Mount Toby from South Sugarloaf Mountain, Deerfield, Mass

A panoramic view looking east from South Sugarloaf Mountain in Deerfield, toward Mount Toby in Sunderland, around 1891. Image from Picturesque Franklin (1891).

The scene in 2021:

These two photos were not taken from the exact same spot, as shown by the different angles of the bridges in the lower right, but they show the same general view of the Connecticut River, the town of Sunderland, and Mount Toby in the distance. Both were taken from near the summit of South Sugarloaf Mountain, a relatively small hill that forms the southern end of the Pocumtuck Range, which is part of the larger Metacomet Ridge. Sugarloaf is best known for its dramatic views of the valley to the south, but this eastern view is also offers impressive scenery.

South Sugarloaf is often referred to simply as Sugarloaf Mountain, although it is the smaller of the two summits that comprise the mountain. However, the northern peak, while nearly 200 feet higher in elevation, has only limited views from the summit, and is rarely visited. By contrast, the southern peak has long been a popular tourist destination. Rising to an elevation of 610 feet, it is about 500 feet higher than the Connecticut River, which passes just a third of a mile from the summit.

The first photo was likely taken from the Summit House, which was built here in 1864. These types of mountaintop hotels were popular in the northeast during the second half of the 19th century, and several others were located on nearby summits on the Metacomet Ridge, including the Prospect House on Mount Holyoke and the Eyrie House on Mount Nonotuck. Even Mount Toby briefly had a tower and hotel at the summit, but the buildings burned in 1882. This was a common fate for summit houses, given their isolated locations far above water sources, and the summit house on Sugarloaf Mountain would eventually be destroyed by a fire in 1966.

Mount Toby, which towers in the distance beyond the town of Sunderland, is geologically related to Sugarloaf Mountain. It is the highest peak on the Metacomet Ridge, and at 1,269 feet it is more than twice the height of South Sugarloaf. However, as the photos show, the mountain is not a single peak. Its rugged landscape has many different summits, the highest of which is on the northern side, on the far left side of both photos.

The mountain is said to be named for Elnathan Toby, supposedly the first white settler to climb it. In the 19th century, though, the prominent geologist Edward Hitchcock criticized this rather bland name. Hitchcock, who would later serve as president of Amherst College, published a report on the state’s geology in 1841. In it, he included Mount Toby, along with Sugarloaf and a number of other peaks, as part of a list of “uncouth and vulgar names” for Massachusetts mountains. Hitchcock tended to prefer Native American names, and he succeeded in renaming several peaks, including Hilliard’s Knob, which was renamed Mount Norwottuck in a large mountaintop ceremony in 1846. He made a similar attempt on Mount Toby three years later, naming it Mettawompe in honor of the Native American chief who had sold the surrounding land to white settlers. However, unlike Norwottuck, this name didn’t stick, apparently because of local opposition among Sunderland residents, and the mountain has continued to be known as Mount Toby.

Aside from the ill-fated attempts to operate a summit house on Mount Toby during the 19th century, the mountain has remained largely undeveloped, and today it looks essentially the same as it did when the first photo was taken around 1891. The town of Sunderland has also retained much of its rural appearance, and many of the houses along Main Street are still standing, as is the 1836 First Congregational Church, which is visible on the right side of both photos. Another town landmark in this scene is the Buttonball Tree. Although not identifiable from this distance, it stands near the center of the scene in both photos, about a quarter mile north of the church. With a girth of over 25 feet, this sycamore tree is one of the widest trees in the region, and it is estimated to be over 350 years old. Overall, probably the only easily-noticeable difference in these photos is the bridge over the Connecticut River. The one in the first photo was built in 1877, and it spanned the river until 1936, when a bridge further upstream was washed away in a flood and crashed into this bridge.

In the meantime, here on South Sugarloaf, the mountain continues to offer some of the finest mountaintop views in the state. It is now part of the Mount Sugarloaf State Reservation, and there is an auto road to the summit, along with several short hiking trails. In place of the 19th century summit house, the mountain is now topped by an observation tower with several different levels of platforms.

