Pemigewasset, E. Branch, |
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| Name | Range | Updated | Level |
|---|---|---|---|
| EAST BRANCH PEMIGEWASSET RIVER AT LINCOLN, NH | 350 - 3000 cfs | 00h34m | 172 cfs (rc= -0.1 ) |
The East Branch of the Pemigewasset is a natural flow river best run in late April and May with
the snowmelt from the high peaks of the White Mountains.
The river gets its start in the mountainous federally designated wilderness area upstream from
the put-in. As a result the water is clean, clear, and usually cold when the river is running.
Don't be fooled if the water looks too low; local river lore states that if it looks like there's
enough water then it's probably too much!!!
This river is a classic New England run. Continuous whitewater, a few more difficult rapids, and
lots of technical moves required. Many boaters consider this river one of the best regularly run
rivers in New England.
With the exception of a few bigger rapids on either side of Loon Mountain, the entire run is
similar in character. (Although some purists claim that the upper section, reachable only by
walking upstream is the best.) The river is relatively wide (85') for a New England river. It is
strewn with car (and larger) sized boulders. These boulders create extreme turbulence during high
water. The rapids are continuous and at high water all blend all together for a long class IV-V
run. Any swim at high levels may result in the loss of one's boat as it is quickly swept many
miles downstream. Be aware because of the nature of this river, boulders (even large ones) move
and shift every spring changing the river character.
The Upper East Branch of the Pemigewasset run starts below Franconia Falls at the confluence of
Franconia Brook and the North Fork of the Pemigewasset. To reach it you must walk/carry/drag your
boat up the Wilderness Trail three miles along the river. The upper section is a bit more
technical and unforgiving then the lower sections. Additionally the riverbed is more wide open,
requiring a bit more water to paddle.
If a long walk just to paddle a beautiful river doesn't appeal to you, then start your run (as
most do) on the middle section of the East Branch at the Lincoln Woods Parking Area (sometimes
called the Wilderness Parking area.) This section benefits from the added water coming in from
the Hancock Branch just below the put-in.
The lower East Branch (starting at Loon Mountain) holds its water a little longer than the upper
(ie, it can be paddled at slightly lower levels). The river bed narrows somewhat allowing for
less choice of passages. You will notice a lot more civilization in this section. Condos, ski
area base lodges, and parking lots are found along much of the run; even a hidden sewage
treatment lagoon located between the takeouts. Still, the river is pretty, seems secluded in most
spots, and has a few nice swimming holes. During late spring weekends the scenery basking in the
sun on warm days is especially nice.
Loon Mountain Rapid is the only section where scouting is required. The rapids immediately above and below Loon Mountain require more caution for the boater new to the river, as does the fourth major drop in the upper section. The rest of the river can be easily boat-scouted. Indeed, given the large number of drops and the changing nature of the river each year, it is impossible for one to know what is coming and each run is always a new experience.
Culvert Rapid, a short distance above Loon Mountain has a large steel pipe (culbert) in the
middle of the channel at the bottom. It's easly avoided as long as you know it's there.
At the bottom of Loon Mt. Rapid there is a large curved steel plate in the center of the right
main channel of the river. The upstream end appears to be into the riverbed and the downstream
end is up on a rock, so it just looks like a pour-over from upstream. From downstream you can see
it is a large curved plate similar to the culvert plating in Culvert Rapid, but not a full
section and not sticking up as much. It is located about 10 to 20 yards downstream of rapid
section shown in the photo on the AW site description of Loon Mt. Rapid, at the last drop just
before the left "sneak" route rejoins the main flow.
Since the beginning of April 2004, three strainers have fallen into the lower part of Potash
Rapid (about 1.1 miles downstream of the Lincoln Woods put-in) on the E Branch Pemi. Two of the
strainers, a Birch and an Evergreen, fell some time the week before 4/25 and the third, a tall
dead Spruce, fell some time the week before 5/9. The branches of the dead Spruce can be seen
sticking up well above the river as you approach that part of the rapid. Some of the branches of
the dead Spruce stick down into the water and are close enough together that it is not possible
to get a boat through. The trunk is far enough above the water that it looks possible to duck
under it before the first branch, but the other two strainers are just downstream and stick out
quite a bit beyond that. At low levels, portaging or lining on the left side of the channel is
advised. At medium and high levels, it might be possible to maneuver around the strainer to the
left, but scouting first is advised as rocks choke the left side of the channel.
(Thanks to Tommy T. and Norm R. for the above info.)
Note that the steep mountainous watershed causes the river to rise and fall rapidly. During
periods of heavy rain the river can rise especially fast. This may catch old hands by surprise
who expect a few hours of delay before any rain takes noticable effect.
An example is shown below (taken from the USGS Lincoln Gage). Note that in the space of only 15
minutes the flow increased by over 500 CFS; the increase over a two hour period was almost 2000
cfs, peaking at almost 3000 CFS before dropping back over the subsequent four hours. The
Woodstock gage several miles downstream showed the same pattern of increase/decrease delayed by
20 minutes.
