ARCTIC ROUTES

In the discussion of the migration of the Arctic tern (p. 31) it was

noted that this species makes a very distinct west-to-east movement

across northern Canada, continning the flight eastward across

the Atlantic Ocean toward the western coast of Europe. It seems

likely that there are other species, including the parasitic jaeger

(_Stercorarius parasiticus_) that regularly breed in the northern

part of the Western Hemisphere but migrate back to the Old World

for their winter sojourn. Some others, as the red-legged kittiwake

(_Rissa brevirostris_) and Ross's gull (_Rhodostethia rosea_), remain

near the Arctic region throughout the year, retreating southward

in winter only a few hundred miles. The emperor goose _(Philacte

canagica_) in winter is found only a relatively short distance south

of its breeding grounds, and eider ducks (Somateria and Arctonetta),

although wintering in latitudes well south of the breeding grounds,

nevertheless remain farther north than do the majority of other

species of ducks (fig. 21).

The routes followed by these birds are chiefly coastwise, and in the

final analysis may be considered as being tributary either to the

Atlantic or to the Pacific coast routes. The passage of gulls, ducks,

and other water birds at Point Barrow, Alaska, and at other points

on the Arctic coast, has been noted by several observers, and from

present knowledge it may be said that the best defined Arctic route

in North America is the one that follows around the coast of Alaska.

=EVOLUTION OF MIGRATION ROUTES=

From the foregoing descriptions of migration routes it will be

observed that the general trend of migration in most species of North

American birds is northwest and southeast. It is comparatively easy

to trace the probable steps in the evolution of the migrations of

some species, and some routes have developed so recently that they

still plainly show their origin.

The tendency is for eastern species to extend their ranges by pushing

westward, particularly in the north. For example in the Stikine

River Valley of northern British Columbia and southwestern Alaska

the eastern nighthawk (_Chordeiles minor minor_), eastern chipping

sparrow (_Spizella passerina passerina_), rusty blackbird (_Euphagus

carolinus_), eastern yellow warbler (_Dendroica aestiva aestiva_),

redstart, and others have established breeding stations at points 20

to 100 miles from the Pacific Ocean. The robin, flicker (Colaptes

auratus), slate-colored junco (_Junco hyemalis hyemalis_), blackpoll

warbler, myrtle warbler (Dendroica coronata), and ovenbird (_Seiurus

aurocapillus_), all common eastern species, also are established as

breeding birds in western Alaska, the ovenbird having been detected

on the lower Yukon River. These birds, however, do not migrate in

fall by any of the Pacific routes, but instead retrace their journey

across the mountains and move southward along the broad flyways of

the interior.

The red-eyed vireo (_Vireo olivaceus_), a striking example of an

obundant woodland bird, is essentially an inhabitant of States

east af the Great Plains, but an arm of its breeding range extends

northwest to the Pacific coast in British Columbia (fig. 27). It

seems evident that this is a range extension that has taken place

comparatively recently by a westward movement from the upper Missouri

Valley, and that the invaders retrace in spring and fall the general

route by which they originally entered the country.

[Illustration: B4506M

Figure 27.--Distribution and migration of the red-eyed vireo. It is

evident that the red-eyed vireo has only recently invaded Washington

by an extension of its breeding range almost due west from the

upper Missouri Valley. Like the bobolink, however (fig. 23), the

western breeders do not take the short cut south or southeast from

their nesting grounds, but migrate spring and fall along the route

traversed in making this extension.]

In the case of the bobolink, a new extension of the breeding range,

and a consequent change in the migration of the species, has taken

place since the spread of settlement in this country (fig. 23). A

bird of damp meadows, it was originally cut off from the Western

States by the intervening arid regions. But with the advent of

irrigation and the bringing of large areas under cultivation, small

colonies of nesting bobolinks have appeared at various western

points, and now the species is established as a regular breeder

in the great mountain parks and irrigated valleys of Colorado and

elsewhere almost to the Pacific coast. In retracing their course

to reach the western edge of the route followed by the bulk of the

bobolinks that breed in the northern United States and southern

Canada, these western pioneers must fly long distances along a line

that runs almost due east and west.

