One of the many benefits of living in the northeast is the variety of winter recreational opportunities that are afforded to us. One of the most rewarding of these is ice fishing. It is accessible to young and old alike and the cost to get started can be less than other outdoor winter activities in New York.
New York State Parks has a long tradition of promoting ice fishing events with tournaments at many of their facilities. Northeast of Albany, Grafton Lakes State Park Grafton Lakes State Park has been holding a tournament every winter for the past 33 years. This year’s tournament will be on January 19th and runs from 5 am to 2 pm. There will be prizes for the three longest fish of each species–trout, yellow perch and walleye/chain pickerel–for both the adult and child group. It’s a great day of family fun. Thompson’s Lake at Thacher State Park will be holding their tournament two weeks after Grafton’s on February 2nd. For more information about these tournaments contact the Parks.
If learning to ice fish is more up your alley, you can try out Thompson’s Lake on January 19th when DEC’s I Fish NY staff will be on hand to offer a clinic and free day of ice fishing. Moreau Lake State Park’s “Ice Fishing for The Kids” program will be on January 26th from 10 am-2 pm. There will be snacks and refreshments offered by the Friends of Moreau in the warming hut. On February 20thGlimmerglass State Park will host the Otsego Lake Ice Fishing Clinic, also free to the public, from 9 am-3 pm. For more information about these events call the associated park.
There are many other opportunities throughout the season to learn how to ice fish. Governor Cuomo has designated February 16-17th a free fishing weekend as part of his NY Open for Fishing and Hunting Initiative. No fishing license will be required for those partaking over this weekend. Beginning ice anglers are encouraged to download the Ice Fishing Chapter (PDF, 3.7MB) of DEC’s new “I FISH NY Beginners’ Guide to Freshwater Fishing” for information on how to get started ice fishing. Additional information, including a list of waters open to ice fishing, can found on the DEC ice fishing web page and the Public Lakes and Ponds map.
When ice fishing, please keep in mind that anyone 17 years and older needs to have a fishing license in their possession (except on designated free fishing weekends). Fishing licenses are valid for 365 days from date of purchase. If using live bait, it must be certified, and excess live bait can never be discarded into a waterbody. This prevents the spread of diseases and invasive species.
Of utmost importance is safety. Do not go on ice that is less than 4 inches thick and be especially wary of ice on moving water like streams or rivers. Ask the experts and don’t go alone. Remember that tracks left by others is not an indication of safe ice; conditions can change quickly. Areas near docks and shorelines may be less safe.
If you follow these simple guidelines and dress appropriately, you and your family and friends will be able to enjoy a fun filled day of fishing and fresh air. Always keep in mind that ice fishing is a weather dependent sport and you need to be aware of the conditions. State Parks loves to see pictures of your adventures out on the ice — be sure to share them with staff at your favorite State Park. Happy Fishing!
This time of year, much of New York’s landscape is dappled with bare-branched deciduous trees and dark, evergreen conifers. These cone-bearing conifer trees are adapted to survive harsh, cold weather, from the microscopic structure of the leaf to the overall shape of the entire tree. Despite the needle-like shape, conifer leaves serve much the same function as the flat, broad leaves of a sugar maple or oak tree. Most conifers keep their needles year-round. Do you know which New York native conifer drops its needles every fall? It is the tamarack (Larix laricina), a member of the larches, shown below.
On the left, these tamaracks are changing color. Every autumn the needles turn bright yellow and will fall off the tree by winter, so they are not considered an “evergreen.” On the right, a closer view of tamarack needles, which grow from a woody spur in clusters of ten to twenty. The needles are approximately ¾” to 1 ¼” inches long.
When talking about evergreens, pines may first come to mind, but conifers also include firs, spruces, hemlocks, and others. But how do we tell which is which? Here are a few quick tips to help narrow down the tree group simply by looking at the needles.
First, let’s look at pines. Pine trees have needles in bundles on the stem. The number per bundle depends on the species, but if you find bundles of five needles or less, you’ve likely discovered a pine. There are six native species of pine in New York, but two you may be most likely to encounter are white pine (Pinus strobus) and red pine (Pinus resinosa).
The eastern white pine (left) and its bundled needles (middle and right). This species of pine has five needles per bundle (and as a memory trick, there are five letters in the word “white”). The needles are soft and flexible, measuring about 2 to 4 inches long.
Spruce trees have needles that are individually attached to the branch with small woody pegs. A key characteristic for spruce needles is that they are square and can roll easily between your fingers. They are usually sharply pointed. Also, if any needles are shed the woody pegs make the branch feel rough, unlike the smooth branches of firs. There are three native spruces in New York: the white spruce (Picea glauca), the black spruce (Picea mariana), and the red spruce (Picea rubens).
