The Goddard spent the fall and winter of 2021-2022 in New Mexico and then Arizona, and in the spring we headed back north to visit Colorado for a while. Spring is a great time to watch birds: they’re very active as they gather material for nests and later find food for their fledglings. Leaves on trees also begin to emerge as the weather warms up, which I was to discover makes photographing birds much more difficult than in the fall and winter.
Here are some birds we saw doing their spring thing in Arizona, New Mexico, and Colorado.
Our campground in Holbrook was next to a residential area, which doesn’t happen very often because usually campgrounds are on the outskirts of towns. It gave us a chance to walk by houses and see birds perched in the trees.
Grants, New Mexico
Albuquerque, New Mexico
Our next stop on our return north was Albuquerque, which Nancy and I really enjoy visiting. There’s a lot to see and do there, and plenty of great Mexican restaurants and grocery stores to enjoy.
Las Vegas, New Mexico
In mid-April we made our way to Las Vegas, which we had also stayed at the previous fall. It was incredibly windy during our stay there in the spring (and the area would be subjected to several wildfires shortly after we left), so we didn’t venture out much. I did take a few photos at the campground, though.
Lathrop State Park, near Walsenburg, Colorado
We returned to Colorado around the end of April, choosing to camp once again at one of our favorite state parks. Located west of Walsenburg in the southern part of the state, Lathrop State Park has two large lakes, good hiking trails, and incredible views of the Spanish Peaks and Blanca Peak, each of which still had snow. The park attracts an enormous number of permanent and migratory birds each year.
By the time we left Lathrop State Park on April 24, I’d seen 51 different species of birds in three different states in 2022. It had become obvious that being around water, whether it’s a river or a lake, greatly increases both the chance of seeing birds and the opportunity to see different species of birds. That would become even more clear at the next Colorado state park at which we’d camp.
We made our first visit to Petrified Forest National Park on March 25, 2022, restricting our time to only the northern, smaller section of the park. That part doesn’t have much in the way of petrified wood, but it has plenty of awe-inspiring views. We returned the next day, with Gunther, to experience the southern side, and we did see some fossilized wood. And how!
Petrified Forest National Park, which measures about 350 square miles, receives about 600,000 visitors per year. That number, while impressive, makes it just the third-most-visited national park in Arizona, following Saguaro National Park in Tucson (1 million visitors per year; Nancy and I were two of those people a couple of weeks earlier) and the most-visited park in all the land, Grand Canyon National Park (4.5 million). Incidentally, Rocky Mountain National Park in north-central Colorado is just behind Grand Canyon, at 4.4 million visitors per year. If you’ve been to Rocky Mountain National Park in the last 20 years and felt a bit cramped, it’s probably due to 4.4 million other people visiting a park measuring 415 square miles.
But we’re here to talk about rocks. A piece of petrified wood isn’t really wood any longer: it no longer contains any organic material and it is most definitely a rock. The process of petrification takes several important factors, including a tree, water, sediment, and time. Lots and lots of time.
Let’s start at the beginning. The scientists believe that the trees in Petrified Forest National Park were alive between 210 and 227 million years ago. At that time, the Late Triassic Period, the current area of the park was just north of the equator – in fact, it was close to where Costa Rica is today. The land was much different then: covered with forests of immense trees as well as large rivers and other wetlands. Huge amphibians and early dinosaurs roamed the forests and dwelled in the rivers. (Although there were many dinosaur species in the ensuing years, famous dinosaurs such as Tyrannosaurus rex and Triceratops wouldn’t appear until the Late Cretaceous Period, almost 160 million years later.)
Many of these coniferous trees (there are nine species identified in the park; all are now extinct) grew to be enormous: some may have grown to 200 feet in height. When the trees died they lost their branches and bark, then eventually toppled over after being undercut by a river. If the tree fell into the river, it may have eventually been covered in sediment being carried by the waterway. This relatively rapid burial is critical to later petrification: the water sealed the dead tree away from both oxygen and bacteria, which helped prevent decay. That delay gave time for silicic acid in the rivers to percolate throughout the tree. This process chemically altered the wood into a mineral called opal that still retained the tree’s fine features, like the grain of the wood, or indications of where branches once sprouted from the trunk.