Deerfield River Valley, Charlemont, Mass

The view looking east along the Deerfield River in the western part of Charlemont, around 1891. Image from Picturesque Franklin (1891).

The scene in 2021:

These two photos show the road heading toward the center of Charlemont, with the Deerfield River on the right and the distinctive summits of Mount Peak in the distance. Today, the road is known as the Mohawk Trail, and its route through the Berkshires offers some of the finest scenery in the state. However, the current road is largely an early 20th century creation, and its route over the mountains bears little resemblance to its predecessors.

The northern Berkshires have long been a major obstacle to east-west travel through the area. Unlike further south, there are no low-elevation mountain passes here. For a westbound traveler, heading in the opposite direction of where these photos are facing, the Deerfield River valley provides an easy route deep into the mountains. However, a few miles to the west of here, the narrow valley turns abruptly to the north at the base of the Hoosac Mountains. These mountains form a continual ridgeline for miles in either direction, with elevations exceeding two thousand feet.

In the pre-colonial period, Native Americans crossed the mountains by way of a footpath, but not until the 1750s did European settlers build a road across the mountain. This road was later improved and partially rerouted in the 1760s, and it appears to have followed the Deerfield River before ascending along the northern slope of Clark Mountain.  Then, in 1797, the Second Massachusetts Turnpike was incorporated to construct a toll road across the mountains. Rather than beginning the ascent at Clark Mountain, this road followed the river along present-day Zoar Road and River Road almost as far as the current site of the Hoosac Tunnel, before climbing up the mountain by way of Whitcomb Hill Road. However, many travelers chose to continue taking the older road in order to avoid paying tolls on the new turnpike, so the older road came to be known as a “shunpike.”

This information is relevant to this particular site here in Charlemont, because the rest area on the right side of the present-day photo is known as the Shunpike Rest Area. It features a historical marker, installed by the Mohawk and Taconic Trail Association in 1957, that reads:

To the Thrifty Travelers of the Mohawk Trail who in 1797 here forded the Deerfield River rather than pay toll at the Turnpike Bridge and who in 1810 won the battle for free travel on all Massachusetts Roads.

However, despite the claims of this sign, there seems to be little historical evidence to suggest that this spot in Charlemont was where shunpike travelers would ford the river. The turnpike bridge over the Deerfield River was some 3.5 miles further upstream from here, at the border of Charlemont and Florida. That bridge was also the eastern end of the turnpike; the company’s original charter allowed it to construct a turnpike over the mountain “from the west line of Charlemont.” In addition, that bridge was the point where the turnpike and the older road diverged, so it seems more likely that these “shunpikers” would have crossed the river somewhere near that bridge, rather than several miles downstream at this spot.

In any case, the first photo was taken sometime around the early 1890s, only a few decades before the road through the mountains was substantially upgraded with the construction of the Mohawk Trail. Heading west through Charlemont, it follows existing roads as far as this spot here, but just to the west of here, in the opposite direction of these photos, the Mohawk Trail crosses to south side of the Deerfield River. It then follows the steep, narrow gorge of the Cold River, a smaller tributary of the Deerfield, before making its final ascent to the plateau at the top of the ridgeline.

With its current route, the Mohawk Trail completely bypasses the earlier roads up the eastern side of the mountain, including both the turnpike and the earlier shunpike. It also does not go anywhere near the part of the Deerfield River where turn-of-the-19th-century shunpikers would have most likely forded the river. If that is the case, it raises the question of why this historically-dubious marker would have been placed here at this rest area.

The answer might have something to do with the date that this historical marker was installed here. The modern-day Massachusetts Turnpike, which bears no relationship to similarly-named roads of the 19th century, opened in 1957, the same year that this marker was installed. According to newspaper articles from the period, local residents along the Mohawk Trail were concerned that the new highway would hurt business here in the northern part of the state. So, the Mohawk and Taconic Trail Association created the slogan “Go turnpike—return shunpike” in the hopes of encouraging motorists to make a grand tour of western Massachusetts, rather than taking the turnpike in both directions.

