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Posts Tagged ‘Ice Formations’

I should mention, for newer readers, that these “Things I’ve seen” posts are made up of photos I’ve taken of things that didn’t fit into other posts, usually because the other posts were already far too long. Quite often I end up with too many photos to fit in one post but I don’t want to waste them, so here they are.

The pond in this shot shows very well what “rotten ice” looks like. Specks of dirt and bubbles get between the ice crystal bonds and weaken their strength, and when it looks like this, with a dark matte finish, you certainly don’t want to walk on it. Of course this was taken when we had a warm spell. The ice has firmed up now and is covered with about 6 inches of snow.

The pond in the previous photo connects to a swamp by way of a culvert under a road and beavers use it to travel back and forth, stopping long enough to cut some trees on the way.

The beavers have been very active here this year and have cut many young birch trees in this area. They do this every few years and then cut somewhere else, giving the birches time to grow back. I’ve seen these clumps grow back at least twice in the 30 years or so that I’ve paid attention.

You know you’re seeing some strange weather when a tree drips sap in January.

But then it got cold; cold enough to grow ice shelves on the Ashuelot River.

How enticing they are to pig headed little boys who don’t like to listen to their elders. I know that because I was one of those once, and I walked right down the middle of the frozen river. All of the sudden I heard what sounded like rifle shots and I ran as fast as I could for the river bank. When I was able to peel myself from the tree I had a death grip on and take a look, I saw water where I had been walking. It scared me more than anything else ever has I think, and I doubt I’ll ever forget it.

Even the stones were coated with ice.

The Ashuelot was tame on this day and there were no waves to take photos of.

The river had coughed up an ice bauble which caught the sunshine but didn’t melt. I’m always surprised by how clear river ice is. This bauble was so clear I could see a V shaped something frozen inside it.

Jelly fungi are made almost entirely water so of course they were frozen too. This amber example felt like an ice cube rather than an earlobe as they usually do. Freezing doesn’t seem to affect them much, I’ve noticed.

The seed eating birds have been busy picking all the prickly looking coneflower seeds in my yard. They had just gotten started on this one.

And they had just about finished with this one. Odd that these seed heads are hollow.

I don’t know if birds eat the tiny seeds of forked blue curls (Trichostema dichotomum) but the seed pods look almost like a trough that would make them easy to reach. I can’t remember this pretty little annual plant having such hairy parts in life but they certainly do in death.

I thought the color of these dead fern stems (Rachis) was very beautiful on a winter day. I think they might have been hay scented fern (Dennstaedtia punctilobula,) which grow in large colonies and have stems that persist long after the leaves have fallen.

Many things are as beautiful in death as they are in life, especially fungi. I don’t know if I’d go so far as to call this one beautiful but it was certainly interesting.

This isn’t a very good photo but it does help illustrate how strange our weather has been, because you don’t see too many flies flying around in January in New Hampshire. Last Tuesday it was -13 degrees F. and everything was frozen solid. By Thursday it was 50 degrees; warm enough apparently to awaken this fly. It was also warm enough to cause an unusual snow slide in Claremont, which is north of here. A large amount of snow suddenly slid down a hillside and slammed into a house, partially destroying it. It also pushed a parked truck about 75 feet.

It’s easy to see how the horse hoof fungus (Fomes fomentarius) got its name. It’s also easy to see how this fungus grows, because its spore bearing surface always points toward the ground. If you see a fallen log with this fungus on it and its spore bearing surface doesn’t point toward the ground you know that it grew while the tree was standing. If it does point toward the ground it grew after the tree fell. This bracket fungus produces spores at all times of year but through spring and summer studies have shown that it can produce as many as 800 million in a single hour; fine as dust and nearly impossible to see. The fungus is also known for its ability to stop bleeding and was recommended for that purpose by Hippocrates, who is considered the father of medicine.

Lemon drop fungi (Bisporella citrina) start life as a tiny bright yellow disc and look as if they lie flat on the log, but they actually hover just above the surface on a short stalk. As they age each disc becomes cup shaped. The Citrina part of the scientific name comes from the Latin Citrin, which means “lemon yellow.” They are very small, so you’ll need a loupe or a macro lens to see them properly.

Longtime readers of this blog know that I like looking at buds at this time of year and some of my favorite buds are found on the red elderberry (Sambucus racemosa.) They’re about medium size as buds go, and nice and chubby. I love their beautiful purple and green color combination.

I think my favorite thing this time around is this river ice that caught and magnified the blue of the sky. I thought it was quite beautiful, but blue is my favorite color so that could have something to do with it.