Converting the wood into opal took only a few thousand years. Further layers of sedimentation over millions upon millions of years would cover the logs with tons upon tons of soil and rock. This process recrystallized the logs, converting the opal into quartz and a few other minerals. Over many other ensuing millions of years, erosion and geologic upheaval brought the logs back to the surface of the earth to once again see the light of day – this time as petrified wood.
Now that you know the factors involved in creating petrified wood, can you name the states in our country that contain it? The answer is below – keep on scrollin’!
The visitor center at the southern end of the park, which is part of the original monument created in 1906 (it was made a national park in 1962), contains some interesting fossils of both trees and animals. The fossilized remains of many amphibians and some dinosaurs dating to the time that the trees were alive have been discovered in the park (and the process for creating animal fossils is much the same as that used to create petrified wood). The museum also exhibits some handwritten letters: apparently, some visitors over the years were unable to withstand the temptation (and federal law) to leave the petrified wood where it lay within the park. Upon their return home with a fossilized wood souvenir, some of them inexplicably fell into bad fortune, such as personal or business relationship issues, and returned the rocks via mail, with an apologetic letter, to the national park.
After going to the visitor center and museum, and walking the Giant Logs Trail behind the building, we decided to go on a longer walk to see some more rocks. The Long Logs Trail, located a short distance from the visitor center, is so named because some of the petrified wood is more than 180 feet in length.
About the states that contain petrified wood: were you able to name them? If you named all 50, you’re correct. Although each U.S. state contain some amount of petrified wood, northern Arizona is able to display one of the largest concentrations in the nation because of the geologic upheaval processes that brought the logs to the surface of the earth.
Progressing east and west, Interstate 40 divides Petrified Forest National Park into northern and southern sections. The interstate generally follows the path of historic U.S. Route 66, which connected the midwestern United States to the country’s west coast in the first half of the 20th century. Although Route 66 stretched more than 2,200 miles from Chicago to Los Angeles, Petrified Forest is the only national park with former segments of the historic highway within its boundaries. The area south of the interstate, much larger in size than the northern part, contains most of the petrified wood specimens in the park. The northern area, however, boasts incredible roadside vistas of the Painted Desert and a sizable national wilderness area. Nancy and I visited the northern part of the park in late March. Gunther stayed with Rusty in the Goddard, but Nancy and I would enjoy the dog’s company when we returned to the park the following day.
We briefly stopped in at the northern visitor center, which was undergoing significant renovation at the time, then proceeded to drive along a route that included a number of overlooks of Petrified Forest National Park.
I decided to use my 14mm wide-angle lens for taking pictures the day we visited the Painted Desert. I got it a couple of years ago to primarily take pictures of the night sky but thought its properties would help capture the feeling of the vast open landscapes of Petrified Forest National Park. There is a disadvantage to using this lens, though: it’s not automatic, so the aperture, ISO, and other settings all must be set manually. I’m no good at any of that. Many of the photos I took were over- or under-exposed, and I had to make manual adjustments using a couple of pieces of photo editing software.
Petrified Forest National Park contains only a small part of the Painted Desert, which stretches across almost 8,000 square miles of northeastern Arizona. The colorful rocks, primarily mudstone and sandstone, of this region are called the Chinle Formation. Deposited from 227 to 205 million years ago during the Late Triassic Period while most of the land area on Earth was on the single supercontinent Pangaea, the rocks have been buried, lifted, and eroded during Pangaea’s breakup and shift into today’s major continents.
During the Late Triassic Period, the land comprising Arizona’s Petrified Forest National Park was located just north of the equator and supported a much different environment (different enough, for example, to support a forest of 180-foot-tall trees that would later become petrified). As Pangaea divided, the land mass migrated north and the land itself underwent massive changes.
