The Great Southern Tour Redux – Britton Hill Florida

The Southern Highpoint Tour of 2012

 

Britton Hill, Florida, 345 ft.

 

April 29th, 2012

 

Wes Chapman

 

 

The Great Southern Tour Redux

 

Last year Martha and I joined the High Pointers Club – a group whose members set as a goal visiting the high points of all 50 states. High pointing includes climbing a lot of great mountains, but also a lot of small hills scattered across states not normally noted for such things. Hitting the high points of all 50 states requires a fair amount of training and experience as a mountaineer (and some luck on Denali), but ultimately the quest needs to be about more than just climbing. This is really getting out and getting to see America from other than a fly-over perspective. We started this quest last year, and started this trip with the count at 22, with the prospect for 5 more during the second and final edition of the Great Southern Tour – and no threat from avalanches to worry about.

 

The objectives this year are simple – the highpoints of FL, LA, AR, MS, and MO. Kickoff for this year’s tour is Britton Hill, located 40 miles outside Panama City Beach Florida. Martha found us a bed at the Choctaw Lodge on the Choctawhatchee River in the town of Ponce de Leon about halfway there. We had no idea what this place was all about, but it got great reviews on Trip Adviser, and we decided to give it a shot.

 

We stopped for dinner at the Bruce Cafe in the eponymous town.  We are both devotees of American Diners, and this one gets 3.5 stars – a very good rating – good food, great prices, and terrific ambience. It was full of local people having dinner, and closed at 7:00 – time that decent folk were at home and in bed.

 

The Bruce Café

 

Down 4 miles of bad road to the banks of the Choctawhatchee River we landed at the Choctaw Lodge, owned and operated by the delightful couple, Ron and Kathryn Hardy. This area drains a huge part of the State of Alabama, and one inch of rain in Alabama produces one foot of flood in Ponce de Leon. As a consequence the area floods prodigiously, and all of the houses are built on stilts or up on the bluffs further up the river. The guest house that we had was more like a weekend home – which Ron and Kathryn used it for before moving from Panama City Beach full-time and building their new home next door.

Our bungalow at Choctaw Lodge

 

The Hardy’s are self-described river rats, and live with a menagerie that includes two labs – Grace and Annie – a blood hound and the neighbor’s pet pig, Boris. Ron is a fellow hunter, harvesting much of their meat locally, and an accomplished naturalist with a tremendous knowledge of the flora and fauna of the river. Before his “retirement” he owned and operated the largest dive operation in the US, out of Panama City Beach. After a restful night’s sleep, we headed out on the river with Ron, Annie and Grace for an hour’s tour beginning at 7:00 am.

 

The tour was equal parts naturalist and local color. We saw 9-10 snowy egrets, a few heron and had a chance to head through the canals into a couple of the natural lakes that make up part of the drainage system. This area is part of thousands of acres of wildlife conservation preserve, and it showed in the wildlife – I’m a huge fan.

 

Of the local characters, the most compelling is Johnny Savage, a local boy who made good and went on to get a DDS, LLD, and served as a state legislator. He is now 77, can still do 20 chin-ups and has a vibrant dental practice overlooking the river. It has no waiting room, to facilitate conversation between Johnny, and waiting patients and, presumably, the patient himself, as circumstances permit. Johnny, together with Ron and several other guys play poker in a tree house three days a week – presumably so that inadvertent floods will not interrupt the game.

Annie and Grace on the River Tour

A snowy egret

Sun up on the Choctawhatchee River

 

After a delightful breakfast of eggs benedict – one of two treats I never get at home – we bade goodbye to Ron and Kathryn to let them prepare for their departure to the Okavango Delta in Botswana. They guide tours to Africa for photo safaris, and this will be their 20th trip. Ron and Kathryn were terrific hosts, with a wonderful home. This is a 5 star + experience and makes a trip to the lowest high point in the US – Britton Hill Florida – a worthwhile undertaking.

 

Big sign, no elevation – Britton Hill Florida

 

Proud success at the summit

 

Leaving Britton Hill, we headed East on I 10 and made our way cross country to Vicksburg to tour the battleground and spend the night at another B&B, Ahern’s Belle of the Bends. We vastly enjoyed the drive across Mississippi, having some great fried oysters along the way, and enjoyed the company of the Spirit riders Bike Club, with whom we traveled for almost 45 miles on routes 98 and 49. These guys were serious about their bikes and had done this before – it was a tightly choreographed performance and a lot of fun to watch.

