Peculiar Eruptive Mountains on the Colorado Plateau

The La Sal Mountains rise 8000+ feet above the Colorado Plateau (source).

In 1875, two geologists employed by the US government were studying mountains in southeast Utah. They worked 90 miles apart, each one in an isolated cluster of peaks rising above the mostly horizontal Colorado Plateau. They found the same strange type of structure and the same kinds of igneous rocks, and in their reports published two years later, they reached the same conclusions.

Albert Charles Peale was an employee of the War Department, specifically the Geological and Geographical Survey of the Territories led by Ferdinand Vandeveer Hayden. His party—one geologist, two topographers, two packers, and a cook—was surveying the Grand River District in western Colorado and eastern Utah (1). They spent a week in the Sierra la Sal, "which afforded magnificent opportunities for work" and then headed south. But hostile locals ("Indian trouble") brought field work to a sudden end. In their hasty exit, "all [rock] specimens had to be abandoned."

Grove Karl Gilbert was an employee of the Department of the Interior, specifically the Geographical and Geological Survey of the Rocky Mountain Region led by John Wesley Powell. On his descents of the Colorado River, Powell had seen an unmapped cluster of peaks to the west, which he named the Henry Mountains (2). They looked volcanic—domed, with dark lava-like rock on the top. Volcanology was a young science then, and geologists were debating whether volcanos were elevated craters or built from accumulated lava. So Powell sent Gilbert to the Henrys to "determine the facts" (Hunt 1988). He and his party stayed two months, more than enough time to answer the volcano question.

Peale worked in the La Sals, Gilbert in the Henrys; map based on data from National Atlas, labels added.

That winter Peale wrote up his findings, but two years would pass before Geological Report on the Grand River District was published (3). He estimated they had surveyed 6000 square miles of which "the greater part ... is plateau in character, the Sierra la Sal being the only mountain group." It was an isolated cluster of about 30 peaks arranged in three "eruptive centers". Peale was emphatic about origins: "there can be no doubt of the eruptive character of the mountains... porphyritic trachyte has been pushed up through the sedimentary layers which now dip away from the mountains" (Peale 1877a).

Peale called the La Sals "eruptive mountains of a peculiar type ... igneous and yet non-volcanic" (1877b). They were non-volcanic because lava didn't reach the surface. But neither were they plutons emplaced deep underground. Instead, magma had stopped somewhere in between, deforming the overlying rocks. The intruded rock was exposed much later by erosion. There was no name for this type of structure, so he described it in detail, pointed out its peculiarity, and left it at that.

Sections across Sierra la Sal showing tilted sedimentary strata on intruded trachyte (Peale 1877a, cropped).

From the Sierra la Sal, Peale studied the Henry Mountains off to the west. He knew John Wesley Powell (Gilbert's boss) thought they were volcanic—"the summits of these mountains mark in reality the level of former valleys down which the volcanic material flowed" (Powell 1875, quoted by Peale). But even from ninety miles away Peale could see that was incorrect. "l am inclined to class the Henry Mountains with the Sierra la Sal and Abajo [Mountains], as their outline is similar ..."

From his vantage point in the heart of the Henrys, Gilbert "agreed" with Peale (unknowingly). The peaks were neither elevated craters nor accumulated lava nor even volcanic. In fact they were a novel type of structure, as he warned his readers:

"If the structure of the mountains be as novel to the reader as it was to the writer, and if it be as strongly opposed to his preconception of the manner in which igneous mountains are constituted, he may well question the conclusions in regard to it while they are unsustained by proof. I can only beg him to suspend his judgment until the whole case shall have been presented." (Gilbert 1877)

Gilbert gave the novel structure a name—laccolite—thereby making the Henry Mountains the type locality for laccoliths (today's term). He distinguished them from volcanic eruptions, where lava reaches the surface and accumulates. "The lava of the Henry Mountains behaved differently ... it stopped at a lower horizon, insinuated itself between two strata, and opened for itself a chamber by lifting all the superior beds."

Gilbert's sections across the familiar Mountain of Eruption (volcano) and the novel Laccolite.

Like Peale, Gilbert had to wait two years for publication of his findings. He finished his monograph the winter after his second season in the Henrys. "It was at once put in type, and in anticipation of a speedy issue the current year [1877] was marked on the imprint..." But the many illustrations caused delays. Geology of the Henry Mountains was finally bound and distributed in 1879.

By that time a wealth of information about igneous mountains had accumulated, prompting Gilbert to prepare a second edition (1880). It differed from the first mainly in the addition of an Appendix: Recently Published Descriptions Of Intrusive Phenomena Comparable With Those Of The Henry Mountains. At the end of the section about Peale's findings in the La Sals, Gilbert concluded, "All of these features are paralleled in the Henry Mountains and they leave no reasonable doubt that the structures are identical."

