Climbing and Geography of Cathedral Ledge

North Conway, New Hampshire, is a renowned mountain town known for Cathedral Ledge, a granite bluff popular among rock climbers. Formed by glaciers 12,000 years ago, its intimidating vertical face was first scaled in 1931. Today, it serves as a training ground for climbers. Despite its beauty, the ledge poses significant risks, prompting climbers to name paths with ominous titles. New Hampshire has long been a destination for thrill seekers, even before its statehood.

What makes North Conway, New Hampshire, a notable location in the US?

• It is a famous beach town.

• It is known for its historical museums.

• It is a popular mountain town for rock climbers.

• It is a major financial hub.

How was Cathedral Ledge formed?

• By river erosion.

• By glaciers sculpting the granite.

• By volcanic activity.

• By human construction.

When was the vertical face of Cathedral Ledge first scaled?

• In 1931

• In 1951

• In 1921

• In 1901

Why do climbers use Cathedral Ledge?

• To enjoy the beach.

• To practice for major peaks out west.

• To visit historical sites.

• To participate in skiing competitions.

What is a common practice among climbers before starting their ascent on Cathedral Ledge?

• Taking a group photo.

• Saying a prayer.

• Checking weather forecasts.

• Consulting a map.

Which of the following is NOT a name of a climbing path on Cathedral Ledge?

• Mountain Peak

• End of Days

• Final Gesture

• Book of Solity

What has historically attracted adventurers to New Hampshire?

• Its beaches.

• Its shopping centers.

• Its challenging landscapes.

• Its urban nightlife.