Notom-Bullfrog Road

It is one of the great drives of the earth.  The Notom-Bullfrog Road (NBR) runs parallel along much of the spectacular 100-mile-long Waterpocket Fold.  The Waterpocket Fold, or locally, simply The Fold, is a monocline, which is a geological term that suggests a step.  The NBR links Utah State Route 24 (SR-24) with the Bullfrog Bay Marina in Glen Canyon National Recreation Area (aka Lake Powell).  The entrance to the Notom-Bullfrog Road is located approximately 9 miles east of the Capitol Reef NP Visitor’s Center  along SR-24, with an alternative entrance another 3.6 further east along SR-24.  The overall distance from SR-24 and the Bullfrog Bay marina boat ramp is approximately 68 miles.  The northernmost 10 miles and the southernmost 25 miles of the NBR are paved, but in between it is basically a wide ATV track.

The view at the beginning of the traverse is dominated by the eponymous Capitol Reef domes shown above.  There are all sorts of options here, from wide angle view as above through tight telephoto shots of the domes.  The view is toward the southeast, so the best times for photography will be in the morning hours.  The image above was recorded at 09:00 MDT on AUgust 26, 2011 using the Nikon D3s and the AF-S NIKKOR 24-70mm f/2.8G ED at 56mm.  Exposure was f/11 and 1/400s (+0.33EV, normalized in post-processing), ISO at 400.

The NBR crosses countless washes as the route continues southward.  After about 4 mile from the junction of the NBR and SR-24, the road meanders through several growing fields.  By this point it will be clear that you have been traveling through a desert, and the prescence of brilliantly green alfalfa fields comes off as a bit of a shock.  As the NBR crosses from Wayne County into Garfield County (about 10 miles south the the NBR/SR-44 junction) the road changes from a narrow paved surface to a graded dirt surface. As the road continues south it draws closer to the Capitol Reef monocline and at about 25 miles south of the junction with SR-24, the NBR enters Strike Valley.

The image above was made looking south from on top of a ridge that along the center of Strike Valley.  The image was recorded at around 11:00 MDT on August 26, 2011, using the D3s and the AF-S NIKKOR 24-70mm f/2.8G ED at 48mm.  Exposure was f/16 and 1/100s (+0.33EV, normalized in post-processing), ISO at 200.

As the road continues south it continues to approach the monocline, providing impressive views of the geology.  The images above (toward the northwest) and immediately below (looking west) provide a hint of what is possible.  These two images were recorded from the same location at around 11:40 MDT, using the D3s and the 24-70mm f/2.8G ED.  The image above was recorded at a focal length of 34mm at f/16 and 1/160s (+0.33 EV), ISO 200.  The image below was record at a focal length of 38mm at f/11 and 1/250s (+0.33 EV), ISO 200.

The NBR crosses over the main ridge that runs along the length and near the middle of Strike Valley at a point about 35 miles south the SR-24 junction.  Just before the ridge crossing, a minor road heading directly south leads, after 0.5 miles, to the Post Corral.  The Post was a stopover for cowboys working cattle herds along the Burr Trail – more on The Post in a future entry.  The following four images were recorded from the Post Corral at about 13:30 MDT using the D3s and either to 24-700mm f2/2.8 lens (first image, immediately below), or the AF-S NIKKOR 70-200mm f/2.8G ED VR II at near 100mm (next three images).

Beyond The Post, the NBR continues along for several more miles before departing The Fold as it heads southwesterly toawrds Glen Canyon NRA,  The route runs along the western edge of Clay Canyon, which is itself a spectacular bit of scenery that provides a hint of what the area might have been like prior to the creation of Lake Powell.

Garfield County; wherein much of Capitol Reef NP is located, wants to pave the remaining wild sections of the NBR.  Why would you want to pave a wild road?  My guess is that they think it might be a good idea to invite truck-boat rigs to pass through Strike Valley.  Currently, it is not feasible to haul a boat up the Notom-Bullfrog road, but if it were completely paved, you could shave about 30 miles by traveling this route.  How they could possibly generate any significant revenue in the long-term with this road-paving scheme is beyond me.  I’m personally against this plan for many reasons, and hope that the Garfield County commissioners find some better projects to spend County/State/Fed money on.