The Chinle Formation is itself divided into five members: Mesa Redondo, Blue Mesa, Sonsela, Petrified Forest, and Owl Rock. Each member represents a transition of the land from wet to dry environments over millions of years: the Mesa Redondo, the oldest layer and therefore the one underlying the rest of the formation, consists of red sandstone originally laid down 226 million years ago, and the youngest, Owl Rock, includes pink and orange mudstone at the top of the formation that was deposited 207 million years ago.
Older rock formations in the Painted Desert are at the bottom of the geologic column, and the layers of rock grow younger in age as the elevation increases. The colors of these rocks come from the iron they contain. Drier climates allow the minerals to become exposed to oxygen, causing the iron to rust and develop distinctive red, brown, and orange colors. When the climate is wet, moisture essentially covers the sediments and prevents their oxidation. Those layers are colored blue, gray, and purple.
Nancy and I took a short hike along the rim of the basin, and one of the highlights of that walk was a stop at the Painted Desert Inn, which was originally built as a respite for travelers on Route 66. The highway passed just a short distance south of the building, and a spur road brought visitors to the inn for refreshments.
The interior of the Painted Desert Inn now serves as a visitor center for the Painted Desert as well as a museum with artifacts from the inn’s heyday. It’s all very impressive and you’re going to have to take my word on that because none of the pictures I took inside turned out.
Despite my photographic foibles, we really enjoyed this first visit to Petrified Forest National Park. I grew up on the eastern plains of Colorado, and I know long, uninterrupted distances. They are nothing compared to what can be seen in northeastern Arizona.
We’d see more of the park, and a little bit of actual fossilized wood, the next day. (Actually, we’d see a lot of fossilized wood. So. Much. Fossilized. Wood.)
Holbrook, Arizona, located in the northeastern corner of the state, is the seat of Navajo County, which was split off from neighboring Apache County in 1895. Both counties are still huge: Navajo measures 9,960 square miles, and Apache still has more than 11,000 square miles even after the division. Navajo County is bigger than the state of Vermont and just slightly smaller than Massachusetts. (For reference, my home county in eastern Colorado, Kit Carson, is considered very large at 2,162 square miles; in fact, Navajo County is about a tenth the size of the entire state of Colorado.)
Nearly two-thirds of Navajo County is designated Native American reservation land, including parts of the Hopi Indian reservation, the Navajo Nation, and Fort Apache Indian Reservation.
We camped in Holbrook for a week because of the town’s close proximity to Petrified Forest National Park – the park is only 25 miles northeast of the city – but we found plenty to like about the town itself.
The Navajo County Courthouse, completed nearly 125 years ago, is now home to the Navajo County Historical Society’s museum. Built in 1898 at a cost of $15,000, including a $3,000 jail, the courthouse was in use until 1976 when the Navajo County Correctional Complex was constructed on the south side of Holbrook.
The museum was open on a Sunday afternoon in March after the Goddard’s arrival in Holbrook, so we were able to spend a few pleasant hours touring the exhibits.
The first exhibit in the museum is the county jail, which is to the right after one enters the courthouse. The jail was built in Kansas City, Missouri, by the Pauly Jail Company, which began operations in 1856 and is still in business today – be sure to consider it for any incarceration needs you may have. The jail was then shipped by rail to Holbrook and placed in the still-under-construction courthouse.
Firmly deciding to continue living our lives on the straight and narrow path, Nancy and I proceeded to other parts of the museum. Volunteers for the Navajo County Historical Society spend more than 2,000 hours each year curating and conserving artifacts from Holbrook’s past. The items represent the lives of Native Americans, Euro-American settlers, ranchers and cowboys, bankers, homemakers, railroad employees, teachers, merchants, and travelers through the area over the past centuries. Like many community historical museums we’ve visited, the exhibits in the building show a tremendous range of cultural, social, and economic pursuits. I wish other museums, however, were as well curated as Holbrook’s: the society has really done a fine job of keeping the exhibits relevant and reasonably sized.