The appearance of things changes according to the emotions; and thus we see magic and beauty in them, while the magic and beauty are really in ourselves. ~Kahlil Gibran

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Robin Hood Park is a 110-acre park located in the northeastern corner of Keene that I visit often at all times of year, but especially in summer to see all of the amazing fungi and slime molds that grow there. In 1889 George A. Wheelock sold a piece of land known as the Children’s Wood to the City of Keene for a total of one dollar. This area was eventually combined with an additional parcel of land purchased from Wheelock, known as Robin Hood Forest, to form Robin Hood Park. This park has been enjoyed by children of all ages ever since. I decided to go there last Saturday because I couldn’t remember the last time I had been there.

The small pond in the park has drawn ice skaters for a very long time, but this year the unusual warmth has kept people off the ice. This is where I learned how to ice skate 50+ years ago.

There are various small streams and rivulets that feed into the pond. Even though it was only 22 degrees F. on this day none of them had frozen over but they were trying, as this one shows.

There were lots of bubbles in what ice there was.

The spot where the little stream enters the pond showed just how thin the ice was.

But still, even with all the warnings both natural and man-made, someone had shoveled off a large rectangle to skate in. We humans can be very stupid at times. Note how wet the snow is where the water is coming up through the crack in the ice.

I got away from the pond and followed the trail that leads around it. There are many interesting things along this trail and I see things I’ve never seen almost every time I come.

Unfortunately there was nothing new about the thick ice on parts of the trail. There is a lot of groundwater here and ice like this is common in winter so I wore my new micro spikes. With them on I walked right over this ice and didn’t slip or slide one bit. It’s amazing how they grip; you feel like you couldn’t slip if you wanted to.

One of the things I saw on this day that I’ve never seen before is a liverwort called the Bifid crestwort (Lophocolea bidentata.) It grew on a log and at first I thought it was a moss.

But I’ve never seen a moss that looked like this and I suspected right off that it must be some type of liverwort. It is a leafy liverwort and each leaf is flattened with two notches at its tip (Bilobed.) Each lobe is drawn out to a long, narrow point. As you move up the stem the leading edge of each leaf is tucked behind the trailing edge of the leaf ahead of it. Both of these features help with identification as does the pale yellow green color. What I didn’t know at the time I saw it is that the plant is very aromatic, so the next time I see it I’ll have to smell it.

There was no question that this was a moss. Broom moss (Dicranum scoparium) gets its name from the way its curly tipped leaves look like they have all been swept to one side. In fact the scoparium part of the scientific name is Latin for broom. It prefers dry shaded places and won’t tolerate wet feet. Florists call it mood moss but I’m not sure why.

Mosses can change color in the cold and so can lichens. In the summer the blue gray lichens on this stone will become ashen gray and all but disappear into the color of the stone. It’s something I’ve noticed happening for years but I’ve never been able to identify the chameleon like lichen.

This buttressed tree root reminded me of a beautiful yellow slime mold I saw here one day a few years ago. Buttressed tree roots usually grow on all sides of the tree but this huge old oak has just the one. Roots that grow like this are said to grow because of nutrient poor, shallow soil but if that were true then it seems like all of the trees in this forest would have them. They are usually found in rain forests on very tall trees.

Something I’ve never been able to explain is the zig zag scar on this tree. I’ve shown it here before and blog readers have kicked around several ideas including lightning, but none seem to really fit.

The scar is deep and starts about 5 feet up the trunk from the soil line. If it were a lightning scar I would think that it would travel from the top of the tree into the soil. I happened upon a large white pine tree once that had been hit by lightning very recently and it had a perfectly straight scar from its top, down a root, and into the soil. The bark had been blown off all the way along it.

I’ve seen some strange things in the woods and this is one of them. Someone put a chain around this tree for no apparent reason. What will happen is the tree will grow around it and over time simply absorb it. It will become a tree cutters nightmare; one of those thing you hope you never run into with a chainsaw.

This granite stone has a spear of either quartz or feldspar in it. I think, if I remember my geology correctly, that it would be called an intrusion or vein. Granite itself is considered an intrusive igneous rock.

Turkey tail fungi (Trametes versicolor) are common enough but you don’t often find them growing on a standing tree as these were. There were many hundreds of them all around the tree.

Some of the turkey tails were quite colorful with lots of orange and lavender bands.

Other turkey tails on the same tree were much less colorful and this is interesting. For years I’ve tried to find out what determines the color of these fungi and I assumed it must be the wood itself, but these examples with widely varying colors were all growing on the same wood, so that can’t be it. These are in fact wood eaters which decompose wood so it can be returned to the forest soil to be used again by a new generation of trees. Life is a circle and not a single molecule is lost or wasted.

