Abstracted Cloudscapes #6 & 7

Back in the painting groove again after our trip, and here are the latest two in the abstracted cloudscape series.

Both are on Strathmore 400-series pastel paper.  I was beginning to run low on my existing pad, so I went down to our local art store.  Apparently, they don't carry the 400-series pastel paper in 12x18" anymore, so I bought some 500-series tinted charcoal paper.  We'll see how that goes when I switch to it.  I like the paper simply because it's pretty inexpensive and so I don't worry about wasting it.  It accepts blending and layering much better than Canson M-T, but because its tooth is limited, it does force one to be a bit more judicious with pastel placement.

abstracted cloudscape series #6 - desert cirrus sunrise

12 x 12 inches

I did this painting yesterday afternoon, under less than optimal lighting conditions.  My studio table, which is in our living room, has a west-facing window.  When I have my computer monitor on to view the reference image, the afternoon light often causes the true colors and subtle nuances to be obscured.  So, this morning, when I came down and looked at it, it needed color adjustments.  Setting the painting aside for hours, or a day, is hugely helpful to see these and other discrepancies that were overlooked during the painting process.  

abstracted cloudscape #7 - sunset salute

12 x 12 inches
SOLD

Another high-chroma sunset.  This was done on rust-colored paper, about the same as the orange/rust colors in the clouds.  I am having trouble resisting the urge to finger blend these paintings, and while it does give a soft look to parts, at other times, it makes the piece look overworked.  I'm still trying to figure out the best way to approach the blocking in of clouds like these, where there are areas of multiple colored clouds that have smudges or tiny patches of blue sky showing through.  And, I've also found that despite the usual rules of pastel painting - light over dark - this doesn't always work so well.  Laying yellow over the darker mauves and purples often results in an ugly dulled color.  

I need to resist the urge to finger blend on some of these, even if paper shows through, and see how I like it.

Oh - a milestone here:  #6 makes the 100th pastel painting I've completed to date since I started painting last fall.  I suppose now I can officially call myself an "artist" now :).   

Labor Day trip to north rim of GCNP- Part II: the Canyon

The north rim of the Grand Canyon differs from the south rim in several ways.  For one thing, only about 10% of the visitors to GCNP go to the north rim,  making it much less congested.  The elevation is also about 1000' higher than the south rim, resulting in views that allow one to almost look down upon the distal horizon.  The reason for this is the series of faults and the east Kaibab monocline that produced the Canyon:  the earth rose and the water cut a channel through the sedimentary layers along the fault line.  Side canyons formed as water found its way to lower points, causing more rapid erosion.  There probably remains some debate amongst geologists, but I believe it is generally accepted that the Canyon itself is about 5-6 million years in age.   It averages 10 miles across,  a mile deep, and is 277 miles in length.  The rocks that form it span in age from 245-1700 million years [1.7 billion].    Simply put, the magnitude and scope make it hard not to be impressed.

We arrived at Timp Pt. around 5:30, AZ time, on Friday afternoon.  Monsoon season was either over or was on a brief hiatus, so there were no concerns about rain.  In fact, it was a cloudless day for most of the drive, which is always less than optimal when hoping to get some great photos.   However, clouds had appeared to the west as we drove, and some lingered over the canyon itself that evening.

We secured a campsite, but after taking a walk down the road, discovered that the next site over actually had a better view (a plus for me, as I had planned to paint, and wasn't keen on hauling my pastels and easel out 1/2 mile to the other vista we found).  So, we relocated our gear, just as the sun was setting.

Sunset at Timp Pt.

This was the view about 20' from our campsite.   The view is to the south and slightly west.  Not a high-drama sunset that can often be seen at the south rim due to the direction of the light, but this instills a sense of calm, I think.  There was a lot of haze in the Canyon, either from Las Vegas or dust particulates from the dry air and wind.

Mid-morning light
Because of the haze and lack of clouds, I didn't end up taking that many photos, or at least with the intent that they turn out "photo-worthy".    But,  you can't come to the Grand Canyon and not take at least some photos to remember the stay, so here is one.

The western edge of Powell Plateau is seen to the left, connected by a saddle to Steamboat Mtn.  The Colorado river is on the distal side, running between the sets of reddish cliff sets.  The Havasupi reservation is on the south rim.

