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Posts Tagged ‘Westmoreland Rail Trail’

Westmoreland lies north of Keene and the soil there is lime rich in certain places which means that you can see plants there that won’t grow in the more acidic soil of Keene, so last Sunday off I went down one of my favorite rail trails. I used to try to ride my bike out here but the gravel of the trail is very soft and I had such a time getting through it that I ended up walking the bike for much of the way anyhow, so now I just walk it. Though it was cloudy it was a great day for hiking with all of the beautiful spring green and singing birds.

This maple was that green that only happens in spring; kind of a yellow green, I guess you’d call it.

Though it doesn’t mind acidic soil red elderberry (Sambucus racemosa) does well here in the more alkaline soil.  There were several plants which were flowering well with panicles of whitish flowers growing from the axils of the upper leaves.

Each greenish white flower is about 1/8″ across. They have 5 petals (petaloid lobes) that curve backwards sharply. The flower’s 5 stamens have white filaments and are tipped with pale yellow anthers. There is also a pistil with 3 small stigmata. If pollinated each flower will become a small bright red berry.  Though the plant is said to be toxic many Native American tribes steamed, dried and ate the berries. They are said to be very bitter unless prepared correctly.

There are plenty of reminders of exactly where you are out here, like this old signal base.

When the rails were torn up the railroad left all the ties stacked up along the railbed. People came and took what they wanted but there are still plenty to be seen, slowly rotting into the soil.

The boulder in the previous photo had a golf ball size hole in it, probably made by a steam drill so it could be blasted apart when they were laying the rails. For some reason they decided not to blast it.

Almost there; the dark circle in the distance marks the end of one leg of this journey.

Wild sarsaparilla (Aralia nudicaulis) wears bronze for its new spring coat, but its leaves will green up quickly. Wild sarsaparilla grows all through our forests and is a common sight. The plant sets flower buds quickly just as its leaflets have unfurled, and often before they’ve changed from their early deep bronze to green. In botanical terms the “leaves” are actually one leaf with a whorl of 3 compound leaves, which have groups of 3-7 leaflets. People sometimes confuse the plant with poison ivy before the flowers appear because of the “leaves of three” as in leaves of three, let them be. One easy way to tell the difference is by looking for a woody stem; poison ivy has one but this plant does not.

Wild sarsaparilla always starts out with its three compound leaves held vertically and clasping at the very top.

I was surprised to see logging going on in this part of the forest, but not completely. There are many hardwoods here like beech, oak and maple and very few conifers. Hardwood always brings more at the mill.

A logging road had to be built to get to the section of forest to be logged, so huge boulders were bulldozed into a place that needed a retaining wall. These stones are new, meaning they were just dug or cut. You can tell by how clean they are, and by their color. Most stones will turn gray in just a few years.

Here we are at the man made canyon that showed as a dark circle in a previous photo. There are a few of these along this section of trail, and they were all blasted out of the bedrock almost 150 years ago for the Cheshire Railroad.

I don’t know what it is that draws them here, but many interesting plants not easily seen in other places grow on these ledges.

Purple or red trillium (Trillium erectum) grows here in fair numbers. Each flower averages about as big as a quarter, or about an inch across.

Trilliums are all about the number three. Even the name trillium comes from the Latin tres, meaning three. On the purple trillium the three green sepals just are behind the three red petals. Once they open the flowers often nod under the three leaves (actually bracts,) and are mostly hidden from view for a short time before finally standing erect above the leaves. Inside the flower are six stamens and three stigmas. If flies pollinate the flower a three chambered, red fruit will grow.

False Solomon’s seal grows well here. Though it’s too early for their June bloom time the plants were budded. In about three weeks they should have small white, star shaped flowers in a branching cluster (raceme) at the end of their stems. The blossoms will give way to small but beautiful reddish and tan speckled berries that provide food for many birds and other wildlife.

The wild columbines (Aquilegia canadensis) are what I came here to see and as usual they stole the show. They like to grow on partially shaded rocky slopes so this area is perfect for them. How they got here is anyone’s guess but their numbers have been steadily increasing since I first found them. The rich alkaline soil is very unusual in this part of New Hampshire and many rare plants are known to grow in this area. The trick is in finding them; though I’ve spent 50 years walking through these woods this is the only place I’ve ever seen wild columbine.