The Mother Road
Holbrook makes much of its location on the former Route 66, one of the original highways of the U.S. Highway System. Established in 1926, Route 66 connected Chicago, Illinois, with Santa Monica, California, and passed through the states of Missouri, Kansas, Oklahoma, Texas, New Mexico, and Arizona in its 2,448 miles.
Route 66 was an extraordinarily important highway in the first half of the 20th century, serving as the primary means by which Americans migrated to the West – especially during the Great Depression (John Steinbeck’s novel “Grapes of Wrath” alludes heavily to the highway). The route proved to be an essential economic driver for dozens of cities and towns along the way, as businesses provided food, fuel, shelter, and services to those who traveled the highway. Route 66 was officially removed from the U.S. Highway System in 1985, having been mostly replaced by a variety of segments of the U.S. Interstate Highway System.
The Hashknife Outfit
In addition to the town’s Route 66 connection, the Holbrook museum also features extensive exhibits on the Aztec Land & Cattle Company. The company was founded in Boston, Massachusetts, in 1884 to take advantage of significant drops in cattle prices in Texas. Many large ranches in that state had continued to add to their herds, intending to reap profits when the beef markets improved. However, lingering drought caused prices to drop even further.
Aztec bought the Continental Cattle Company and its Hashknife brand (so called because the cattle brand resembled a bladed kitchen utensil), then shipped a total of 60,000 cattle and 2,200 horses from Texas to northeastern Arizona. The cattle were grazed on land purchased for 50 cents an acre from the Atlantic & Pacific Railroad. The grazing lands stretched about 300 miles from just south of Flagstaff to the New Mexico border (Arizona and New Mexico were both U.S. territories until 1912). With the ranch headquarters in Holbrook, the company’s employee base was a significant economic force for the town. However, Holbrook’s population of 300 residents found that not all of the Hashknife Outfit’s cowboys were of the law-abiding type. Cases of armed robbery and cattle rustling escalated, and there were 26 shooting deaths in 1886 (again, in a town of 300 people).
As was typical in the days of the Old West, range wars involving different ranches and their possessions were common. Many of the cowboys involved, either current or former Aztec employees, were incarcerated or outright killed.
The original end of Aztec as a beef-raising company came in 1902, with a drought, flooding, and overgrazing that destroyed the land on which the cattle were grazed. Aztec sold off its land and its remaining cattle, and the Hashknife brand was sold to a family in Flagstaff (and Aztec continues today as the third-largest private landowner in Arizona).
However, many of the cowboys of the Hashknife Outfit would go on to become respectable citizens of Holbrook and the surrounding area as independent ranchers, law enforcement officers, businessmen, and community leaders.
Although it was definitely the largest, the Aztec Cattle & Land Company wasn’t the only cattle concern around Holbrook and the museum has many artifacts about the ranching way of life.
Charles Goodnight, a Texas rancher and cattle trail developer, is credited with introducing the chuckwagon, a mobile kitchen used to keep cowboys’ bellies full, in 1866. Goodnight’s model was a modified wagon from the U.S. Civil War, to which he added a box with drawers and shelves for food and supply storage. Goodnight’s cattle drives took cattle from Texas to New Mexico on the Goodnight-Loving Trail (which also followed part of the Butterfield Overland Mail route). He’d later go on to drive cattle from New Mexico up into Colorado and Wyoming. Cooks for the cattle drives would also serve as barbers, dentists, and bankers for the outfits, and were so important that they were usually second in command to the trailbosses.
Back to the Triassic
One of the things I really appreciate about community historical museums is the breadth of items they display. The artifacts can range in dates from the times of ancient Native American cultures up to the Great Depression of the 1930s and even more recent. As I wrote, the Navajo County Historical Society has excelled at displaying just a few items from each era in order to abstain from overwhelming visitors. Let’s go back even further in time for a moment:
We enjoyed a one-week stay in Camp Verde, Arizona, in mid-March of 2022, which allowed easy access to two National Park Service (NPS) sites. The first was Montezuma Castle National Monument, a cliff dwelling on which construction began a thousand years ago and which we visited on a couple of consecutive weekday late afternoons. The second was Tuzigoot National Monument, another ancient Native American dwelling site located about 20 miles northwest of Camp Verde. Tuzigoot was declared a national monument on July 25, 1939. Nancy and I visited the monument on a pleasant but overcast Saturday in mid-March.
