Showing posts with label sunset. Show all posts
Showing posts with label sunset. Show all posts

Saturday, April 18, 2026

Roswell: Highway 285 to Berrendo Road - The Land

 Roswell is situated in the northern region of the Chihuahuan desert. Roswell is on the Great Plains. Roswell is grasslands. Roswell isn't obviously karst but it's karst nevertheless  Roswell is flat but not perfectly so. Roswell is dry but Roswell is an oasis.


Roswell is at 33° 23' 39" N 104° 31' 22" W. Selma, Alabama, where I used to live is at coordinates  32° 24' 59", about one degree latitude difference. So why is the environment so different. Selma is forested..... Roswell is desert. We'll get to that later.

The city is at 3,615 feet altitude. People are surprised by that after seeing how flat it is around here 

The Pecos River flows 7 miles to the east of the city. The highlands that rise to Sierra Blanca begins about 40 miles to the west. The Rockies are about 70 miles to the west. In Denver, I had the requisite photo of the Rockies in my blogs. Here, it will be Sierra Blanco. 

The city has an area of 29.776 square miles (according to the United States Census Bureau). Chaves County, of which Roswell is the largest city, has 6,075 square miles. 

There are actually natural streams in Roswell. Some are dry now because the springs that fed them have been repurposed for industry and agriculture, but Spring River in South Roswell still flows (I think. I haven't made it that far yet.)


The land between Berrendo Road and Pine Lodge is primarily landscaped by Berrendo Creek and the Pecos River.



Pine Lodge from my house

It's flat around here. On my 1.7 mile walk into town, I get an elevation gain of 13 feet (according to measurements made by my AllTrails app.)

There is a blog discussing Berrendo Creek and I'll be posting a blog about Bitter Lakes Wildlife Refuge soon. That park is nestled beneath the Comanche Bluffs in the flood plains of the Pecos River  Berrendo Creek meets the Pecos River a little south of this section.

I say that the land is flat here but there is a little topography 


A draw on highway 285 North truck route north of my house.


Road cut on highway 285

The largest incline I'm aware of is the ravine that Berrendo Creek has cut through town, now dry, something between 20 and 30 feet deep.


Berrendo Creek 

Like the Denver area, the Chihuahuan desert was once an inland sea and many layers of sand, lime, and gypsum have been laid down to make up the rock under my feet. The ground outside looks like ceramic but is actually soft.


Desert soil

It is limestone, or at least dust blown in from limestone. That's evident when it's mixed with vinegar.



If you want to know if a substance contains a carbonate, just add acid. Vinegar is a weak acid but it will make calcite (calcium carbonate) fizz quite nicely, giving off carbon dioxide and leaving calcium acetate behind in solution. Dolomite (magnesium carbonate) may need a little warming to effervesce.

The main bedrocks in the area are limestone and shale but there have been a lot of diverse layers laid down over a long time. My primary source is the strategraphic column provided by the Rockd geology app. (Childs, O.E. (1985) Correlation of strategraphic units of North America, COSUNA.AAPG Bulletin 69:173-180).

The top layer is very recent Ogallala formation deposited by area streams. It's mostly sandstone and gravel. Beneath that is a later of volcanic material from 63 to 19 million years ago. We're just east of the Rio Grande Rift where North America tried to pull itself apart. There has been a lot of recent (geologically speaking) vulcanism in the area. That big mountain on the horizon, Sierra Blanca, is an extinct stratovolcano.

About a thousand meters down is the Grayberg and San Andreas formation limestones overlaid by about 300 meters of impermeable sandstone and shale. The limestone layer is interlaced with cracks that allow storage of a lot of groundwater. The shale cap keeps the water under pressure so that when it finds a channel to the surface it forms the many artesian springs in the area. It also feeds the Roswell water wells.

The Ogallala formation is also an aquifer but, here, it's recharge rate is slow and it can be emptied quickly. Most of Roswell's water comes from the deep aquifer. According to the city website, there are 20 deep wells that draw water up, chlorinates it, and distributes it out to the city. 

Roswell takes samples of treated wastewater daily, 60 samples a month, to test for bacterial contaminants and tests drinking water quarterly for chemical contaminants.

I bought a test kit (H2O OK Plus) to check our tap water. Most of the tests are on three test strips although the coliform test requires a tube of water plus reagent to sit a while.





The tests were easy and I was very happy with the results  



The water is hard but 247 parts per million is far below EPA requirements.