 

Traveling up close & personal with The Spirit Riders

 

Vicksburg was home to one of the two great battles the concluded around the 4th of July in 1863 – the other being Gettysburg.  The battle was a 45 + day siege campaign waged by Generals US Grant and WT Sherman against Confederate forces led by General John Pemberton. Like all of the siege campaigns waged by Grant, this was relentless, overwhelming and merciless. The tour of the battlefield was awe inspiring and the state monuments were exceptional. It is amazing to think of the amount of state treasure represented by these colossal monuments – particularly when compared to the virtual total lack of corresponding efforts today – even at the national level.

 

Union gun emplacements with the Michigan Memorial in the background

The Illinois Memorial – remembering the 36,000 who served from that State

 

Vicksburg battlefield at Sunset

 

We did a one hour tour at sunset – a particularly poignant time of day for such an undertaking. Most impactful was the tour of the Union Cemetery – the Confederate dead were all buried in the city cemeteries. The Cemetery is absolutely beautiful – on the bluffs overlooking the Mississippi. The Federal Act providing for National Cemeteries was passed late in the War, and the dead, who had been buried pretty much where they had fallen, were moved to the new National Cemetery at Vicksburg; with tall stones for the identified dead, and short stones for those known only to God. The short stones outnumbered the tall ones by at least 4:1.

Adios from Vicksburg

 

Hiking Moosilauke on Easter and Tax Day

Hiking Mt. Moosilauke – a Tale of Two Weekends

 

10 Miles, 4,802 ft.

 

 April 8 & 15, 2012

 

The Prouty Mountaineering Program

(the first Prouty Challenge Event benefitting Dartmouth-Hitchcock Norris Cotton Cancer Center)

 

Wes Chapman

 

 Mt. Moosilauke April 8, 2012 – a frosty, windy Easter

 

 Mt. Moosilauke – April 15, 2012 – a warm and wonderful day

 

Mt. Moosilauke – Hikes on Easter and Tax Day

 

Spring brings a lot of changes in the weather, and these are amplified in the mountains. The last two Sundays have seen: 1) horrible, cold weather with 60 mph winds, and 2) gorgeous weather, and mild spring breezes with 60 degree temperatures. I had the opportunity to visit Mt. Moosilauke with my friend Rick Morse in both.

 

I’ve written much about Mt. Moosilauke – I’ll let the photos from these hikes speak for themselves. Enjoy.

Easter hike up Glen Cliff Trail in fresh snow

The Tax Day hike – Rick Morse, following climbing beavers

Rick Morse, dressed for the weather on Easter

Wes dressed for a warm lunch on the summit

 

Baby & Ted – ears flying in the breeze on Easter

 

Enjoying the “bald place” of Moosilauke

 

Mt Washington and the Presidential Range from the summit

 

Franconia Ridge

 A sporting climb on a warm day up the Beaver Trail

Adios from Mt Moosilauke

Chaos Theory, Sub-Prime Mortgages & Positive Feedback Loops

Capitalism at a Cross Roads

Considerations of Persistent Disequilibria and Positive Feedback: Finding the Butterfly

Wes Chapman

April 8, 2012

 

PREFACE

The twin marvels of truly awful weather and systemic market meltdowns have a lot in common. First they feed on persistent disequilibria in their respective systems – weather systems feed on temperature and pressure differentials which can only be resolved through long time frames for adjustment or short term violence – storms. Similarly, economic and financial disequilibrium tend to be founded on regulatory or information impediments, leading to persistent positive feedback loops – first running markets up, and then, inevitably, leading to collapse.

Awful weather – a self-feeding phenomena

Really chaotic behavior in weather systems and financial markets requires that several positive feedback phenomena – think low interest rates, rising housing prices, systematic mispricing of securities, failed regulation, and systemic level fraud – are required to produce a real financial apocalypse. What makes the process interesting is that these factors may exist in the system functioning perfectly for decades, and only when combined a special brew a la the Three Witches of Macbeth do we get the resultant fiasco.

There has been a steady stream of metaphorical comparisons of Sebastian Junger’s book, The Perfect Storm, with the Great Recession in general, and the meltdown in sub-prime mortgages in particular. It is worth taking a look at what actually made the Perfect Storm unique, and what comparisons are meaningful to the sub-prime meltdown vis-à-vis complexity theory.