To state that there are no services along this patch of road misses the point.  There are few people along this road.  There is virtually no mammalian life along this road – at least that can be seen.  There are a few, a very small number, of birds that seem to stray in from time to time.  Except immediately after a deluge, there is no water along this road.  If you break down along this road it may be hours, perhaps days before you are offered a rescue.  If you are unprepared and your vehicle fails you, you may die.  Recall the Boy Scouts motto:  Be Prepared.  Shovel, check.  Tow lines, check.  Food & abundant water, check, check.  Extra fuel if you can manage it, but otherwise a full tank.  First aid kit, always.  We also carry the Motorola Iridium Satellite phone model 9555.  It works flawlessly.  We suggest that you rent or buy this phone if you travel in the Utah back country.

A list of mileages is given below:

9.1 Miles from CARE ranger station to the NBR junction

From the junction of the NBR and SR-24:

2.1 mile to first river crossing

3.9 miles to the first large growing fields

10 miles to Wayne/Garfield County line, end of the paved road north.

32.6 miles to junction with Burr Trail heading west through the Burr Trail Switchbacks (2.5 miles to top of the Switchbacks)

35 miles to Ridge Crossing (turnoff to Post Corral)

43.5 miles to junction with road that heads SE to Bullfrog Bay and return to paved road

63 miles to junction with SR-276

65.5 miles to airport

65.7 miles to Garfield/Kane county line

66.8 miles to Ferry Road Junction

68.3 miles to Bullfrog Bay boat ramp

A Google Earth Image of the Post Corral appears below:

Copyright 2012 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

Updated Lee Filters Website

Lee Filters has announced the release of a new and updated website:

http://www.leefilters.com/

It’s pretty nice alright.  Perhaps we can also hope for Lee to clear their backlog of orders.  Anyone seen a Big Stopper?  I’ve been waiting for more than a year…

Copyright 2012 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

Lightroom 4 Beta Available for Download

Adobe Labs has announced the release of the much-anticipated Lightroom 4 beta.  Soft-proofers of the world rejoice (hopefully).  You can download the beta at:

http://labs.adobe.com/technologies/lightroom4/

Copyright 2012 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

Nikon D4

The much-anticpated announcement of the latest incarnation of Nikon Pro Digital has just appeared on the official Nikon site and other popular review venues:

Nikon:  http://imaging.nikon.com/lineup/dslr/d4/

dpreview.com:  http://www.dpreview.com/news/2012/01/06/NikonD4launched

dpreview.com:  http://www.dpreview.com/articles/7799914638/nikon-d4-overview/

Joe McNally:  http://www.joemcnally.com/blog/2012/01/06/shooting-the-d4/

Engagdget:  http://www.engadget.com/2012/01/05/nikon-d4-dslr-camera/

The new camera specifications follow very closely to what has recently been reported on the rumors sites – good Sherlocking gang!

Okay D4, git in the shoppin’ cart!

Copyright 2012 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

In the Valley of the Goblins

Goblin Valley, UT.  Deposition and Erosion.  For millions of years, sediments were carried by ancient streams and deposited in ancient lakes, forming what would eventually become alternating layers of sandstone, siltstone, and shale.  Later, tectonic forces caused an uplifting of the region we now know as the Colorado Plateau.  The forms we call Goblins are the result of erosion, with harder caps of sandstone lying above softer layers of siltstone and shale.

Based on the presence of Barrier Style Art nearby, we can presume that humans have been visiting the area for thousands of years.  In historical times, the area was visited by cowboys throughout much of the 19th century.  Arthur L. Chaffin, a prominent Utah engineer and entrepeneur, discovered the area with companions sometime in the 1920′s (Wikipedia ref).  By the 1950′s, the area was actively being marketed to the world.

This unique geographical location was known for many years simply as Goblin Valley.  More recently, the State of Utah, or perhaps Emery County Commissioners in league with local entrepreneurs, have seemed to want to rename the area ‘The Valley of the Goblins’, as if to give the area a more posh appellation.  No matter what you call it, the small basin that contains what Mark Milligan has called the ‘wonderfully grotesque stone sculptures’, is a geological wonder not to be missed.

