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"North
America Migration Flyways" - Nutty Birdwatcher
The
Flyway Systems:
The routes followed by migratory birds are numerous, and while some
of them are simple and easily traced, others are extremely complicated.
Differences in distance traveled, in time of starting, in speed
of flight, in geographical position, in the latitude of the breeding
and wintering grounds and in other factors all contribute to great
diversity. No two species follow exactly the same path from beginning
to end; geographical groups of species with an almost continental
distribution may travel different routes.
Bird migration is generally thought of as a north-and-south movement,
with the lanes of heavier concentration following the coasts, mountain
ranges and principal river valleys. In general, it may be said that
the great routes of migration do conform very closely to major topographical
features when these happen to lie in the general direction of the
travel to be performed. It happens to work out nicely in North America
where the coasts, mountain chains and come of the larger rivers
do not depart from a north-and-south alignment.
The terms "migration route" and "flyway" are to some extent theoretical
concepts, while the latter has, in addition, come to have an administrative
meaning. Migration routes may be defined as the lanes of individual
travel from any particular breeding ground to the winter quarters
of the birds that use them. Flyways, on the other hand, may well
be conceived as those broader areas in which related migration routes
are associated or blended in a definite geographic region. They
are wide arterial highways to which the routes are tributary.
There are four (4) major North American flyways that have been named
the Atlantic, the Mississippi, the Central and the Pacific Flyways.
Except along the coasts, the flyway boundaries are not always sharply
defined and both in the northern breeding, and the southern wintering,
grounds there is more or less overlapping. As a matter of fact,
in the region of Panama, parts of all four flyways merge into one.
North American Migration Flyways with Routes
(Click
to see image)
Atlantic
Flyway:
The Atlantic Flyway may be described as extending from the offshore
waters of the Atlantic Coast west to the Allegheny Mountains where,
curving northwestward across northern West Virginia and northeastern
Ohio, it continues in that direction across the prairie provinces
of Canada and the Northwest Territories to the Arctic Coast of Alaska.
The flyway embraces several primary migration routes and many more
that are important as tributaries, some of the latter being branches
from primary routes of other flyways. The Atlantic Flyway route
from the northwest is of great importance to migratory waterfowl
and other birds some of which are flocks of Canvasbacks, Redheads
and Lesser Scaups that winter on the waters and marshes south of
Delaware Bay. The coastal route of the Atlantic Flyway, which in
general follows the shore line, has its northern origin in the eastern
Arctic islands and the coast of Greenland. This is a regular avenue
of travel, and along it are many famous points for the observation
of migrating land and water birds.
There is one route (not shown in image) that may be considered although
it is so exclusively oceanic that it is included under "Pelagic
Migration." This lane of travel passes directly over the
Atlantic Ocean from Labrador and Nova Scotia to the Lesser Antilles,
and across a group of small islands to the mainland of South America.
It is not known to be used by any of the smaller land birds, but
is followed by thousands of water birds and by shore birds of several
species. Since it lies over the sea, this route is definitely known
only as its terminals and from occasional observations that have
been made in Bermuda and the Antilles. In the autumn, some of the
shore birds that nest on the Arctic tundra of Mackenzie and Alaska
fly southeastward across Canada to the Atlantic coast and finally
follow this oceanic course to the mainland of South America.
Many of the birds that breed east of the Allegheny Mountains parallel
to seacoast, move southwestward in fall, a direction they apparently
maintain from northwestern Florida, crossing the Gulf to the coastal
regions of eastern Mexico where they have a land route for the balance
of the journey. A more direct route involving even longer flights
lies directly across the Caribbean Sea, but despite that fact it
is used almost entirely by land birds. After taking off from the
coast of Florida, the migrants on this route find only two land
masses in their course where they can pause for rest and food. Over
60 species cross the 150 miles from Florida to Cuba, where about
half of them remain for the winter. Others fly the additional 90
miles between Cuba and Jamaica. From that point to the South American
coast, there is a stretch of unbroken ocean 500 miles across, and
scarcely a third of the North American migrants leave the forested
mountains of Jamaica to risk the perils of this ocean trip.
