Snowy owls have been getting a lot of attention this season, mainly due to the large influx we are seeing in the Northeast.

These owls aren’t the only birds that prefer the comparably mild Massachusetts winter over the extreme temps in the Arctic tundra. Snow buntings—sometimes known as the “snowflake”—also vacation here.

Feathers like Snow

At first glance, you might confuse a flock of snow buntings for a swirl of snowflakes. These birds are brown and white when they are in non-breeding plumage, and they have luminous white patches on their wings.

During the summer breeding season, the female snow bunting turns grayer, and the male is mostly black and white (think of a snowman studded with bits of coal). Amazingly, this species doesn’t grow new feathers to achieve this look. Instead, it rubs against snow until the brown feather tips are worn away, revealing the differently-colored feather bases.

A Northern Bird

Why do snow buntings come here for the winter? They’re actually escaping harsh weather in a place much farther north: the high Arctic. Up on the tundra, they spend the warmer months raising young. They build nests heavily lined with fur, grasses, and feathers, so their chicks will stay warm on the chilly, rocky terrain.

Once the breeding season is over, snow buntings leave the Arctic and its severe oncoming winter in favor of more hospitable lands, like the northern half of the United States. Here, you’ll find flocks foraging in open grassy areas like roadsides, farmers’ fields, and beaches, merrily searching for tasty seeds amongst drifts of snow.

A Bird in Trouble?

Some evidence suggests that the snow bunting population in North America may be declining sharply. Climate change and a host of resulting effects like changing amounts of snowfall may be altering this bird’s Arctic home. It’s another good reason to get serious about tackling the impacts of climate change.

Have you seen any “snowflake birds” in your neighborhood this year?

Photo courtesy of Dave Larson

Esker at Ipswich River Wildlife Sanctuary

It may be cold now, but this polar vortex much of the United States is experiencing has nothing on our glacial history.

Thousands of years ago, an ice sheet up to a mile thick moved across Massachusetts, creating well-known features like Cape Cod, Walden Pond, Plymouth Rock, and even the drumlin that gives Drumlin Farm its name.

The Time of the Glaciers

Glaciers—huge bodies of ice that move across the landscape—have blanketed our state many times in the past. Although their causes are complex, one major factor is a regular shifting of the Earth’s orbit that changes how much sunlight or energy from the sun we receive. (Note that this natural factor isn’t the cause of today’s fast-moving climate change.)

Continent-wide glaciers are called ice sheets. The most recent one covered Massachusetts between about 22,000 and 14,000 years ago, scraping away the land right down to the bedrock. When it melted away, plants and animals returned from the warmer ice-free south. Some slow-moving life still hasn’t reappeared. For example, the glaciers destroyed native earthworms—all our earthworms are imports from Europe.

Glacial Clues To Look For

Massive sheets of ice in motion leave behind plenty of evidence. Here are six of the many signs you can see:

• Glacial till. New England’s famous stonewalls are made of rocks that farmers removed from fields so they could plow. They’re part of a layer of unsorted rubble called till that was left behind as the glacier scoured soil and bedrock. Find stonewalls at many of our wildlife sanctuaries.
• Erratics. Glaciers also carry big boulders and drop them “erratically” in improbable places on the landscape. Plymouth Rock is one such erratic. You’ll also spot them at Rocky Hill in Groton and Moose Hill in Sharon.
• Drumlins. These hills are formed when a glacier pushes up debris into an egg-shaped mound. Some examples include Bunker Hill, the Boston Harbor islands, and the drumlin that gives Drumlin Farm in Lincoln its name.
• Kettle ponds. When giant blocks of ice fall off glaciers and become partly buried, they form kettle ponds. The famous Walden Pond in Concord is one.
• Eskers. As glaciers recede, rivers of meltwater course through them, leaving behind snaking trails of gravel and other streambed material called eskers. Walk along eskers at Ipswich River in Topsfield and Stony Brook in Norfolk.
• Moraines. Glaciers also create huge piles of debris called moraines. Nantucket and Martha’s Vineyard mark places where the glacier stopped its southward crawl, leaving sediment it had been pushing along. In fact, much of Cape Cod is a huge moraine created by a pause when the glacier was retreating. Explore moraines at Wellfleet Bay and other wildlife sanctuaries in the area.