because from what I’ve read there isn’t another that has it. A prothallus is defined as a “differently colored border to a crustose lichen where the fungus is actively growing but there are no algal cells.” The brownish field or body of this lichen is considered a sorediate thallus, meaning it has powdery structures called soredia that can fall from the lichen and grow new lichens.

If you see this do not touch it, because this is what a poison ivy vine can look like in winter. Poison ivy can appear as a plant, a shrub, or a vine and if you’re going to spend much time in the woods it’s a good idea to know it well. In the winter a vine like this can help identify the plant because of the many aerial roots that come directly out of its bark. It’s best not to touch it because even in winter it can cause an itchy rash. Other common vines like bittersweet, grape, and the trumpet creeper vine do not have aerial roots. They climb by twining themselves around the tree.

What I believe was a dead banded tussock moth was lying on a windowsill where I work. I was shocked when I saw the detail that my new phone camera captured. I think it has passed the macro test.

“Big deal,” I can hear someone say “it’s just an old leaf.” But to me, in the depths of winter when the world sometimes seems black, brown and white, a beautiful spot of color like this will stop me dead in my tracks. Can you be taken out of yourself by an old witch hazel leaf? Can you see that the beauty that you behold is in its essence, who you are? Can you melt into the gratitude that washes over you from having been given such a gift? Yes you can, and nature will show you how if you will let it.

Piglet noticed that even though he had a Very Small Heart, it could hold a rather large amount of Gratitude. ~A.A. Milne

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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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Last Sunday the weather people said it would be windy and cold with possibilities of snow squalls but I wanted to be in the woods, so I headed for a rail trail in Swanzey that I hadn’t been on since last year sometime. When I left the house it wasn’t bad; 36 degrees F. and cloudy, with a slight breeze. I was hoping the snow squalls wouldn’t happen because they can take you into white out conditions in an instant. When they happen you can’t see very well so I made a plan to just stand under a pine or hemlock tree until it passed. Luckily, I didn’t need a plan.

The trail was icy because we’d had rain all day the day before and then it froze up at night, but someone still had their bike out. You wouldn’t catch me doing that.

Though the trail was iced over the forest along the trail was mostly clear. Pines and hemlocks keep a lot of snow from hitting the ground.

The old whistle post wasn’t covered by forest debris yet. The W stands for whistle and the post is called a whistle post because it marks the spot where the locomotive engineer was to blow the train’s whistle. When there is a crossing very nearby, where the railbed crosses a road, the whistle would have alerted wagon or auto drivers that a train was coming. Some whistle posts were marked – – o -, which meant “two longs and a short” on the whistle. I grew up hearing these whistles (actually horns) daily as the old Boston and Maine diesel freights went by our house.

There are houses not too far from this rail trail and years ago someone planted a privet hedge and let it go. Now it has fruit.

I saw lots of big red stem moss (Pleurozium schreberi) out here. This is a common moss that I often see growing in very large mats, sometimes even overrunning and choking out other mosses. In fact I’ve never seen a moss grow as fast as this one. A few years ago I hardly saw it and now I see it just about everywhere I go. I’ve read that it is native but it seems bent on taking over the earth.

There are lots of small oak trees out here that have been cut again and again by the people who maintain these trails, and this is one of them. It stopped me when I noticed all the various colors in its leaves. Beautiful warm browns, orange, and even pink.

Many of the oak leaves were covered with small spots, which I think were some type of fungus.

One of the oaks had galls on it and a bird had pecked them open to get at the galls inside. Years ago I thought at first it was woodpeckers that did this but I’ve seen blue jays and even chickadees pecking at them.

High up in the branches of many oaks jelly fungi grow on the limbs, and when these limbs fall we get a good chance to see them. I think that the most common of all jelly fungi is this one; the amber jelly (Exidia recisa,) because I see it all the time, especially after a rain. This one always reminds me of jellied cranberry sauce. Jelly fungi dry out when it’s dry and appear as tiny colored flakes that you’d hardly believe could grow as much as they do, but they absorb water like a sponge and can grow to 60 times bigger than they were when dry. Jelly fungi have a shiny side and a kind of matte finish side and their spores are produced on their shiny sides. After a good rain look closely at those fallen limbs, big or small, and you’re sure to find jelly fungi.

One side of this trail is bordered by Yale forest and there is plenty to see there. Yale University has a hands on forestry school in this forest so you can occasionally see it being selectively logged.

It’s easy to see how white tipped moss (Hedwigia ciliata) got its common name. This is a fairly common moss that seems to like to hang from the sides of boulders and ledges. Another name for it is Medusa moss, because when dry its leaves press close to the stem and it takes on a very wiry, string like appearance. Its ball shaped orange spore capsules (sporophytes) are hidden among the leaves on very short stalks, so they’re hard to see. This moss will even grow on asphalt roofs, so it is a perfect choice for green roof projects.

Due to the rain of the day before this particular moss looked happy and beautiful.

Before I knew it I was at the trestle.

There are good views of the river from these old trestles so I’m glad they’re still here.

Many trees topple into the river each year and that’s why you usually only see kayaks or canoes on it when the water is high in spring. I have a feeling that leaning maple will be in the water before too long.

I’ve been out here when the leaves were on the trees so I know they’re silver and red maples, but even if I hadn’t seen the leaves, those buds would tell the story.

I walked on past the trestle and saw a few stones with drill marks but I didn’t see any ledges or boulders that they might have come from. Usually you can tell right where they are from.

It was nice to see green leaves in January. I think the overhanging evergreens must have helped protect these blackberry leaves from the cold.

I saw a few partridgeberry plants with the berries still on them. Usually turkeys and other birds snap them up quickly so they can be hard to find. Partridgeberry is one of the lowest growing evergreen plants on the forest floor, hardly growing more than 3 or 4 inches high. Plants have a vining habit but do not climb. Instead they form dense mats by spreading their trailing stems out to about a foot from the crown. Roots will often form at leaf nodes along the stems and start new plants. The berries will remain on the plant for long periods unless eaten, and can sometimes still be found the following spring.

Partridgeberry flowers come in pairs that are fused at the base. Once pollinated, the ovaries of these flowers will join and form one berry with 8 seeds. Partridgeberry plants can always be easily identified by the two indentations on the berries that show where the flowers were, and these can be seen in the photo above.  Other names for this plant include twinberry and two-eyed berry. The berries are edible, but mostly tasteless.

I saw a stone that was shot full of mica. I’ve had a hard time getting a good shot of mica in the past but this one came out reasonably well.

After a time I saw the river again and I knew it was time to turn around, because from here it is just a short walk to the other end of this leg of the trail where several roads meet. I was glad the snow squalls held off until later in the day.

Forests, lakes, and rivers, clouds and winds, stars and flowers, stupendous glaciers and crystal snowflakes – every form of animate or inanimate existence, leaves its impress upon the soul of man. ~Orison Swett Marden

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