Cross Country By Rail Continued

In my last post, I left Bellingham, WA and crossed the Cascade Mountains via Amtrak’s Empire Builder. On day two of the journey to Pittsburgh, the route and landscape would prove to be even more contrasting than the previous twenty-four hours.

Overnight the train route crossed eastern Washington and Idaho. I woke around sunrise to a foggy scene along the Kootenai River. The river along this stretch harbored few rapids that I could see, but it was brimming with muddy water. Spring and early summer is the season of high runoff in the Rockies.

river flowing through foggy valleyThe train soon left the Kootenai River and passed through the Salish Mountains to the Flathead River valley. After Whitefish, Montana we began a slow climb toward the continental divide. Along the middle fork of the Flathead River, between Glacier National Park to the north and the Great Bear Wilderness to the south, lies one of the most scenic stretches of rail on the route. Every bend provided new views of the snow-capped mountains bounding the narrow valley.

view of forested mountainsWhile I enjoyed the mountain scenery, for me the real highlight of this section was the stark contrasts in vegetation and climate. The low valleys on the west side Glacier National Park capture enough precipitation to support the growth of species also found within the wet forests Washington’s Cascades. At West Glacier I caught glimpses of the some of the eastern-most stands of western red-cedar (Thuja plicata). This species, you could say, likes it feet wet and it won’t grow where soil moisture is too low. In this part of North America, a lack of suitable habitat squeezes the red-cedars into narrower and narrower confines, and it quickly disappeared as we traveled east.

Western red-cedars wouldn’t be the only species to vanish in the next fifty miles. On the approach to the continental divide, lodgepole pine (Pinus contorta) and Douglas-fir (Pseudotsuga menziesii) predominated. Lodgepole pine was especially abundant in areas that had experienced forest fires in the last two decades. As the train crossed the continental divide at Marias Pass (el. ~5200 feet) the forest began to disappear, partly from the elevation (treeline was only a thousand or so feet higher) and largely from increasing aridity.

Terrestrial habitats often intergrade slowly, mixing in quilted patches before one finally yields to another. At East Glacier, Montana though, the montane Rocky Mountain forest seemed to simply end where the short grass prairie began. Here is one of the most dramatic terrestrial biome shifts to be found in the United States.

rolling prairie with snow-capped mountains in backgroundLike the Cascades, the Rocky Mountains create a strong rain shadow across northwestern Montana. Browning, MT, east of the mountains, receives only half the precipitation of West Glacier. For the next thousand miles across Montana and North Dakota prairie dominated where the land was not cultivated or otherwise appropriated by people. The only trees were either planted or grew along creek and river bottoms where their roots could tap into a shallow water table.

prairie and wheat fields across north central MontanaWildlife became easier to spot on the open prairie. Through Montana the railroad took us just south of the true prairie pothole region, but many of the low-lying areas adjacent to the track held water. Every little puddle seemed to harbor a few pairs of ducks and geese. I casually spotted at least ten waterfowl species during the day. Undoubtedly more used the habitat. I just failed to see them. Small prairie dog towns, frequented by red-tailed and Swainson’s hawks, occupied some of the ranching areas. I counted at least two-dozen pronghorn grazing or resting small, scattered bands.

In eastern Montana, badlands appeared in the distance and became more prominent as we approached and crossed the North Dakota state line. Parts of this area are rich with fossils and I wanted more than a little bit to poke around the hills for ancient bones.

badland bluffIn North Dakota, fracking wells became a prominent sight as the sun set.

oil wells silhouetted by the setting sunOn the morning of my third and final full day on the train I woke up somewhere in Minnesota where the prairie had long since yielded to cornfields. This was, historically, a battleground between prairie and forest. In this area, where precipitation is great enough to support tree growth, fire was the prairie’s greatest ally. Periodic burning kept the forest at bay. After American settlement, the prairie was plowed and fires suppressed. Along this ecosystem margin today, you’re more likely to see farm fields bordered by trees than a patchwork of prairie and forest.

Spring was also much less advanced in west-central Minnesota compared to the Puget Sound area where my trip began. Quaking aspen was washed with small vibrant leaves but some of the paper birches had barely broken bud.

For over a hundred miles south of Minneapolis and St. Paul, the route followed the Mississippi River where tall bluffs bordered the river valley…

wide river with tall bluffs in background…and the floodplain forest drowned in water.

flooded marsh bordered by forestThe train crossed the Mississippi one final time at La Crosse, WI. Heading upland into central Wisconsin, jack pine (Pinus banksiana) appeared on sandy soil. This species is essentially the eastern equivalent of lodgepole pine and the two hybridize where their ranges overlap. Like it’s western sibling, jack pine is well adapted to fire, often holding serotinous cones on its branches for years before fire melts the cones’ resin and releases its seeds.

forest and rolling hills

You’ll have to take my word for it: Those are jack pines in the middle ground.