Probably not coincidentally, this was the same association that, around the same time, dedicated this historical marker “To the Thrifty Travelers.” It would not have been possible to place such a marker on the Mohawk Trail at the seemingly more plausible site of the shunpike ford, since the road does not go there. Instead, the road’s promoters seem to have played fast and loose with the history in order to appeal to nostalgia and Yankee frugality, in order to boost tourism through here.

Regardless of the accuracy of the historical marker, though, this particular section of the Mohawk Trail has been part of the east-west route through the northern Berkshires since at least the 18th century, with maps as early as the 1790s showing it taking this same course eastward toward Charlemont. The road is very different from its appearance in the first photo, and the rest area now takes the place of the meadow next to the river, but the road is still in the same spot, and this scene is still easily recognizable from the first photo because of Mount Peak in the distance.

Ocean Bank, Stonington, Connecticut

The First National Bank building, formerly the Ocean Bank, on the north side of Cannon Square in Stonington, in November 1940. Photo by Jack Delano, courtesy of the Library of Congress, FSA/OWI Collection.

The scene in 2021:

The first photo was taken in November 1940 by Jack Delano, a noted photographer who was employed by the Farm Security Administration in the late 1930s and early 1940s. In this capacity, he was part of a team of photographers who traveled around the country, documenting life in America during the Great Depression. He was in Connecticut during the fall of 1940, where he visited a number of cities and towns, including here in Stonington. His caption for this photo is simply, “A bank for sale in Stonington, Connecticut,” and he perhaps chose this subject as a way of representing the effects of the Depression on the once-prosperous whaling and fishing port.

Nearly a century before its demise in the Great Depression, the First National Bank of Stonington had its origins in 1851, with the incorporation of the Ocean Bank. This small Greek Revival bank building was constructed around this time, and the bank’s first president was Charles P. Williams, a former whaling ship captain. Williams had gained considerable wealth in the whaling industry, and he went on to further expand his fortune through real estate speculation. By the time he died in 1879, he was said to have been the wealthiest man in eastern Connecticut, with an estate valued at around $3 million.

In the meantime, the Ocean Bank became the First National Bank of Stonington in 1865, and it would remain in business here in this building for the next 75 years. However, the bank ultimately closed in February 1940, leaving the town of Stonington without any financial institutions. The bank’s president at the time, Judge J. Rodney Smith, explained in newspaper accounts that, although the bank itself was financially sound, the business conditions in town made the bank unprofitable for investors. He apparently did not cite specific reasons for this, but a likely cause was the ongoing Great Depression, along with the recent hurricane in September 1938, which battered coastal Connecticut.

As the sign in the first photo shows, the bank building was still for sale when Jack Delano took the photo some nine months after the bank closed. The building would ultimately be acquired by the Stonington Historical Society in 1942. The organization originally intended to turn the building into a museum and headquarters, but over the years it has instead been used as a rental property. Today, the historical society still owns the building, which has remained well-preserved in its 19th century appearance. It has also retained its original use as a bank, and it is currently a branch of Dime Bank, as shown on the sign on the left side in the 2021 photo.

Boston and Albany Railroad Arch Bridge, Becket, Mass

An early 20th century postcard showing the view looking east along the Boston and Albany Railroad, with a stone arch bridge on the left side and the Westfield River on the right. Image from author’s collection.

The scene in 2021:

The first railroads in the United States were constructed starting in the late 1820s. These were mostly concentrated in the northeast, and they tended to be relatively short lines that linked neighboring cities. Here in New England, Boston soon emerged as an important railroad hub, and by the mid-1830s it had three different lines that radiated outward as far as Lowell, Providence, and Worcester. However, railroad investors had far more ambitious plans, including one proposal that would extended the line west of Worcester all the way to Albany.