Like the nearby Montezuma Castle, the Sinagua Native Americans began construction on Tuzigoot pueblo about a thousand years ago. Also like Montezuma Castle, Tuzigoot is misnamed: it’s a corruption of the Tonto Apache phrase “Tú Digiz,” which means “crooked water” and refers to a bend in the nearby Verde River. The pueblo, located on a hilltop with 360-degree views for miles around the area, featured 110 rooms.
The proximity to Montezuma Castle, and to other pueblo communities like those in New Mexico’s Aztec Ruins National Monument and Bandelier National Monument, as well as Colorado’s Mesa Verde National Park, points to the fact that the residents traveled frequently between the dwellings and traded ideas and goods with each other. Again, much like the other pueblos in the area, the dwellings were abandoned beginning in the 1300s most likely due to a variety of reasons (depletion of natural resources, climate change, possible threats from other native cultures) rather than just one. Also, the Hopi, who count themselves among the Sinagua culture’s descendants, believe their forebears were naturally nomadic and didn’t like to stay in one place for too long.
The Tuzigoot National Monument experience begins with the site’s visitor center, which is itself a historic structure (although not as historic as the pueblo, since the visitor center dates only to 1936). The visitor center was built as a museum by local Clarkdale residents, who also helped professional archeologists with the initial excavation of the Tuzigoot pueblo. The center contains actual artifacts – not reproductions – that were found during the site’s excavation in the 1930s.
The visitor center is on the National Register of Historic Places and has a collection of 3,158 objects, not all of which are on display. The collection includes ollas (large pottery pieces serving as bowls or baskets), woven baskets, projectile points, and jewelry.
The Tuzigoot site was first described by Anglo-Americans in the 1850s but wasn’t professionally excavated for nearly a century after that. Following the departure of the Sinagua, centuries of neglect, along with countless rain- and snowstorms, freezing temperatures, and the desert heat, left the pueblo in severe disrepair. The site was first excavated in the early 1930s and Portland cement was used to stabilize the rocks. Unfortunately, that material can, over time, damage the original rocks used in the buildings. In the late 1990s, researchers began to replace the Portland cement with mortar that is a better match with the bonding materials that were used a thousand years ago during initial construction.
The 190-mile-long Verde River, which flows to the north and east of the Tuzigoot pueblo, drains an area of almost 6,200 square miles. The Verde flows just a few feet from where our campsite was in Camp Verde, which derives its name from the river. It eventually empties into the Salt River east of Phoenix, which in turn flows into the Gila River west of the city. A nice trail leads north from the Tuzigoot visitor center to a natural area called Tavasci Marsh (named after the family that once owned a dairy there). About 10,000 years ago the marsh was part of the river but it has since been separated through erosion and other geological forces to become a separate, but connected, wetland. There were, hundreds of years ago, many marshes in the Verde Valley. They’ve since been drained for human development and pasturelands, and today marshes are very rare in Arizona. The trail is a half-mile walk to an observation deck that overlooks the marsh, and there are more opportunities for birdwatching and plant appreciation.
Tuzigoot National Monument is a fine example of the diversity of ancient Native American pueblos. As conserved by the National Park Service, the monument is a great opportunity to not only learn about its former residents, but to also see some great natural attractions.
Having nothing at all to do with Montezuma, the early 16th-century emperor of the Aztecs (known now as Moctezuma II), nor a castle in any sense of the word, Montezuma Castle National Monument is still a very rewarding site to visit.
Because access to enter the actual structures is limited to those who really need to go in them, the park also focuses a lot on native species of flora found in the region and provides a lot of interpretive signage next to examples of plants to explain how the plants were used by the occupants of the dwellings. As an (extremely) amateur botanist, this was fine by me.