East of Madison, the landscape quickly became suburbanized then urbanized as we approached Milwaukee. We never seemed far from Lake Michigan, but I only caught a couple of glimpses of the great lake.

I transferred trains in Chicago for the final leg of the journey to Pittsburgh. Through Gary, Indiana, the land remained very urban with the exception of the forested dunes on the inland side of Indiana Dunes National Lakeshore. Night hid most of Indiana and all of Ohio. After a rough night of sleep, I arrived in Pittsburgh at 5 a.m.

There’s a lot of sitting on a railroad trip from Puget Sound in Washington to Pittsburgh and I felt very antsy, so I capped off my first day in town with a fifty-mile bike ride on the Great Allegheny Passage. The exercise and change of pace was welcome, but so was watching the landscape through the train window.

Cross Country By Rail Day One

Since I live across the continent from most of my family, I’m obliged to return east periodically. During my time in Alaska I flew almost exclusively on this migration, primarily because it was the most expedient way to get to where I needed to go. If I have the time though, I’d rather travel by other means. With some time to spare before my summer job at North Cascades National Park begins, I traveled by train from Bellingham, WA to Pittsburgh, PA.

I’m not a train fanatic, but the railroad allows me see a good deal of the landscape and perhaps some wildlife without the risks involved with highway driving. On the train, I could sit in my seat and gaze eagerly out the window to watch the landscape pass by. My first wildlife sighting began even before I stepped onboard.

While waiting for the train in Bellingham, I watched a crow land in a parking lot with something large in its bill. This was nothing unusual as crows are fond of scavenging garbage, but as soon as the crow landed I noticed its prize was moving. I hurriedly yanked my binoculars out of my daypack to get a better look.

The crow had caught and was killing a semi-neonate cottontail rabbit. After it dispatched and partly consumed its prey, the crow returned to catch and kill another kit. With more than it could eat, the crow cached pieces of the rabbits in nearby trees and shrubs. It was a fairly gruesome death for the rabbits, but crows gotta eat too.

view through fence of crow

Life and death struggles happen even in city parking lots.

Once onboard the train and traveling from Bellingham to Seattle, I witnessed no more battles between predator and prey. The rest of the ride, in fact, was quite pleasant. The Cascade route provided plenty of views of Puget Sound, where many birds lounged and fished in the water near shore. I enjoyed glimpses of birds like blue herons, cormorants, gulls, more crows, and brant.

view of water with clouds and boulder in middle foreground

Puget Sound is a glacially carved trough. The boulder in the middle foreground is likely a glacial erratic.

Where I couldn’t see the water, the route often passed through rich farmland where large rivers like the Skagit and Snohomish have deposited broad floodplains.

Fallow farm fields and farmhouseAfter transferring to the Empire Builder in Seattle, my route reversed north before it turned east up the Snohomish and Skykomish rivers valleys toward the Cascade Mountains, which were quite showy under clear skies.

Farmland with view of tall snowcapped mountains in backgroundThis section of rail, besides letting me enjoy scenes of lush forest, provided a conspicuous example of habitat changes due to climate, particularly the Cascades’ rain shadow effect. When moisture-laden storms from the Pacific reach the Cascades, the rising air cools and drops a considerable amount of its moisture on the west side of the mountains. Far less remains to wet the mountains’ eastern slopes.

Skykomish, WA at 900 feet in elevation, for example, receives a whopping 91 inches of precipitation per year. The forests of this valley, except where recently clear-cut, are lush and thick and moss hangs prominently from stout big leaf maple branches.

Forests on snow-covered mountainside

Lush forest cloak the western slopes of the Cascades.

 

Around 2900 feet in elevation, the train entered an eight-mile long tunnel and passed underneath the Cascade crest. When the train exited the tunnel on the east side of the Cascades, the forest was noticeably different. Trees were sparser and included a higher proportion of drought tolerant species like ponderosa pine.

Sparsely snow covered mountain

Many mountainsides east of the Cascade crest are noticeably drier and less forested than equivalent areas to the west.

As the train descended the Wenatchee River valley to the Columbia River, the climate became drier and drier. Soon enough, sagebrush and bitterbrush mixed with widely scattered trees as we approached Wenatchee around sunset. About 780 feet in elevation, Wenatchee receives only 11 inches of annual precipitation. Along the Columbia River, as night fell, the route crossed a dramatically drier environment compared to the lush forests not far to the west. I could see few trees except those planted by people.

Darkness concealed central and eastern Washington’s landscape, which I knew would happen but was still disappointing because I missed viewing any of the unique and spectacular channeled scablands. I went to bed looking forward to more sightseeing.

In a future post, I’ll describe days two and three on the train where the land continued to offer more reasons to be glued to the window.