They are beautiful things; well worth the hike. Each red and yellow blossom is about an inch and a half long and dances in the slightest breeze at the end of a long stalk. The Aquilegia part of the scientific name comes from the Latin Aquila, which means “eagle” and refers to the spurred petals that Swedish botanist Carl Linnaeus thought resembled an eagle’s talons. Some think they resemble pigeons around a dish and the name Columbine comes from the Latin Columbinus, which means “pertaining to doves or pigeons.” It is said that Native American men rubbed the crushed seeds on themselves to be more attractive to women. Whether they did it for color or scent, I don’t know.

I couldn’t stop clicking the shutter, always hoping for a better shot. The wind was blowing through the canyon so I was sure every photo would be blurred. There have been years I’ve had to come back three or four times for that very reason.

Wild columbine flowers have 5 petals and 5 sepals. Each petal is yellow with a rounded tip, and forms a long, funnel shaped nectar spur that shades to red. The oval sepals are also red, and the anthers are bright yellow. When they grow on ledges some of them are up overhead, so you can see the nodding flowers in a way you never could if they were growing at ground level. 5 funnel shaped holes lead to nectar spurs and long tongued insects and hummingbirds probe these holes for nectar. Some say that these holes look like dovecotes, which is another reference to birds. We’re so very lucky to have such beautiful things in these woods.

In some Native languages the term for plants translates to “those who take care of us.”
~Robin Wall Kimmerer

Thanks for stopping in.

 

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1-trail

We’ve had some cold nights and a little snow over the last week or so and it seems like winter might be here to stay, so I decided to visit the deep cut rail trail in Westmoreland recently. Once the cold settles down inside this man made canyon it’s reluctant to leave, and spectacular ice formations grow here.

2-ice

The ice is fueled by the groundwater that constantly seeps through the bedrock that the railway workers hacked their way through in the mid-1800s, and ice columns as big as tree trunks are commonplace. I’ve seen huge ice columns here many times but I’ve never seen their birth, so that was the object of today’s hike.

3-ice

Ice was forming almost everywhere on the vertical walls of the canyon. It was very cold this day and even in the bright morning sunshine the ice wasn’t melting. That’s the secret of the why the ice grows to such giant proportions here; the temperature seems to stay about 10 degrees cooler in both winter and summer. On a hot July day the natural air conditioning is very welcome, but in December it can be like walking into a freezer so you had better be dressed for it if you plan on spending much time here.

4-ice

The groundwater seems to follow the natural lay of the stone and seeps between the layers winter and summer. The water doesn’t seem to ever stop seeping so when an icicle forms more and more water flows over it, increasing its length and girth drip by drip. There can be enough ice here in February to cover the stone ledges completely in many areas.

5-ice-climber

Unless you’ve seen them the ice formations are hard to imagine, so I’ve used this photo from last February to better illustrate the size of both the ice and the place. Last winter was mild so the ice shown is tame in comparison to previous winters but still, ice climbers came to train. The New Hampshire branch of the Appalachian Mountain Club holds regular ice climbing clinics here and seeing climbers on the ice is fairly common on weekends. I expect that I’ll see a few this winter.

6-waterfall

There is almost always the sound of water dripping here. Usually it comes from the seeping groundwater but in at least one spot water gushes through a rift in the wall with enough force to be called a stream. I wonder if a stream on the hillside above somehow changed course, because I doubt that the railroad engineers would have left it this way.

7-drainage-ditch

All that water has to go somewhere so the railroad built drainage ditches on either side of the railbed to direct it where they wanted it to go. The ditches have kept the railbed dry for over 150 years but I saw that a rockslide further down the trail had dammed up one side and now water is washing away the railbed. With no railroad to maintain these rail trails it’s now up to private groups like snowmobile clubs to do all the work. They do a great job but it they might not be aware of the washout.

8-rock-fall

This is a shot of where the rocks have fallen across the drainage ditch and dammed it up. What isn’t seen in this photo is how all the water in the ditch has been forced into the railbed, washing it away. The rocks are big and I’m sure are very heavy but I would think that two men with crowbars could at least slide them over enough to let the water through.