We were able to make a couple of late weekday visits to fully explore this monument, which is located just a few miles north of our campground in Camp Verde, Arizona. It was also the first opportunity for Gunther to earn a B.A.R.K. Ranger certification (more on that later).
The structures in the monument were built by the Sinagua, Native Americans who migrated to this area about 1,400 years ago and began building the cliff dwellings about a thousand years ago – hundreds of years before Moctezuma II was born. The current name of the monument, Montezuma Castle, comes from European Americans who in the mid-1800s were extremely interested in the Aztec, Mayan, and Incan cultures of present-day Central America and wanted to bestow exotic names on nearly everything they found.
The cliff dwellings are built in Verde Formation limestone, a relatively soft sedimentary rock. Over millions of years, the erosional forces of water and wind have had their way with the limestone to carve many holes into the rock. The erosional holes that are enlarged by humans into structures are called cavates by archeologists. At Montezuma Castle, most cavates extend about 10 feet into the cliff. By closing up naturally open spaces, and building exterior and interior walls with masonry, the Sinagua were able to construct secure housing for their culture.
The Sinagua built and occupied the dwellings between the years 1100 and 1425, leaving the residences about 70 years before Columbus set sail. Montezuma Castle was at the crossroads of a Native American trading network that stretched from the coast of present-day California to eastern New Mexico, and from Utah into Mexico. That central location provided the Sinagua with many resources that weren’t available in the Verde Valley:
Obsidian, used for projectile points, came from the San Francisco Mountains north of the castle
Wild game and plants were taken from the Mogollon Rim, located east of the structure
Strong trading relationships with the Hohokam culture, in present-day southern Arizona, provided much more than was available in the Verde Valley
Contrary, perhaps, to popular opinion, because of that trading network the Sinagua had an awareness of their world that stretched for thousands of square miles.
Where the Sinagua went, and why, after about the year 1425 is still up for debate, but most researchers believe the exodus was due to at least one of three factors: drought, depletion of food resources, and threats from newly arrived cultures.
The Hopi culture, which may be descended partially from the Sinagua, believe this structure wasn’t meant to be the final home of their ancestors. When a culture stays too long in one place, the Hopi believe, environmental disasters and societal collapses remind them of their migratory nature – and they move on. The Zuni and other Puebloan groups are also said to be descended from the Sinagua.
Between 1991 and 1994, an inventory of the plants and animals at this national monument was taken by a team of researchers from Northern Arizona University and the United States Geological Survey. That research resulted in the cataloging of 784 species of plants and animals in this 859-acre (less than 1.5 square miles) site; only 11 percent were non-native species.
Looters of the 19th century took many of the contents of the structures, and today the ruins are open only to scientists for research, inspection, and maintenance. This is in contrast to Gila Cliff Dwellings National Monument in southwestern New Mexico, in which visitors are allowed to enter the structures. Part of that policy us is perhaps due to proximity. Gila Cliff Dwellings National Monument is one of those places you have to want to get to, since it’s nearly a two-hour drive from the closest large city; Montezuma Castle is just a couple of miles off Interstate 17 in central Arizona. About 350,000 people visit Montezuma Castle each year; Gila Cliff Dwellings gets about 42,000 visitors annually.
Montezuma Castle National Monument was established by the administration of U.S. President Theodore Roosevelt. During his administration (1901-1909), five national parks, 18 national monuments, 150 national forests, and 51 bird sanctuaries. In all, Roosevelt authorized a total of 230 million acres (almost 360,000 square miles) for the enjoyment of future generations like ours.
We didn’t see much in the way of wildlife while at the monument (Nancy and I were both surprised at the number of late-day visitors each day, but that was probably due to the monument’s easy access from the Interstate); however the habitat’s diversity (holes in cliffs to dry meadows to riparian areas) supports all kinds of bats, foxes, mice, owls, songbirds, snakes, lizards, and turtles.