The white spruce (left) and its needles (right), notice the woody pegs that attach the needle to the branch. Needles are stiff and measure about ½” to ¾” inches long. This species is sometimes called skunk spruce or cat spruce due to the strong odor from broken needles.
Fir needles are also individually attached, but unlike spruces, they are attached by what resembles a suction cup (look for a circular base). They are typically soft and flat with rounded needle tips. There are two whitish lines on the bottom of the needle. Another distinguishing characteristic of firs is that their cones stand upright on the branches, rather than droop down. The only native fir that can be found in New York is the balsam fir (Abies balsamea).
A stand of balsam fir (left) and its needles (right). Balsam fir needles are dark green and measure around ¾” to 1 ½” in length. The tips of the needles can be blunt, rounded, or notched.
Hemlocks have individually attached needles that are flat. Unlike firs, each hemlock needle has a small stem attached to a woody peg. In New York there is only one native hemlock species, the eastern hemlock (Tsuga canadensis). While you’re out testing your needle identification skills, keep an eye out for the invasive pest hemlock woolly adelgid, which creates white woolly masses at the base of hemlock needles. This insect causes tree health to decline and can lead to the death of the hemlock in as little as four years.
A young eastern hemlock stand (left) and its needles with stems (right). Needles are usually a shiny green. On the underside of each needle, you can see two characteristic white lines (shown in the picture). The needles are typically one inch or less in length.
So there you have it! Next time you’re out scratching your head, wondering if you’ve encountered a white spruce or a white pine, ask yourself these simple questions:
Are the needles in bundles or individually attached?
Does the needle roll easily between your fingers or is it flat?
Are the needles attached to a stem, woody peg, or a “suction cup” structure?
Just by taking a quick look (and maybe pluck) at the needles, it is often possible to categorize the conifer into pine, spruce, fir, or hemlock. If you come across a conifer that doesn’t fit into these categories, try looking at cedars or junipers too. And the best part of studying conifers is that you can look at needles all year long! Unless it’s a tamarack, of course.
If you’d like to learn more about some key conifers, check out this blog post to learn about identifying specific species you may encounter in State Parks!
Over the last 12,000 years, the landscape of the Finger Lakes region has undergone colossal change. Hidden in cracks and valleys throughout the region are wondrous geologic remnants of that change. So abundant is the splendor of these wonders that many locals have become numb to the consistent gurgling of waterfalls on their daily commute through, for example, the Village of Montour Falls, just south of Watkins Glen State Park, where residents often pass Aunt Sarah’s Falls on Route 14. Yet no two of the over 2,000 gorges that call the Finger Lakes home are the same; each has a different fingerprint with a different number of curves, caverns, and cascades.
The Finger Lakes themselves are a unique natural phenomenon. There are no other lakes quite like them in the world. Eleven north flowing lakes, varying in length and depth, span over 120 miles of the western section of New York. They range from Canadice Lake, at a mere 3 miles long, to Cayuga Lake, which stretches for 38.2 miles; and from the relatively shallow Honeoye Lake, at 30 feet deep to Seneca Lake, which plunges steeply for 634 feet.
About 2.5 million years ago dawned the age of ice. In this region, glaciers are thought to have been over 3,000 feet high, or about the size of two Empire State buildings stacked on top of each other! It is a result of these glaciers growing that we now have “finger lakes”; before we had “finger rivers.” All our U shaped lake basins were originally V shaped river valleys. As the glaciers bulldozed their way through the valleys, the unrelenting force gouged out the walls. About 12,000 years ago, a change in climate warmed the earth, ending the reign of the Ice Age.
As the glaciers started to recede, their melting ice filled the lakes and exposed steep U shaped valley walls. All around would have been hanging valleys comprised of massive waterfalls dropping straight into the lakes. Today, every gorge near the lakes, including those south of the lakes, began its story as one of those waterfalls and has since eroded back into the rock.
“Ithaca is Gorges” is an iconic phrase in Ithaca, referring to the numerous gorgeous gorges around this city at the base of Cayuga Lake. This clever pun, however, has a forgotten key third part. As the massive waterfalls started to erode back into the rock, the eroded sediment built up at the base of the lake. This erosion was so rapid that our lakes are miles shorter than they were originally. “Ithaca is Gorges” because it was formed by the gorges and would not exist without them!