Date CFS Level 2000.05.13 23:45:00 1190 2.85 2000.05.13 24:00:00 1160 2.82 <<< Flash flood starts 2000.05.14 00:15:00 1680 3.22 <<< 15 min 500 cfs increase 2000.05.14 00:30:00 1900 3.38 2000.05.14 00:45:00 2150 3.56 2000.05.14 01:00:00 2340 3.68 2000.05.14 01:15:00 2720 3.92 <<< Next hour 1000 cfs increase 2000.05.14 02:00:00 2860 4.01 2000.05.14 02:45:00 2910 4.03 <<< Peak 2000.05.14 03:00:00 2560 3.82 2000.05.14 04:00:00 2500 3.79 2000.05.14 05:00:00 2170 3.57 2000.05.14 06:00:00 2180 3.58 2000.05.14 07:00:00 1960 3.43 <<< Drops off over four hours
Put in elevation........ 1410'
Lincoln Woods elevation. 1178'
Loon Mountain elevation. 943'
Upper takeout elevation. 817
Lower takeout elevation. 688'
Total drop.............. 722'
Average drop/mile....... 81'...Including Loon Mtn rapids
Distance................ 8.9 miles
Upper East Branch
Mile 0-1 drop......... 93'...Starting just below Franconia Falls
Mile 1-2 drop......... 55'
Mile 2-3 drop......... 74'...Ending at Lincoln Woods Parking Area
Middle East Branch
Mile 3-4 drop......... 63'...Includes Hancock
Mile 4-5 drop......... 95'...Includes Potash
Mile 5-5.4 drop....... 69'...Includes Culvert and Loon Mtn Rapids
Lower East Branch
Mile 5.4-6.4 drop..... 89'...Includes Gov Adams
Mile 6-4-7.4 drop..... 67'...Includes Mill Dam
Mile 7.4-8.4 drop..... 84'...Incl South Mtn Rapid & Lincoln Bypass
Mile 8.4-8.9 drop..... 15'
Upper section width avg (not measured)
Middle section width avg 85'
Lower section width avg.55'
River geology...........Medium and large granite boulders, some ledges,
smaller boulders near lower section take out,
some ledge
River water quality.....Excellent, crystal clear upper and middle
sections; some degradation on lower section
after Lincoln sewage treatment plant (between
first & second takeout) at lower water levels.
Scenery.................Excellent mountain and forest scenery on Upper
& Middle sections. Good mountain scenery, ski
area, and condos line the banks most of the
lower section. Some old dam remains on lower
section with log cribbing and some rebarr.
Wildlife................Occasional deer, moose, tourist
Food: McDonalds, pizza and sub shops and more expensive eating establisments
located in Lincoln.
Lodging: Many hotels and motels located in Lincoln and Woodstock.
Campgrounds: Hancock campground, located just before the put in on route 112, is
run by the National Forest Service is open year round has nice wooded tent and small camper sites
with picnic tables, modern outhouses, pump water, no electricity. Lost River Campground located 4
miles west of exit 32 on route 112 is a familly campground with all the amenities. Wooded sites
with electricity, water available at sites. Sites for tents and campers of any size. Open early
May until Columbus day.
Gas: There are several gas stations in town at the exit but it is expensive. The
further south on 93 you get gas the less expensive it is. Exit 20 in Tilton (40 miles south) has
the cheapest gas in the region.
Etc. Franconia Notch 6 miles further up interstate 93 has many hiking and biking
trails, scenic areas such as the Basin, Flume, Cannon Mtn Arial Tramway. Rock climbing on Cannon
Mountain. There are several outdoor shops in Lincoln. Outback Kayak located at the Mill
marketplace on route 112 has paddling equipment.
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| Upper Pemi Region |
| Map by Mark Lacroix |
There are two gages commonly used by paddlers. There is a painted boaters gauge on the downstream river right abutment of the Kancamaugus bridge near the Lincoln Woods put-in. A USGS gauge on the East Branch in Lincoln came online in 1994. Both gages have had changes in measurements over time. The USGS gage has been recalibrated several times due to changes in the riverbed cross-section. Further complicating correlations between the USGS gage and the visual paddlers gauge has been the work performed on the Kancamaugus bridge during the summer of 2001. The table below is the best guess as to paddling levels for both gages. This table will be updated as more information is collected.
Lincoln USGS Visual gauge Boating level
EB Gauge cfs @ Kanc bridge Interpretation
350 cfs – 450 cfs about .6’ to .9’ Scratchy low
450 cfs – 1120 cfs about .9’ to 1.5’ Low to medium
1120 cfs- 2500 cfs about 1.5’ to 1.9’ Medium
Over 2500 cfs greater than 1.9’ High
The painted paddlers gage on the Kancamaugus bridge has been there for decades and is a well-known paddling reference. However during the summer of 2001 work was performed on the bridge. Many rocks were disturbed and the channel leading up to the visual gage was partially reconstructed. Additionally some of the boulders washed down below the gauge and formed a small dam backing the water up to the painted gage. Recent reports (Spring 2004) suggest that the river may be scouring out the channel restoring the riverbed. The graph below shows the current best-guess regarding correlations between older (pre-2001) and current readings. The graph will be updated as more information is collected. Paddlers with either older (1994-2001) or current observations of gage correlations are requested to send them to the streamkeeper.