I visited the Henry Mountains in 2012, accompanied by the spirit of Grove Karl Gilbert. I camped at Starr Springs as he had, and hiked to the spectacular south face of Mount Hillers, "revetted by walls of Vermilion and Gray Cliff sandstone" as he explained.

South face of Mount Hillers—steeply tilted sandstone on flanks, intruded trachyte on crest (Jack Share).

Vermillion sandstone "tilted almost to the vertical".

Since then, I've been keen to visit more of the peculiar eruptive mountains on the Colorado Plateau. Last September I finally did, spending a week in the Sierra la Sal.

La Sals upper right; snow highlights 3 clusters of peaks. Upheaval Dome upper left. (Google Earth)

Peale's three eruptive centers live on, though they're now called intrusive centers ("eruptive" means volcanic). But these are special intrusions—emplaced at depths intermediate between volcanos (surface) and plutons (deep). They now have their own descriptor—hypabyssal, aka subvolcanic (but still laccoliths).

Two hypabyssal intrusion-cored peaks: Castle Mountain (left) retains a cap of sedimentary rock; La Sal Peak (right) is trachyte (Ross 1998, cropped).

The three intrusive centers of the La Sal Mountains are conveniently named northern, middle, and southern (4). All normally are accessible via the paved Loop Road, but road construction kept me in the northern one. From a very nice small primitive campground, I hiked to see what I wanted to see—the distinctive features of these peculiar eruptive mountains.

It was a short walk to Castle Valley Overlook with views of the Colorado Plateau. The Plateau doesn't look horizontal, but the rock layers are. The spectacular landforms—towers, buttes, rims. deep winding canyons—are erosional. True uplifts like the La Sal Mountains are uncommon. Gilbert called them "disturbances in a region of geological calm."

Looking northwest near Castle Rock Overlook; in the valley bottom left of center is Round Mountain, a small intrusion perhaps connected to the La Sals.

Let's head on down and see what we can see.

Among Peale's important observations were tilted sedimentary strata that "now dip away from the mountains". He concluded they were pushed up and tilted by rising magma. The hike provided good views of steeply tilted sedimentary rocks.

Nearly vertical beds of reddish sedimentary rocks below trachyte slopes of Grand View Mountain (left); high peaks visible on horizon just right of center.

With part of the Loop Road closed, the high peaks weren't easy to access. So the next day we hiked up a rough dirt road to view trachyte. It's common above the flanking sedimentary rocks, forming steep slopes and discouraging travel as Peale noted. "The only difficulty met with in the study of this interesting region is the great amount of debris that has accumulated ..."

Some kind of outcrop (could be rhyolite) beyond steep slope of "debris".

Trachyte with a dark xenolith—country rock broken off and carried up by magma. 

Fall colors on trachyte.

Mount Peale, a large laccolith and high point of the La Sals (Suffusion of Yellow).

Peale was hesitant to identify the igneous rock of the La Sals, without specimens to give to petrologists for "critical examination". But it looked very much like rock he had seen in similar intrusions in Colorado. So he assigned it to a general category—porphyritic trachyte. It seems trachyte was the accepted name for shallow intrusive rocks low in silica in Peale's time (see Appendix in Gilbert 1880). Now it may be trachyte or diorite, depending in part on whom you ask (5). Being very much a 19th century naturalist at heart, I will stick with trachyte.

On the other hand, everyone agrees the rock is porphyry—visible crystals (phenocrysts) in a fine-grained matrix of trachyte. This is a very cool rock, with an interesting history. As the magma rose it gradually lost heat, eventually dropping to a temperature where hornblende and plagioclase formed crystals. This changed the composition of the remaining molten magma, and when it stopped c. 6–10 km below the surface, it rapidly crystallized to form the trachyte matrix (Ornduff et al. 2006; see also Fractional crystallization).

Porphyritic trachyte mementos from Henry Mountains (left) and La Sal Mountains.

As I drove away from the La Sals, I thought a lot about the pioneering geologists of the American West. Like me, they were inspired by geology and the beauty of the landscapes, but their geotripping was very different. Travel (route-finding required) and camping were much more challenging. And where specifically should they go? (no guidebook). However they had the promise of discovery, which surely made up for all the hardships!

AC Peale and two unidentified men, probably during the
Geological & Geographical Survey of the Territories (Smithsonian Archives).

Notes

(1) The Grand River was the section of the Colorado above the confluence with the Green. Its name was changed in 1921.