Throughout the colonial era, and into the early 19th century, Boston had been one of the most important seaports in the present-day United States. However, as settlers moved west, and as the country acquired new territory, Boston found itself on the far eastern edge of a nation that was rapidly expanding westward. The opening of the Erie Canal in 1825 further threatened Boston by linking New York City with the Midwest, making it the primary seaport for trade with the inland regions.

As early as 1826, the Massachusetts state legislature had begun exploring the possibility of a railroad from Albany to Boston. This would prevent Boston from becoming economically isolated from the rest of the country, by providing an alternate route to the sea for goods transported along the Erie Canal. The state subsequently hired prominent civil engineer James F. Baldwin to examine potential routes through the state. The most promising was a southerly route, which would head west from Worcester through Springfield and Pittsfield before crossing into New York. This is, more or less, the route that would ultimately be opened a little over a decade later.

To achieve this goal, the Western Railroad was incorporated in 1833, although construction work did not start until 1837. The eastern half of the railroad, from Worcester to Springfield, was relatively easy to build, and it opened on October 1, 1839. However, the western portion, which crossed the mountains of the Berkshires, was a far more challenging engineering feat. By this point, railroad technology was still in its infancy, and there were still significant questions about the ability of steam locomotives to operate on steep grades. Some doubted whether a locomotive could handle grades greater than one percent (one foot of vertical rise for every hundred feet of track), and many early railroads used steam-powered inclined planes to pull trains up steep sections of the route. However, any crossing of the Berkshires would require consistent grades in excess of one percent, in some places even exceeding 1.5 percent.

To reach the divide between the Connecticut River and Housatonic River watersheds, the route of the railroad followed the Westfield River to the west of Springfield. In the town of Huntington, the river splits into three main branches, with the railroad continuing upstream along the west branch. From there, the river valley becomes increasingly narrow and winding, particularly in the last 13 miles from Chester to the watershed divide in Washington.

In order to oversee this project, the railroad hired George Washington Whistler as chief engineer. An 1819 graduate of West Point, Whistler was one of the nation’s leading civil engineers, and he was involved in the construction of many early railroads. He would go on to earn international fame from his accomplishments here on the Western Railroad, and Czar Nicholas I of Russia subsequently hired him to build the Saint Petersburg–Moscow Railway. However, Whistler’s fame would ultimately be eclipsed by his son, the prominent artist James Abbott McNeill Whistler, who was a young child living with his family in Springfield when George Washington Whistler built the Western Railroad.

For Whistler, the most difficult part of the project would be the 13 miles between Chester and Washington, where the railroad rose in elevation from 600 feet in Chester to 1,459 feet at the watershed divide. This was a serious challenge, given the concerns about the technical limitations of steam locomotives, but Whistler also had to build this railroad within the confines of a narrow, sinuous river gorge. This meant the railroad would require a series of deep rock cuts and high embankments, along with repeated crossings of the river, in order to maintain a reasonable grade. Even so, the finished railroad would have a six-mile section with an average grade of 1.51 percent, and a maximum grade of 1.57 percent.

Probably the most distinctive feature of this section of the railroad is its many bridges. The railroad crossed the river a total of 21 times in these 13 miles, and ten of these bridges were masonry arch bridges, including the one shown here in these two photos. The original intent had been to use simpler bridges with rubble masonry abutments, but these would have been vulnerable to spring flooding, so the railroad opted for more substantial arch bridges. This required excavating down to bedrock to anchor the abutments, and it also meant bringing in quarried stone from elsewhere, since the local stone proved to be of inferior quality. This was a significant expense for the railroad, as these quarried blocks—which weighed upwards of a thousand pounds each—had to be transported along rough roads to these remote work sites along the river.