If they merge – you get the perfect storm

The Great Recession is a rolling disaster that the world economy seemingly stumbled into in the spring of 2008 led by a housing collapse which began in the sub-prime mortgage market.  This rolling economic Verdun was born many years before in a series of ill-conceived and poorly understood policy initiatives championed by consumer advocates and industry groups alike. These reforms – generally characterized as deregulation – were targeted at the seemingly laudable targets of risk mitigation and fairness, and categorically achieved just the opposite. In this paper I take a look at the human faces behind the fiasco, it takes clever and dedicated people to create a mess this big.

A result of negative feedback

Each of these examples is a terrific case study of chaos theory at work. In chaos theory, a small action/change in a complex/dynamic system can have enormously disproportionate impact in the future. The classic example is posited by Lorenzo in his 1972 paper, Predictability: Does the Flap of a Butterfly’s Wings in Brazil set off a Tornado in Texas? What is most important to remember here is that chaos theory is very sensitive to initial conditions, and unpredictable beyond very short periods of time. For those making economic policy this requires a constant vigilance for the undesirable unintended consequences of policy changes – clearly the butterfly did not intend the tornado.

It is to the quest of finding Lorenzo’s butterfly that I dedicate this series of articles.

Considerations of Complexity and Chaos

Complexity is a relatively new area of study, in which the nice equations that we learned in economics and physics are tested against the vagaries of reality. From a practical perspective, it is, at its core a study of the realistic implications of physical and social entropy that we see all around us. To a large degree, complexity theory borrows heavily from the study of biological systems, and applies those lessons to areas as diverse as meteorology to economics. All complex systems share four fundamental characteristics:

1) Autonomous Agents All of the independent actors in any complex system are autonomous agents which produce results in the system. These agents may be storms in a weather system, or stock and bond traders in financial markets. Diversity is a key factor in Autonomous agents – the less diversity, the less complexity and potential variation in outcomes.

2) Connected All Agents in a complex system must be connected – directly or indirectly. Typical examples might include connections via energy sources or communication patterns.

3) Interdependence All Agents in a complex system influence each other through one or more series of connections, and are therefore interdependent, although autonomous.

4) Adaptation Any complex system adapts to external influences in unpredictable ways, and complex social systems are capable of and depend upon learning.

Complex systems are normally open systems like weather, which exist in a thermodynamic gradient and function to dissipate energy in a fundamentally unstable system – a persistent disequilibrium.

Such complex systems frequently produce negative or positive feedback loops, in which actions in the systems in turn impact the system itself – producing more of the original activity. A good example is the self-feeding nature of a hurricane, which continues to grow by deriving energy from heated water, which increases the size and force of the storm, which in turn adds more energy and leads to further growth.

A common positive feedback loop in finance is the positive effect that ample mortgage finance has on real estate prices, feeding more transactions at ever higher values. Such a system is said to be in a persistent disequilibrium until the availability of mortgage financing is curtailed.

Chaotic systems: 1) Are sensitive to initial conditions, 2) Are topologically mixing, and 3) Have dense periodic orbits. Of these three, point one is the object of interest for any amateur historian/scientist – can you figure out where and when the butterfly flapped its wings?

Not too surprisingly, the description of the inputs to complex systems depends – to a large degree – on the academic background and orientation of the party doing the explanation and evaluation. Physicists tend to describe complexity as requiring constant inputs of energy and developing closed feedback loops limiting the dissipation of energy. That might be a pretty good description of a super-charged storm system like a hurricane.

Economists talk of the primacy of information, learning and adaptation and the central role of competition in the adaptive process. In either case, while you are dealing with radically different systems and agents, the same four fundamental characteristics apply.

The following chart gives a pretty good idea of how different branches of study use complexity to explain the same thing – the driving force in each system.

Looking at the simple chart above, it highlights the complexity of a system involving humans; as we are uniquely driven by all of the above factors.

The Perfect Storm as a Metaphor for the Great Recession

Sebastian Junger did a great job touching the mystery and horror associated with the Great Halloween Storm of 1991 in his book, The Perfect Storm. What made the storm particularly noteworthy was its absolutely unique origin – the merger of 1) the remnants of a blown-out hurricane (Grace), 2) an extra-tropical low pressure system, and 3) a vigorous, early season cold front blowing out over the Gulf Stream – which was still unusually warm for relatively late in the season – around 80 degrees.