Being open only to researchers is also due to the fact that ladders must be used to access the cliffside ruins: the buildings were definitely at least partially planned with defense in mind. Additionally most of the cliff faces south, which allows the dwellings to be warm in the winters and cool in the summers. The elevated location also protects the dwellings from occasional flooding of Beaver Creek, which flows beneath the cliffs.
The National Park Service has a pretty nifty program in which dogs can earn their B.A.R.K. Ranger certification in certain parks and monuments. Gunther knows, and you should too, that B.A.R.K. Rangers:
Bag your poop. Always have your humans bag and dispose of your waste properly.
Always wear a leash. When in the park, always wear a leash (6 feet or less) and don’t let your humans leave you unattended.
Respect wildlife. Don’t harass or harm wildlife by making noise or chasing them.
Know where you can go. B.A.R.K. rangers are permitted in parking lots, campgrounds, picnic areas, roads, and designated trails.
The B.A.R.K. Ranger program is really clever: it keeps dogs out of hot vehicles while their owners visit national parks and monuments, while encouraging those owners to be responsible for their pet. Since that great day at Montezuma Castle, Gunther has also earned B.A.R.K. Ranger certification at Petrified Forest National Park, also in Arizona, and Pecos National Historical Park in New Mexico. Look for future blog postings about those visits and more, and look for Gunther on the trails!
We’ve found that many museums and other attractions in the southwest allow visitors to bring their dogs along. That policy is probably, at least in part, so that people don’t leave their dogs in their cars. For whatever reason it is, we’re good with it.
Gunther was able to join us on the second of our two visits to the Pima Air & Space Museum in Tucson. The exhibits that we saw on March 6 were all outside. It was a lovely day and there happened to be an airshow training program taking place at a nearby airfield, so we saw plenty of planes on the ground and in the air. As I wrote in the posting about our first day’s visit, there are hundreds of airplanes on the grounds of the museum, and taking them all in, even with a two-day pass, is a lot to handle.
There are about 400 aircraft at the Pima Air & Space Museum, inside hangers and outside on the ground, and each of them has an interesting story to tell. I wanted to limit the number of photos in this posting to 10 or 12, but couldn’t decide what to exclude. I didn’t include photos of the EWACs (early warning and control) airplanes like the Grumman E-1 Tracer that flew over Europe during the Cold War, or the bombers like the couple of Boeing B-52 Stratofortresses on display. Even with the two-day pass, we could have spent a lot more time looking at these airplanes and learning about their place in history.
Nancy and I decided to pay a visit to the Tucson Botanical Gardens on a quiet Saturday morning in early March. The garden grounds are located in the northwest corner of the city, in a pleasant area of residential neighborhoods and small businesses. The gardens are at an expansive former family home, which adds a decided sense of intimacy to the experience of visiting.
We spent most of the morning wandering around the Cactus & Succulents Garden, which afforded us an opportunity to see some really interesting cacti and some birds as well.
The Cactus & Succulents Garden features plants from around the world that also perform well in the southern Arizona environment. The plants have been divided into four major areas representing the:
Sonoran Desert of North America
Chihuahuan Desert of North America
Desert regions of South America
Desert regions of Africa
Mexico has between 750 and 800 different species of succulents. The United States has about 200 native species, and South America has about a thousand species.
We saw a number of birds at the Botanical Gardens, including five species I’d never seen before.
We were really happy to visit the Tucson Botanical Gardens. It’s always fun to visit a garden that, like Denver’s, is in a residential area, and there were several more habitats in the gardens that showed even more diversity in plants. Even in early March, there were plenty of blooming flowers to enjoy throughout the gardens.
