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8 Geological Wonders of North America

Pewits Nest

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8 Geological Wonders of North America
Source: https://bit.ly/3ypLR3O Photographer: Joshua Mayer CC License: https://bit.ly/3yp1319

We hope that you enjoy this article on 8 Geological Wonders of North America. Every part of our world holds an abundance of such beauty, and this area is no exception to that. These come in a incredible variety of types, all wondrous to behold. Of course, these represent only the smallest fraction of the marvels of Nature you can find in this part of the world, or any part, for that matter. But, we hope that these few will serve to whet your appetite for more.

Hells Canyon

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Hells Canyon Facts

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Hells Canyon Physical Description

First of all, the sheer grandeur of the mesmerizing Hells Canyon must be taken into account. That’s because it’s sheer dimensions only tell part of its story. However, those remain impressive enough on their own.

Firstly, the magical geological wonder has a truly astounding overall width. That holds true because that measures roughly 10 mi (16 km). Further, its maximum depth measures an astounding 7,993 ft (2,436 m). It also has a total length of about 125 mi (200 km).

Also, the beautiful Snake River flows through the fabulous canyon. Yet, at one point it does so at more than 1 mi (1.6 km) below the western edge. Furthermore, on the other side, majestic mountains soar to a height of 7,400 ft (2,300 m) above it.

Additionally, the awesome site serves as home to an abundance of wildlife. This includes large numbers of black bears, elk, cougar, mountain goats, and deer. Finally, several plant species thrive there that exist nowhere else.

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Hells Canyon Location, Formation, and Usage

The sincerely stunning Hells Canyon formed in what now comprises the far northwest section of the United States. This enormous canyon also remains one of the great geological wonders of North America.

It is located roughly along the borders of three states. These consist of Idaho, Oregon, and Washington. Its earliest formation began around 300 million years ago. This began as the result volcanic activity, not tectonic.

Furthermore, due to ongoing volcanic action, enormous quantities of limestone began to be deposited. Much later, tectonic activity then pushed the limestone, along with sedimentary rock, upward.

In addition, about 6 million years ago, the Snake River formed. Its mighty flow slowly but surely carved out the massive canyon. Then, roughly 15,000 years ago, a massive flood from a melting glacier further expanded it.

Lastly, today the site has several primary uses for mankind. First of all, three large hydroelectric dams have been constructed within its confines. Also, numerous recreational activities happen in abundance within it. These include hiking, boating, fishing, camping, and rafting.

Homestead Caldera

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Homestead Caldera Facts

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Homestead Caldera Physical Description

Firstly, geological evidence indicates that Homestead Caldera formed nearly 10,000 years ago. Furthermore, it constitutes only one of many found throughout the region. The impressive dome itself measures roughly 55 ft (16.7 m) in height. That dome also spans roughly 400 ft (122 m) in diameter.

Secondly, the marvelous structure remains mainly composed of limestone, and formed gradually over time. This remarkable formation occurred via the depositing of minerals from the geothermal spring. Subsequently, as a result of internal pressure, the newly-formed dome itself pushed outward. 

A relatively small hole in the top of the dome allows sunlight to filter in naturally. Additionally, for tourist purposes, a tunnel was drilled into the side of the dome to allow better access. The geothermal activity also maintains a steady water temperature of between 90-96 F (32-36 C).

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Homestead Caldera Location, History, and Nature

Perhaps most notably, the magnificent Homestead Caldera formed near what now constitutes the city of Midway, Utah, in the United States, in North America.  To the surprise of many, the magnificent caldera actually represents a geothermal spring contained inside a naturally formed dome.

Additionally, an ongoing archaeological project works to retrieve objects left behind over time by thoughtless humans from the silt. These include coins and antique firearms. Those, and numerous other objects, are retrieved from the silt deposits that line the bottom of the hot spring.

Also, the water found at the site has a typical,and somewhat surprising, depth of nearly 65 ft (19.8 m). Meanwhile the silt itself measures roughly 14 ft (4.3 m) deep in places. This extreme depth makes locating, not to mention retrieving, the various paraphernalia difficult.

Fortunately, however, the owners have committed to every effort to return the site to its natural pristine condition. Those same individuals have also committed to exploring the history surrounding the site, as well.