Aside from the bridges, other labor-intensive work included the many cuts and fills along the railroad bed. A little to the east of the bridge in this photo, just beyond the curve in the distance, is a deep rock cut, measuring about 575 feet long and 30 to 40 feet deep. In the days before dynamite and other high explosives, this work would have been done using only black powder and hand tools such as picks and shovels. Beyond this rock cut was an embankment, with a long stone retaining wall that had to be built to keep the railroad bed from sliding off the steep cliff down to the river. A few miles to the west of the stone bridges, at the highest point of the railroad in the town of Washington, was an even larger rock cut. It was about a half mile long, and 55 feet deep at its deepest point.

All of this work, including the unanticipated need for stone arch bridges, led to significant cost overruns for the Western Railroad. In 1838, prior to the start of construction, the cost of building section of the railroad to the west of the Connecticut River was estimated at $2.1 million. The actual cost turned out to be a little over $2.5 million, including nearly $1 million just to build a 13-mile section here in the Berkshires. The single most expensive mile was just a little to the east of the scene in these photos, between mile markers 127 and 128. Within that mile, the railroad crossed the river three times on large stone arch bridges, and cost nearly $220,000. The company’s January 1841 annual report explained some of the reasons for these added expenses, quoting the engineer (presumably Whistler), who wrote about the challenges of building the railroad through this section along the Westfield River:

With the limited knowledge of the character of the stream here, at the time of the original estimate, and, judging of its effects in times of freshets, from the comparatively unstable character of the structures then existing on the turnpike, occupying almost the immediate line of the rail-road, in tolerable security, it was then judged that structures of the more ordinary kind, with common rubble masonry for bridge abutments and side walls, would give ample security to the road, and such was estimated for. But the experience in time of our personal knowledge of the effects of freshets in this stream, proved the necessity of abandoning such structures, and resorting to others of a more costly and permanent character. Stone arches of large openings were adopted, requiring masonry of a very different and superior character to support them;—rendering it necessary too to resort to great depths in search of permanent rock foundations below the bed of the stream. This was the more readily acceded to at the time, from the belief (as every appearance indicated) that materials suitable for such structures would be obtained from the rock cuts in their immediate vicinity. But soon after they were commenced, and the character of the stone exposed by the opening of the cuts, it proved entirely unfit; and the contractor was compelled to resort to quarrying and hauling the stone from a distance, and over roads almost impassible;—thus rendering it necessary to increase his prices to meet this additional cost.

The work of actually building the railroad was largely done by immigrant laborers, primarily the Irish. At one point there were several thousand workers employed here, and this is evident in the 1840 census, which was conducted in the midst of the railroad construction. In a sort of precursor to the later railroad boom towns that would follow the First Transcontinental Railroad several decades later, the town of Middlefield—located on the north side of the river—saw a particularly dramatic increase in population. From a population of 720 in 1830, Middlefield grew to 1,717 in 1840, with the census noting that 686 were from “Middlefield proper,” while the rest were counted as “extraneous population.”

These workers generally lived in temporary shantytowns along the river, and the census indicates that most were in their 20s or 30s, with few over the age of 40. The 1840 census does not provide much specific demographic information, and only the heads of the households are individually named, but the census data suggests that most of these men lived here with their families. Most of the households included both a man and a woman who were between the ages of 20 and 40, along with several young children who were generally under the age of 10. The surnames of the heads of household were overwhelmingly Irish, with Murphy being a particularly common name among the workers in Middlefield.

The arrival of so many foreign immigrants in a small, rural community was not without controversy. Early in the construction process, in the spring of 1839, the Hampshire Gazette published an article titled, “The Irish on our Public Works,” which addressed concerns about the societal impact of the Irish immigrants who were working on the railroad. The article warned that, “[i]f some measures are not taken for the education and moral reformation of the multitudes of Irish and other foreign emigrants that swarm the country, our republic will be much in danger from them.” Perhaps in response to these concerns, a few months later a resident of Middlefield began raising funds to establish three schools for the children of the laborers. It seems unclear as to whether these contributions were motivated by genuine altruism or by nativist fears about an under-educated immigrant class, but a subsequent article in the Boston Evening Transcript declared that the students were “learning rapidly, and doing credit to the labors of their benefactors.”