When I was a boy I found a book in the attic called “Nibbles and Bobtail.” It was all about animals of the forest acting like people, and their escapades. The animals lived in stone houses with thatched roofs and had fields bordered by stone walls. I was in my drawing phase then and I was interested in illustration, but this book bothered me because everything made of stone was colored. There were red stones, blue stones, orange, yellow, purple stones, etc. I thought well, it’s obvious this person has never seen a stone wall; everyone knows they’re gray. But it was I who didn’t know what I was talking about because instead of seeing I was just looking, and it took several years for me to finally see that stone walls could indeed be very colorful, as this one shows. Not only are the stones colorful but the lichens on them are as well. The orange in this photo is caused by the sidewalk firedot lichen (Caloplaca feracissima.)

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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My small climb up along 40 foot falls that I wrote about in my last post inspired me to try something bigger, so last Sunday I decided to climb Hewe’s Hill in Swanzey. A diagnosis of COPD took the wind out of my sails for a while and I wondered if I’d ever climb again, but the medicines they have given me seem to work well and I was able to climb on this day at least as well as I could last year. I started by walking through this frosty meadow.

At about 20 degrees F. it was cool but there was little snow to be seen, so I hoped for a trail without ice. This trail is well traveled and ice is always a problem when constant foot traffic packs down snow and turns it into ice.

Thankfully the trail was ice free, probably because the hemlock boughs overhead have kept a lot of the snow from falling on it. We’ve also had rain and warm temps and I’m sure that helped. I was glad to see it, because I’ve been here when the ice was so bad here I had to leave the trail and go into the woods to make it up the hill.

I think it was about 10 years ago when this hemlock (Tsuga canadensis) was wounded, and I think that because I counted the rings on the scar. I’ve read that hemlock is the only tree that heals scars with growth rings that can be counted.

I also saw a large number of hemlock trees with this yellow crust fungus on them; more than I’ve ever seen. I believe it is the conifer parchment fungus (Stereum sanguinolentum,) which is also called the bleeding parchment because of the red juice they exude when they’re injured. The examples I saw were very dry and thin, almost as if they were part of the bark, and though I tried to scratch one with my fingernail it remained undamaged. Conifer parchment fungus causes brown heart rot, which is a reddish brown discoloration in the wood of conifers. This tree and many others I saw won’t be with us much longer, I’m afraid.

More ice needles than I’ve ever seen in one place grew all along the center of the trail, meaning the soil was saturated. Groundwater at the soil surface is one of the requirements for ice needle growth, and the other is a below freezing temperature right at the very surface of the soil while the soil and groundwater remain thawed. Hydrostatic pressure forces super cooled groundwater out of the soil where it freezes instantly into a needle shape. As more water is forced out of the soil the process is repeated over and over, and each needle grows in length because of more water freezing at its base. Each needle is hexagonal and several will often freeze together into ribbon like bands like those seen here. As they grow they sometimes force the forest floor to heave up, which can be seen happening here.

There are many small holes in the ground made by chipmunks, snakes, and other animals, and these holes often grow hoar frost around their openings. This frost forms when the warm moist breath of the earth meets the cold air at the surface.

The trail gets darker in spots because of overhanging evergreens but on this day it clouded over and made it seem even darker.

I saw some colorful bracket fungi growing in the crack of a tree but I’m not sure what they were. I am sure that they were frozen solid, whatever they were.

I couldn’t account for the beautiful colors of this fallen limb, and I still can’t even guess what would have caused it except weather and age.

A blue jay lost a feather at some point, but on this day the woods were totally silent with no bird songs and no chatter from chipmunks or squirrels. It seemed very strange to have it so quiet.

The steepest part of the trail is near the summit so I knew I was almost there at this point. I was huffing and puffing but no more so than last year or the year before so that was a pleasant surprise. I do know that nature can heal because I’ve experienced it but I don’t know to what extent that healing can happen. I think maybe the only thing that is holding me back is me, but I’m keeping an open mind and believing, and will be very grateful each time I reach a summit.

You don’t realize how much water travels through the soil under our feet until winter. There really is an incredible amount of water moving about in this area, even on our hills.

My daughter and son in law were with me on this climb and all of us tried to move the 40 ton glacial erratic named Tippin Rock, but it wouldn’t budge. I think it was frozen right to the bedrock it sits on. I was a little disappointed because I wanted them to be able to see it move. For new readers, this boulder rocks back and forth just like a baby cradle when you push on it in the right spot, but apparently not in winter.

The big stone has quite a crack in it and someday it might be two stones, which would be too bad. It is a local legend.

The sun had gone, the sky was milk and the views were poor, but since the view isn’t why I climb it was little more than a passing annoyance.