Purple Sand Beach

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Purple Sand Beach Facts

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Purple Sand Beach Physical Description

First of all, the dazzling and unique Purple Sand Beach actually owes its distinctive color to the nearby mountains. This holds true partly due to the fact that these formed in extremely close proximity to the seashore. This extremely unusual placement represents only the first in a series of factors that created the unique beach.

Secondly, playing yet another part in that chain of factors, these mountains also remain especially rich in mineral deposits. Further, in a most unusual occurrence, the mountains contain vast amounts of the mineral manganese garnet. As you probably guessed, this delicate mineral also forms a purplish-colored silicate.

Thirdly comes the final step in the remarkable process. Local rains wash fine crystals of the mineral down to the nearby seashore. This, therefore, provides a naturally and continually renewing pigmentation of the beach. However, while pure purple predominates, traces of lilac and magenta can also be seen.

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Purple Sand Beach Location and Geology

Located in North America, the lovely Purple Sand Beach does not merely represent a one-hit wonder of geology. This beach forms part of the Los Padres National Forest, in California, United States. Its brilliantly colored sand, however, is not the only distinctive feature found in this one location.

In addition to the incredible marvel of the beach itself, several marvelous sea caves also appear just along the shoreline. Quite understandably, these natural features remain extremely difficult to access, however. The ocean waves typically remain strong enough to make entering these extremely hazardous.

Additionally, just offshore sits the locally famous Keystone Arch, with a naturally occurring hole near its center. Due to its angle and placement, an incredible coincidence of Nature takes place here. That’s because the setting sun shines directly through the keyhole only during the weeks of the Winter Solstice.

Pewits Nest

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Pewits Nest Facts

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Pewits Nest Physical Description

First of all, the Nature Reserve containing Pewits Nest actually only covers a surprisingly small region. That holds true due to the fact that it encompasses a total area of only 9 acres (3.6 hectares). However, the site perfectly proves the old adage that beauty comes in all sizes.

In addition, this awesome wonder of Nature formed across the landscape only about an estimated 10,000 years ago. It must be pointed out that, in geological terms, this makes it quite young. The wondrous site formed through the actions subsequent to the retreat of the last glacier in the region.

That’s because the action carved a narrow, and relatively deep, gorge into the soft and pliable sandstone of the area. The depth of the beautiful gorge ranges across its length. This runs from a depth measuring about 30-40 ft (9.1-12.2 m), not including the height of the several small cliffs which surround it.

In addition, the melting of the glacier also resulted in the creation of multiple small waterfalls, as well. Numerous formations known as potholes also formed, along with a small creek, known locally as Skillets Creek. In fact, this small waterway continues to run through the Reserve even today.

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Pewits Nest Location, Nature, and Preservation

The truly breathtaking Pewits Nest sits in the state of Wisconsin, in the United States, in North America. Further, the state of Wisconsin Department of Natural Resources owns and maintains the site. Its designation as a protected State Natural Area occurred in 1985.

Bountiful and beautiful flora thrives there, perhaps because the location resides within a small dry-mesic forest. The region also consists of rather dense undergrowth and numerous trees. The majority of these consist of white pine, hemlock, red cedar, and yellow birch.

Numerous small animals also such make their home in this magical area. Among others, this includes rabbits, squirrels, and multiple types of birds. Quite sadly, however, the species known as the peewit, from which its name derives, is rarely seen now.

Furthermore, the Pewits Nest State Nature Area remains open to the public. But, quite regrettably, few people outside of the immediate area know of its existence. The parking zone only holds 7-8 cars, since the government makes every effort to maintain the beauty of this small wonder.

However, the officials do not maintain the numerous trails, so visitors to the Nature Reserve must watch their step. Finally, Pewits Nest once contained a small mill, where a water wheel made use of the falls, but no trace of it exists today.

Giant Crystal Cave

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Giant Crystal Cave Facts

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Giant Crystal Cave Physical Description

First of all, the incredible Giant Crystal Cave serves as home to the largest crystals on earth. In point of fact, some of these attain a size as great as 34 ft (11 m) long and as estimated weight 55 tons. These monstrously large crystals have a composition primarily consisting of selenite. This mineral, the nearby magma chamber deposited over the course of countless centuries.