These workers remained here throughout the summer of 1841, and the railroad was ultimately completed in the early fall, with the final tracks laid at the rock cut in Washington on October 2, 1841. The railroad opened two days later, linking Boston and Albany. In the process, the railroad set a number of records. It was, up to that point, the longest and most expensive railroad in America, and it was also the first to be built through mountains without using steam-powered inclined planes to assist locomotives. As such, it was a significant engineering milestone, and it was enough to gain the attention of the czar, who brought Whistler to Russia as soon as his work here on the Western Railroad was finished.

However, despite the completion of the railroad, there would continue to be challenges, including a fatal accident that occurred on October 5, 1841, just a day after the line opened. The railroad originally just had one track, with occasional passing sidings for trains heading in opposite directions, including ones at Chester and Westfield. On this particular day, both the eastbound and westbound trains were given instructions to meet at Chester before proceeding. However, the eastbound conductor apparently never received this message, and was expecting to meet the other train further down the line in Westfield. This resulted in a head-on collision about four miles west of Westfield, killing the conductor of the eastbound train and one passenger, along with injuring many others. The accident was a personal tragedy for George Washington Whistler, whose niece, Caroline Bloodgood, was on the train. She was among those injured, and her young son was the one passenger who was killed in the accident.

The Western Railroad did manage to help dispel the myth that steam locomotives were unable to ascend steep grades under their own power, but the section of the railroad here in the Berkshires was nonetheless challenging for trains. Whistler had selected locomotives that were built by Ross Winans of Baltimore, a friend of his whose daughter Julia would later marry his son George. Nicknamed “crabs,” presumably because of their eight drive wheels and Maryland origins, these locomotives proved unreliable here on the Western Railroad, and the railroad ultimately resorted to custom building their own mountain locomotives at their shops in Springfield.

Despite these setbacks, the railroad overall proved to be a success, and for many years it was the only east-west railroad through the Berkshires, providing an important transportation link between Boston and the rest of the country. Although it was originally built as a single-track railroad, Whistler had wisely designed the bridges and other structures to accommodate a second track. This made the initial construction costs higher, but in the long run it saved the railroad money by making it easy to add a second track without having to reconstruct all of the bridges.

For travelers along the route, this section through the Berkshires was a highlight of their journey. The 1847 travel guide A Chart and Description of the Boston and Worcester and Western Railroads, published only six years after the railroad opened, provides the following description:

No language that we are master of could give the traveller any proper description of the wildness, the grandeur, or the obstacles surmounted in the construction of this portion of the route. The river is exceedingly crooked, and the lofty mountains, which are very steep and rugged, and of solid rock, shut down quite to the river on both sides, their sharp points shooting by each other, rendering crossings at every bend of the stream indispensable. In addition to this, the points of the hills must be cut away, and for many miles these rock cuttings and bridges follow each other in regular and rapid succession. . . . Nor does the passing traveller, hurling along as rapidly as he is, see much of the beauty of this mountain gorge. It is not until he has seen, from the base of these mighty structures of art, the passage of the cars, that their magnificence is really felt.

The Western Railroad would ultimately merge with the Boston and Worcester in 1867, forming the Boston and Albany Railroad. This company would, in turn, be leased by the New York Central starting in 1900, although this line retained the Boston and Albany name well into the 20th century. In the meantime, the railroad continued to make improvements to the route, including some changes here along the banks of the Westfield River. A few of the original bridges were replaced, including the easternmost one, which was replaced in 1866 with the current double arch bridge. The next bridge upstream from there was replaced in 1912 with the current steel deck truss girder bridge, although the original stone abutments appear to still be there, encased in poured concrete. Much further upstream, the westernmost two bridges were apparently reconstructed in 1928 after having been damaged in a flood, although it is possible that portions of the original bridges are still underneath the concrete.