(2) Powell named the cluster of peaks for Joseph Henry of the Smithsonian Institution, who helped secure funding for Powell's exploration of the Colorado River.

(3) Publication of Peale's report was delayed through no fault of his own. As his boss, FV Hayden explained, it was caused by "the great increase of labor incident to the International Exposition at Philadelphia", labor that would have gone toward preparation of reports. In general, the regular Reports of the Geological and Geographical Survey of the Territories were inadequate for sharing discoveries. In 1874, a new publication—Bulletins— was created to "publish without delay ... new or specially interesting matter". Peale had an article in Bulletin No. 3, about the peculiar eruptive mountains of Colorado and adjacent Utah, including the La Sals (1877b).

(4) Some sources refer to the La Sal intrusive centers as composite plutons or coalesced intrusions.

(5) Ross (1998) reported that La Sal igneous rocks were 59–71% Si02 (silica), and called them trachyte based on "the Total Alkali-Silica classification of LeBas and others". Wilson and others (2016, based on reports from 1953, 1959, and 1992) reported that igneous rocks of the Henry Mountains were 58–63% SiO2, and called them diorite. (Thanks to Mike for taking a stab at trachyte vs. diorite.)

Sources

Bartlett, RA. 1962. Great Surveys of the American West. Norman, OK: University of Oklahoma Press.

Fillmore, R. 2011. Geological evolution of the Colorado Plateau of eastern Utah and western Colorado. Univ. Utah Press.

Gilbert, GK. 1877. Report on the Geology of the Henry Mountains. GPO. BHL.

Gilbert, GK. 1880. Report on the Geology of the Henry Mountains. 2nd edition. GPO. Google Books PDF. Appendix p 153–161 contains added material about igneous mountains.

Gould, LM. 1927. Geology of the La Sal Mountains, Utah Papers of the Michigan Academy of Science, Arts and Letters Vol. 7: 55-106. HathiTrust

Hunt, CB. 1958. Structural and igneous geology of the La Sal Mountains, Utah. USGS Professional Paper 294-1. PDF

Ornduff, RL, Wieder, RW, Futey, DG. 2006. Geology Underfoot in Southern Utah. Mountain Press Publishing. (see Vignette 32, Intruders in a sedimentary domain)

Peale, AC. 1877a. Geological report on the Grand River District, in Hayden, FV. Ninth annual report of the United States Geological and Geographical Survey of the Territories (p. 31–101). BHL

Peale, AC. 1877b. On a peculiar type of eruptive mountains in Colorado. Art. XVIII in US Geological and Geographical Survey of the Territories Bulletin No. 3: 551–564. BHL

Powell, JW. 1875. Exploration of the Colorado River of the West. Geographical and Geological Survey of the Rocky Mountain Region (Henry Mts p. 200-203).

Ross, ML. 1998. Geology of the Tertiary intrusive centers of the La Sal Mountains, Utah; influence of preexisting structural features on emplacement and morphology in Laccolith complexes of southeastern Utah; time of emplacement and tectonic setting. USGS Bull. 2158: 61-83. PDF

Wilson et al. 2016. Deformation structures associated with the Trachyte Mesa intrusion, Henry Mountains, Utah, Implications for sill and laccolith emplacement mechanisms. J. Structural Geology 87: 30-46. free online

The Monthly Fern: Northern Holly Fern, a spore shooter

This month's South Dakota fern is Polystichum lonchitis, Northern Holly Fern (Andre Zharkikh).

It was the first paragraph on the first page of Robbin Moran's Natural History of Ferns that hooked me—specifically the words of a thief in Shakespeare's Henry IV:

"We steal as in a castle, cock-sure; we have the receipt of fern-seed, we walk invisible."

So intriguing! Or maybe not. Maybe you doubt that fern-seed can bestow invisibility (1). But think about it ... have you ever seen fern seeds? 

In Shakespeare's time no one had seen fern seeds because they were invisible. In our time we haven't seen fern seeds because they don't exist. And for those who answered "yes" to the question above—spores are not seeds (2).

Northern Holly Fern, well-armed with clusters of sporangia, aka spore shooters (Andre Zharkikh, bar added).

Northern Holly Fern is widespread in the Northern Hemisphere, but often uncommon where it occurs. It's considered an arctic-alpine, boreal, and montane species, which may seem odd for a South Dakota plant. However it grows specifically in the Black Hills (3), which are famous for plants seemingly out of place. Northern Holly Fern is likely a relic of the last Ice Age, when western South Dakota was much cooler (but not glaciated).

Circumboreal Polystichum lonchitis (Cremastra); Black Hills added (location approximate).

