Dru

Not a yak.

I'm certain you can calculate the mass of the bear from the knowledge that the rope did not break and it looks like yellow polypropylene boat line. Answers on a single sheet of paper please class. No cheating

Well look at the give in the rope as seen by angle it goes up to the far tree at.

that IS the crag name

cirque of the uncrackables

The photos are making the rounds via email, they were taken near Long Lake in Ontario. Looks like that bear is a cub/young adult to me, not full grown. But think if that feeder was your food bag or haulbag!

Mandrax and jack-in-the-pot

What about sit starts

Can you make hummus from s

All you need is horsecock, tinned sardines, prunes and rum.

Since those are south facing, they almost never freeze all the way down... Shaun and I have been in there like 3 times now, no dice.

and the weather mostly looked like this

i have over 100 bug bites on my right hand and about 75 on my left!

I figure being a raven or a vulture would be pretty good. Or a Mesonychoteuthis hamiltonii if'n a sperm whale didn't eat you.

Say goodbye to your balls.

I've never been on a date

Roughly speaking the geologic contacts, are at the top of p6 and p15, respectively, if using the belays marked in the Beckey topo. Also the start of the red line that I drew differs from the topo start, which would go up from the snowpatch, to and through the B in Batholith, and then trend right along the ledge that the first geologic contact follows.

Flight 810 Buttress at left and South Peak East Face at right Navvy Wall route line in red Geologic contacts an approximation Lithology from personal experience and the geologic map of the area. The gneiss is really just the most metamorphosed part of the phyllite, the two are really the same geologic unit but the gneiss has undergone greater metamorphism along the Chilliwack Batholith contact, IMHO anyways.

Slesse consists of a variety of rock types, separated from each other almost vertically. From east to west one goes through Chillwack Batholith then several older rocks ending up with Carboniferous-aged (IIRC) metamorphics on the west side. The Navvy Wall is Chilliwack Batholith granodiorite on the bottom and metamorphic on the top. See photo below...

oK, i missed the solstice but I'm still going see ya in July

Pack Animal Direct