Mt. Washington

Great Gulf, Mount Washington, New Hampshire

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The Great Gulf, seen from just north of the summit of Mount Washington, around 1900. Image courtesy of the Library of Congress, Detroit Publishing Company Collection.

The scene in 2021:

These two photos show the view looking north from Mount Washington, with the Great Gulf in the foreground and the summits of the northern Presidential Range beyond it. Mount Washington is the highest peak in New England and the northeastern United States, and it stands at the center of the Presidential Range, a north-south oriented range that contains many other high peaks. The five highest peaks are named after the first five presidents, mostly in descending order of elevation, and each one is higher than any other mountain in the northeast outside of the Presidential Range.

Mount Washington, the highest, is 6,288 feet above sea level. It is followed by Mount Adams (5,774 feet), which is seen on the right side of this scene; Mount Jefferson (5,712 feet) on the left side of the scene; Mount Monroe (5,384 feet) out of view on the opposite side of Mount Washington; and Mount Madison (5,367 feet) on the extreme right-hand side of this scene.

Just out of view in the foreground on the right side is a portion of Mount Washington, which extends to the northeast away from the summit area. That slope of Mount Washington, along with the northern Presidentials in the distance, form the walls of the Great Gulf, a large glacial cirque. There are a number of different cirques around Mount Washington that were formed by glacial activity, including Tuckerman Ravine, Huntington Ravine, and Ammonoosuc Ravine. However, the Great Gulf is by far the largest of these, extended more than two miles in length and over a mile in width.

The first recorded description of the Great Gulf comes from Darby Field in 1642. Although this was still very early in the history of European colonization in New England, and several centuries before recreational hiking became popular in the region, Darby Field and his two Native American guides became the first known people to have climbed Mount Washington. This achievement was considered remarkable enough that John Winthrop, governor of the Massachusetts Bay Colony, provided a lengthy account of Field’s expedition in his journal. Regarding the final ascent to the summit, Winthrop wrote:

They went divers times through the thick clouds for a good space, and within 4 miles of the top, they had no clouds but very cold. By the way among the rocks, there were two ponds, one a blackish water, and the other reddish. The top of all was plain about 60 feet square. On the north side was such a precipice, as they could scarcely discern to the bottom. They had neither cloud nor wind on the top, and moderate heat. All the country about him seemed a level, except here and there a hill rising above the rest, and far beneath them. He saw to the north, a great water which he judged to be 100 miles broad, but could see no land beyond it.

Although Winthrop’s description was secondhand information at best, the account seems reliable, since it contains information that Field would only have known if he had actually reached the summit. The “two ponds” are likely the Lakes of the Clouds, located along the ridgeline between the summits of Mount Washington and Mount Monroe, and the description of the “plain” at the summit likewise corresponds to reality. And, his description of the Great Gulf also helps to verify the account, since Field would have only known about “such a precipice, as they could scarcely discern to the bottom” if he and his guides had actually stood here at the edge of the Great Gulf headwall.

Aside from Field’s journey, there were very few recorded ascents of Mount Washington during the colonial period. However, this began to change by the early 19th century, as New Englanders began to travel to the White Mountains to experience the scenery here. By 1819 there was a footpath from Crawford Notch to the summit, and this was later followed by a carriage road in 1861 and a cog railway in 1868. The summit area became a seasonal community, with several hotels and even its own newspaper.

However, despite the extensive development on Mount Washington, the other summits on the Presidential Range remained largely untouched, as did the Great Gulf. Visitors were generally happy to admire these scenes from afar, and there were few landscapes that could compete with this view here in these photos. Writing in his 1856 book Incidents in White Mountain History, Benjamin G. Willey provided the following description of this scene:

[G]oing a few rods northward, you come to the brink of an almost unfathomable abyss, known as the Great Gulf. It is a rocky, precipitous descent of two thousand feet. Rising up opposite you from the bottom of this Gulf, almost perpendicularly, is the great range of mountains, comprising Clay, Jefferson, Adams and Madison. This vast range may be seen from their roots to their summits by one standing on the brink. Deep down in the very bottom of the hollow are rough, confused piles of rocks, with narrow and deeply-worn ravines between them. Springing up occasionally, near the very base of the mountain range, are tall spruces, while further up on their sides are birches and small firbushes. Toward the east, the Gulf has an opening, surrounded on all its other sides by mountains.

