The New and Gauley Rivers
Camping:
http://www.nps.gov/archive/neri/pdf/camp02.pdf
A tutorial
Written by Chuck Brabec on 8/30/07 to prepare for the Labor Day Weekend
PDF map of the area:
link
For those of you who don't know how the levels on the New and Gauley rivers are related, here is a (not so) brief explanation.
The New river has its headwaters in the mountains of North Carolina. From there, it flows northward into Virginia and then turns west into West Virginia. I don't know of any dams on the New in NC. In VA, there is a dam that forms Claytor Lake, just upstream of Radford. What is released from Claytor Lake heads down past Radford and Pearisburg. At Glen Lyn, the New flows into WV and into Bluestone Lake (the second major dam on the New). Just below Bluestone Dam is the confluence of the New and Greenbrier Rivers. The water in the New from Hinton downstream is what comes out of Bluestone Dam plus whatever joins it from the Greenbrier. The most relevant river gauges for those of us paddling the New below Hinton are at Hinton and Thurmond. The level at Hinton reflects what will happen in 12-16 hours at Thurmond and a couple hours after that at Fayette Station (the takeout for New River Gorge).
The Huntington COE web page (
link) includes flows for the New in Virginia at Galax, Radford and Glen Lyn and in West Virginia at Hinton and Thurmond. It also includes the flow that is being released from Bluestone Dam. All of this information will give you some idea of what is and will be happening to the level on the New in and above NRG.
The trend on the New using the data from this morning indicates that it will continue to drop (1451 cfs at Thurmond, 1382 cfs at Hinton, 1240 cfs from Bluestone Dam, 1294 cfs at Glen Lyn and 815 cfs at Radford). How much it will drop depends on rainfall and what the COE decides to release from Bluestone Lake.
My guess is that the New at Thurmond and Fayette Station on Saturday will be about 1100-1300 cfs (-1.5 to -2.0 feet on the paddlers gauge).
What does all of this have to do with the Gauley?
The Gauley is natural flow above Summersville Lake. The COE manages the flow at Summersville Dam based primarily on the lake level and what is flowing into the lake from the Gauley headwaters (including the Williams, Cranberry and Cherry Rivers). However, the COE also has to consider the potential for flooding in the towns below the dam and the requirement for a minimum flow on the Kanawha River. The Huntington COE web page (link above) also includes the river levels for the Gauley watershed and the current flow being released from Summersville Dam (419 cfs). The release from the dam is what you have on the Upper Gauley until you get to the confluence of Meadow and Gauley rivers. Then you have the increased flow from the Meadow (a paltry 31 cfs this morning). There are a few other creeks that flow into the Gauley as it heads downstream, but right now they are even more insignificant than the Meadow.
Why is the Kanawha River important?
The New and Gauley rivers merge at Gauley Bridge, where it becomes the Kanawha River. As I mentioned before, the COE is required to maintain a minimum flow on the Kanawha. When the flow gets too low on the New they have to release more water from Summersville Dam on the Gauley River. The "too low" point is somewhere around 1000-1300 cfs on the New at Thurmond. Another way to look at it is to view the USGS gauge for the Kanwaha River at Kanawha Falls (
USGS link). It shows that the COE normally tries to maintain about 2000 cfs at that gauge.
The main question is "Will the New drop enough to cause the COE to increase the release from Summersville Dam?"
My answer right now is "Maybe".
BTW, the COE maintains 2 levels for Summersville Lake - summer pool and winter pool. The difference is 75 feet of elevation!! The COE is mandated by law to start bringing the lake down to winter pool beginning the weekend after Labor Day. That is why we have "Gauley Season".
More from Chuck about the low water New:
Posted by: Chuck Date: Tue Jun 24, 2008 6:46 pm ((PDT))
I have some experience with NRG at low levels (zero to -2 feet at Fayette Station). Here are the hazards that I watch out for:
Lower Railroad
I take a line through the rock garden to the right of center, well right of Clamshell Rock. The line far left (almost on shore) is also open but there are some rocks in the drop that can surprise you. That is where the rafts like to play too, so you have them to contend with. I prefer just right of center.
Middle Keeney
There is a ledge that you have to contend with if you take the normal line just to the left of Moss Rock. I find it best to be a bit father left of Moss Rock with a slight angle right to miss most of the ledge and line up with the tongue over the left part of the ledge. Get too far left and there is a pretty sticky hole that can grab you.
Lower Keeney
Stay away from the rocks on river right (Meat Grinder). This actually applies at all levels. That is pretty easy to do as long as you don't swim in Middle Keeney. If anyone in your group does swim, get them to calm water in the big pool well above Meat Grinder on river right or the pool on river left well above the beginning of Lower Keeney. Once you get into Lower Keeney, watch our for the ledge coming out from the large rock on shore near the bottom of the rapid. This ledge, which forms the last hole in the rapid, is barely under water at low water levels. This is not a good place to be upside down. I personally know of 2 kayakers who had pretty bad neck injuries sustained when they went over that ledge upside down. There is a small tongue right next to the rock that you can use to avoid the hole formed by the ledge.
Double Z
I usually run this rapid starting at the eddy on river right. Form there I go behind Barry's Rock (the big rock in the middle of the rapid) and then to the left of Table Rock (the rock in the middle at the bottom of the rapid - where the video boaters congregate). Just don't go too far left and Breadloaf Rock is not in play.
Undercut/Miller's Folly
I think of this as 2 rapids with a short pool at low water levels between the Undercut part and the Miller's Folly part. Stay away from Undercut Rock in the first part. When I get to Miller's Folly, I look for the rock just a bit left of center at the top of the rapid. I go just right of that rock and just right of the rock downstream of it at the bottom of the rapid. Keep away from the left side of these rocks as that route will put you right in Bloody Nose - the really shallow rock slide at the bottom of the rapid. That's not a good place to be.
Fayette Station
Avoid the hole about 3/4 of the way down the rapid by staying to the left of it. The hole is formed by a rock ledge coming out from river right. At low levels, the holes is a grabber. I ended up in it sideways several years ago. When I came out of my kayak, I was sucked down. After what seemed like forever, my toes finally touched bottom and I was able to push off with enough force to get to the top of the water downstream of the hole. I do not want to repeat that episode again!
On the plus (?) side, the pools are long at -1 foot to -2 feet.
Chuck
On 6/24/08, Rich K wrote:
> I'm familiar with the New over a range of levels from nomimal (1') to high (6') but not where it's sitting now: about -1' (Fayette Station approximation based on Thurmond gauge).
Camping options
Burnwood NPS campground
http://www.nps.gov/neri/planyourvisit/f ... ations.htm
Confluence
http://www.confluenceresort.com/camping.htm