The extremely fast rate of erosion in our gorges alludes to its rich ancient natural history dating back long before the Ice Age. The 380-million-year-old layers of rock in the gorge were each once the bottom of an expansive inland ocean that covered much of the eastern states. The earth, as we know it, was unrecognizable; life was just beginning to take a foothold on land. In the little town of Gilboa, NY, proof of this timeframe can be found in the oldest fossilized trees worldwide. The early roots of these Gilboa trees were pioneering the rocky, unforgiving earth on the edge of the Devonian sea.
This tropical inland sea – which was at that time located below the equator – was the result of a collision between the North American and European continents. When they collided, North America subducted, or went under Europe, and Europe crinkled up creating the Acadian Mountain range just off the coast of New York. These impressive mountains were estimated to have been as big, if not bigger, than the Himalayas are today!
Much of the sediment found in the inland sea would have come from the erosion of these mountains, but the depth of this water would have, over time, also affected the type of sediment found on this ocean bottom. Gradually, the buildup of layers would have caused enough pressure to solidify the underlying sediment into rock. This is known as compaction. This means that every layer of rock in our gorges, be it the more brittle rocks, such as shale, or the denser rocks, such as sandstone and limestone, were once at the bottom of an ocean!
The layers however are only half of the puzzle influencing the speed of erosion in the gorge. Breaking up the layers, in a stunning display of natural masonry, are countless straight line fractures. There are fractures or joints that follow the gorges east to west and those that span across the gorge north to south, intersecting at almost perfect right angles. Notice the unnatural looking straight lines and right angles in the photo of Robert H. Treman State Park.
These joints date back about 300 million years. At this time, all the continents were joining together to form one enormous supercontinent. Pangea, which translates directly to “all earth,” stretched from pole to pole. If you study a map of the world’s continents, you may notice that the western edge of Africa matches up with the eastern edge of the United States like a jig saw puzzle. The stress of this collision alone, however, was not the force required to create the fractures.
Instead, it caused straight line weak points in the rock perpendicular to the pressure. Meanwhile, a batch of methane gas had matured under pressure and heat and took advantage of the weak points to escape from the depths of earth. After this event, 30 million years quietly passed while Africa unassumingly rotated around North America. This quiet rotation was disturbed 270 million years ago when another batch of methane gas matured under heat and pressure, again utilizing the weakened rock to escape. The timing of this second release just so happened to occur when Africa was at about a 90 degree angle from where the first batch of methane gas escaped, forming joints that meet up at almost perfect right angles. Next time you find yourself in the Finger Lakes, keep an eye out for these natural right angles, they’re everywhere!
Considering all 380 million years of the gorges’ rich natural history;
the glaciers that created the U-shaped lakes and the hanging valleys
the joints that resulted from the release of methane gas through the weakened rock
and the layers of rock – shale, sandstone, and limestone, remnants of an ancient inland sea
an ingenious combination of forces all working together to form the gorges in only 12,000 years comes to light. In short, as the water easily erodes away the brittle shale and undercuts itself, the joints or fractures that break up the creek bed speed up the erosion process by causing chunks of the denser rocks – sandstone and limestone to fall at a time. The water, therefore, never has to take the time to erode away the denser types of rock. In consequence, we can affectionately say that “Although our gorges are 12,000 years old, their story can be told in no less than 380 million years.”
Post by Tamara Beal, Finger Lakes 2018 Student Conservation Association Intern
Crailo was once a fortified home belonging to Hendrick van Rensselaer, a member of a wealthy Dutch family involved in settling the Upper Hudson Valley during the mid-1600s. For the van Rensselaers and other Dutch colonists, holidays on the Hudson began with the Feast of St. Nicholas on December 6th. According to the legend, the Dutch St. Nicholas, known as Sinterklaas visited homes and filled good children’s shoes with treats and gifts. In 1675, Crailo’s owner, Maria van Rensselaer, purchased suntterclaesgoet, or “Sinterklaas goodies,” (possibly a special type of cookie) in Albany, in what might be the earliest reference to Sinterklass in New Netherland and New York.
St. Nicholas Day began the holiday season in Colonial New York, and Epiphany, commonly known as Twelfth Night, marked the end of the Christmas season. In Western Christianity, the Feast of the Epiphany commemorates the arrival of the Magi, or Three Kings, to Bethlehem. This was traditionally celebrated on January 6th, the 13th day and the ‘twelfth night’ after Christmas.
In the 17th and 18th centuries, Dutch and English residents of Albany and the Upper Hudson Valley celebrated Twelfth Night with both religious services and high-spirited entertainment. While there are no primary sources that describe exactly how the Schuyler family celebrated the holiday at Schuyler Mansion in Albany, letters and journals do mention popular customs such as calling on friends, throwing parties, and hosting elaborate meals. Alongside this, were the traditions of wassailers, or carolers parading through the streets and the Twelfth Night cake – an elaborate confection with a bean baked inside. The person who found the bean in their cake slice was crowned “King” for the evening and led the evening’s toasts!