A few years later, in his 1860 book The White Hills: Their Legends, Landscape, and Poetry, described the scene in even more rapturous language, from an overlook on the nearby carriage road. He wrote:

Yet the glory of the view is, after all, the four highest companion mountains of the range. Clay, Jefferson, Adams, Madison, that show themselves in a bending line beyond the tremendous gorge at the right of the path, absurdly called the ” Gulf of Mexico,” and are visible from their roots to their summits. . . . Except by climbing to the ridge through the unbroken wilderness of the northern side, there is no such view to be had east of the Mississippi of mountain architecture and sublimity. They do not seem to be rocky institutions. Their lines have so much life that they appear to have just leaped from the deeps beneath the soil. We say to ourselves, these peaks are nature’s struggle against petrifaction, the earth’s cry for air.

This scene certainly captivated visitors, but few were adventurous enough to actually descend into this “unfathomable abyss.” Because of its remoteness, the upper reaches of the Gulf escaped large-scale logging, and even the trail builders of the late 1800s tended to avoid the area. A single hiking trail was built through the Gulf as far as Spalding Lake in the lower foreground of these photos, but it did not ascend the headwall of the mountains. Nor did it apparently see much use, because it did not see much subsequent maintenance.

The Great Gulf was still an essentially trailless wilderness when the first photo was taken around 1900, but this would soon change. From 1908 to 1910, Warren W. Hart oversaw the construction of a series of trails in the area, starting with the Great Gulf Trail, which traversed the Gulf, climbed the headwall, and ended near the spot where these two photos were taken. Another trail, named the Six Husbands Trail, was opened to the summit of Mount Jefferson by way of the steep slopes in the right-center of the scene. Two other trails—Adams Slide and the Buttress Trail—climbed Mount Adams, and the Wamsutta and Chandler Brook Trails climbed the northeastern slopes of Mount Washington from the Great Gulf.

At the time, the Great Gulf was still in private hands, but in 1916 it was purchased by the U.S. Forest Service. It subsequently became part of the White Mountain National Forest, and in 1964 it was designated as the Great Gulf Wilderness, which conferred greater protections on the land than other portions of the national forest. As a result, this view from atop the headwall looks essentially the same as it did over 120 years earlier, and in all likelihood it also looks the same as it did over 380 years ago, when Darby Field first described the “precipice” where he could “scarcely discern the bottom.”

Mount Jefferson from Mount Monroe, New Hampshire

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Mount Jefferson and the northern Presidential Range from near the summit of Mount Monroe, around 1900. Image courtesy of the Library of Congress, Detroit Publishing Company Collection.

The scene in 2020:

The first photo here was taken from the same spot, and perhaps even on the same day, as the one in the previous post. However, while that photo shows the summit of Mount Washington from Mount Monroe, this view looks a little further to the west, showing the western side of Mount Washington with Mount Jefferson further in the distance. As was the case with the previous post, I took the 2020 photo without having first seen the 1900 one. I took the photos during a hike along the southern Presidential Range from Crawford Notch to Mount Monroe, and later discovered that several of the photos lined up perfectly with ones that were taken around 1900 by the Detroit Publishing Company. In this particular view, perhaps the most remarkable similarity is that both photos show a Mount Washington Cog Railway train in the exact same location, right in the center of the photo.

The highest mountain visible in this scene is Mount Jefferson, which is a little over three miles away from here. At 5,712 feet, it is the third-highest peak in the northeastern United States, after the nearby Mount Washington and Mount Adams. Along with Mount Madison and Mount Monroe, these comprise the five highest peaks in the region, and they are named in honor of the first five presidents, with the elevation rank corresponding to the order in which they served as president. However, Madison and Monroe are very close in elevation, and subsequent surveys discovered that Monroe is actually slightly higher, despite being named for the fifth president.

Aside from Mount Jefferson, the most visible landscape feature here is Ammonoosuc Ravine, a large glacial cirque in the foreground that forms the western slope of Mount Washington. Further in the distance is Burt Ravine, a somewhat smaller cirque to the northwest of Mount Washington. In between these two ravines is a ridgeline that runs diagonally across this scene. The steep slopes of this ridge, combined with the heavy precipitation here, makes it prone to landslides, and both photos show the scars of large slides here on the southern side of the ridge.

