Mt Hypipamee Crater Atherton Tablelands

Mt Hypipamee Crater 🧭

Mt Hypipamee Crater

🌋 See a 70-metre deep volcanic pipe filled with emerald green water
🌳 Stroll through high-altitude rainforest rich in wildlife
💦 Discover the cascading waters of Dinner Falls
👣 Easy walking tracks suitable for families
📸 A top spot for nature photography and birdwatching
🐸 Look out for tree kangaroos, possums, and rainforest frogs
🚗 Accessible via sealed road – a great stop on your Tablelands adventure

Discover Mt Hypipamee Crater

A volcanic wonder in the heart of the Tablelands rainforest

📍 Located between Atherton and Ravenshoe, Mt Hypipamee Crater is one of the most extraordinary geological sites in the Atherton Tablelands.

🌋 About Mt Hypipamee Crater

Also known locally as The Crater, Mount Hypipamee is a fascinating reminder of the region’s volcanic past. Thousands of years ago, a powerful gas explosion created this deep cylindrical hole in the earth – a rare geological feature called a diatreme. Today, the crater is filled with still, green water, covered at times with delicate duckweed, and surrounded by towering rainforest trees.

A short 400-metre walk leads from the car park to a sturdy viewing platform perched over the edge, offering a breathtaking look straight down into the crater.

🌳 The Rainforest Walk and Dinner Falls

After viewing the crater, follow the 1.2 km return walking track down through the cool rainforest to Dinner Falls – a trio of cascades on the headwaters of the Barron River. The forest here is alive with sound: listen for the calls of whipbirds, the chatter of parrots, and the rustle of pademelons in the undergrowth.

This peaceful walk is perfect for families and nature lovers alike. Just don’t forget your camera — it’s stunning in all seasons!

❓ Frequently Asked Questions – Mount Hypipamee Crater Lake

How was Mt Hypipamee Crater formed?

Mount Hypipamee Crater is a volcanic pipe, or diatreme, formed by a powerful gas explosion thousands of years ago. The result was a deep, vertical shaft in the earth now filled with water and surrounded by lush rainforest.

Is the crater safe to visit with children?

Yes! The path to the viewing platform is short and easy, and there are railings and signage for safety. However, it’s important to supervise young children near the lookout and on the walk to Dinner Falls.

Can I swim in the crater?

No, swimming in the crater is not allowed. The steep sides and deep water make it dangerous. For a splash, head to nearby Dinner Falls or other swimming spots across the Tablelands.

How long is the walk to the crater and falls?

The crater is just a 400-metre stroll from the car park. The full circuit to Dinner Falls is around 1.2 km return, making it an easy and enjoyable walk through beautiful rainforest.

What wildlife might I see at Mount Hypipamee?

The area is rich in wildlife! You may spot tree kangaroos, possums, musky rat-kangaroos, and a variety of birds and butterflies. It’s also a great place to listen for frogs and rainforest sounds, especially after rain.

☀️ Tips for a Great Visit

🧢 Bring a hat, sunscreen, and insect repellent
💧 Carry plenty of water – it’s easy to forget in the cool forest air
🥾 Wear good walking shoes with grip for the Dinner Falls track
🐾 Respect wildlife – observe, don’t approach
🍃 Take only photos, leave only footprints

💡 Mt Hypipamee Crater Fun Fact

The crater is more than 60 metres across and nearly 70 metres deep, but was once believed to be bottomless! Early explorers dropped stones and waited… only to hear the plop much later!

📍 How to Get There

Mount Hypipamee National Park is located on the Kennedy Highway, about 25 minutes south of Atherton. The drive winds through the scenic Evelyn Tableland and is suitable for all vehicles.

🧡 A Must-See Stop on Your Tablelands Journey

Mount Hypipamee is more than just a crater — it’s a journey into ancient earth history, a rainforest retreat, and a moment of awe in the middle of the Tablelands. Take your time, breathe in the fresh mountain air, and let the beauty of nature work its magic.