Paddler's Gage vs CFS: Original values vs current readings. Comparison chart showing change in Paddler's Gage due to bridge reconstruction. |
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Month...........%Chance....Comment
January ............ 0%....frozen.
February.............0%....frozen
March................5%....Usually frozen.
April...............70%....Best chance mid to late April
May ................50%....Best chance in early May.
June................18%
July.................5%
August...............5%....Just a trickle
September...........10%....Tropical storms and their remains
October.............25%
November............45%....Fall rains, dormant trees
December............30%....River starts freezing early to mid month.
Be aware this is averaged out over several years. The % chance refers to the probability of finding the river running on any given day. For instance a 5% probability for August means on average you can only expect 1-1/2 days of water. One year there could be 3 days in August with water, other years none. Spring levels are usually higher than fall levels. The river rises and falls rapidly because of the small steep watershed. An occasional summer storm could bring the river up for a day.
| Name | Range | Updated | Level | ||||||
|---|---|---|---|---|---|---|---|---|---|
| EAST BRANCH PEMIGEWASSET RIVER AT LINCOLN, NH | |||||||||
| usgs-01074520 | 350 - 3000 cfs | 00h34m | 172 cfs (rc= -0.1 ) | ||||||
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| When | River/Gauge | Subject | Level | Reporter |
|---|---|---|---|---|
| Pemigewasset, E. Branch [NH] |
East Branch Pemigewasset USGS Gage Rating Chart |
n/a | Skip Morris | |
| East Branch of the Pemi [NH] |
Joe surfing below Potash |
1.6 bridge gauge | Mark Lacroix | |
| 4y35d02h47m | East Branch Pemigewasset [NH] |
Upper East Branch Put-in |
1.4 | Skip Morris |
| 4y42d02h47m | East Branch Pemigewasset [NH] |
Lincoln Woods Put-In |
1.4 | Skip Morris |
| 6y205d02h47m | East Branch Pemigewasset [NH] |
Loon Mtn Rapids |
1.3 paddlers gage | Mark Lacroix |
| 7y213d02h47m | East Branch of the Pemi [NH] |
Joe running sneak at Mill Dam |
1.6 bridge gauge | Mark Lacroix |
| 7y228d02h47m | East Branch Pemigewasset [NH] |
Low water on East Branch |
100 cfs | Mark Lacroix |
| Mile | Rapid Name | Class | Features (Legend) |
|---|---|---|---|
| 0.0 | Upper Put In | ||
| 0.1 | Alternate (opposite) side put-in | ||
| 0.2 | Typical River Character | ||
| 0.3 | First Major Drop | IV | |
| 0.5 | Second Major Drop | IV | |
| 0.7 | Third Major Drop | IV | |
| 1.1 | Fourth Major Drop | IV+ | |
| 1.5 | Fifth Major Drop | IV | |
| 2.0 | Sixth Major Drop | III+ | |
| 2.2 | Seventh Major Drop | IV | |
| 2.5 | Eighth Major Drop | IV | |
| 3.0 | Lincoln Woods Put-in | ||
| 3.2 | Hancock | IV | |
| 3.4 | Unnamed Rapid | IV | |
| 3.6 | Unnamed Rapid | IV | |
| 4.1 | Potash | IV | |
| 4.9 | Culvert | IV | |
| 5.1 | Upper Loon Rapid | IV | |
| 5.4 | Loon Mtn. Rapid | IV+ | |
| 5.7 | Governor Adams | IV | |
| 5.8 | Unnamed Rapid | IV | |
| 6.1 | Unnamed Rapid | IV | |
| 6.2 | Unnamed Rapid | IV | |
| 6.5 | Unnamed Rapid | IV | |
| 6.9 | Mill Dam | IV+ | |
| 7.4 | South Mountain Rapid | IV | |
| 7.8 | Unnamed Rapid | IV | |
| 8.2 | Unnamed Rapid | IV |
User Comments
I ran this yesterday (4/20/06).
The level during my run was just under 1 foot on the Kank. Bridge boaters gage. The rapids were
definitely "white," not green flowing water. I would call it a delightful and exciting level on the
low side of "medium," definitely not a scratchy low water run. Thus the meaning of the gage has
continued to evolve and now seems to be back to the early days of the first gage when 1 foot meant
a good medium level.
The strainer identified in the river left drop by the island requiring a portage in 2004 is no
longer a problem. The trunk of the tree is still there, but has settled into the river deeply
enough that with good control, a clear run is available.