One thing the views from here always show though, are the endless miles of unbroken forest stretching out in all directions. When you stand in such a place you can’t help but wonder, if it was 1760 and you stood here with only an axe head and a gun, what would you have done? It must have been just a bit overwhelming.

I’ve had a great fear of heights since I fell out of a tree and fractured my spine when I was young  so this is as close as I dared to get to the cliff edge. I wanted to show you what a forest looked like from above, but this is the best I could do. You can believe me when I say that this is a drop you would never survive.

There are some huge granite outcrops up here. That tree is a fully grown white pine.

I saw lots of amazing things up to this point but the main reason I chose this hill to climb was so I could visit my friends the toadskin lichens (Lasallia papulosa.) Though I expected them to be very dry from lack of rain or snow a few surprised me by being deep, healthy green. This is their natural color when they’ve had plenty of water and are happy. These lichens attach themselves to stones at a single point that resembles a belly button, and that means they are umbilicate lichens. I always feel as if I’m looking deep into infinity when I look at a toadskin lichen and I may be; there are many who believe that lichens are virtually indestructible and therefore immortal.

Though I doubt toadskin lichens like drying out I kind of like the way they look in their dry, ashen state. They are much like a potato chip when dry and they’ll break almost as easily so I only touch them when they’re green and pliable.

These toadskin lichens were under a good two or three inches of ice and that ice acted like a magnifying glass. Those black spots on the upper one are the lichen’s apothecia where its spores are produced, and without ice magnifying them they’re about the size of the head of a common pin. It’s kind of amazing to see them so big in a photo.

Only in the woods was all at rest for me, my soul became still and full of power. ~Knut Hamsun

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We’ve seen some unusual below zero F. cold lately and when it gets cold like this my thoughts usually turn to a deep cut rail trail up in Westmoreland that ice climbers call the icebox. The groundwater constantly seeping from thousands of cracks in the stone walls of the manmade canyon freezes into ice columns that can easily reach the size of trees. It can be very beautiful but since it is only November I wasn’t sure what I’d find. Though I doubted there would be much ice to see, last Saturday I made the drive to Westmoreland to find out.

There was some impressive ice to be seen but nothing like it will be in January.

There are a lot of minerals in the groundwater that seeps through the stone and they are the only thing I can think of that would color ice like this.

I’ve seen orange, green, blue, red, tan, brown and even black ice here.

The giant ice columns are like a magnet for ice climbers and members of the New Hampshire branch of the Appalachian Mountain Club come here to train beginning climbers. I was surprised to see some of them here on this day since it is so early in the season.

This should give you an idea of the scale of the place. Though the ice might look impressive it is much less so than it will be in a couple of months. This climber said she was a beginner but she had climbed just about as far up as she could. The ledges in this spot I’d guess are about 50 feet high. Though it was cold at about 40 degrees this day I’ve read that the ideal conditions for climbing happen at between 20 and 35 degrees, because those temperatures produce the just right “plastic” ice; not cold enough to shatter and not warm enough to melt. Ice climbers swing sharp tools called picks into the ice and embed them in it so they can hang onto them as they climb, and I would guess that the last thing they want to see is shattering ice. Since the temperature in the canyon is always colder than the surrounding countryside it must have been just about perfect for plastic ice on this day.

This view looks back the way we came in. It can be very cold in here because the sunlight rarely seems to reach the canyon floor in winter. There is almost always a breeze blowing through the canyon as well, even when there is no breeze outside. It’s as if it makes its own wind.

The railroad engineers used a lot of the stone they blasted out of the canyon to build massive retaining walls along the parts of the trail outside of the canyon. They are some of the best examples of stone wall building that I know of and you won’t find a teaspoon of mortar in any of these walls. Note how the wall leans back into the hillside at about a 10 degree angle, as any good retaining wall should. I’d bet next week’s paycheck that a bed of crushed stone or gravel extends out at least two or three feet from the back of the wall into the hillside. This is for drainage so wet soil doesn’t freeze behind the wall and heave it apart. You want the back of the wall as dry as possible.

I like to see how the ice forms according to the conditions. This little grotto scene looked almost other worldly.

This ice looked like a necklace made of clear crystal, all formed by drip after drip of water.

In places the ice was rotten, and you can tell that by its matte gray, opaque “sick” look and the dull thud it makes when you tap it. Ice becomes rotten when air  and / or dirt get in between the grains of ice and it becomes honeycombed and loses its strength.

In some places where the sun reached the walls of the cut ice had been falling, and in fact I saw (and heard) some  fall while I was here.

I thought how, if I was a teenager once again, I’d find a way to slide down this giant ice slide.