Like most ferns, Polystichum lonchitis has little clusters on the underside of its leaves. These are sori (singular sorus), and deep inside are spores. Shape and position of sori are helpful in identification. Often each sorus has a little cover, the indusium, and its shape (or absence) also is useful in identification. Sori of holly ferns are round, lined up between the leaflet midrib and edges, and have peltate (umbrella-like) indusia—tiny round membranous covers on short stalks.

Northern Holly Fern's round sori with peltate indusia (Andre Zharkikh).

Now a short tour of sori diversity, providing a glimpse the level of detail needed for identification. It's handy to have a 10X magnifier.

Left: Maidenhair Fern, Adiantum pedatum, has linear sori partly covered by rolled leaf edges (false indusia). Right: Bracken, Pteridium aquilinum, has continuous sori with indusia hidden under rolled leaf edges (MWI & MWI).

Top: young Fragile Fern, Cystopteris fragilis, with round sori; indusia will wither as spores mature. Bottom: Wood Fern, Dryopteris carthusiana, with round sori covered by kidney-shaped indusia (MWI & MWI).

Common Polypody, Polypodium virginianum, has plump yellow sori with no indusia (MWI).

However we still haven't seen any spores. The sori's brown or yellow dots are not spores, they are sporangia. Inside the sporangia, finally, are the spores—in abundance!

 

Fern leaf with sori containing sporangia containing spores (and some scattered about); USDA Forest Service.

Fern spores are tiny, usually 30–50 micrometers across (1 µ = 0.001 mm), which is narrower than a human hair (source). Or think of it this way—a fern frond just 60 cm long will produce something like 7,000,000 spores! (source) As fine as dust, spores can fly in the lightest breeze, especially if the sporangium kicks them out of the house.

Holly Fern spores, scale bar = 10 µ. © Robbin Moran 2012.

In some ferns, the sporangia simply split open and let their spores fall to the ground. Last month's Sensitive Fern is an example. But in Holly Ferns, in fact in many ferns, sporangia hurl their spores. I like to call them spore shooters, as does Robbin Moran. Others call them launchers or catapults. In any case, their spores can reach speeds of 10 m/sec! (Llorens et al. 2015)

The diagram below shows a spore-shooting sporangium in action. The ring of blue and red cells is the annulus; the cells are filled with water. As the outside dries the annulus curves back, opening the sporangium and cocking the catapult or shooter. Elastic pressure increases until the annulus suddenly collapses, sending spores flying. They get quite a boost in speed, but probably just as important, they're dislodged from the interior of the sporangium. Apparently my "house" analogy above was appropriate. These clingy spores need encouragement to go out into the world.

Modified from Llorens et al. 2015.

Some readers may still be bothered by my earlier statement that spores are NOT seeds. After all, won't a spore give rise to a full-sized fern, like the pea that becomes a pea plant? Well ... yes, but not directly. A true seed has a full set of chromosomes (diploid), and can give birth to a seedling. But a spore has only half a set (haploid). Before a fernling can arise, fertilization must take place.

This leads us to the fern life cycle, which even pteridomaniacs call "the bugbear of botany students". Maybe "fern sex" would be less scary. In any case, stay tuned. I will squeeze it in amidst the beauty and intrigue of the next Monthly Fern.

Northern Holly Fern. Thanks to Andre Zharkikh, who kindly shares his many plant photos "to show other people the beauty of nature".

Notes

(1) To provide invisibility, fern seed must be collected precisely at midnight on Midsummer's Night Eve, while it's falling from the plant.

(2) If you thought spores were seeds, you're in venerable company. Carl Linnaeus, father of modern taxonomy, did also. He first thought the fine dust shed by ferns was pollen. But he then admitted he knew too little about primitive plants to conclude "whether what I see is seed, or dust of the anthers." However years later, in 1751, he announced that the dust was fern seed (Moran 2004).

(3) Flora North America and USDA Plants, sources usually considered reliable, do not include South Dakota in the known range of Polystichum lonchitis (the latter shows it as reported but without documentation). It was first documented in the Black Hills in 1977, and has been found elsewhere in the northern Hills since (see map from SEINet herbarium search, zoom in to South Dakota).

Sources, in addition to links in post

Llorens, C, et al. 2015. The fern cavitation catapult: mechanism and design principles. J. R. Soc. Interface 13: 20150930.

Moran, RC. 2004. The Natural History of Ferns. Timber Press.

Pinson, Jerald. About Ferns. American Fern Society.

Summers, A. 2005 (Dec). Spore Launchers; Ferns and fungi that explosively reproduce. Natural History.

USDA Forest Service. Ferns. Helpful information, photos, and diagrams for aspiring pteridomaniacs. And there are coloring pages! (have a range of greens ready)