Saturday was "do your own thing" day; Wayne went on a hike along the Rainbow Rim trail, Dave and Eva took their mountain bikes along the same trail, and I attempted to paint.  I had earlier cased out the prime location for setting up an easel, and thought I'd be able to do at least a few paintings.  But, it ended up being quite hot, and instead of setting up the easel in the sun, I pulled a chair over and painted in the shade.  Because it was so difficult for me to narrow down a composition sitting there, I ended up using a photo and sketching the basic shapes in from the thumbnail view, and then working from the view.

The painting isn't posted because it got pretty significantly smeared when it was taken out of the car after we got back.  I may try to fix it, but haven't had the desire to thus far.  It suffered from the limitations of my pastel palette, although as with the previous plein air paintings, it was a valuable process nonetheless.

On Sunday, our group decided to go hike along a different portion of the Rainbow Rim trail.  This trail, which starts at Timp Pt. and ends at Parissawampitts Pt., is 18 miles in length, one way.  It's a multi-use single track trail open to any non-motorized form of transportation.  It follows the contour of the rim, much of which requires long cut-backs through the forest in order to cross the drainages to the side canyons before they become impassable cliffs...

We drove out to North Timp Pt., and before we knew it, we'd decided to go all the way to Locust Pt., 6.5 miles away.  None of us were planning such an ambitious hike, but given that the trail was essentially level with minor changes in elevation, and in shade much of the way, it didn't take on Death March proportions.

View approaching Locust Pt.

We had to hike 6 miles through the forest before the rim came into view again.  N. Timp Pt. is immediately to the left.  Steamboat Mtn. is above it to the left.
The gray-white cliff formation is Coconino sandstone, which overlays the dark red Hermit formation.  In this part of the canyon, the Hermit is frequently covered with vegetation.

Eva, Dave and Wayne at Locust Pt.
Everyone is happy that we made it and can now turn around and hike the 6.5 miles back to the car.  North Timp Pt, and the location of our car, is right above Eva's right shoulder.

It's easy to underestimate distances and scale in the Canyon; it is probably less than a mile as the crow flies, but impossible to get to without a hike of several miles.

The hike back:  Ponderosas and a view
I opted to take photos of the trail on the way back.  Better lighting and a more leisurely pace.

This is looking back towards Locust Pt., showing the hint of the rim ahead, and the beautiful ponderosa pines.

Through the aspens...

This is heading back to N. Timp.  We are still on the north side of the drainage heading east, well before cutting back across the draw.  The trail heads through this lovely stand of aspen before dropping down on its approach towards the cutback part of the trail.






...and a grassy meadow
After the trail drops down from the N. Timp Pt. ridge, it enters the draw - a beautiful grassy meadow with aspen, fir and pine.




After another ~3 1/2 miles or so, we are back at N. Timp Pt.  Dave and Eva had powered through the hike without stopping, having been a bit low on water.  It was after 4 p.m., and the light was turning the Canyon into a series of silhouetted shapes, ever fading as they disappeared into the western horizon.

N. Timp Pt. pano

What is car camping with friends all about?  Hikes like these, sitting around a campfire each night after a hot meal, and of course, drinking beer.  No one came unprepared, and especially after a 13 mile hike, cold beer sounded like an excellent idea.    Here is the informal "beer tree" or "beer shrine" that was going at the campsite.  It looks rather white trash until you realize there is no Coors,  Old Milwaukee, or Budweiser, or cans - just Ska microbrews and some Sam Adams and Full Sail Pale Ale:  the Good Stuff.  The spontaneous placement of the bottles in this common location appealed to our artistic aesthetics (and sense of humor), so it had to be captured on digital film before the bottles were collected prior to our departure.  

Sunrise at Timp Pt.


Due in part to both early morning insomnia and my motivation to actually get up and out of the tent for the 1/2 mile walk down a spur trail off of the Rainbow Rim trail to the actual Timp Pt, I did manage some sunrise photos.

There is something special about sitting on the rim of the Canyon before sunrise and watching as those first rays hit the far edges of the rim and then sweep across the depths, casting shadows here and there on the buttes and canyons.  It was quiet, save for some small birds that were diving and cavorting through the otherwise still air.   As much as I'd like to be, I'm not much of a morning person.  So, being able to actually get up and watch the sunrise (around 5:45 a.m.) was a treat.  Dave, an accomplished photographer, had gotten up the morning before to shoot sunrise photos, so that also helped motivate me to get up.