I have a feeling that it’s going to be a good year for ice formations even though the forecast is for rain and above freezing temps this week.

Drainage ditches along the railbed have been doing their job of directing all of this water out of the canyon for around 150 years, but heavy rain overwhelmed them last summer and washed away parts of the railbed. It’s a hard thing to see this place being so severely damaged but there is only so much the snowmobile club volunteers can do, I suppose. One day instead of a railbed here it might be a stream.

In places the stone is stained by years of mineral seepage.

In other places the colors on the walls come from living things, like this algae, but I don’t think they color the ice because they don’t grow where a lot of ice accumulates. This is actually a green algae called Trentepohlia aurea but the same pigment that colors carrots orange makes green algae orange as well. It’s also very hairy, but I couldn’t get close enough to show you.

Colorful foam gathered on one of the drainage ditches in what I thought were beautiful swirling patterns. What caused it to appear and what colored it, I don’t know.

I didn’t have my high rubber boots with me on this trip so I couldn’t get close enough to the canyon walls to get close shots of the algae or the great scented liverworts (Conocephalum conicum) seen here. This beautiful, reptilian liverwort gets its common name from its fresh, clean scent. It will only grow near water that is very clean and it grows here on the  canyon walls just above the drainage ditches. Groundwater constantly splashes them and keeps them wet in warm months. In winter they are often encased in ice, which has just started happening to the plants in this shot.

We’re having some wet heavy snows this month but the old lineman’s shack still somehow stands, even though people have been pulling it apart for as long as I’ve known about it. It just goes to show how the railroad built things to last. Their carpenters were as good as their stone masons. I hope it’s still standing a month from now when I come back to see how the ice has grown.

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

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Quite often I get an irresistible urge to be in the woods and, since I’m lucky enough to be able to find woods in any direction I travel, getting there is no work at all. The thought hit me the other day that I hadn’t been to Goose Pond in Keene since last year, so that’s where I went last Sunday. I also wanted to see how deep the snow was in the woods and since this is a five hundred acre wilderness area I would certainly be able to see plenty of woods. As the above photo of the trail to the pond shows, there was no snow in this area.  Odd since Goose Pond isn’t that far from Beaver Brook, where I saw plenty of snow in the woods just the day before.

The pond was still mostly frozen over. It’s interesting how ponds and lakes start melting at the shore and work toward the middle, and rivers start in the middle and work toward the shore.

Goose Pond was called Crystal Lake and / or Sylvan Lake in the early 1900s. The pond was artificially enlarged to 42 acres in 1865 so the town of Keene would have a water supply to fight fires with. Wooden pipe fed 48 hydrants by 1869 but the town stopped using the pond as a water supply in the 1930s, and in 1984 it was designated a wilderness area. The vast forest tract surrounding the pond has been left virtually untouched since the mid-1800s. The deciduous trees over on the left shoreline are red maples. You can just see some red in the branches from the opening flowers.

Even in the winter the trail darkens quickly due to all of the pines and hemlocks.

There are stone walls here and there along the trail around the pond. They tell the history of the place. It’s hard to believe that much of this land was cleared for sheep pasture by the early 1800s, but it was. These walls have most likely been here for over 200 years.

I’m reading the book The Hidden Life of Trees and in it author Peter Wohlleben speaks of how much strain a tree that is bent like the one in the above photo is under. As he explains it a curved trunk has trouble simply standing upright because “The enormous weight of the crown isn’t evenly divided over the diameter of the trunk but weighs more heavily on the wood on one side.” He also explains that “Evenly formed trees absorb the shock of buffeting forces, using their shape to direct and divide these forces evenly throughout their structure.” If you are interested at all in trees, this is the book for you.

I saw lots of trailing arbutus (Epigaea repens) along the trail. This creeping evergreen is also called Mayflower, though it often blooms earlier. It was one of my grandmother’s favorite flowers.

Some of the trailing arbutus plants were well budded. These small white flowers are extremely fragrant and were once collected nearly into oblivion for nosegays. It is one of those plants that has a close relationship with fungal hyphae in the soil and will not grow unless the fungus is present, so digging it up to transplant somewhere else is a waste of time. It’s also illegal in some areas.

There are many streams flowing down off the surrounding hills to the pond and in two spots there are bridges, but in many places you have to cross by hopping from stone to stone or simply walking through the water. I always wear good water proof hiking boots when I come here. On this day I saw some college age people going down the trail wearing bright white sneakers. I can guarantee that they weren’t white when they came out of the woods, and they probably weren’t dry either.

This bridge was chained to a nearby tree, not against theft but flooding. There has been severe flooding here in the past. It would be an awful lot of work hand carrying enough lumber to build a bridge all the way out here so I don’t blame them for not wanting to have it washed away and smashed on the rocks.