Furthermore, these enormous and remarkably impressive crystals formed as a result of an extremely special combination of factors. This process began with greatly heated groundwater being saturated with sulfide ions. Subsequent to this action, significantly colder surface water leaked down and contacted the mineral-saturated hot water. This formed the next step in the process of formation.

However, the two supplies of water did not mix together. This occurred due to the difference in the relative densities of the two separate water supplies. As a result of these unique factors, hydrated sulfates, primarily gypsum, formed at an extremely slow rate over the course of at least 500,000 years. As these crystallized, they formed the enormous crystals present in the cave today. 

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Giant Crystal Cave Location, Condition, and Exploration

The absolutely astounding Giant Crystal Cave formed in a region that now constitutes the area of Chihuahua, Mexico, in North America. In addition, and rather surprisingly to those who discovered it, the cave sits a mere 1000 ft (300 m) beneath the surface. Despite that, it remained unknown until modern times.

But, despite its proximity to the surface, due to the extreme conditions within the remarkable cave, humans still know very little about it. What we do know can be summed up rather briefly. Further, for the moment, no plans exist to explore the cave further, to preserve it in its natural state.

The amazing cave formed in what approximates a roughly horseshoe shape. It also lies within an enormous limestone deposit. Also, faceted crystalline blocks cover the floor, and the enormous crystalline beams protrude through these. This creates incredible patterns, serving to enhance its beauty.

When man originally discovered the cave, water filled the inside. The cave later became accessible only because the nearby mining operation which discovered it kept pumping the water away. Only authorized scientific researchers had access permits, due to the conditions. Finally, experts made the decision to allow the site to flood again, because exposure to air was beginning to erode the crystals.

Mount Ranier

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Mount Ranier Facts

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Mount Ranier Physical Description

In the minds of most individuals who encounter it, the most notable characteristic of Mount Ranier likely remains its sheer size. This peak possesses a height measuring 14,411 ft (4,392 m) at its highest point. Its sheer height isn’t the only reason the site stands out, though.

That’s due to the nature of the region surrounding it. Relative to the lowest region around it, it stand the highest of any point in its region of the world. It additionally has a proportionately great width, making for an outline that stands out for any who see it.

More precisely, the total area of the base of this majestic formation measures an astonishing 100 sq mi (259 sq km). At its top, however, yet another volcanic feature captures one’s attention. Amazingly, the summit possesses not one, but two incredible craters.

Each of these, furthermore, measures more than 1,000 ft (300 m) in diamter. The one on the eastern side measures slightly larger than the one on the western side. The eastern of the mountain on also slightly overlaps the one formed on the western side of the volcano.

In the western crater, though, yet another feature merits attention. That’s due to the fact that, here, a small crater lake exists. This roughly rectangular measures roughly 130 ft x 30 ft (39.6 m x 9.1 m). It’s shallow, however, only averaging around 16 ft (5 m) in total depth.

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Mount Ranier Location, Geology, and Ecology

The breathtaking Mount Ranier formed in a region of the Northern Hemisphere well known for geological activity. In fact, it lies only about 90 mi (145 km) from Mount Saint Helens. More precisely, it sits in the state of Washington, in the United States, in North America.

Its exact location, in fact, further places this remarkable stratovolcano only 54 mi (87 km) southeast of the city of Seattle. Its height, combined with the nature of the local geography, means that in clear weather it’s possible to see it from Portland, Oregon, 135 mi (217 km).

The majority of the mass of this fabulous volcano consists of a combination of debis flows, lava flows, and pyroclastic ejecta. Geological evidence indicates that the mountain began forming roughly 840,000 years ago. Most of its mass now is about 500,000 years old.

Astonishingly, most of its outer surface area has a covering of permanent snowfields and glaciers. Astoundingly, a total of 26 major glaciers presently cover much of the mountain. Due to this, it ranks as the most heavily glaciated site in the continental United States.

Fortunately, the entirety of Mount Ranier lies within the boundaries of the Mount Ranier National Park. The government of the country established this site as its 5th National Park, on March 2, 1899. This therefore provides it with a measure of protection.