Light across points and plateaus
In this telephoto view to the southeast, Stina Pt. remains in shadow, while the upper sandstone cliffs of Powell Plateau receive early morning light.  A small, distal triangle of the south rim falls between. The elevation drop between north rim (of which Powell Plateau is part of) and the south rim is evident in this photo.




So, after a wonderful weekend enjoying the tranquil beauty of the north rim with friends, we packed up and headed home on Monday morning.

Hmm...just realized it is Friday already!  Sky Friday posts to resume next week.

Labor Day trip to north rim of GCNP- Part I: getting there

One of the most joyous things about returning back in the southwest is once again being close to the canyon country of the Colorado Plateau.  I love the mountains of the San Juans here in Durango, but the canyons and landscape of northern AZ and southern Utah are truly where my heart and soul belong.   To my eye, it is the most beautiful and fascinating landscape in this country, if not the world.  The earth's skin is exposed, not covered by endless forests or oceans or pavement or malls, and able to be experienced in all its glory.

Rock layers formed over hundreds of millions of years from shallow seas, mudflats, and sweeping sand dunes, long before mammals (let alone humans) were even a blip on the evolutionary map.  After they were formed, time, water, wind and plate tectonics worked to carve and sculpt the most amazing forms out of the earth.  And, wherever you go within the geologic province known as the Colorado Plateau, there will always be something different and uniquely beautiful to see.

During the eight years I lived in Flagstaff and Prescott, I made countless trips to my favorite destination:  the Grand Canyon.  I hiked, ran and backpacked along the many trails and routes found within its depths, and never once did the novelty wear off; in fact, the more I was there, the more I *wanted* to return and immerse myself within it.   It remains, and will always remain my favorite place on this earth to be.   During the time I lived in CT, I was terribly homesick for this landscape.

So, when Flagstaff friends Dave and Eva sent out an Evite for a Labor Day car camping trip to the north rim of the Grand Canyon, it didn't take long for Wayne and I to agree come!

The drive from Durango to the Grand Canyon is without a doubt one of my all time favorites.   It's what road trips are all about.   For closet geologists like myself, it's a never-ending, always changing wonder of the earth's beauty.  It goes through a good portion of the Navajo Nation as well, which means never worrying about large, ugly tracts of cities or suburbia or, for that matter, much human influence at all.  Most of the ugly is confined to the perfunctory HUD prefab junk homes or run-down single-wide trailers so 'graciously' provided to the Navajo by the "ever-so-generous" federal government, in small, scattered pockets throughout the reservation.  An occasional hogan made from local materials is a comforting reminder that not all native culture has been completely squeezed out of the area.

I have decided to spit this into two separate blog posts.  I took over 400 photos during the trip, most of the drive itself, because it was just amazing.  So, it needs its own post, as does the Canyon.  I hope you enjoy the trip through this photo essay, and perhaps can understand why I love this country so much.

Church Rock and Comb Ridge pano

Church Rock is one of the many volcanic necks, or diatremes, in the area.  These form when lava and gases erupt through a weak point in the earth's crust.  Shiprock, in northern NM,  is another, larger example.  Comb Ridge is an example of a monocline, or one-sided tilted fold, in the earth.  Click on the photo to see the uplifted rock of Comb Ridge, formed from Jurassic period Navajo sandstone.  It looks small in the photo, but each of those notched uplifts of rock are probably over 200 feet high.

These unusually eroded forms of Entrada sandstone are known as the "Baby Rocks", and are at the base of Baby Rocks Mesa, on the south side of Hwy 160.  This photo was actually taken on the way home when I could shoot through an open window.

Whimsical formations like these, found commonly throughout the CP region, are also generically known as "hoodoos". 

Hwy 160 towards Kayenta.   Black Mesa, seen to the left, is formed of Cretaceous period deposits, ranging from sandstone to shale and the flammable rock known as coal.  To the right, Organ rock monocline, is visible as large pink arcs of rock.  The town of Kayenta is to the right and barely visible.  Monument Valley is also to the right, approximately 22 miles to the north.

Close-up of Organ Rock monocline.  Composed of Navajo sandstone, as it abuts the Shonto platform to the north.  Navajo sandstone is the principal rock that forms the dramatic cliffs present in Glen Canyon/Lake Powell.  It is also prone to forming natural arches, and suggestions of arch formation can even be seen in this photo.