Similarly it is possible to sketch what seems to be the logical

evolution of the remarkable routes of the golden plover (fig. 22). It

may be assumed that the eastern birds of this species first followed

an all-land route from the South American winter quarters through

Central America, Mexico, and Texas to the western parts of the

Mississippi Valley. As the migration route lengthened northward with

the retreat of the ice and the bird's powers of flight developed, it

would have a tendency to straighten the line and to shorten it by

cutting off some of the great curve through Mexico and Texas. First

a short flight across the western part of the Gulf of Mexico was

probably essayed. Proving successful, this was followed by flight

lines that moved farther east, until finally the roundabout curve

through Texas was entirely discarded and the flight made directly

across the Gulf to southern Louisiana.

As the great areas in Canada were gradually added to the bird's

domain, other important factors arose, the chief being the

attractiveness of the vast stretches of coast and plain of the

Labrador Peninsula, which in fall offered a bountiful store of

berries. The fall route therefore worked eastward to the Gulf of

St. Lawrence thence southwest through the interior to the coast

of Florida and across the Gulf of Mexico to the Central American

mainland. A series of shortening flights followed to take out the

great curve of the New England coast. A relatively short ocean flight

was probably attempted, say from Cape Cod to the Bahama Islands,

Cuba, and Jamaica, followed eventually by the long direct oceanic

route as it is now known.

As the Labrador Peninsula in spring is bound by frost and shrouded

by fog while the season advances rapidly through the interior, the

oceanic route proved useful only in fall, and the spring flight

continued through the Mississippi Valley. The above outline gives

a probable and fairly plausible explanation of the origin of this

wonderful route, particularly when it is remembered that migration

routes as now known are evolutions--age-long modifications of other

routes.

The evolution of the migration of the Pacific golden plover may be

explained in a similar fashion. At first the route probably followed

the Asiatic coast, through the Malay Peninsula and Oceania, thence

east in a great curve to the Low Archipelago, with individuals and

flocks dropping out to winter at many points along the way. The

Siberian birds probably continue to follow this ancient flyway,

but those nesting in Alaska began a long evolutionary series of

flights that cut down the length of their journey by shortening the

curve, until finally the transoceanic route of the present day was

developed.

=VERTICAL MIGRATION=

In the effort to find winter quarters furnishing satisfactory living

conditions, many North American birds fly hundreds of miles across

land and sea. Others, however, are able to attain their objective

merely by moving down the sides of a mountain. In such cases a

few hundred feet of altitude corresponds to hundreds of miles of

latitude. Movements of this kind, known as "vertical migrations", are

found wherever there are large mountain ranges. In the Rocky Mountain

region they are particularly notable, as chickadees, rosy finches

(_Leucosticte_), juncos, pine grosbeaks (_Pinicola_), and some other

species that nest in the Alpine Zone move down to the lower levels to

spend the winter. It has been noted that such species as Williamson's

sapsucker (Sphyrapicus thyroideus), and the western wood pewee

(_Myiochanes richardsoni_), which nest in the higher mountains, move

down to the lower regions in August following the breeding season.

At this time there is a distinct tendency also among the young of

mountain-breeding birds to work down to the lower levels as soon as

the nesting season is over. The sudden increases among birds in the

edges of the foothills are particularly noticeable when cold spells

with snow or frost occur at the higher altitudes.