The surrounding region thus provides a safe haven for numerous species of flora and fauna. Some of these are not only endemic, but appear nowhere else. The area further possesses a highly diverse ecosystem, due to differing climates at varying altitudes.

Fields surroung the volcano have a gorgeous covering of varied wildflower varities. The region also boasts large forests, some great in age. A vast array of insects and animals also live here, including 65 types of mammals, along with many birds and reptiles.

Fantasy Canyon

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Fantasy Canyon Facts

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Fantasy Canyon Physical Description

Firstly, the astounding rock formations found throughout the aptly-named Fantasy Canyon originally deposited during the late portions of the Eocene Epoch. This amazing action occurred between 38-50 million years ago. However, the extraordinary features of the canyon, contained within a scant 10 acres (4.6 hectares), do not constitute its only claim to distinction.

Furthermore, the subsequent erosion eventually led to the creation of the incredible features present today. However, this happened in conjunction with the particular composition of the rocks themselves. Furthermore, horizontal mineral deposits also run through the rock formations, with actually two different mineral veins present.

In addition, one of these two veins of mineral deposits consists of Gilsonite. This is a fascinating mineral based on hydrocarbons. The other vein remains comprised of magnetite, which forms a mineral containing unique magnetic properties. Therefore, the site remains distinctive for its composition, as well as its remarkable appearance.

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Fantasy Canyon Location and Uniqueness

Most notably, the utterly astounding Fantasy Canyon formed in what now constitutes northeast Utah, in the United States. Also, the region in which the canyon formed originally bordered an ancient lake. This body of water therefore served as the original source of the sandstone in the area.

Further, ongoing sedimentation over the passage of time deposited various other minerals and material in the region. These primarily include sandstone, siltstone, and shale. These various minerals erode at different rates, however. But, the sandstone appears to be much more durable than the others.

Also, as the other deposited minerals eroded, the unique features of Fantasy Canyon developed. These have been further augmented by wind erosion over the ensuing millions of years. To top things off, the canyon also serves as home to an extensive number of fossils, dating back to the Eocene Epoch.

Hamilton Pool

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Hamilton Pool Facts

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Hamilton Pool Physical Description

First of all, the magnificent Hamilton Pool remains rather unique in several ways. The water of the awesome site comes from a small waterfall which steadily feeds and maintains the popular pool. Furthermore, this small but nonetheless picturesque waterfall plunges a total of about 50 ft (15.2 m).

Yet that is not the only remarkable trait of this fabulous geological marvel. That holds true due to the fact that the waterfall never completely dries up. But, it does slow to a trickle at times, due to various factors. As a result of this, the dimensions of the pool vary greatly. However, in terms of depth, the pool stays quite shallow.

The surrounding rocks are composed of limestone, and the natural filtering action keeps the water a jade green. The pool even remains surrounded by numerous large limestone slabs. And last but not least, numerous stalactites can even be seen hanging from the ceiling of the underground portion.

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Hamilton Pool Location, Formation, and Ecology

It must be noted that the stunning marvel that we call the Hamilton Pool, with its picturesque beauty sits about 23 mi (37 km) west of Austin, Texas, in the United States. Its beauty stands out among the otherwise relatively harsh nature of its surroundings in this portion of North America.

Geologists remain uncertain when Hamilton Pool formed, yet believe it happened at least 10,000 years ago. But, its formation occurred due to the forces of erosion, working over a vast span of time. In addition, the dome covering an underground river collapsed at that time, forming the grotto.

Also, the waters of the breathtaking pool eventually flow into the mighty Colorado River. This area forms a small oasis in the region and, as a result, teems with flora and fauna. The stone overhang stays covered in dark green moss, and the banks teem with mountain juniper and various small shrubs.

Not only that, but several rare bird species also make their home around the pond. Officials allow public swimming, yet carefully monitor the activity since they do not artificially maintain the water quality. As a result, the site occasionally closes to public swimming, for public safety.

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8 Geological Wonders of North America

We sincerely hope that you have thoroughly enjoyed reading and learning about these 8 Geological Wonders of North America. Countless others await your discovery among our other articles. We invite you to peruse them at your leisure, and share them with your friends for all to enjoy. But many of these marvels are in need of our help. They must be preserved for future generations to enjoy them as well. To that end, let us all do everything we can to ensure their preservation.

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