While the wind speed of the storm was only around 60-75 mph, it took a very unusual track – heading directly back toward shore, and producing some truly gigantic waves. The tides and waves produced some historic damage including the sinking of the Andrea Gail – which was the story line of both the book and movie.

The factors that make the Perfect Storm a good metaphor for the financial wreckage of the Great Recession are: 1) It was born of the merger of a number of small and seemingly normal phenomena into a super storm, 2) It incorporated a number of previously dissipated tempests and reinvigorated them with the infusion of new energy, 3) It brought together common factors – the Gulf Stream and Canadian air masses – in a unique and enormously powerful and destructive manner, and 4) The storm track was very unusual and dramatically amplified the damage from the storm. This sounds like a pretty reasonable group of factors to degrade complexity into destructive chaos.

The Distant Origins of the Sub-Prime Fiasco

Vast amounts have been written about the origins of the Great Recession. Most of it is correct, and all of it (as far as I can tell) is incomplete. The closest that I have found is the work of McLean & Nocera in their book, All the Devils are Here, which begins with the original securitization of mortgages in the early ‘80’s. They focused on the splendid trio of characters Lewis Ranieri of Solomon Brothers, David Maxwell of Fannie Mae, and Larry Fink of First Boston. Of the three, Ranieri was doubtlessly the most colorful – an up-the-hard-way kid from the streets of Brooklyn, who wanted to be an Italian chef, but was chased out of the kitchen by asthma, and into the mailroom at Salomon Brothers, from which he ultimately rose up to be Vice Chairman.

These three guys were simultaneously fierce competitors and iron-bound allies in negotiations and lobbying the Federal Government and Congress for legal and regulatory accommodation to create the securitized mortgage industry. They were tireless, driven and ultimately successful.

Lewis Ranieri – The father of Mortgage Securitization

McLean & Nocera begin their tale at the right point in time, and with the right characters, but fail to correctly identify the fundamental reason that securitization was perceived and sold to the American people and regulators as an absolute necessity. They correctly identify that the Baby Boomers were coming of age and needed mortgages, and the entire S&L industry which would normally provide them was in desperate straits – hemorrhaging cash and on the verge of mass extinction. The fundamental disequilibrium that caused this fiasco – they never addressed; and that is where all the fun was.

In the late 70’s and early 80’s, Paul Volker, dramatically increased interest rates, successfully reversing the pervasive inflation expectations born of the unilateral abrogation of Bretton Woods and resulting currency collapse under the Nixon Administration. There was at the time a little noted regulation – known as Regulation Q – which limited the amount that S&L’s could pay on deposits. The regulators in Washington refused to allow S&L’s to pay market rates, and deposits fled in droves, forcing the S&L’s into the capital markets for liquidity when they could, or to Government funding when they could not. This financing was at rates up to 18%, the vast majority of their assets paid interest at less than 6% – and they were bleeding cash –and lots of it. This was a system in massive disequilibrium caused solely by the Federal Government.

The S&L’s did what they could to try to attract deposits, including giving away appliances as “gifts” to depositors willing to accept below market interest rates. During this period most banks in the US came to resemble hardware/appliance stores – but with armed guards. It was all very strange, and could have been fixed with a little Reagan era deregulation – simply repeal Regulation Q. That, however, would have eliminated the need for mortgage securitization (and money market funds, also born of the same disequilibrium) – the fundamental underpinning that ultimately fed the sub-prime fiasco – and Wall Street profits for 20 years. The combined lobbying forces of Wall Street and the GSE’s (Fannie, Freddie and Ginnie) in Washington simply overwhelmed the local bankers from the S&L’s, the most successful system of home financing in history was tossed into the trash, and the mortgage backed securities industry was born. When historians undertake to total the costs of the bailout for the Great Recession, they must include the $300 billion that was spent to clean up the S&L mess in the late 80’s and early 90’s.

Motivations

Can you identify the motivations?

Among the Devils – Consider David X. Li

Cry, ‘Havoc!’ and let slip the dogs of war. (3.1.268)

William Shakespeare, Julius Caesar

Much has been written about David X. Li and his pesky little formula that nearly destroyed the world. Li left China in 1987 (a singularly inauspicious start date) to come to the West to study the ways of finance – and apparently he mastered the art of the fomenting uncontrolled market crashes. He spent several years after arriving in Canada studying business and then statistics, ultimately earning a PhD with a focus on actuarial issues. In 2000 he published the seemingly simple paper entitled, “On Default Correlation: A Copula Approach”, and the fuse was lit on the real estate bomb that exploded in full force in 2008. The formula that was the highlight of the paper, relied on an old actuarial principal of correlation – specifically developed around the predictive value of the demise of one marital spouse on the demise of the second. This coupling or copula was the fundamental concept that was extended to bundles of assets – mortgages, auto loans and the like – to the value of credit derivative swaps (CDS’s) used to insure against the failure of the assets in question, or similar securitized assets.

