The Garibaldi Ranges are a subdivision of the Pacific Ranges of the Coast Mountains. Deriving its name from Mount Garibaldi, the Garibaldi Ranges cover the huge stretch of mountains between two enormous river valleys. The Lillooet River valley on the east side and the Cheakamus River/Green River valley on the west. Whistler is located on the west edge of the Garibaldi Ranges, while Pemberton near the north end and Vancouver at the south end.
Alexander Falls 
Ancient Cedars 
Black Tusk 
Blackcomb Mountain Brandywine Falls Brandywine Meadows Brew Lake Callaghan Lake Cheakamus Lake 
Cheakamus River 
Cirque Lake Flank Trail Garibaldi Lake Garibaldi Park Helm Creek Jane Lakes Joffre Lakes Keyhole Hot Springs Logger’s Lake Madeley Lake Meager Hot Springs Nairn Falls Newt Lake Panorama Ridge Parkhurst Ghost Town Rainbow Falls Rainbow Lake Ring Lake Russet Lake Sea to Sky Trail Skookumchuck Hot Springs Sloquet Hot Springs Mount Sproatt Taylor Meadows Train Wreck 
Wedgemount Lake Whistler Mountain
January February 
March April May 
June July August 
September October November December
The subdivisions of the Garibaldi Ranges include Garibaldi Névé, Fitzsimmons Range, McBride Range, Spearhead Range, Golden Ears, Misty Icefield and the Bastion Range. The Fitzsimmons Range is a subsection of the Garibaldi Ranges that covers the area between the valleys of Cheakamus Lake and Fitzsimmons Creek. Fitzsimmons Creek cuts between Whistler Mountain and Blackcomb Mountain and largely originates from the Fitzsimmons Glacier. The Fitzsimmons Glacier and Mount Fitzsimmons are part of the Overlord Massif, which gets its name from the highest peak in the area, Overlord Mountain. Massif is a term used in geology to refer to a compact group of connected mountains that easily identify into one large mountain mass. Massif is a French word that means “massive”.
The Fitzsimmons Range includes several locally famous summits, including the summit of Whistler, Oboe Summit, Piccolo Summit and Flute Summit. These form the Musical Bumps trail which is a gorgeous route to the Russet Lake campground in Garibaldi Provincial Park. Next to Russet Lake is The Fissile, and next to The Fissile is Overlord Mountain. Near Russet Lake and connecting to the Musical Bumps trail is the Singing Pass trail that ascends along Fitzsimmons Creek to Whistler Village at the base of Whistler Mountain.
The Spearhead Range is a subsection of the Garibaldi Ranges that runs in an arc that connects Whistler Mountain and Blackcomb Mountain. The Spearhead Range is effectively the brother of the Fitzsimmons Range which runs east from the summit of Whistler Mountain to Russet Lake. The Spearhead Range covers the area on the north side or Blackcomb Mountain side of Fitzsimmons Creek. Fitzsimmons Creek runs down the valley between Whistler Mountain and Blackcomb Mountain. Where the Fitzsimmons Range ends at Fitzsimmons Creek, the Spearhead Range begins and continues along a set of peaks resembling spearheads to Blackcomb Mountain. These peaks include The Spearhead, Mount Trorey, Tremor, Shatter, Shudder, Quiver, and more.
The McBride Range is a subsection of the Garibaldi Ranges and covers a 357 square kilometre area east of Cheakamus Lake and Garibaldi Lake. Where the Spearhead Range ends, the McBride Range begins. Owing to its central location in the middle of Garibaldi Provincial Park, the McBride Range is often referred to as the backbone of Garibaldi Park. The McBride Range is a morass of brutally steep mountains and glacier valleys that expert skiers have plotted a route through. The McBride Traverse is an astoundingly difficult and beautiful, week long route through the McBride Range. Along the route you encounter several monster mountains with wonderful names, including Decker Mountain, Mount Patterson, Tremor Mountain, Sir Richard Mountain, The Gatekeeper, Forger Peaks, Isosceles Peak, Mount Carr, The Bookworms and The Sphinx.
