Central Gully

Valley in Cumberland Allerdale

England

Central Gully

Scafell Pike (behind) and Scafell from Over Beck Credit: Johnny Coop

Central Gully is a prominent geographic feature located in the Cumberland Valley, a region in the northeastern United States. Situated in Cumberland County, Pennsylvania, the gully is a natural formation that stretches approximately 10 miles long and 1 mile wide. It is a significant topographical landmark in the area, known for its steep sides and deep channel. Central Gully is believed to have been created by glacial activity during the last ice age, around 15,000 years ago.

The gully is characterized by its V-shaped profile, with its sides rising up to 200 feet in some places. It is primarily composed of sedimentary rocks, including limestone, sandstone, and shale. The presence of these rocks contributes to the gully's unique geological features and its rich biodiversity. The gully is home to a variety of plant and animal species, including rare ferns, wildflowers, and several bird species.

Central Gully is also significant for its historical importance. It served as a natural pathway for Native American tribes, such as the Shawnee and Lenape, who used it as a travel route between the Susquehanna River and the Appalachian Mountains. The gully facilitated trade and communication between these tribes and played a vital role in their daily lives.

Today, Central Gully is a popular destination for outdoor enthusiasts and nature lovers. It offers scenic hiking trails and opportunities for wildlife observation. The gully's impressive geological features and historical significance make it an important landmark in the Cumberland Valley region.

Show me another place!

If you have any feedback on the listing, please let us know in the comments section below.

Central Gully Images

Images are sourced within 2km of 54.46595/-3.192763 or Grid Reference NY2208. Thanks to Geograph Open Source API. All images are credited.

Scafell Pike (behind) and Scafell from Over Beck

Johnny Coop

Borrowdale from Ruddy Gill

Looking down the valley from alongside Ruddy Gill. Derwent Water is just visible in the distance.

Ian Taylor

Styhead Tarn

Anthony Foster

Styhead Tarn

Anthony Foster

Ruddy Gill

Ruddy Gill about to enter its gorge which is on the eastern side of Sprinkling Tarn. To the right slopes rise towards Allen Crags, Glaramara is distant at the centre.

Trevor Littlewood

Boulders and rock outcrops on Seathwaite Fell

There are many minor outcrops on Seathwaite Fell, topping its knolls and projecting from slopes. The outcrop in the image overlooks the valley of Ruddy Gill / Grains Gill, beyond which is Glaramara.

Trevor Littlewood

The Scafell range from Bow Fell

The grassy hill in the middle distance is Pike de Bield. On the skyline are Sca Fell (in cloud), the gap at Mickledore, and Scafell Pike (clear), with Ill Crag on the right.

David Purchase

Styhead Tarn

A stone is about to join the fishes. Great End is seen beyond the tarn but the rest of the Scafell Pike ridge is shrouded in low cloud.

Trevor Harris

On the Corridor Route

Looking back towards Sty Head with the slopes of Green Gable beyond.

Trevor Harris

Sty Head from the Breast Route

Looking back down on Sty Head while ascending Great Gable by the Breast Route. The path to Sprinkling Tarn is ahead centre.

Trevor Harris

View into Wasdale

From the Corridor Route to Scafell Pike, looking down into upper Wasdale with Great Gable to the right.

Trevor Harris

Scafell Pike

Approaching the summit having climbed by the Corridor Route via Lingmell Col. Across the boulder field the summit is ahead.

Trevor Harris

Crossing scree on Bursting Knott

The Moses' Trod path climbs steadily up the southern flank of Great Gable towards Styhead Pass, here crossing a substantial scree slope.

Richard Law

On Toad How

The Moses' Trod path crosses another scree patch above Toad How, on the southern side of Great Gable. Ahead, the crags of Spout Head are split by the deep Skew Gill.

Richard Law