I could have sat here all day just listening to the chuckling and giggling of the stream and the joyous, excited birdsong but it wasn’t warm on this day and there was a stiff wind coming off that ice, so I had to move on after too short a time.

I saw the pine tree that was hit by lightning last year. The bolt blew the bark right off the trunk in strips, and pieces of the strips still lay by its roots. It also followed a large root right into the ground, leaving the same trace on it.

A birch polypore (Formitopsis betulina) was coated with ice. Someday I’m going to try drying one of these mushrooms and sharpening a knife with it because another name for it is the razor strop fungus. Even more useful than its ability to sharpen a knife though, is its antiseptic, antibacterial and anti-inflammatory properties. It contains betulinic acid, which is a compound that has shown to also promote the death of cancer cells. It has been used medicinally for thousands of years.

Soon the island will be surrounded by water again instead of ice. I’d love to be able to explore it to find out what kind of plants grow there. I’m guessing that they aren’t much different than those that grow here on shore, but you never know.

Great long ice crystals grew in the cold night and were melting now. That’s how this entire winter has been; cold enough to snow one day and then warm enough to melt it all over the next few days. Then comes another storm, but that cycle seems to have finally been broken now.

There are many side trails here and some are very easy to get onto without realizing it, but it would still be hard to get lost if you pay attention and stay on the trail that circles the pond. If the pond is on your right when you start it should be on your right all the way along the trail until it ends, because you have just walked in a circle. Maybe it took you a while to do it but it’s still just a big circle. Even so I have met people here that seemed to have no idea where they were or which way to go. It just goes to show that what seems simple to some of us might not be so simple to others. I’ve been lost in the woods before too, and it can be unsettling, to say the least.

I knew right off what the small black lumps all over this beech stump were.

Annulohypoxylon cohaerens fungus forms hard black lumps on beech bark. The fruiting bodies seen here are “cushion like round or flask shaped masses of fungal tissue with nipple or pustule shaped pores.” Each body is very small; less than half the diameter of a pea. They usually grow on fallen beech logs but these were on a standing stump. It originally took me three years to identify them.

The trail had ice on it here and there but this is mostly level ground so it wasn’t bad. Next winter I’ll have micro spikes, hoping all the while that I don’t need them.

I saw the unnatural stone that lives in the middle of the trail, toward the end if you go clockwise around the pond. Of course I can’t prove it isn’t natural but I’ve worked with a lot of stone and I’ve never seen such a perfect 90 degree angle and such smooth faces on a natural stone. I can’t imagine how it got way out here or why.

This is a special place for several reasons. First is because it’s the only place I know of where you can actually get a photo of the woods while you are in them. An old pine fell and opened a hole in the canopy and that lets in enough light for a shot of something I am rarely able to get on film. Taking a photo of a forest while you’re in it is a lot harder than you might think, because of all the trees. Another reason this spot is special is because the only example of a northern club spur orchid I know of grows here. I found it about 4 years ago and hope to see it bloom again in July. The final reason this place is special to me is because it’s so beautiful and peaceful here. If you feel the need to just sit and “soak” in the woods this is the place to do it. I hope you have a place like it.

It is very important to go out alone, to sit under a tree—not with a book, not with a companion, but by yourself—and observe the falling of a leaf, hear the lapping of the water, the fishermen’s song, watch the flight of a bird, and of your own thoughts as they chase each other across the space of your mind. If you are able to be alone and watch these things, then you will discover extraordinary riches which no government can tax, no human agency can corrupt, and which can never be destroyed. ~ Jiddu Krishnamurti

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The word “Ashuelot” is pronounced Ash-will-ot if you’re from this area or Ash-wee-lot if you’re from away. The word is a Native American one meaning “collection of many waters.” For years I read that the word meant “the place between” but that didn’t make a lot of sense. “A collection of many waters” makes much more sense because that’s exactly what the river is. Wandering the banks of the Ashuelot is something I’ve done since I was too young to even retain the memory of doing so, and I do it often. On this day I was happy to see that the ice shelves had melted and the sandy / stony shoreline was back. The river has been very high for over a month and it’s good to see it finally ready to absorb the next big rain storm, which should come sometime in April unless that month has gone haywire too.

I stopped to admire some ice formations and take some photos so I wouldn’t have to try and explain how cold it was. Actually it wasn’t bad in the sunshine when the wind wasn’t blowing but it was blowing almost constantly along this stretch of river, so it was a day to be wrapped up like you would be in January.

The ice had formed discs on every twig that was in the water and this was remarkable only because the ever splashing water usually forms icy tear drop shapes on the twigs. In fact I don’t think I’ve ever seen these disc shapes here before.