Hard water is water with high mineral content, usually calcium and magnesium carbonates. It happens when water is stored in a limestone or gypsum aquifer. Roswell's aquifer is mostly limestone but there is still plenty of gypsum and even some interesting evaporates.....minerals that form when landlocked lakes evaporate. They're touchy for mineral collectors because they tend to draw humidity out of the air and then dissolve in it.

Hard water might have some health benefits (except for kidney stones for people predisposed to it) but it can play havoc with pipes and laundry. Calcium carbonate tends to precipitate out in cakes. Also, the calcium ions will combine with the sodium stearate (soap) to firm an insoluble, slimy, scummy precipitate of calcium stearate. The best way to tell if the water from your tap is too hard is that you can't get soap to lather. We get scum but the soap will lather. And unlike some folks, I like the mouth feel of coffee creamer in hard water 

Roswell gets it's water from the deep aquifer but there are three major streams and a few intermittent tributaries that run through town. I explore Berrendo Creek in an earlier blog. Most of its length is usually dry but when it's wet, there's a flood.

I haven't seen the other two yet.....they are Spring River and Hondo Rio. All of these streams are tributaries of the Pacos River that flows 7 miles east of Main Street  I'll talk about the others when I get to explore them.



The Pacos River at Bitter Lakes 

Most of the natural water here is green. The green isn't pollution..... it's calcium. Here's another calcium loaded stream in Alabama 


Brushy Lake, Northwestern Alabama

The climate here is hot and dry with occasional cold (night and winter) and rare rain, which is sometimes devastatingly torrential.

My family moved down from Denver late in October of last year (2025). The days were warm and cool. It was a good time to move into the desert. The nights, as is normal year round, was cool. By December, the days were cooling down. The vegetation which plagued me on my trips to town for supplies was dying down to stubble. We had some cold days and one snow between January and March. I think it has rained three times since we moved, never hard. Wet ground evaporates quickly. The sunsets are always gorgeous given the capacity for the dry air to hold dust suspended and the frequent hard winds that whip it up. The skies are vast and blue.







The following is from the Wikipedia article about Roswell.

We have a cool, semi arid climate and four distinct seasons. Winter is cool and there is occasional snow that doesn't hang around long. Spring oscillates between warm and cool but there can be cold snaps.  There can be fierce winds. I clocked one gust last week at around 40 mph. I had to fight to walk against it. Summer is hot. Roswell experiences around 30 days out of the year above100° F. The North American monsoon season occurs during the summer and can bring torrential downpours and disastrous flash floods. The three streams that run through town can become raging rivers. The Berrendo ravine can fill up quickly.  Autumn brings relief. Things cool off although there can still be hot days, and snow is possible from October to March 

Since humidity is generally low and humidity causes changes to be more gradual, shade is considerably cooler than sun.

The record low: -24° F. (January 11, 1962, February 8, 1933)
The record high: 114°F. (June 27, 1994)

But the ground is that pretty cream color with glossy ground cover.....high albedo! This is a solar furnace. Hot anywhere else is HOT here.



So, the weather report for today (I'm taking a day off!):

Air Quality Index is fair at 45
No precipitation expected
Wind at 5.9 miles per hour from the west (prevailing winds here are mild breezes from the mountains (west) and brutal winds from the south in the leading edges of fronts and from the north after the front passes - beware the tumbleweeds. They're cute but vicious!
Ultraviolet index is high ( as usual, at altitude, there isn't a lot of filtering from the atmosphere)
Humidity is 17%
Barometric pressure is 30.17 inches of mercury. (About 1.02 bar, practically sea level.)

Why is Roswell so different from Selma? 

The strip of land bordering the Rocky Mountains to the east used to be a vast, shallow inland sea. Over millions of years, plankton died, sank to the bottom, and left a thick layer (several thick layers, actually, interspersed with mud) of their calcium carbonate skeletons and shells. That turned into limestone....highly reflective limestone that baked and efficiently reflected heat back up into the air when the sea dried up 

But more importantly, New Mexico is in the rain shadow of the Rocky Mountains. As humid air flows in from the Pacific Ocean, it rises up over the Cascades and the Sierra Nevada mountains and the Rockies into cooler heights where most of the humidity precipitates out. This is the air that Montana, Wyoming, Colorado, New Mexico, and Mexico gets. The eastern United States gets humidity pumped in constantly from the Atlantic and the Gulf of Mexico. It's dry and there's nothing to buffer the heat 

So my journey to adapt to desert life continues. This Arctic wolf is going to have fun. It's not like I can lock myself in an air conditioned house and never come out. My heart condition requires real activity.

Well, adventure might be painful, but it's fun. No pain.....no gain!