Both photos also show the Mount Washington Cog Railway, which runs along this ridge between Ammonoosuc and Burt Ravines. Completed in 1869, this three-mile railroad was a major engineering feat, with trains rising about 3,500 feet in elevation from the base station to the summit. This was far too steep for conventional trains, so the railway’s founder, Sylvester Marsh, developed a rack-and-pinion system with a gear on the locomotive that engaged a rack in the center of the track. This allowed the gear to pull the train up the mountain, and then safely lower it in a controlled descent on the return trip.

The Mount Washington Cog Railway was the first of its kind in the world, and it today it is the world’s second-steepest railroad. The single steepest part of the route is a trestle known as Jacob’s ladder, with a maximum grade of more than 37%. This trestle is visible in the center of both photos, and coincidentally both photos show a train at the same spot at the base of the trestle. As was the case more than a century ago, the trains still climb and descend with the locomotive always on the downhill side of the train and a single passenger coach facing uphill. The only difference is the type of locomotive; for most of the railroad’s history it operated steam locomotives, but it now primarily uses biodiesel locomotives, which are more environmentally friendly and less expensive to run.

Overall, the type of locomotive on the trestle is essentially the only difference between these two photos. Although the summit of Mount Washington has been heavily developed with over the years with many buildings and other structures, the rest of the Presidential Range has remained largely unchanged, with few signs of human activity aside from hiking trails. Most of the range, along with much of the surrounding land, is now protected as part of the White Mountain National Forest, which was established in 1918 and has grown to over 750,000 acres of land in New Hampshire and Maine.

Mount Washington from Mount Monroe, New Hampshire

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The summit of Mount Washington, seen looking north from Mount Monroe in the Presidential Range of the White Mountains, around 1900. Image courtesy of the Library of Congress, Detroit Publishing Company Collection.

The view in 2020:

Rising 6,288 feet above sea level, Mount Washington is the highest peak in the northeastern United States. It stands at the center of the Presidential Range, a north-south oriented mountain range that forms a massive ridgeline of bare rocks and alpine vegetation. The range is infamous for its harsh and unpredictable weather, particularly at the summit of Mount Washington, which for many years held the world record for fastest surface wind speed ever recorded, at 231 miles per hour. Hypothermia is a year-round threat to hikers, and although there is no permanent ice cap, pockets of snow can linger well into the summer, as shown in the 2020 photo, which was taken on June 18.

Aside from Mount Washington, most of the other peaks in the range are also named for presidents. The five highest peaks are named after the first five presidents, in order of elevation, so that Mount Adams is the second-highest and Jefferson the third-highest. However, Mount Monroe, where these photos were taken from, is actually the fourth-highest, but it was named for the fifth president because of a surveying error. Monroe is the southernmost of these five major peaks; to the south are several lower peaks in the Presidential Range, including Mount Eisenhower and Mount Pierce.

Mount Washington’s high elevation and inhospitable climate have long attracted visitors to the summit. The first recorded ascent occurred in 1642, when Darby Field climbed the mountain accompanied by two Native American guides. Governor John Winthrop recorded the event in his diary, referring to the mountain as “the white hill,” since the mountain’s eventual namesake would not be born for another 90 years. Field’s exact route is uncertain, but he evidently approached it from the south, as Winthrop mentions two ponds along the way, which were likely the Lakes of the Clouds shown here in this scene. Aside from helping determine Field’s route, the mention of the lakes also helps to verify his ascent, since he would not have known about them unless he actually climbed at least this far.

The mountain was only occasionally climbed during the rest of the 17th and 18th centuries, but this began to change in the early 19th century. In 1819, local residents Abel and Ethan Allen Crawford cut an 8.5-mile path from Crawford Notch to the summit of Mount Washington, following the ridgeline of the southern Presidential Range. The trail passed through this scene just to the East of the summit of Mount Monroe, and most of it is still in use today as part of the Appalachian Trail, making it the oldest continuously-maintained hiking trail in the country. Ethan Allen Crawford built a cabin, and later a hotel, at the base of the trail, and he also acted as a guide for hiking groups setting out from Crawford Notch. The Crawford family later improved the trail for use as a bridle path, and by the 1840s visitors could ride to the top of the mountain on horseback.