Here is what I’m more used to seeing. Ice baubles I call them, but there weren’t many to be seen. They happen because of the way the current makes the water constantly rise and fall along the shoreline, so one second the twig is in the cold air and the next it’s under water. The runoff freezes and layer by layer and an ice bauble is made. It reminds me of dipping a wick in melted wax over and over again to make a candle.

This is where I come to practice my wave catching skills but there were none to catch on this day because the water was too low. It has to be at just the right height for good waves to form. Too low or too high and there are no waves. I took some photos anyway though, because the water looked like satin as it poured over the unseen stones that cause the waves.

Oak leaves huddled together as if to warm each other in the chilly breeze. I love the warm, orangey brown color of last year’s oak leaves, but I won’t be sorry to see them finally fall.

The oak buds seemed to be swelling a bit but it was hard to know. Oaks are one of our latest trees to leaf out in spring.

I saw a chubby little bird in a bush which looked like it was hoping I wouldn’t see it. I think it was a dark eyed junco but I’m not 100% sure of that. I see these small dark colored birds feeding in flocks along roadsides where the snow has melted away from the pavement , exposing the soil and grass. I’ve read that dark eyed juncos come here as winter sets in and leave in spring, so they must like the cold. There are said to be about 630 million of them from Alaska to Mexico, and all across the U.S. from coast to coast.

I wondered if the juncos were eating the sumac seeds so I had to look it up. Apparently they eat smaller seeds like those of grasses, lamb’s quarters and the like, and in warmer months they also eat insects. Robins, blue jays, grosbeaks, ruffed grouse, cardinals and other larger birds eat the sumac fruit, but it never disappears here until spring.

I went to visit the Ashuelot Falls on West Street in Keene. I used to fish here quite often when I was a boy but back then the river wasn’t as clean as it is now so I didn’t catch that many fish. An occasional perch or dace was about it but that was fine, because my being here really didn’t have much to do with catching fish anyway. I’d let a forked stick hold my pole while I explored the river bank. Now they catch trout here, I’m told.

I wouldn’t have been surprised to see ice pancakes in January but this was March, so I was surprised.

Ice pancakes form when the river foam stirred up by falls or other turbulence comes together into a misshapen lump. As the current moves the misshapen lumps they bump and jostle each other until all the rough edges are shaved off and they’ve become round like a pancake. Then they begin to freeze and their edges build up into rims.

Here is what an ice pancake looks like when it starts life, before its friends smooth out all those angles.

Canada geese waded in the shallows. More and more of them are returning to nest and raise their young in the reed beds along the river. There is always one lookout standing tall while the others preen, sleep, or eat and they count on their lookout to sound the alarm. I wondered if most of these birds even knew I was there.

My pointing the camera at them was too much for one or two of the geese and they swam off quickly.

Normally a river gets deeper as you go toward its middle but a sandbar has grown here, so the water in the middle is quite shallow. Not good for navigation but the geese know they can stand here rather than swim and they take advantage of being able to rest while still in the water. The shading from dark to lighter brown in this photo shows where the sandbar is.

A maple tree had been pecked full of holes by an unseen woodpecker.

I didn’t have to see this woodpecker to know it was a pileated woodpecker, which is our biggest. Its holes are large and almost always rectangular. All of the holes in the previous photo would fit inside this one with plenty of room to spare.

The hole in this old red maple (Acer rubrum) was the biggest of all but I doubt very much that it was made by a bird or an animal. I think the river has washed the soil out from under it.

The hole was plenty big and roomy enough for me to comfortably sit in, almost like a hobbit.

I knew the old tree was a red maple by its buds. The bud scales in many of these examples had pulled back to reveal the many pinkish flowers inside. Those over on the left were even protruding a bit from the bud, but it was still too early to tell if they were male or female blossoms. It’s a good thing they hadn’t fully opened because the temperature fell to zero degrees on this night. The cold isn’t going to leave quickly this year but today is the first full day of spring, even if it doesn’t seem it.

I was born upon thy bank, river,
My blood flows in thy stream,
And thou meanderest forever,
At the bottom of my dream.
~Henry David Thoreau

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It was a nice warm sunny Saturday when I set out for the Beaver Brook Natural Area in Keene and the weather people said it would be sunny all day, but as soon as I got there clouds moved in and decided to stay for a while. Actually the clouds stayed the entire time I was there and the sun didn’t show itself again until I left.

This was the only blue sky I saw the entire time I was there.

But the trail was well packed down and not really as icy as it looks here.

Beaver Brook was roaring. In the summer it giggles and chuckles along beside you but in the winter it roars, and that’s all you hear. Unless it’s covered by ice; when it’s iced over it whispers and is quieter than at any other time.