Painted Desert along Hwy 89.  

Ten miles past Tuba City, Hwy 160 terminates into Hwy 89.  We are now headed north, and this view is to the east.     These colorful rocks, known as the Chinle formation, formed from Triassic-period mudstones deposited over 200 million years ago, and are what make up the Painted Desert region of northern AZ.  The rock is soft and easily eroded; often, a small harder cap of rock is all that keeps it from eroding into the surrounding alluvial deposits.

                                                                                       

Echo Cliffs along Hwy 89.  The Echo Cliff monocline is to the east side of the highway, running over 30 miles and across the UT border.  It is formed from the Glen Canyon group of Navajo sandstone (top layer), Kayenta formation and Wingate sandstone.    These cliffs apparently got their name from a member of the second Powell expedition, after hearing his voice echo after.  Marble Canyon and the Colorado River are to the left/west a few miles.  

Vermillion Cliffs towards Marble Canyon.  This is the view right before the road drops and heads over the bridge crossing the Colorado river and near Lee's Ferry.  Lee's Ferry is named after a Mormon, John D. Lee, who was made a scapegoat for the infamous Mountain Meadow Massacre, where almost 150 settlers headed from Missouri to CA were killed by Mormon zealots under the leadership of Brigham Young.  It is now a popular fishing area and put-in location for all boat trips through the Grand Canyon.

 Monocline meets Plateau.  More enigmatic geology.  To the right, we have the Vermillion Cliffs, which form the southern border of the Paria plateau, made of up of Chinle and Moenkopi formations (both Triassic).  To the left is the beginning of the East Kaibab Monocline.  Its surface rock is Kaibab limestone (or formation), a Permian-period rock of 245 million years.  This is the rock you stand on at the edge of the Grand Canyon.  All the younger Triassic rock, deposited over millions of years, has eroded away.  How?  Why?  Now, a small rift valley separates the two, filled with alluvial deposits of rock, old and new.

 On the Kaibab Plateau.  After leaving House Rock Valley (shown above), Hwy 89 winds up the monocline through pinon-juniper to Ponderosa pine on top of what now becomes the Kaibab Plateau.  At Jacob Lake, Hwy 67 now heads due south and towards the rim.  It continues to climb in elevation, and soon the predominate trees become aspen, fir and spruce.  The road soon opens into a long meadow.  Unlike the east coast, where essentially all meadows and fields are man-made, these meadows are natural.  Filled with grasses, wildflowers and occasional outcroppings of rock, they add to the scenic drive towards the rim.

Along FSR 22.   This shot was actually taken the morning we left, but I include it here as it shows the roads taken to arrive at our final destination on the north rim:  Timp Point.

Aspen and ponderosa pine make up most of the forest along the FS roads, as shown in this photo.    On the north rim, many locations at the rim itself are on FS land vs. NPS.  Camping is at-large and there are no fees to camp (but no facilities, either).  It also means no crowds...and that is one of the things that makes the north rim so special.

Next post:  Three days at the north rim.

Go Take a Hike: CT from Little Molas lake

Colorado is the state for people who like to be outdoors.  Not only is the scenery spectacular wherever you go, but trails are everywhere.  And not the sad excuses for "trails" that continually disappointed me in CT, where they cross roads, playgrounds and pass right up against people's backyards, where traffic sounds and other human-caused noise were never far away and having to be concerned about loose dogs from someone's adjacent property chasing you was always an issue.  Plus, there was never a "destination" - it was just hiking through the same deciduous forests along trails with no view, to some other point that essentially looked the same.

Not so here in CO.  This state takes its recreational responsibilities seriously, as well as the importance of preserving land as "wilderness areas".  For those not familiar with what a wilderness area designation, it means:  1) no human development (buildings, roads, etc.);  2) no vehicles of any kind, including bicycles.  Hikers, equestrians, nordic skiing, snowshoeing - those are all good.  Two long trails traverse a good section of this state:  the Continental Divide trail, which goes from the Mexican to Canadian border across 5 states, and the Colorado Trail (CT), a more modest 500 mile trek going from Durango to Denver.

Plus, there are mountains, so the trails here almost always lead to a view, even if they start out in a pine or fir forest.  Sometimes, it's a bit of work to get to it, but it's always worth it.