The first building at the summit was a small hotel that opened in 1852. It was joined a year later by the rival Tip Top House, which still stands atop the mountain today. At the time, the only ways to get to the top were by foot or by horseback, but this would soon change. The Mount Washington Carriage Road opened in 1861, bringing visitors up the east side of the mountain, and the Mount Washington Cog Railway followed eight years later on the western slopes of the mountain. These two routes helped to spur more development, and by the time the first photo was taken around 1900 the summit was crowded with buildings, including the Tip Top House, a weather observatory, and the massive Summit House hotel, which could accommodate 150 guests. The summit even had its own daily newspaper, Among the Clouds, which was published during the summer months from 1877 to 1917.

By the late 19th century it was easier than ever to reach the summit, but many visitors chose to test their abilities by hiking up the mountain. However, because of the mountain’s notorious and often unpredictable weather, this sometimes led to tragic consequences for unprepared or unlucky hikers. The first known fatality in the Presidential Range was Frederick Strickland, who began his hike on October 19, 1849, when the mountain was already covered in deep snow. He climbed via the Crawford Notch, and he would have passed through this scene on his way up the mountain. Strickland made it to the top, becoming the first known hiker to do so in winter conditions, but he ultimately succumbed to hypothermia while descending the western side of the mountain. His body was discovered well below the tree line, near where the present-day Jewell Trail crosses Clay Brook.

One of the most famous tragedies on the mountain occurred on June 30, 1900, when William Buckingham Curtis and Alan Ormsbee both died of hypothermia while ascending the mountain. Both men were experienced outdoorsmen, and Curtis was renowned as an athlete and promoter of amateur athletics. As with Frederick Strickland a half century earlier, they hiked up the Crawford Path from Crawford Notch. Their goal was to attend the Appalachian Mountain Club meeting at the summit, but they faced harsh conditions along the way, including dense fog, sleet, and high winds. They climbed to the summit of Pleasant Dome (now Mount Eisenhower), and they were last seen alive soon after by a descending group that warned them of the deteriorating conditions ahead.

The first photo was probably taken within a year or two of Curtis’s and Ormsbee’s deaths, and it shows the section of the mountain where their journey came to an end. It is unclear as to whether they took the Crawford Path to the east of Mount Monroe, or if they took  the loop trail over the summit, but just to the north of Monroe they took shelter in a dense stand of stunted spruce trees. For unknown reasons, they subsequently left this shelter, and Curtis’s body was discovered a short distance beyond the trees, somewhere near the foreground on the far right side of these two photos. Ormsbee managed to continue up the mountain, but he ultimately died just a few hundred feet short of the summit.

In the aftermath of this tragedy, the Appalachian Mountain Club built a small shelter here in the area between Mount Monroe and Mount Washington, near the spot where Curtis died. It was completed in 1901, and was large enough for about six to eight people, yet uncomfortable enough to discourage use for anything other than an emergency situation. However, hikers nonetheless used the shelter for regular camping, and in 1915 it was replaced by the Lakes of the Clouds Hut, which was built a little lower on the slope on the far left side of the scene. Far more than just serving as an emergency shelter, this hit was staffed by the AMC, and provided overnight accommodations along with meals for hikers.

Today, around 120 years after the first photo was taken, Mount Washington remains a popular destination, accessible either by train, by car, or by foot. The Lakes of the Clouds Hut has been expanded several times over the years, and it now has bunk space for 90 hikers. The hut is located at the convergence of several major trails, including the Crawford Path, which still follows essentially the same route that the Crawford family laid out more than two centuries ago. The only significant change to the path is here between Mount Monroe and Mount Washington, where it was rerouted to access the hut, and to eliminate unnecessary switchbacks.