The brook hasn’t been completely iced over this winter that I’ve seen, but huge ice shelves had formed here and there. You can see how there is nothing under the shelf but air, so it walking out on it would be a foolish thing to do.

The ice shelves had teeth.

I have a lot of old friends living here along the brook, like this smoky eye boulder lichen (Porpidia albocaerulescens.) I see this lichen just about everywhere I go but nowhere else are its fruiting bodies (apothecia) so blue or its body (thallus) so golden. The gold color comes from the minerals in the stone I think, and the blue color comes from the way the light falls on the waxy coating that covers the apothecia. Whatever it is that causes the colors in this particular place, this lichen is one of the most beautiful I’ve seen and this is the only place I’ve ever seen it look like this.

I also stopped to visit the only example I’ve ever seen of stair step moss (Hylocomium splendens.) This is a boreal moss that grows quite far north into the arctic and I’ve seen it here covered with ice, but it isn’t as delicate as it looks and it always comes through winter unscathed. When it’s dry it has a shiny sheen and that’s most likely why another common name for it is glittering wood moss. New growth “steps up” off the midrib of the previous year’s growth and that’s where the “stair step” name comes from. It’s a beautiful moss and I wish I’d see more of it.

The rose moss (Rhodobryum roseum) came through winter looking fine and I was glad of that because this is the only example of it I know of. I did find another small patch on a stone in Swanzey once, but I can’t remember where. It’s nice to know there are more of them out there but I’d still have to call this moss rare. I love its little aspirin size rosettes of leaves that someone thought looked like roses. They look more like dahlias or chrysanthemums to me, but they’re beautiful no matter what we choose to call them.

There were some impressive ice formations on the ledges and I was surprised, because they don’t usually grow so big here. With the up and down weather we’ve had this year though, I probably shouldn’t be surprised by anything weather related.

Last time I came here the brook was flooding in places and it was a downright scary thing to see. The water mark on the far embankment showed just how high the water had been, and I’d guess that it was a good 6 feet higher than it was on this day. I met an old timer up here one day who told me that he had once seen the water over the old road. That’s something I hope I never see.

In places the snow had melted and revealed that there really wasn’t that much covering the road. Since we’re supposed to have warm days all week there’s a good chance that the road will be snow free this weekend.

Where the snow had melted you could see part of the old double yellow no passing lines.

Off on the side of the road a branch had fallen, and it was covered by what I thought at first was milk white, toothed polypores.

But the spore bearing surface of this fungus was more maze like than toothed, so that had me confused until I got home and was able to see the photos. After some searching I came up with what I think is a crust fungus called the common mazegill polypore (Datronia mollis.) It may be common in some places but I think this is only the second time I’ve seen it.

A little further up the road I found another fallen branch that was covered with inch in diameter, colorful crust fungi which I think were young wrinkled crust fungi (Phlebia radiata.)  These are winter mushrooms and that’s the only time I ever see them. They aren’t common; I’ve only found them three or four times. As they age the center of the fungus becomes very wrinkled, and that’s where their common name comes from.

There isn’t anything odd or rare about tinder fungi (Fomes fomentarius,) but a closer look at this one revealed something that was both odd and rare, at least in my experience.

There were squirrel teeth marks ( I think) all over one of the colored bands on it. Recently I’ve seen the same thing on a few lichens and have found that squirrels do indeed eat lichens, and I’ve seen them eating mushrooms but I’ve never seen them do this. It made me wonder if it was algae they were after, because algae grow on both lichens and fungi. I can’t imagine what else they’d get out of scraping their teeth over this fungus unless it was to keep their ever growing teeth in check. Tinder fungi are very tough and woody, so maybe the animal was simply trying to wear down its teeth.

Another fallen branch displayed what I thought from a distance were shield lichens but once I got closer I realized they weren’t anything I had ever seen.

They were obviously not lichens at all, but instead some type of hairy fungi.

They grew like bracket fungi and their spore bearing surfaces were maze like and faced outward. Each flower like cluster like the one shown above couldn’t have been more than three inches across, so they weren’t very big. They were pliable and rubbery to the touch, and felt much like an ear lobe. They look very pink to me but my color finding software tells me they’re mostly tan with some peach puff and dark salmon here and there.

They didn’t have to be big to be beautiful and I thought they were very beautiful things, but after looking through 4 mushroom books and spending several hours online I can’t find anything that even looks close to them, so they’ll have to remain a mystery for now. Maybe one of you knows their name. If so I’d love to hear from you.

A path well-traveled may still yield secrets that only one person may discover. ~Anthony T. Hincks

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