A young Ganoderma tsugae, Reishi mushroom.
A shy cottonmouth, aka water moccasin.
Wild terrestrial orchid, “Pink lady’s-slipper”
A Snapping turtle waiting to cross the path.
A maturing Reishi mushroom.
Entrance to Demon Pond.
A beaver lodge.
This particular place had a nice feeling to it. The water level is above you as you walk past the beaver dam in the background, holding back Demon Pond.
Young Alder trees.
A two mile long path unfolds through wetlands, logging trails and high ridges overlooking beaver marshes. The one hundred and ten acres of land is managed by the Conservation Commission and Forestry Committee. It was created by volunteers in 1991.
A vernal pond under the heavy canopy of an old growth section of forest.
At the highest point, one can see down this steep ridge to a vast marshland in the distance.
There are lots of sunny patches in this forest due to “skid trails” or wood harvested areas.
The last harvest was done in 1990.
A tightly grouped cluster of young maples along the path.
Some of the vegetation includes poisonous sumac and a rare colony of rhododendron native to North America.
In 1983, a man by the name of Gilbert Knowles offered the Dowst-Cate Town Forest to the public. He wrote to the officials saying, “I have always had a warm place in my heart for Deerfield (and) I would be happy to do something for Deerfield.” His wishes were that this property be used as a “town forest and park”.
The snow lantern or snölykta was made the day after a storm which left us about five inches of wet snow. The next day, being sunny and in the upper thirties, was perfect for making snowballs.
The first night was a little too windy so the candles kept going out. The following day I placed two tall candles in the igloo and lit them in the evening just as the sun was going down and it stayed alight well into the early morning hours.
Pawtuckaway State Park is located in Nottingham New Hampshire. There are several trails to take in this 5000 acre preserve, one being Boulder Trail. If one takes a look at the satellite image of Pawtuckaway’ s Mountain range, you can see a circular formation called a ring dyke made by an ancient volcano about 130 million years ago. During the Ice Age, approximately 18,000 years ago, a mile high ice sheet sat on top of this area and moved these gigantic rocks as it melted, known as glacial erratics. Now we have boulders resting amongst trees in a beautiful forest for people to climb and admire.