Atlantic Flyway with Routes
(Click
for see image)
Mississippi
Flyway:
This flyway is relatively simple although it presents some features
of interest, chiefly as they affect the migratory waterfowl. It's
eastern boundary runs through the peninsula of southern Ontario
to western Lake Erie, then southwestwardly across Ohio and Indiana
to the Mississippi where it rather closely follows the river to
its mouth. The western boundary does not have such precise definition
as the eastern boundary, and for this reason in eastern Nebraska
and western Missouri and Arkansas the Mississippi Flyway merges
imperceptibly into the Central Flyway. The longest migration route
of any in the Western Hemisphere lies in this flyway. It's northern
terminus is on the Arctic coast of Alaska and its southern end in
Patagonia. During the spring migration some of the shorebirds traverse
the full length of this great artery and several species that breed
north to Yukon and Alaska must twice each year cover the larger
part of it. For more than 3000 miles, from the mouth of the Mackenzie
to the delta of the Mississippi, this route is uninterrupted by
mountains. There is not even a ridge of hills on the entire route
that is high enough to interfere with the movements of migrating
birds, and the greatest elevation above sea level is less than 2000
feet. Well timbered and watered, the entire region affords ideal
conditions for the support of hosts of migrating birds. The two
rivers that mark it, the Mackenzie emptying on the Arctic coast
and the Mississippi in the Gulf of Mexico, have a general north-and-south
direction, another factor in determining the importance of this
route which is used by large numbers of ducks, geese, shorebirds,
blackbirds, sparrows, warbler and thrushes,
The majority of North American land birds, seeking winter homes
in the tropics, that come south through the Mississippi Flyway take
the short cut across the Gulf of Mexico in preference to the longer,
though presumably safer, land or island journey by way of Texas
or the Antilles. During the height of migration some of the islands
off the coasts of Louisiana and Texas are wonderful observation
places.
It was once thought that most of the North American birds that migrate
to Central America made a leisurely trip along the west coast of
Florida, crossed to Cuba and then made the short flight from the
western tip of that island to Yucatan. The map will suggest this
as the most natural route, but as a matter of fact, it is used by
only certain swallows and shorebirds, or an occasional individual
of some other species that has been driven from its accustomed course.
Mississippi Flyway with Routes
(Click
for see image)
Central
Flyway:
In the United States, the Central Flyway merges toward the east
with the Mississippi Flyway and bounded in that direction by the
Missouri River. In the south on this side, it runs through western
Missouri, Arkansas and Louisiana, and then follows the Gulf coast
of Mexico southward. On the northwest Arctic coast, where this great
flyway has its beginning, the same territory involved that also
sends hosts of migrants down the Mississippi Flyway, but farther
south, in Canada, the western boundary follows closely the eastern
base of the Rocky Mountains. In western Montana, however, the continental
divide is crossed and the line passes through the Great Salt Lake
Valley and then somewhat east of south across the tableland of Mexico.
It may be called "the flyway of the Great Plains" as it encompasses
all of that vast region lying between the valley of the Mississippi
River and the Rocky Mountains, the principal wheat-growing region
of both Canada and the United States.
On its western boundary is an important breeding area for waterfowl
at the northern end of Great Salt Lake, Utah. The Central Flyway
is relatively simple, as the majority of the birds that use it make
direct north and south journeys from breeding grounds in the North
to winter quarters in the South.
Central Flyway with Routes
(Click
for see image)
Pacific
Flyway:
The Pacific Flyway includes the Arctic archipelago as Melville,
Banks and Victoria islands from which region the eastern boundary
tends to the southwest between Great Bear and Great Slave lakes
to the western boundary of the Central Flyway along the eastern
base of the Rocky Mountains in Canada. The territory of this flyway,
comprises the western Arctic, including Alaska and the Aleutian
Islands and the Rocky Mountain and Pacific coast regions of Canada,
the United States and Mexico, south to where it becomes blended
with other flyways in Central and South America.
The passage of gulls, ducks and other water birds at Point Barrow,
Alaska and at other points on the Arctic coast may be the best defined
Arctic route in North America. This route across the Alaska Peninsula
and the Gulf of Alaska and parallels the coast line of British Columbia,
Washington, Oregon and California. The Pacific oceanic route is
used by the Arctic Terns that breed in Alaska and those from the
more western tern colonies of Canada. The vast delta region of the
Yukon River in Alaska is a breeding ground for many species of waterfowl
and this area marks the northern terminus for some of those that
use the coastal route for most of all of their migratory flights.
The longest and important route of the Pacific Flyway is that originating
in northeastern Alaska and passing for most, if not all, of its
length through the interior. Most of the waterfowl that travel the
United States section of this route come from Alaska and the Mackenzie
Valley and other interior areas. Starting in Alaska, Yukon and Mackenzie,
this route runs southward through western Alberta. The Pacific Flyway
element apparently closely parallels the eastern foothills of the
Rocky Mountains. Near the international border, the route branches
and while large flights continue southeastward into the Central
and Mississippi flyways, others turn southwestward across northwestern
Montana and the panhandle of Idaho, follow along the Snake and Columbia
River valleys and then turn southward across central Oregon to the
interior valleys of California. Suitable winter quarters for birds
are found in California from the Sacramento Valley south to Salton
Sea and in the tidal marshes near San Francisco Bay.
The southward route of migratory land birds of the Pacific Flyway
that in winter leave the United States extends through the interior
of California to the mouth of the Colorado River and on to the winter
quarters that are principally in western Mexico.
Pacific Flyway with Routes
(Click
for see image)
Texto
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