Goblin Valley may be reached from either the north or south from Utah State Route 24 (SR-24).  SR-24 runs between US Highway 70, 11 miles west of Greenriver south to Hanksville, where it then veers west through Capitol Reef and Torrey to Bicknell, and then turns northeast, eventually ending at Salinas.  From the north, travel south from the junction with US 70 about 24 miles to the junction with Temple Mountain Road.  From the south, travel north from Hanksville about 19.5 miles to the Temple Mountain Road junction.  Turn west onto Temple Mountain road and travel about 5 miles to the junction with Goblin Valley Road.  Turn south onto Goblin Valley Road and travel 6.4 miles to the entrance station (daily use fee as of 12/2011 was $7.00 per vehicle).  The valley overlook is 1.2 miles beyond the entrance station.

The two images directly above are representative examples of the structure of the Goblins, with the smooth rounded Entrada Sandstone caps near the center of the image on top of the softer gravely silt layer which dominates the lower right corner.  The Goblins vary considerably in height, from a about one meter up to perhaps 10 meters.

Images in this entry were recorded between 16:00 and 17:00 MDT on August 28, 2011, using the Nikon D3s and the AF-S NIKKOR 24-70mm f/2.8G ED at various focal lengths.  Exposures were f/11 and f/16, with shutter speeds of 1/125s and 1/80s respectively (+0.33 EV), ISO 200.  The images were deliberately overexposed by 0.33 EV and normalized to correct exposure in Raw conversion (ACR 6.6) to reduce noise.  Images were converted to BW using Nik Software Silver Efex Pro 2 with additional processing in Nik Color Efex Pro 4.

A Google Earth image of Goblin Valley is shown below:

An excellent guide to the geology of Goblin Valley written by Mark Milligan is available online:

Copyright 2011 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

A Trickster in Hayden Valley

A number of native American Indian cultures have identified the coyote as The Trickster.  A trickster is a sort of cunning character who makes use of subterfuge, i.e., illusion, misdirection, etc., usually with the goal of committing some sort of fraud.  Accepting for the sake of discussion that it is valid to anthropomorphize wild animals, then to my eye, the suggestion that the coyote is a trickster is an apt judgement – they always seem to be up to something slightly sketchy.

This trickster nature is apparent in the way the coyote carries itself, which a bit shifty, moving through the sagebrush or tall grass like a pickpocket working the crowds at a carnival.  The short, persistent gait of the coyote is distinct from that of the wolf, which has longer legs and a resulting much more open stride. Parenthetically, although there are several ways to distinguish wolf and coyote, the difference in gait is the thing that I notice first.

And of course that Coyote face, which is so full of mischief…  Is it my imagination, or are these guys always squinting?

Perhaps it is their opportunistical feeding behavior that impresses me most.  Unlike wolves that hunt large prey in organized hierarchical groups, the coyote bounces around solo or in pairs, and will eat anything it can.  Voles seem to be a staple food of the coyote.  We have watched coyotes consume half a dozen voles in a single episode – in fact I cannot recall seeing coyotes eat anything but voles!

Leaving out the anthropomorphic judgements, there is no doubt but that the coyote is a highly adaptable and highly successful creature.  The Trickster even adapts relatively well to urbanization.  Although it is most common to observe coyotes hunting solo or in pairs, within Yellowstone, coyotes live in packs of up to seven individuals.

Prior to the reintroduction of wolves into Yellowstone in 1995, the coyote population grew to relatively large numbers due to the lack of a major predator.  In the years immediately following restoration of a stable wolf population, coyote numbers fell 30-50%, but the population has now stabilized.  The Yellowstone Resource and Issue 2011 report* does not provide a specific population esitmate for coyotes, and lists the population only as ‘numerous but unknown’.

Images in this entry were recorded in the Hayden Valley, Yellowstone National Park, at around 13:30 MDT on September 21, 2011, using the Nikon D7000 and the AF-S NIKKOR 200-400mm f/4G ED VR II  at 400mm (600 mm FX equivalent).  Exposures were made at f/5.6, f/7.0, and f/8.0 with shutters speeds at either 1/1000s or 1/1250s.  Tripod setup was the Gizto GT5541LS and the Wimberly WH-200 gimbel head.

*The Yellowstone Resource and Issues 2011 report is issued annually, and is produced by the Division of Intepretation, Yellowstone National Park, Mammoth Hot Springs, WY.  The report is available at the park bookstores and online at the followstone site:

http://www.nps.gov/yell/planyourvisit/resourceandissues.htm

Copyright 2011 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

Meredith’s Garden

Hidden amongst tall firs a few miles east of the Willamette River, there is a secret garden.  Meredith’s garden.  From the outside, it’s anyplace SE PDX, but inside, well inside, it’s a magic world.