Overall, this scene has changed very little since the first photo was taken, aside from the construction of the hut. The surrounding land is now protected as part of the 750,000-acre White Mountain National Forest, which was established in 1918. The Presidential Range is a particularly important part of this national forest, as it features a number of rare alpine plants, including the Robbins’ cinquefoil, an extremely rare flower that can only be found here on the slopes of Mount Monroe. Because of the fragile nature of many of these plant species, combined with the thousands of people who climb Mount Washington each year, one of the present-day challenges here is balancing conservation with recreation in order to ensure that this view continues to remain unchanged for the next 120 years and beyond.

Halfway House, Mt. Washington, NH

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The Halfway House on the Mount Washington Carriage Road in New Hampshire, around the 1870s. Image courtesy of the Mount Washington Auto Road.

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The scene in 2016:

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Mount Washington is the tallest peak in the northeastern United States, and it has been a popular tourist destination since the mid-19th century. By the end of the 1860s, the mountain had a hotel at the summit, along with both a cog railway and a carriage road to bring visitors to the top. The nearly eight-mile long carriage road opened in 1861, and this small building along the side of the road served an important purpose for early travelers. Known as the Halfway House, it was located about four miles up the road, hence the name, and it was used as a toll house. It was also a good resting place during the four-hour carriage ride up the mountain, and when necessary its location just below the treeline made it a refuge from the unpredictable and often dangerous weather in the alpine zone.

The building in the first photo was later replaced with a more substantial two-story structure. This one served the same purpose as the original, but over time it suffered from vandalism because of its isolated location, and it was finally destroyed by a fire in 1984. Today, the carriage road is now the Mount Washington Auto Road, and aside from cars replacing horses, not much has changed about the road, which still follows the same route that was laid out in the 1850s. The drive to the summit now takes about 30 minutes, and while the Halfway House no longer stands here, the site is still used as a stopping place. It is no longer necessary to rest horses here, but the climb is still taxing for cars, so the site here is used by drivers heading up the mountain to cool their radiators, and by those heading down to cool their brakes.

Mt. Washington Cog Railway

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The Mt. Washington Cog Railway, near the summit, probably in the early 1870s. Photo courtesy of New York Public Library.

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The scene in 2013:

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The first photo was probably taken within a few years of the opening of the Mt. Washington Cog Railway.  By the mid 19th century, the White Mountains had become a popular summer destination, and Mount Washington in particular became a favorite destination.  The only problem was getting to the top; this was first solved by the Mount Washington Carriage Road (today the Auto Road), but even before the road opened, another man had an even more ambitious idea – to build a railroad to the top.

Railroads were still in their infancy in America in 1852, and many major cities still did not have rail connections, but Sylvester Marsh had a plan to build a cog railway to the top, something that had never been done up the side of a mountain before.  The New Hampshire legislature gave him a charter in 1858, with one legislator reportedly remarking that they should give him a charter to make a railway to the moon, indicating how impossible it seemed to build a railroad to the top of the tallest peak in the Northeast.

The railroad was completed to the summit in July 1869, only a couple months after the completion of the Transcontinental Railroad.  It is about 3 miles long, with an average grade of about 25%, and it set the stage for future mountain-climbing railroads such as the one up Pikes Peak.  The locomotives in the first photo indicate that it is an early photo of the railroad; they appear to be the George Stephenson and the Hercules, which entered service in 1869 and were replaced in 1878 and 1874, respectively.

The present-day scene here is remarkably similar; the trains are still operating (most of the locomotives are modern biodiesel ones, but several date back to the 1870s), and there seems to be as many people riding in the 2013 photo as there were nearly 150 years earlier, although clothing styles have changed a bit.  It’s not visible from here, but the road to the top is also still there, although it is no longer the Carriage Road but the Auto Road.  There are a lot more buildings at the top than there were in the 1870s, although the Tip Top House is still there; it is older than either the Auto Road or the railroad.

Summit of Mt. Washington

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The summit of Mt. Washington, around 1860. Photo courtesy of New York Public Library.

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The summit in 2013:

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I don’t know if the two photos were taken from the same angle – it’s impossible to tell without any landmarks – but they clearly show how popular the northeast’s tallest mountain has become.  On the day that we went, there was literally a line of people waiting to ascend the pile of rocks that form the summit.  Some climbed to the top, while others took the Cog Railway or, like us, drove to he top.  If the 1860 date is correct, however, neither of these options were available to the individual standing on the top – the carriage road was not completed for another year, and the railway not until 1868.