Needless to say, after 3 1/2 years e wasted no time getting back into hiking after moving here.   In southwestern CO, the mountain range is the San Juans, which are part of the Rocky Mountains.  However, unlike the front range and northern Rockies, which were formed as a result of plate tectonics that occurred 45-70 million years ago during what is known as the Laramide orogenic event,  the San Juans are primarily volcanic in origin.  This makes for atypical shapes, erosion patterns and colors of the rock, and amazing views, even driving along the state highways.

This series of photos was taken along a section of the CT near Molas Pass, which is about a 45 min. drive north of Durango on Hwy 550, and heading in the direction towards Durango.  Some of these photos were taken with my Olympus p&s camera before I had the 18-70mm for my Nikon, so the limitations of its sensor are apparent by the limited dynamic range (aka "blown out skies").

Trail winding through spruce and fir approximately 1/2 mile from trailhead

A field of colorful fireweed is right off the trail, while a monsoon storm builds to the west.  Wildflowers were abundant on this hike, and included various Aster species (daisies), Western Paintbrush, Pearly Everlasting and other species I couldn't identify.

View back to the east shows Little Molas Lake (the same elevation as the trailhead), and a view of the Grenadier Range of the San Juans.  Despite what the photo shows, the skies were quite dark due to storms forming from the east and west.

The sculpted form of a long-dead tree makes up the foreground for this shot of a peak to the west.  Note the varying colors and forms of the strata that are visible.  

Cumulonimbus over Engineer Peak.  Engineer is one of those landmarks that everyone knows about.  On an earlier trip we made to Durango in '06, we hiked/climbed to within a few hundred feet of its summit (~12,900').

Pano shot of Sultan Mountain (center) and Grand Turk (right).  Not much further up the trail, we opted to turn around due to the impending thunderstorms; getting caught in a storm with lightning above timberline is a Bad Idea.

We ended up hiking about 5 miles, and got back to the car without getting caught in rain.  We drove to Silverton (~8 miles to the north) for some coffee, and that's when it began to rain.  

Sky Friday - cloud panoramas

If you've ever taken a series of photographs and used software to stitch them together into a panorama shot, you know how addicting creating "panos" can be.

Back when I had PS Elements 4.0 on my old PC, I used that pano stitching program, but found it a bit time-consuming and it had major limitations and shortcomings, like a really poor blending tool and frequent error messages about not enough memory to complete the task that seemed to take forever.

I still haven't purchased the latest edition of Elements, but recently started taking some pano series shots for the time when I had the software available again.  Then, on a whim, I decided to do a search for "panorama software, iMac", and read some reviews.

Written by a Danish software engineer (I assume that's his title) called "Double Take" came up as an easy-to-use, stand-alone stitch program.  And, you could download a trial version of it for free.  The registered version is only $24.95, which seemed like a deal if it worked well.  The official site is here, where you can read more, download and/or purchase the program.

Anyhow, I tried it on a set of photos I took a few weeks ago on one our hikes, and was amazed at: 1) how simple it is to use; 2) how well it works.  I'd previously tried Hugin, which is a free Linux-based stitching software, based on a review by Ken Rockwell, but I couldn't get it to do anything, and it was far more complex and confusing than I wanted.  Double Take, on the other hand, is simple yet has features that make it vastly superior to the pano program in Elements.  Even when I do get around to purchasing Elements, I'll keep using Double Take for all panos.

* You open up a new file and literally drag and drop as many photos, one at a time, as you want.  The program automatically matches up each one as you drag it.  You can then re-adjust each if needed.  I found the program did a better job than I did.

* You can then edit each one to adjust for exposure, gamma, saturation, brightness and contrast, and correct the geometry of each, if needed, for rotation, pitch and scale.  You can also select it to crop automatically and lock each stitch into place.

In short, it is great.  I ended up ditching all my previous pano shots made in PS Elements and re-did them in DT, in a fraction of the time, with far better results.

Since then, I've gone on a bender with the pano shots.  Even with my zoom lens that allows for wide-angle shots, I still find that a two-shot pano gives more detail and will allow for a bigger size, should I ever care to print it, than a single wide-angle shot.

So, this Sky Friday features several sky panos.  Locations vary, but most were shot on my deck.  All are two-shot panos.  I should also add that most of these were shot in RAW format, and the program handles that just fine, probably as iPhoto jpeg conversions.