9-ledges

There are many mosses, liverworts, and other interesting things growing on these walls that I don’t see anywhere else so I put on rubber boots and walk across the drainage ditches to get close to them. I’ve seen large stones that have fallen into the railbed and in the winter falling ice is always a possibility, so I have to be very aware of what’s going on around me. I always look up before I cross a ditch to get to a section of wall to make sure that I’m not going to be standing under overhanging ledge like that seen in this photo. I’ve never seen one fall but fallen stones litter both sides of the trail all down its length.

10-liverworts

For me this is what makes coming here worth any small amount of risk involved; I can get close to so many plants that I’ve never seen before, like the great scented liverworts (Conocephalum conicum) seen here. They are very particular about where they grow, insisting on just the right amount of light, humidity and temperature and they have found the perfect spot here, where they grow in great numbers. Though they are said to be common I never see them anywhere else.

11-liverwort-close

The great scented liverwort is also called the snakeskin liverwort, and with good reason. I love its reptilian skin and its scent, which is so clean and fresh it always makes me wish it came in a spray bottle when I smell it. Each more or less hexagonal leaf cell has a central pore over the top of an air chamber. On the floor of the air chamber are photosynthetic filaments called chloroplasts, and the pores through its skin let in enough light for the chloroplasts to do their work, which is photosynthesis. It’s quite amazing, as is all of life.

12-liverworts

Though the liverworts might seem fragile they are actually very tough as all of the plants that grow here have to be, because they are often completely encased in ice throughout the winter months. From what I’ve seen it doesn’t seem to bother them.

13-ferns

Any thoughts I had about the delicacy of our evergreen ferns went right out the window when I saw them growing here. They too are often covered in ice through the winter, but still green.

14-moss

Mosses also have to be able to withstand the ice. Curiously, though this one was surrounded by ice it was quite dry, as its twisted leaves show. I think it might be tall tornado moss (Tortella tortuosa) which has leaves that twist and contort when it dries out. It grows in the thin soil that forms on boulders and on rock ledges, and likes limestone.

15-algae

One of the strangest things that grow here  is a green algae called Trentepohlia aurea. Though it is called green algae a carotenoid pigment in the alga cells called hematochrome or beta- carotene, which is the same pigment that gives carrots their orange color, hides the green chlorophyll. It’s very hairy and produces spores which, when produced in high enough concentrations, can even color rain. I was just reading about a blood red rain that fell in parts of Spain in 2014. Many worried that it was a bad omen or extraterrestrial in origin, or a plague worthy of the Bible, but it was actually caused by the algae Haematococcus pluvialis. The same thing happened in Texas in 2013, in Sri Lanka in 2012, and in India in 2001, each seemingly caused by different algae. Yellow, green, and black rain has also been reported. It seems that colored rain can happen just about anywhere on earth when conditions are right. The blue in this photo is the sky reflected in ice.

16-mineral-staining

I’ve never seen colored rain falling in this place but I have seen plenty of colored ice, and I think at least some of the ice colors are caused by minerals in the groundwater, like the iron staining shown on the stone in this photo.  The ice here can be blue, green, red, orange, yellow, brown, and even black.

17-mineral-staining

Another example of mineral staining on the stone, this time in a sandy, orangey brown color.

18-colored-ice

And this photo from last year shows what the minerals can do to the ice. At least that’s my assumption. Neither I nor readers of this blog have been able to come up with any other theories except in the case of blue ice, which can become blue simply because of its own density.

19-linemans-shack

It takes a while to get used to this kind of cold again and by the time I had reached what’s left of the old lineman’s shack I couldn’t feel my toes any longer, so I thought I’d better do a little less lollygagging and more walking, and I trudged back down the trail at a high rate of speed (for me.)

20-ice

Watching ice melt might not be very exciting but watching it grow is, so I’ll be coming back here often throughout winter.

He who marvels at the beauty of the world in summer will find equal cause for wonder and admiration in winter. ~John Burroughs

Thanks for coming by.

 

 

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