The Garibaldi Névé is the large icefield that stretches out along the east side of Mount Garibaldi. With a size of 35 square kilometers(14 square miles), the Garibaldi Neve is a subdivision of the Garibaldi Ranges, which in turn is a subdivision of the Pacific Ranges of the Coast Mountains. The Garibaldi Névé Traverse is a tremendously beautiful and very treacherous winter skiing route that runs between Elfin Lakes and Garibaldi Lake. It is generally done as a three day expedition beginning and ending at two BC Parks Garibaldi Provincial Park trailheads. The Diamond Head(Garibaldi) trailhead in Squamish and the Rubble Creek, Black Tusk(Garibaldi) trailhead halfway between Squamish and Whistler. A common itinerary is the Diamond Head(Garibaldi) trailhead to Elfin Lakes on the first day. Sleeping in the very nice and well equipped Elfin Lakes hut. The second day covers the difficult Garibaldi Névé which runs from the Opal Cone north of Elfin Lakes to the foot of Sentinal Glacier northeast of The Table. The second night is usually spent at the Burton Hut at the east end of Garibaldi Lake. The third day involves crossing the length of Garibaldi Lake to the Garibaldi Lake campground and then the comparatively easy descent to Rubble Creek. The south to north route is favoured over the north south route because of the net elevation loss and much prized north facing ski descents.
Here are two excellent books on hiking and geology of British Columbia. Matt Gunn's Scrambles in Southwest British Columbia includes the various routes to the summit of Wedge Mountain as well as summit routes to the neighbouring peaks, Weart, Cook, Parkhurst and Rethel. Mount Weart is the second highest mountain in Garibaldi Park and is located just north of Wedge Mountain, separated by the Wedge-Weart Col. Published in 2005, Scrambles in Southwest British Columbia is still the best guide in print or online. Geology of British Columbia: A Journey Through Time by Sydney Cannings, JoAnne Nelson and Richard Cannings is a beautiful history of BC's geology and the 200 million year history of creatures living in this extraordinary corner of the world. The authors take us on a journey through time, describing the collisions of island chains called terrains, the sliding of plates, the erupting of volcanoes, and the movement of glaciers that created British Columbia as we know it today. They also describe the rich legacy of fossils left behind as a result of all this geological activity.
Ablation Zone Accumulation Zone Adit Lakes Aiguille Alpine Zone Arborlith/Lithophyte Arête ARRTI Armchair Glacier The Barrier Battleship Islands Bears Bench Bergschrund Bivouac Blue Face Bungee Bridge Bushwhack Cairn/Inuksuk Carter, Neal Parkhurst Cat Parkhurst RD8 Chimney Cirque Parkhurst Cletrac Cloudraker Coast Douglas-fir Coast Mountains Col Columnar Jointing Cordilleran Cornice Corrie Lake Crevasse Dalgleish, Alec Deadfall Emerald Forest Erratic The Fissile Fitzsimmons Creek Fitzsimmons Range Fyles, Tom Garibaldi Ranges Garibaldi Volcanic Belt Gemel Glacier Window Green Lake Green Lake Loop Hoary Marmot Krummholz Lodgepole Pine Moraine Mt Garibaldi Mt James Turner Mountain Hemlock Northair Mine North Arm Farm Nunatuk Nurse Stump Overlord Pacific Yew Paper Birch Parkhurst Ridge Parkhurst Sawmill Parkhurst Wye Peak 2 Peak Plow Tree Rainbow Lodge Roundhouse Rubble Creek Scree Spearhead Range The Table Tarn Townsend, Charles Usnea Waterbar Wedge Creek Western Hemlock Western Redcedar Whistler Spruce Winram, Mills
Alexander Falls Ancient Cedars Black Tusk Blackcomb Mountain Brandywine Falls Brandywine Meadows Brew Lake Callaghan Lake Cheakamus Lake Cheakamus River Cirque Lake Flank Trail Garibaldi Lake Garibaldi Park Helm Creek Jane Lakes Joffre Lakes Keyhole Hot Springs Logger’s Lake Madeley Lake Meager Hot Springs Nairn Falls Newt Lake Panorama Ridge Parkhurst Ghost Town Rainbow Falls Rainbow Lake Ring Lake Russet Lake Sea to Sky Trail Skookumchuck Hot Springs Sloquet Hot Springs Mount Sproatt Taylor Meadows Train Wreck Wedgemount Lake Whistler Mountain
January February March April May June July August September October November December