However, the most significant change to this portion of the railroad occurred in 1912, when about a mile of the railroad was rerouted, including the section shown here in these two photos. The first photo was probably taken only a few years before this occurred. The postcard is undated, and does not have a postmark, but it has an undivided back, suggesting that it was printed before 1907. As part of this realignment, the railroad shifted to the south side of the river, eliminating two of the river crossings. One of the original bridges, located about 300 yards west of here, was demolished as part of this project, in order to make room for a new bridge. Three other original bridges were simply abandoned, including this one here, which is the westernmost of the three.

Today, more than a century after the railroad was rerouted, these three bridges are still standing. One of them, the easternmost, is still on land owned by the railroad, and it is directly adjacent to the active rail line, so it is not accessible to the public. However, the other two bridges, along with the 3,000-foot section of abandoned railroad right-of-way between them, are now owned by the state as part of the Walnut Hill Wildlife Management Area. The bridges are accessible by way of the Keystone Arch Bridge Trail, a 2.5-mile long trail that starts in Chester. Despite being over 180 years old, and despite not having been maintained in well over 100 years, these bridges remain in good condition, clearly fulfilling Whistler’s goal of creating bridges of “a more costly and permanent character.”

As the travel guide had indicated back in 1847, it is hard to get a sense of the scale of these bridges from the railroad. Even today, it is hard for visitors to tell just how big these bridges are while standing atop them, and photographs are likewise unable to capture the full scope of these structures. Only by climbing down to the river and looking up at the arches can a visitor fully appreciate the size of the bridges, and the work that went in to building them in the middle of a river gorge in one of the most remote areas of the state.

Of the three surviving bridges, the one here in this scene is the largest. Including the wingwalls, the structure of the bridge is over 500 feet long, the bridge deck is about 25 feet wide, and the top of the bridge rises about 75 feet above the river. The bottom of the arch is about 60 feet above the water, and the total span of the arch is 54 feet. The bridge is mostly in its original condition, although about three-quarters of the parapet stones are gone, having apparently been pushed over the edge by vandals over the years.

In 1980, this bridge was added to the National Register of Historic Places as a contributing structure in the Middlefield–Becket Stone Arch Railroad Bridge District. Then, in 2021, the two surviving stone arch bridges on public property, including this one, were designated as National Historic Landmarks as part of the Western Railroad Stone Arch Bridges and Chester Factory Village Depot district. The district is also comprised of the railroad bed in between the two bridges, including the large rock cut and stone retaining wall, along with the historic railroad station in the center of Chester, several miles to the east of here. This station is owned by the Chester Railway Station and Museum, which features an extensive collection of artifacts relating to the Western Railroad and the construction of these bridges.

For more information on the history of these bridges, the National Historic Landmark Nomination Form is an excellent resource. The Friends of the Keystone Arches also has an excellent website, with plenty of historical information and photographs, along with information about hiking to the bridges.

Eastern View From Catskill Mountain House, Catskill, New York

The view looking east from the Catskill Mountain House, around 1902. Image courtesy of the Library of Congress, Detroit Publishing Company Collection.

The scene in 2021:

These photos were taken from the same spot as the ones in the previous post, but these are facing more to the east, directly across the Hudson River Valley. When the first photo was taken, this was the site of the Catskill Mountain House, a hotel that had been constructed here in 1824. Because of its dramatic views and easy accessibility from New York and other large cities, the hotel soon became one of the country’s most popular resort destinations. These views also helped to inspire a number of prominent artists, including Thomas Cole, the founder of the art movement that would come to be known as the Hudson River School.

Originally, most guests would have reached the Mountain House by taking a Hudson River steamboat to the village of Catskill, which is located in the distance on the far left side of these photos. From there, it was a 12-mile stagecoach ride to the Mountain House, which took about three or four hours. However, by the time the first photo was taken at the turn of the 20th century, railroads had shortened this travel time to just 40 to 50 minutes. The narrow gauge Catskill Mountain Railroad took guests to the base of the escarpment, and then the remaining portion of the journey was by way of the Otis Elevating Railway, a 1.3-mile-long funicular railroad that rose more than 1,600 feet in elevation from the valley to the Mountain House. A portion of this railroad, including the large trestle near the base of the incline, is visible in the lower center of the first photo.