The Formula Credited with the Sub-Prime Crisis

A Mathematical Expression of a Positive Feedback Loop

The Harbinger of Financial Chaos

In Mr. Li’s defense, he did not initially actively promote his formula as a solution for the pricing of portfolios of sub-prime mortgages or other financial dross, but once it started he participated full on. The formula is a dramatic simplification, relying on a constant of correlation to describe the future movement of asset values and performance. Nothing in any complex system is ever correlated by a constant value. The very concept of a concept of a constant of correlation is an oxymoron in a complex system. I guess that for Mr. Li financial markets in junk securities would follow a smooth and even course to maturity – despite all of the evidence to the contrary. In any event, Wall Street bought in hook, line and sinker – and entered into the headlong rush to the apocalypse.

I have only hit the highlights of this story, and would recommend to the reader checking out Felix Salomon’s terrific article in Wired for a more thorough and entirely entertaining read on the subject,  http://www.wired.com/techbiz/it/magazine/17-03/wp_quant?currentPage=all .

 

4.5x Growth following a pesky little equation

A Bolt of Lightning into the Primordial Goo

My high school biology teacher described the origins of life as caused by a bolt of lightning into the primordial goo. I always loved the imagery, and the obvious link to Mary Shelley’s Frankenstein brought the fantastic to life. This was the same effect that David Li’s little equation had on the primordial goo waiting in the sea of mortgage finance. Securitization allowed the direct sale of risk and CDS’s allowed the insuring against them whether or not you even owned the underlying risk. Li’s equation allowed Wall Street to quantify the risk of a portfolio of assets without even knowing what was inside. Better still, the rating agencies bought into all of it, and were rating portfolios sight unseen. The wonder of it all.

This equation led directly to the muscle-bound thugs running around poor communities selling mortgages the same way that they used to run numbers. Like the Canadian cold front teaming up with defunct Hurricane Grace and the energy in the Gulf Stream in the Perfect Storm, David Li’s equation hit the primordial goo of cheap money, dozy regulators, off-exchange CDS’s, compromised rating agencies and securitization machines craving product. In both cases, the positive feedback loop was spectacular, and the results disastrous.

Time for a Regulatory Re-think

Alan Greenspan used to say that he could not recognize a bubble until it popped. While I find this to be nonsensical, I’ll humor the position by suggesting that in each of the articles in this series I have clearly identified that there has been disproportionate growth – or shrinkage – in a major class of financial instruments presaging every financial catastrophe that I’ve examined. In each case there has been some change in the environment which created a fundamentally unstable system – and led directly to either a positive or negative feedback loop. These aren’t hard to identify, even with the use of retrospective data as favored by regulators.

From a practical perspective, the purpose of financial regulation is always two-fold; 1) Isolate the transaction into a singular event equally understood by both parties, and 2) Create the greatest level of information parity between the parties. The purpose of the derivative markets is to confound the first, and gaining an information edge is the second oldest profession. The pace of change, asset concentration and venue selection opportunities make old static regulatory regimes and strategies almost worthless.

Positive and negative feedback loops are more common in finance today than ever before, but they can be identified simply by looking at differential rates of growth of asset classes in the economy. In short, if it is busted – fix it.

 

Can you hear the butterfly wings flapping yet?

 

Reaping the Whirlwind

 

Breadloaf Mt and Mt. Wilson – An early spring hike

Prouty Logo
Breadloaf Mountain 3,835 ft. & Mt. Wilson 3,745

 

15 Miles, April 1, 2012

 

The Prouty Mountaineering Program

(the first Prouty Challenge Event benefitting Dartmouth-Hitchcock Norris Cotton Cancer Center)

 

Wes Chapman

 Breadloaf Mt. Vermont – In the VT Presidential Range

 

Breadloaf Mountain and Mt. Wilson – Spring in Vermont

 

Breadloaf and Wilson are two of the 100 highest mountains in New England, and therefore ended up in the crosshairs of my pals Gary and Jill Rogers, numbers 90 and 91 on their list; additionally offering a great training opportunity for their trip to ski the Haute Route in Switzerland and France next week. With us was Seamus, a buddy from Dartmouth and also a participant in the prospective European Adventure. This was my second trip up these Hills, and offered a chance to get some hiking preparation for my trips up Mt. Hood (11,249 ft. and the high point of Oregon) and Mt. Driskell (535 ft, and the high point of Louisiana) next month.

