About Brandywine Falls
Brandywine Falls was arguably the most significant and attractive waterfall remaining in the state of Ohio let alone the apparent main scenic attraction of the Cuyahoga Valley National Park.
This 60-65ft year-round waterfall on Brandywine Creek was one of the primary reasons why we incorporated the city of Cleveland to our Great Lakes itinerary.
Thus, it opened the door for us to experience other attractive waterfalls within reach of the greater Cleveland and Akron area like Paine Falls and Lanterman’s Falls (a typical benefit of waterfalling in unfamiliar places).
We were anticipating seeing this waterfall juxtaposed with fall colors, but it turned out that the peak of the colors was still a week or two away.
Apparently, the transition season was late to begin during our visit in the first week of October 2015.
So while the gorge and falls were very beautiful, the scenery here was still predominantly green.
Experiencing Brandywine Falls
Our visit of this bridal veil-like waterfall was a breeze as it started from a busy parking lot (see directions below).
Then, the trail proceeded on a gentle wheelchair-friendly boardwalk (veering right as it branched away from the Stanford Trail) before reaching a fork on the boardwalk itself less than a 1/4-mile from the start.
We first opted to go right, which was an upper path leading to an obstructed view of Brandywine Falls from a viewing platform that was wheelchair-accessible.
We continued a little further past this lookout where stairs took us by the ruins of the former site of the Champion Electric Company (destroyed by lightning in 1937).
Eventually, we got to a view over the brink of the falls and into the gorge.
Apparently, we could have continued towards Brandywine Road, then cross the bridge to see the falls from the other side of the gorge near the Inn at Brandywine Falls (something we didn’t do).
Back at the boardwalked fork, we then took the left path to descend deeper into the gorge on a combination of steps and cliff-hugging boardwalk.
This path brought us up close to the cliffs responsible for the rugged terrain of this gorge.
By the way, the gorge was composed of a soft Bedford and Cleveland shale layer capped by a hard Berea Sandstone layer exposed by the glaciers that gave rise to the Great Lakes, which retreated some 10,000 years ago.
Then, we descended the final series of steps (comprising the remainder of the 160ft elevation change) to the lookout platform right in front of the Brandywine Falls itself.
When we showed up, there were already a few tripod-wielding photographers looking for that money shot, but it didn’t take long before this lookout was full of people waiting their turn to take photos just a few minutes later.
I guess this was a consequence of the popularity of the falls, especially on the weekends, which was certainly the case on our Sunday midday visit.
Anyways, this was the turnaround point of our short excursion, and we returned back the way we came coming face-to-face with the gorge walls once again on the way out.
The excursion lasted about 45 minutes away from the car.
Why Cuyahoga Valley National Park?
Finally, while Brandywine Falls was very naturesque, perhaps what piqued our curiosity more was why Cuyahoga Valley (pronounced “ka-ih-OGH-ha” which was Native American meaning “crooked”) was set aside for federal protection in the first place.
Typically we thought of National Park System reserves to be of a grander scale like a Yosemite or Yellowstone.
Apparently, the area had seen its industrial heyday in the 1800s when Brandywine Creek was being exploited to power a sawmill.
Brandywine Village was even surrounding this waterfall, which produced other things like whiskey, grist, and wool.
Eventually, the Ohio and Erie Canal as well as railroads caused the decline of Brandywine as an industrial town (only the Inn at Brandywine Falls remained of the old Brandywine Village).
However, the area wasn’t allowed to recover until the hydroelectric infrastructure from the Champion Electric Company whose remnants we saw at the top of the falls was destroyed by lightning in 1937.
Since that time, Brandywine Falls became a place of refuge, and over time, the Cuyahoga Valley National Park was created in 1974 to further ensure the protection of this pocket of greenspace between Cleveland and Akron.
Apparently another purpose of the park was to preserve the heritage of the nation-building industrialism in the incorporated parts of the recovering landscape of Cuyahoga Valley itself.
Brandywine Falls resides in Cuyahoga Valley National Park near Cleveland and Akron in Summit County, Ohio. It is administered by the National Park Service. For information or inquiries about the area as well as current conditions, visit their website.
Our visit to Brandywine Falls was made complicated by a lot of road construction on the I-271 that essentially closed off just about all of the key offramps that would’ve efficiently taken us directly to the waterfall.
We’ll try to describe the path we were supposed to have taken (at least coming from the east when we came over from Lantermans Falls).
Then, we’ll discuss the route we took when we returned to Cleveland, where we were staying.
But with the confusion of all the crazy detours that we had to take, I’m sure there might be better ways to get here than what we had to do.
Driving from Cleveland to Cuyahoga Valley National Park
From downtown Cleveland, head south on the I-77 for about 13 miles to exit 149A at East Royalton Rd.
Then drive east on East Royalton Rd for about 6 miles to Brandywine Rd (East Royalton Rd became Chippewa Rd then West Aurora Rd over this stretch).
Turning right onto Brandywine Rd, we then drove south for about 2.5 miles to the turnoff for the parking lot for Brandywine Falls, which was just past the Inn at Brandywine Falls and the bridge over Brandywine Creek.
This route took us roughly 30 minutes.
Driving from Lanterman’s Falls to Cuyahoga Valley National Park
From Lantermans Falls at Youngstown, Ohio, we turned left onto Canfield Rd, then another left onto Glenwood Ave.
We followed Glenwood Ave north all the way to its merging with Mahoning Ave (past the underpass of the I-680), then we turned right onto Edwards St before making another right onto Marshall St, where we finally got onto the I-680 west.
We followed the I-680 west for about 5 miles before it merged onto the Ohio Turnpike toll road (I-80), which we then followed for the next 43 miles.
Then, we got off the Ohio Turnpike at exit 180, and after paying the toll, we should have kept left then approached the ramp for the Dean Memorial Pkwy.
This ramp would then eventually curl down to East Boston Mills Rd, where we would’ve then turned left, and then go right onto Olde 8 Rd after 0.3 miles.
We followed the Olde 8 Road (eventually becoming Brandywine Rd) for about 2.2 miles before turning left onto the well-signed parking lot for Brandywine Falls.
This drive should have taken us under an hour, but because of the detours, we wound up spending an hour and 15 minutes on this drive (going as far north as Broadway Ave off the I-480 before turning back).
Finally, here’s some additional geographical context. Cleveland, Ohio was 39 miles (under an hour drive) north of Akron, Ohio, 169 miles (over 2.5 hours drive) south and east of Detroit, Michigan, 133 miles (over 2 hours drive) northwest of Pittsburgh, Pennsylvania, and 142 miles (over 2 hours drive) north of Columbus, Ohio.
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