Some species that normally breed in the Hudsonian or Arctic Zones

find suitable breeding areas on the higher levels of the mountains,

as for example the pipit, or titlark (_Anthus spinoletta rubescens_),

which breeds on the tundras of Alaska and northern Canada and also

south as far as Colorado on the summits of many peaks in the Rocky

Mountains. On the other hand a few species, as the Clark's crow, or

nutcracker (_Nucifraga columbiana_), nest at relatively low altitudes

in the mountains and as the summer advances move higher up, thus

performing a vertical migration that in a sense is comparable with

the post-breeding movements of herons on the Atlantic coast. These

illustrations show that the length of a migration route may depend

upon factors other than latitude.

=VAGRANT MIGRATION=

The most striking feature of the migrations of some of the herons

is a northward movement after the nesting season. The young of

some species commonly wander late in summer and in fall, sometimes

traveling several hundred miles north of the district in which they

were hatched. The little blue heron (_Florida caerulea caerulea_)

breeds commonly north to South Carolina, and by the last of July

the young birds begin to appear along the Potomac, Patuxent, and

Susquehanna Rivers, tributary to Chesapeake Bay. Although almost

all are immature individuals, as shown by their white plumage, an

occasional adult may be noted. With them come snowy herons (_Egretta

thula thula_) and egrets (_Casmerodius albus egretta_), and on

occasion all three species will travel in the East as far north as

New England, and in the Mississippi Valley to southeastern Kansas and

Illinois. In September most of them disappear, probably returning

south by the same route.

The black-crowned night heron (_Nycticorax nycticorax hoactli_) has

similar wandering habits, and young birds banded in a large colony

at Barnstable, Mass., have been recaptured the same season north

to Maine and Quebec and west to New York. This habit seems to be

shared by some of the gulls also, although here the evidence is not

so conclusive. Herring gulls (_Larus argentatus smithsonianus_)

banded as chicks at colonies in the Great Lakes have scattered in all

directions after the breeding season, some having been recovered well

north in Canada.

These movements may be considered as migration governed only by

the availability of food, and they are counteracted in fall by

a directive migratory impulse that carries back to their normal

winter homes in the south such birds as after the mating period have

attained more northern latitudes. They are not to be compared with

the great invasions of certain birds from the North. Classic examples

of the latter in the eastern part of the country are the periodic

flights of crossbills. Sometimes these migrations will extend well

south into the Carolinian Zone.

Snowy owls are noted for occasional invasions that probably are

caused by a shortage of the lemmings and rabbits that constitute

their normal food in the North. At least nine notable flights of

these birds occurred during the period 1876 to 1927. In the great

flight of 1926-27 they were noted as far south as Iowa, Ohio, West

Virginia, and North Carolina.

In the Rocky Mountain region great flights of the beautiful Bohemian

waxwing (_Bombycilla garrula pallidiceps_), are occasionally

recorded. The greatest invasion in the history of Colorado

ornithology occurred in February 1917, at which time the writer

estimated that at least 10,000 were within the corporate limits of

the city of Denver. The last previous occurrence of the species in

large numbers in that section was in 1908.

Evening grosbeaks (_Hesperiphona vespertina_) likewise are given to

performing more or less wandering journeys, and curiously enough,

in addition to occasional trips south of their regular range, they

travel east and west, sometimes covering long distances. For example,

grosbeaks banded at Sault Ste. Marie, Mich., have been recaptured on

Cape Cod, Mass., and in the following season have been re trapped

at the banding station. Banding records demonstrate that this

east-and-west trip across the northeastern part of the country is

sometimes made also by purple finches (_Carpodacus purpureus_).

=PERILS OF MIGRATION=

The period of migration is a season full of peril for birds. Untold

thousands of the smaller migrants are destroyed each year by storms,

in unfamiliar habitats, and through attacks of predatory birds,

mammals, and reptiles. If each pair of adult birds should succeed

in raising two fledglings to maturity, the population of migratory

birds would have a potential annual increase of 100 percent and the

world would soon be heavily overpopulated with them. It is evident,

therefore, that there is no such increase, and that the annual

mortality from natural causes is heavy enough to keep it in check.

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