Cumulus congestus afternoon 

August 29, 2010

Stratocumulus sunset

August  30, 2010

Cumulonimbus over Perins Peak

August 25, 2010

Sunset and fading storm

August 25, 2010

Virga over Horse Gulch

August 29, 2010

Altostratus sunset

August 27, 2010

Colorado Wildflowers #3

A temporary break from the paintings to bring you more of the beautiful wildflowers of Colorado.  It's now late summer, and flower season is just about over.  Petals are shrinking and dropping and the flowers are busy going to seed in preparation for winter.

I was delighted that on every hike we went on, I discovered new flowers I'd not seen before.  It made the hikes that much more special.

Here is a random assortment of some of my favorite images taken in various locations in our area.

CT - Colorado Trail

Scarlet Gila or Fairy Trumpet

These eye-catching flowers are found throughout open forests and dry slopes in the region.  

Location:  Dry Fork Cr. trail.  Early August.

Grass of Parnassus

Found near streams and moist areas, this flower is not too commonly seen.  Location:  CT, near Little Molas lake.  Early August.

Colorado Blue Columbine 

It's not hard to see why this lovely flower is the state flower of CO.  Location:  Engineer trail, late July.  Also seen in late Aug. along the Cross Mtn. trail, at timberline. 

Mountain Gentian

Location:  CT, Molas Lake.  Mid-August.

These flowers are seen at higher elevations (~10,000), and usually in open meadows.  We also saw them on the Cross Mtn. trail @ timberline and along the Ice Lake trail below timberline.

Rosy Paintbrush - two variants

Location:  Cross Mtn. trail, above timberline.  Late August.

Rosy Paintbrush is commonly found above timberline, and due to hybridization, the plants are quite variable in appearance and color of the bracts.  We saw these on almost all hikes when we were above timberline (~11,000).

Elephant Flower

CT, near Little Molas Lake.  Early August.

These delightful flowers are found near streams and other moist areas.  This was along the same small stream as the Grass of Parnassus, pictured above.

Alpine Gentain

Location:  Ice Lake Trail, 12,000'.  Late August.

This is one of the last flowers to bloom on the alpine tundra, and is quite lovely.  It was surrounded by colorful groups of Rosy Paintbrush and some type of Aster that I couldn't identify.

Abstracted Cloudscape #5

Here is #5, completed yesterday.  I should title it "Overworked", since it started pushing the envelope of what the paper was capable of dealing with, pastel-wise.  

This one is probably the most surreal and truly abstract of those I've done so far, since it resembles nothing most people associate with clouds.  It's not a commonly seen cloud, and I've never seen on in sunset colors before.  The photo it is based on was taken off my deck during a most fascinating sunset we had last week.   I'll probably post photos at some point.  The clouds you see are known as "mammatus", and are distended pouches seen on the undersides of a cloud.  The name comes from the resemblance to mammary glands.  I've actually seen them several times since being out in CO, usually associated with a cumulonimbus cloud.  These were on the south-facing surface of a large stratocumulus cloud.  No rain, though.  

What happens is as the sun sets, these distended areas are what catch the sun's rays, while the rest of the cloud remains darker.  The curves and shapes of the clouds are made much more visible by the bright light and it produces an eerie and really dramatic effect.  

abstracted cloudscape #5 - mammatus en sunset

pastel on Strathmore 400-series paper

12 x 12 inches

For this piece, I felt it was important to capture the curves of the lightest sections of the clouds, so I applied the pastel in sweeping motions to emphasize this.  There are multiple layers of purples, blues, rusts, and yellows applied, and I had to use lots of finger blending in order to try and achieve the soft transitions seen throughout the clouds.  

I really need to get some good sanded paper to work on, like UArt or Pastelmat, as I think the process would have been a bit less of a struggle.  Nonetheless, I rather like this piece.  It's got purples and oranges, which are two of my favorite colors.

On an unrelated note, we are going to be heading up to the north rim of the Grand Canyon tomorrow for a car camping trip with a few friends over the Labor Day weekend.  I'm hugely excited, as the Canyon is my absolute favorite place on this earth to be.  

I don't know if I'll have time to get another painting finished and posted, but I'm going to try and have several posts scheduled to post Thurs-Mon.  They'll be photos of a variety of subjects that I hope you'll enjoy.