 

Breadloaf and Wilson are part of the Vermont Presidential Range, which celebrate the eclectic mix of Presidents Wilson, Grant and Roosevelt. At the base of Breadloaf is the Middlebury College Breadloaf Campus, dedicated to summer training programs for writers, with a number of very specialized degrees and relationships with four other similar campuses. This is Robert Frost country, to which he escaped after fleeing Dartmouth without graduating. While the hiking is pretty mundane, the setting for a summer writers campus is terrific, and the architecture iconic.

 Buildings on the Breadloaf Campus

 

Given the early spring, the snow had been gone for weeks, but Forrest Service Road 59 was closed about 2.5 miles from the trailhead, requiring a long walk just to get started. We headed up the Skyline Pond Trail 2.5 miles to the Long Trail, which runs along the ridge, leading north to both Breadloaf and Wilson. We hit snow and ice around 3,200 feet, and some fresh snow and a meaningful snowpack (2-5 feet) at 3,500 feet.

Gary & Jill demonstrating the self-cleaning properties of Micro-Spikes

 

Seamus prepares for the Ascent

 

Vermont – A Unique place – Geologically and Otherwise

 

Vermont is the eastern continental margin of the American tectonic plate, which collided with the European plate about 500 million years ago, closing up the proto-Atlantic Ocean and creating what was probably the highest mountain range ever seen on the planet. New England, East of Vermont, is very different rock – principally igneous in origin, much harder and generally giving rise to much poorer soils. The rock in Vermont grades from very highly metamorphic in the East, to fairly un-metamorphosed limestone in the West. The Western edge of the State has a fairly major rift style fault system associated with the Adirondack uplift immediately to the West. In short, Vermont is a an incredibly complex mix of faulted and metamorphosed rock, which has eroded into a series of small, tightly spaced hills and mountains; bounded on the east and west by major fault systems which create fairly significant water boundaries with its neighbors.

 

The Appalachians & Vermont – borne of a continental collision

 

This geology, combined with 500 million years of erosion, produced the complex geography of Vermont today, with all of the resultant limitations of travel – particularly east-west. The mountains and hills of Vermont today are the remnant roots of 30,000+ foot mountains created by the European/American continental collision, and the Connecticut River is a modern-day metaphor for the proto-Atlantic that closed up along the fault system which underlies the River.

 

Like Rhode Island, Vermont has served as a bit of a haven for asylum seekers and counter-culturists since its settlement, offering a convenient place for escape since the influx of Tories in the American Revolution. The difficulties of transportation, combined with the relatively rich soil made it feasible develop isolated, self-sustaining agricultural communities, and fostered a cultural environment amicable to the development of rural culturally affiliated communities like Breadloaf.

 

Vermont is eponymously called the Green Mountain State, not because the mountains are actually any greener than their counterparts in Maine (the Blue Mountains) and New Hampshire (the White Mountains), but because the geology has produced much shorter vistas than in those other states. Because the vistas are short, the atmosphere absorbs very little of the spectrum of light – producing mountains that appear green – the actual color of the vegetation. In New Hampshire, the mountains are much taller, frequently snow-covered and are visible from the ocean – hence the White Mountains. In Maine, the mountains are eroded granite plugs, quite a distance from each other. Because of the relatively greater distance, the mountains are normally seen with much longer vistas, and all but the blue light is absorbed – resulting in the Blue Mountains (the same phenomena producing the blue sky).

 

Fresh snow on the Long Trail between Breadloaf and Wilson

Icicles on the evergreens above 3,600 feet

 

The night before had produced a little fresh snow, which picked up in the afternoon, but on balance the snow was frozen firm and really fast. We had lunch on the top of Wilson, and headed back to check out Skyline Lodge and Skylight Pond before heading down.

 

Bell icicles

The Author checking out the accommodations at Skyline Lodge

Skylight Pond – home of the world’s largest beaver lodge

 

This was a fast hike, just under 6 hours for 15 miles. Somehow it was a long day – but left me hungry to do some more. Mt. Hood, here we come!

Adios from Wilson & Breadloaf