:)

So.....land, air, and water. It's where you live. How is your world? What kind of rock is under your feet? Is there plentiful water or is it dry? Are there caves near you? That's a part of karst geology. Do you have seasons or is it summer one day and.....suddenly winter! Have you tested the water from your tap? Water testing kits are easy to come by, usually from local hardware or home supply stores.


Thursday, August 19, 2021

When you can't see the stars...

Astronomy is a sometime thing (apologies to George Gershwin). Light pollution, haze, clouds, so many things can sabotage a night of stargazing, so what do you do when you want to see a star but can't.

Well, study the thing that blocks your view. I've been impressed with how well phone cameras can perform after the sun goes down. For instance, sunset doesn't necessarily end when the sun goes down. The sun may have set on you but the clouds above you are still in line if sight of a low, red sun.

Here are some low clouds over Centennial, Colorado about half an hour after sunset. 

Recently, we've been having some very uncharacteristic thunderstorms in the area. It's difficult to impossible to capture a lightning strike in a photograph, but a video is a different thing entirely.


Fog, smog, clouds are all interesting in their own light and they show a different face at night than they do during daylight.

Monday, August 10, 2020

Sunsets and mountains

Suddenly, I'm hiking again. The bug has bitten one of my housemates. We have been to the Lair O'the Bear, between Morrison and Kitteridge, Colorado the last two weekends. At the western end of Bear Creek Canyon, it's a short drive from home and it's near a new favorite restaurant, the Switchback Smokehouse, in Kitteridge (they have an ice cream shop next door!), so it's a great destination for me.

I didn't get many photo-ops the first time. Everything's so big it's hard to get a good picture, but Panorama Point provides some workable views. Here are some of the pictures.


Maidenhair ferns

Penstemon. The main wildflower season is done, but there are still some nice surprises out there. We also saw a lot of anemones but they looked pretty tired.


I don't know why there are things in this tree but it makes an interesting subject. There may have been people rappelling off the Point.


View to the southwest

Kitteridge and, in the distance, Mount Evans


I've also picked up some nice shots from home.

An airplane. We're near Centennial Airport and get a lot of air traffic over our house.

The sunsets have been nice recently.

I'm still working on physics and astronomy excursions and should have something to show for it soon. In the meantime, keep exercising that camera.

Wednesday, July 22, 2020

Can I trust my phone? Part 2

A while back, I downloaded an app that would do spectrometry. It would split light coming into the camera into its constituent "rainbow", which is cool since that is a way to analyze a substance. Each element has a rainbow fingerprint.

I was excited! I wondered if the representations of incandescent elements on the Internet would be true enough to create a faithful spectrum, so Zi pulled up a picture of a hydrogen lamp and looked at it with the spectrometer. Hydrogen has a very well known spectrum so I knew what it was supposed to look like. 

Wow! It looked great!...except…why was all that blue there? Hydrogen isn't supposed to have that big blue spike at the left end of it's rainbow.

I took my phone outside and looked at the sky through it's camera  Wow! Blue skies smilin' at me...way too blue skies, did I see. I was blue. I dumped the app.

It wasn't the app's fault. Phone cameras are made to produce pretty pictures and bluer skies are prettier. But they're not true blue and science looks for truth.

My son suggested that I use a yellow filter to remove some of the blue coming into the camera and then use the color balance on the camera to get back to true color, and it worked! On the hydrogen spectrum, it worked, but on everything else, it removed so much blue that I couldn't put any back in. blue again!

But recently I bought a packet of Selens Flight Flash Color Strobist Lighting Gel filters. Gels are plastic films. Less expensive than glass photographic filters, they're often used as compensation filters for different light sources. Slipping the ¼ CTO 6500 to 4500 K lightly yellow correction filter over the camera lens, between the phone and it's case did a great job. I used the SnailCamera Pro app, which gives me considerable color balance control to rebalance the picture and I "eyeballed" it until it looked right.

Here's what the camera saw without the picture.


Here's what the scene actually looked like.


Okay, a caveat. The colors were right but I lost some detail. The individual stones in the chimney lost some definition, but right now I'm more concerned with color values. I think some contrast adjustment could get some, if not all, of the definition back.

But I am impressed with the light capturing abilities of modern cell phones. Here are some early evening pictures I took.


A nice sunset


The same shot after the sun had gone away.


A star. Vega. I could not have seen that with my last cellphone camera.

Cell phones offer a lot of power to record your world but know your instrument. It's primary purposes are communication and entertainment. Accurate records require some finagling.