As you can see, ‘magic’ is pretty much the same thing as trees and bushes, moss and leaves, and wet, plenty of wet.

The images above were recorded at around 12:00 PST on November 25, 2011, using the Nikon D3s and the AF-S NIKKOR 70-20mm f/2.8G ED at various focal lengths.  All of the images in this entry were converted to HDR using Photomatix Pro 4.1.4: Both single-shot and bracketed input images were used.  I currently favor Photomatix over HDR Efex Pro.  Both are excellent software packages, and although the Nik-ware provides a huge array of default styles, only a few of them are actually very useful.  By contrast, Photomatix seems to produce images with greater depth and pleasing contrast and color saturation with little effort.  The recent addition of real-time hints for parameter functions in Photomatix is very useful.  Additional contrast and saturation, as well as increased local/micro-contrast were applied using Kin Viveza 2 and Nik Color Efex Pro 4.

Copyright 2011 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

Rock Wall, Plants, and Light

Having sorted out the Thanksgiving Day feast, I returned to my usual spot looking out the front bay window of Meredith’s house, watching PDX flow by.  It’s an entertaining procession.  Based on my admittedly casual estimate, PDX must be at around the 1000% mark for cyclists.  And it’s not only during the infrequent sun-breaks, these people ride rain-or-shine.  Of there are also plenty of peds strolling by too: Old folks, young folks, odd folks.

Anyway, during a sun-break I noticed a particularly brilliant shaft of light illuminating a short span of rock wall across the street.  But really, it’s not just a rock wall, but a conspiracy of rock, and moss, and wetness, and weeds, and fallen leaves, and it’s remarkable how under the right circumstance a touch of light can change the dull into something interesting.

The images above were recorded at 09:30 PST on November 25, 2011, using the Nikon D3s and the AF-S NIKKOR 24-70mm f/2.8G ED at 70mm.  Exposure was f/8.0 and 1/640s (-0.33 EV), ISO 1000.  Handheld.

 Copyright 2011 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

NE Entrance Road

The NE Entrance Road is one of the major thoroughfares of Yellowstone National Park, linking Tower Junction to the southwest and the northeastern park boundary.  From its western terminus at Tower Junction, the road heads northeast about 0.75 mile to the bridge over Yellowstone River.  The road turns to true east after the bridge.  The road then tracks along the Yellowstone and Lamar Rivers at the base of Specimen Ridge to the bridge at about 4.5 miles, and then another 0.6 miles to the junction with the road leading to Slough Creek Campground.  From the campground, traveling east another 0.75 mile brings you to the west end of Lamar Canyon.  The length of the canyon is about 1 mile, and opens at the east end to the broad expanse of the Lamar Valley.  The road then heads southeast along the Lamar River for 2.75 miles to the Yellowstone Associate Camp, and then another 2.8 miles to the confluence of the Lamar River and Soda Butte Creek.  The confluence of the Lamar River and Soda Butte Creek is a major park reference point, and both rangers and park cognoscenti refer to the location as ‘The Confluence’.  From here to the park boundary the road runs alongside Soda Butte Creek.

Assuming that you are coming from points west, and after passing through the Lamar Valley, it is just when you think you have left Yellowstone’s geothermal features behind that you run nearly right in Soda Butte at 2.3 miles east of The Confluence.  This extinct cone is just a few feet south of the road.  This is where we associate the story with images.  The image above was shot at a turnout about a half mile southwest of Soda Butte (1.8 miles east of The Confluence).  There is a minor stream here that drains the high ground to the north into Soda Butte Creek.  The relatively abundant water supports the growth of Chokecherry and other leafy plants, generating a stark contrast again the pale green of the sage.  The image was recorded at 11:30 MDT on October 16, 2011, using the Nikon D3s and the AF-S NIKKOR 16-35mm f/4G ED VR at 23mm.  Exposure was f/11 at 1/25s, ISO 200, +0.33 EV.  A dark and mostly rainy day.  The image was processed using Photoshop CS5 with Nik Viveza 2 and Color Efex Pro 4 plugins.  Capture and output sharpening was applied using Photokit Sharpener 2.