Until 1947, the U.S. Air Force was a component of the U.S. Army (during World War II the branch was known as the United States Army Air Forces). In 1966, during a celebration of the anniversary of the establishment of the U.S. Air Force, military commanders in the Tucson area realized that many of the historic World War II- and 1950s-era aircraft stored on Davis-Monthan Air Force Base were being lost – as was much of U.S. military history. Airplane parts were being sent to smelters so their metal could be used in modern aircraft production. Base officials began to set aside examples of the aircraft along the base’s fenced perimeter so that the public could see them. Although the practice saved many aircraft from the smelter, this wasn’t an ideal solution. The Tucson Air Museum Foundation of Pima County was formed that year, and the foundation found a 320-acre site of BLM land just south of the Air Force base. The foundation’s first aircraft acquisition was a B-24 Liberator. Many years (and hanger constructions and aircraft acquisitions and hanger expansions) later, the Pima Air & Space Museum is the country’s largest non-government-funded aviation museum. The museum has more than 100 civilian, military, and experimental aircraft in its four indoor hangers (totaling a quarter-million square feet) alone, as well as many more parked on the grounds outside for a total of about 400 aircraft.
Recognizing that its collection is large and takes aircraft enthusiasts a lot of time to visit, the museum smartly offers a two-day pass that Nancy and I took advantage of. Because March 4 was pretty breezy, we opted to spend that day looking at the aircraft inside the hangers. I’ll share just a few of the ones that I enjoyed viewing, listed in order of their year of introduction.
Even if it represents a smaller percentage of its total collection, the aircraft inside the hangers of the Pima Air & Space Museum are truly impressive. They’re historic, they’re beautiful, and some of them are terrifyingly efficient at what they were designed to do. There were dozens of other aircraft that I didn’t include in this posting: a McDonnell FH-1 Phantom, a Grumman F-14 Tomcat, a Hawker Hurricane, a Grumman F-11 Tiger, a Fairchild-Republic A-10 Thunderbolt … the list of aircraft just under a roof at this museum is incredible. Seeing a Huey up-close again, as well as other aircraft that my dad has flown, was really rewarding. Here’s a fun fact: my birth in June 1969 was induced a few days early so Dad could see me before leaving for Vietnam. I was born in McPherson, Kansas, where my two great-uncles (the B-24 Liberator crewmen) were friends a quarter-century before I was born.
In another post, we’ll return to the Pima Air & Space Museum and take a look at the aircraft outside the hangers (some of which my dad has also flown).
In arid areas like southeastern Arizona, water is especially important. Not least of all is its ability to support wildlife, and a wide range of it. Lake Cochise, just east of the town of Willcox, is one of the biggest bodies of water in the region. Located in the Sulphur Springs Valley, an 80-mile-long region stretching from north of Willcox to the Arizona-Mexico border, the lake supports a number of different species of birds and other animals throughout the year. Nancy and Gunther and I visited Lake Cochise in mid-February.
The town of Willcox hosts an annual event each January, Wings Over Willcox, that attracts bird enthusiasts from around the world. In one year, attendees saw 146 different species of birds, ranging from great horned owls to chipping sparrows.
However, Lake Cochise is best known as a primary winter stop for migratory sandhill cranes. Many thousands of cranes spend the winter each year around the lake, with the highest populations present between the months of November and February. In 2008, the Arizona Game & Fish Department counted more than 36,000 sandhill cranes in the area – the highest number ever recorded.
Two groups of cranes spend the winter in the Sulphur Springs Valley: the Rocky Mountain and Mid-Continent populations. The Rocky Mountain group has about 20,000 birds and nests in Wyoming, Montana, Utah, and Alberta, Canada. This is the population that has a major migration stopover in Colorado’s San Luis Valley; the town of Monte Vista has its own crane festival each year to commemorate the event.
The Mid-Continent population of sandhill cranes has about half a million birds and nests in northern Canada and Siberia. This population has a major migration stopover in the Platte River Valley near Kearney, Nebraska. That town, too, has a festival each year – Nancy and I enjoyed a visit there some years ago where we were first introduced to sandhill cranes from an Audubon Society blind next to the river. We also saw and heard sandhill cranes during our stays last year in Albuquerque through Las Cruces, New Mexico.
We had a great time at Lake Cochise, and we encourage everyone to attend a sandhill crane festival if one’s about — the cranes are a lot of fun to watch, and there are always other species to enjoy if cranes aren’t your thing.