For guests at the Mountain House, one of the highlights of their stay was to watch the sunrise from this vantage point. Early in the summer season, the sun rises on the extreme left side of these two photos, but as the summer progresses the sunrise location migrates steadily to the west. By mid-October the sun rises directly above Mount Everett in the center of this scene, and by the winter solstice the sunrise is on the far right side, although few 19th century visitors would have seen it, since the hotel was only open during the warmer months.

Among those inspired by the sunrise here was artist Frederic Edwin Church, a student of Thomas Cole. One of his earliest paintings, Morning, Looking East over the Hudson Valley from Catskill Mountains (1848), shows the sunrise here, with an emphasis on sunlight and clouds that would become a major characteristic of his later works. Church would subsequently travel the world for subject matter for his landscape paintings, but in the early 1870s he returned to the Catskills and built his one, Olana, on the east side of the Hudson River, opposite the village of Catskill. This house still stands as a museum, and it is barely visible in the distance of the second photo.

Today, some 120 years after the first photo was taken, the Catskill Mountain House is long gone, having been deliberately burned in 1963 after sitting vacant for more than 20 years. However, the view from here is as impressive as ever, and from this distance there are not too many major changes to the landscape. Perhaps the most significant difference is the number of trees in this scene. When the first photo was taken, there were many open fields here in the valley. However, with the decreased importance of agriculture in this region, many of these fields have now been reclaimed by trees, resulting in a landscape that is far more forested than what the 19th century guests of the Mountain House would have seen.

Northeastern View From Catskill Mountain House, Catskill, New York

The view looking northeast across the Hudson River Valley from the Catskill Mountain House, around 1900-1910. Image courtesy of the Library of Congress, Detroit Publishing Company Collection.

The view in 2021:

As explained in an earlier post, the Catskill Mountain House was built in 1824 on a ledge along the Catskill Escarpment. This site is located on the far eastern edge of the Catskill Mountains, about 2,200 feet above sea level. From here, the landscape drops abruptly to the east, with the Hudson River just eight miles away. As a result, this site offers dramatic views of the river valley, which is visible for many miles in either direction. Further in the distance, on the eastern edge of valley, are the Taconic Mountains, which run along the New York-Massachusetts border. Among the peaks visible in this scene is Mount Greylock, the highest point in Massachusetts, located 54 miles to the northeast of here.

This view drew visitors to the Mountain House for well over a century, and it was often declared, rather hyperbolically, to be one of the greatest views in the country. While unquestionably an impressive view, it pales in comparison to those from some of the higher peaks in the northeast, let alone the many grand views in the mountain ranges of the west. However, this site was probably the finest view that was readily accessible to the masses during the 19th century, as it was within easy reach of New York City and other large population centers.

The Catskills began to wane in popularity shortly after the turn of the 20th century, not long after the first photo was taken. In part, this was because of expanded transportation options; rather than depending on steamboats or railroads to taken them up the Hudson River to the Catskills, Americans now had the luxury of transcontinental trains, along with private automobiles that could take them to previously unreachable vacation spots. The Mountain House ultimately closed after the 1942 season, and the building steadily deteriorated for the next two decades before being deliberately burned in 1963.

Today, the site of the Mountain House looks very different, with an empty field marking the spot of what had once been the country’s finest resort hotel. However, as shown in these two photos here, the view that enticed so many visitors throughout the 19th and early 20th centuries is still largely unchanged. The Hudson River Valley is certainly much more developed than it was more than a century ago, but it is hard to tell from this view more than 1,600 feet above the valley. From this distance, modern developments like highways and suburban sprawl tend to blend in with the rest of the landscape. It is also interesting to note that there actually appears to be more forested now than in the early 1900s, reflecting changing land use patterns and a decline of large-scale agriculture here in the river valley.