Each January, Schuyler Mansion and Crailo recreate some of these colonial era traditions with their own 17th and 18th century-inspired Twelfth Night celebrations. Schuyler Mansion’s “Salutations of the Season!” features live musical performances, reenactors in 18th century clothing, refreshments, and an evening of cheer. While across the Hudson at Crailo, Dutch colonial reenactors prepare traditional Dutch foods over the open hearth, play historic games, and celebrate “Twelfth Night” in true 17th century style.
Cooking over the hearth in Crailo State Historic Site
Dutch Twelfth Night Fare
Schuyler Mansion’s “Salutations of the Season!” and Crailo’s “Twelfth Night” will be held January 5, 2019 from 4:00 PM to 7:00 PM. These evening programs are a unique opportunity to celebrate the end of the holiday season in historic fashion. The celebrations also represent the rich and storied history of New York’s upper Hudson Valley – settled by the Dutch, taken by the English, and then a hotbed of military and political activity in the era of the American Revolution.
“Salutations of the Season!” and “Twelfth Night” single-site Admission: $6.00 Adults / $5.00 Seniors & Students / $1.00 Children (12 and under) / $4.00 Friends Members. Combination Tickets for Admission to both Crailo and Schuyler Mansion: $8.00 Adults / $7.00 Seniors & Students / $2.00 Kids / $6.00 Friends members. For further information about this or other programs at Crailo and Schuyler Mansion State Historic Sites, please visit www.parks.ny.gov, find us on Facebook, or call us! Crailo: (518) 463-8738 / Schuyler Mansion: (518) 434-0834.
Whether it’s a much-needed elixir after a long holiday season or a first step in making (and keeping!) a resolution to be active in the new year, the 2019 First Day Hikes (FDH) are sure to draw thousands into New York’s great outdoors.
Each year on January 1, the New York State Office of Parks, Recreation and Historic Preservation (State Parks) and the Department of Environmental Conservation (DEC) host these family-friendly events on public parkland across the State. This year’s line-up of 79 hikes includes some exciting new destinations in communities on the shores of Lake Ontario, Lake Champlain, and many more!
The popular, outdoor New Year’s Day tradition is in its 8th year. The first First Day Hikes were held in Massachusetts in 1992, but have since spread nationwide. This year marked the first time the FDH went ‘international’, with events held in neighboring Ontario, Canada.
Here in New York, the event has grown significantly since its inception. The 2019 First Day Hikes will be offered at more than 51 state parks and historic sites with some facilities offering multiple hikes for different age groups, skill level and locations. In addition, DEC will host 19 hikes at wildlife areas, trails and environmental education centers. Staff from State Parks and DEC, along with volunteers, will lead the walks and hikes, which range from one to five miles depending on the location and weather conditions.
For last year’s event, Mother Nature really tested people’s mettle. With frigid temperatures and snowy conditions across the state last New Year’s Day, a number of parks, sites, wildlife areas and nature centers cancelled or postponed their First Day Hike program, but many soldiered on and welcomed participants all bundled up who were looking forward to heralding in 2018 in the outdoors.
In fact, a pair of intrepid First Day Hikers braved the elements and joined not one, but two (!) First Day Hikes out in western New York. A Miami couple honeymooning in Niagara Falls attended the morning First Day Hike at DeVeaux Woods State Park, and had so much fun they decided to join the afternoon ice-covered FDH program at iconic Niagara Falls State Park (shown below).
Some host locations welcome dogs on leashes and several have flat, even surfaces for strollers. Participants are encouraged to contact the park for information and pre-registration where noted. A sample of this year’s programs feature a seal walk, walking history tour, snowshoe waterfall hike, pet-friendly treks, bird count gorge walks, military musicology, canal towpath walk, and other fun options.
If conditions permit, some First Day Hikes may include snowshoeing or cross-country skiing with equipment for rent if available, or participants can bring their own. Many host sites will be offering refreshments and giveaways. A map and details about hike locations, difficulty and length, terrain, registration requirements and additional information are listed at parks.ny.gov and dec.ny.gov.
This New Year’s Day, be inspired by the Florida newlyweds who attended two hikes in a single day in Niagara, or the hundreds of brave souls who joined the gorge walk at Taughannock Falls State Park in the Finger Lakes (shown above), or the families and friends who embrace the winter wonderland at state parks and DEC sites across our state… and start your own tradition today.