A Google Earth image of the location appears below:

Traveling northeast along the road brings you, after 3.3 miles, to the Pepple Creek Campground, the last camping spot along the road. After traveling another 1 mile you will arrive at the Thunderer trail head (3K3) parking lot and the entrance to Soda Butte Canyon.  Soda Butte Canyon is tucked in between the Barronette Peak to the northwest and The Thunderer massif to the southeast.  The road continues through Soda Butte Canyon, coming after about 1.5 miles to the narrow Icebox Canyon.  There is a very nice picnic spot just at the northern end of Icebox Canyon – we saw a small Griz on the far side of the stream here in the early spring of 2011.  The road continues through Soda Butte Canyon reaching the WY state line at about 5.8 miles further, and the park station at about 2 miles beyond the state line crossing.

This region of the park is home to many animals, including both Black Bear and Griz, but because of the relative steepness of the canyon walls on either side, the wildlife is only visible when they are basically right along the road.  This situation presents a minor hazard, since it is possible to encounter Griz with relatively little advanced warning.  If you stop along the road here, I strongly advise you to keep your bear spray close at hand.  On this visit was were fortunate to catch a glimpse of a Black Bear foraging along the north side of the road.  The location was approx 100 meters northeast of the turnout for the Thunderer Trail.  We were able to watch this bear for about 30 minutes before it wandered off into the dense forest. I have come to notice that Black Bear rarely look directly at me, and perhaps even avoid direct eye contact.  Many species consider eyes-on to be a threatening gesture, and I suspect that Black Bear are quite adept at avoiding conflict.  This behavior is quite distinct from that of Griz, which will tend to keep a steely bead on you at all times.

Images of the Black Bear were recorded at around 17:30 MDT on October 16, 2011, using the Nikon D3s and the AF-S NIKKOR 200-400mm f/4G ED VR II at 400mm.  Exposure was f/4.0 and 1/125s to 1/200s, ISO 6400.  Yeah, here as in many posts, these images are possible because the D3s + VR exist.  The noise is actually pretty modest, but the color noise components were reduced using Nik Dfine.  Additional processing was applied using Nik Viveza 2 and Color Efex Pro 4 and Photokit Sharpener 2 plugins.

Copyright 2011 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.

Postcards from Grand Teton National Park

On visits to Yellowstone NP, we often return through the south entrance and continue through Grand Teton National Park along US 89/191.  It makes for a long drive back to Salt Lake, but the scenery is always worth the extra miles.  The image above was recorded just inside the northern boundary of the park entrance, while the image below was recorded just off the Jackson Hole Highway just south of the Willow Flats Turnout, near Jackson Lake Lodge.

The color in the Tetons was amazing this fall.  The Aspens did not only glow a brilliant golden yellow, but deeper shades , all the way to red, as shown above and below, could also be found.

A characteristic of images recorded in the Tetons at this time of year is that they are dominated by orange/red and blue.  There is so little green around that one must be careful to avoid producing images that appear overprocessed, e.g., with too much saturation, too much contrast, and a blueish white balance.  Even though I always follow my own advice, I thought these images had an almost vintage picture-postcard look – much more so in the smaller rendition of the images that appear in this entry.  The image below was hot at the Oxbow Ben Turnout, with the Snake River in the foreground and Mount Moran in the distance.

Grand Teton NP is especially nice to visit this time of year.  The crowds have dramatically diminished, so much so that one can spend an hour in a spot all alone.

The image above was recorded along the Jackson Hole Highway, US 89/191, just a bit south of the Moran Junction.  The image below was recorded at the famous Snake River Overlook Turnout.

 Images in this entry were recorded during the late morning on October 17, 2011, using the Nikon D700 and the AF-S NIKKOR 24-70mm f/2.8G ED  and AF-S NIKKOR 70-200mm f/2.8G ED VR II lens.  Exposures were made at f/8 or (mostly) f/11, ISO 200.  Images were processed using Photokit Capture and Output routines, a Photoshop curves adjustment layer, and Nik Software Viveza 2 and Color Efex Pro 4 plugins.  It is very useful, even essential, to use the Smart Filter feature of Photoshop when applying the Nik (or other) filters, since this makes readjustment easy and provides auto-archiving of the processing protocol.

Copyright 2011 Peter F. Flynn.  No usage permitted without prior written consent. All rights reserved.