Denali is the highest point in North America and by some measures is the tallest mountain in the world.
The Geology of Denali National Park and Preserve
The Alaska Range is a 600-mile long arc of mountains that stretches from the Alaska-Canada border all the way to the Alaska Peninsula. The range is highest at its mid-section, a vast region of towering peaks and massive glaciers that lies within Denali National Park and Preserve. Denali is a region of great geologic activity and complex-ity, and scientists are only beginning to piece together its puzzling past. It has rock for-mations that have been carried there from thousands of miles away, fossils of ancient creatures that have been plowed up from ocean depths, new rocks born of the Earth’s internal fire, and some of the oldest rocks in Alaska. The range’s height and distance from the equator combine to make it a place of eternal winter, and deep snows com-press to form glaciers (creeping rivers of ice which continuously grind away at the still-rising peaks). It would be considered one of the world’s great geologic showcases even if it didn’t contain the highest peak in North America.
Denali is one of the most striking features on the entire planet. At 20,310 feet, it is the crowning peak of the Alaska Range and the highest mountain on the continent. It towers three and one-half vertical miles above its base, making it a mile taller from base to summit than Mt. Everest. Denali's base sits at about 2,000 feet above sea level and rises over three and one-half miles to its 20,310 foot summit. Everest begins on a 14,000-foot high plain, then summits at 29,028 feet.
Denali’s icy north face—the Wickersham Wall—is one of the world’s highest continuous mountain faces, rising 14,000 feet from the Peters Glacier to the North Peak. Permanent snow and ice cover over 75 percent of the mountain, and enormous glaciers, up to 45 miles long and 3,700 feet thick, spider out from its base in every direction. It is home to some of the world’s coldest and most violent weather, where winds of over 150 miles per hour and temperatures of -93˚F have been recorded.
Land of Eternal Winter
Many consider Denali to be the world’s coldest mountain because of its combination of high elevation and its subarctic location at 63 degrees north latitude. Mount Everest (29,028 feet) is the world’s highest point above sea level, but it is at the same latitude (28 degrees north) as Florida’s Walt Disney World. Denali sits 2,400 miles further north. This makes an enormous difference in temperature.
Denali is so massive that it generates its own weather; much the way a huge boulder submerged in a river creates whitewa-ter rapids. All mountains deflect air masses and influence local conditions, but Denali rises so abruptly and so high that this effect is more dramatic here than perhaps anywhere else on Earth. Storms barrel in from the Gulf of Alaska and the Bering Sea and collide with Denali’s towering mass. Weather can quickly change from sunny and clear to blizzard condi-tions with fierce winds, intense cold, and heavy snowfall. Climbers must understand and pay close attention to warning signs of changing weather, and use their observations to plan when to climb, when to retreat, and when to dig in.
The Birth of a Mountain Range
The spectacular mountains we see today are a result of millions of years of rock formation, uplift, and erosion.
Before we discuss the processes that created today’s Alaska Range, let’s review some basics about rocks and their origins.
Three major types of rocks make up Earth’s crust. Igneous rocks are formed when molten rock solidifies. Igneous rocks can be plutonic or volcanic. Plutonic rocks, such as granite, form when magma cools slowly in the depths of the earth. Volcanic rocks, such as basalt, rhyolite, and andesite form when lava cools rapidly on the surface.
Sedimentary rocks are derived from sediments--particles of mineral and organic material which have been deposited by water or wind. Sediments are most commonly carried by rivers or streams and deposited in basins, that is, low areas such lakes and seas. These sediments are buried and compressed into rock strata. Typical sedimentary rocks include sand-stone, limestone, shale, and chert. Fossils found in sedimentary rocks provide clues to ancient environments.
Metamorphic rocks are pre-existing rocks that have been changed due to intense heat and/or pressure deep within the earth without completely melting. The original rocks could have once been sedimentary, igneous or even another meta-morphic rock.
When rocks are squeezed and baked beneath Earth’s surface or by contact with lava at the surface, the minerals may recrystallize and change form. Wavy layers of minerals called foliation may appear. Typical metamorphic rocks around Denali include schist, slate, quartzite, and marble.
How Did Denali Get So High?
Geologists have identified several factors that have probably contributed to Denali’s great elevation. The theory of plate tectonics provides part of the answer.
To briefly tell this story, consider that Earth’s crust is broken into great slabs of rock called tectonic plates. These plates float on the layer of Earth known as the mantle. The mantle is mostly solid, although it can move very slowly.
Heat from the outer core is transferred to the lower regions of the mantle. As the mantle heats, it becomes less dense. This less dense material begins to rise. The cooler mantle under the crust is denser; it sinks. As it sinks, it warms, setting up a cycle called a convection current. Ge-ologists surmise that the convection currents in the mantle cause the tectonic plates on top to move around the surface.
One tectonic plate, known as the Pacific Plate, forms the floor of the Pacific Ocean. It is slowly moving northward at about the rate that your fingernails grow. Oceanic plates are denser than continental plates. When an oceanic plate collides with a continental plate, the oceanic plate sinks below the continental plate in a process called subduction. In the diagram below, the Pacific Plate is diving below the part of the North American Plate that holds Alaska’s mainland. As the Pacific Plate moves northward, it carries chunks of land and pieces of other plates, some from thousands of miles away. These chunks and pieces are called terranes.
The force of the Pacific Plate pushing northward creates tension between the two plates. The build-up and sudden release of tension as these plates slip by one another triggers earthquakes. Much the way the hood of a car buckles under the force of a collision, the process of subduction causes the uplift of the Alaska Range, as well as the coastal ranges.
There are two major faults that contribute to the uplift of De-nali. They are the Denali Fault and the Hines Creek Fault. Land south of the faults moves to the west relative to the north at a rate of about 1 centimeter per year. A large bend in the Denali Fault directly north of Denali causes rocks to bunch up. Denali happens to be in this bend; this is one of the reasons it is so tall. The forces that caused the uplift of Denali continue today. Sci-entists know that Denali rises at a rate of one half of a millime-ter per year. That may not seem like much, but at that rate it will rise one kilometer in the next two million years--a brief period in geologic time.
Its composition is another reason that Denali has grown to such a great height. It is mainly igneous rock granite. Denali’s granite formed below the Earth’s crust as part of a batholith. A batholith is a bubble or mass of magma within Earth’s crust. Plutons are parts of batholiths, defined by their chemical com-position. The chemical composition of the magma determines the type of rock that will crystallize. Other intrusive igneous rocks (rocks that cool within the crust rather than at the sur-face) include gabbro, diorite, and pegmatite. Granite usually happens to be less dense than much of the rock that surrounds it.
Over millions of years, a granitic pluton will float slowly towards Earth’s surface, as it has in the case of Denali. Denali sort of “popped” up to the surface, much like a cork held under water will pop up when released. Just remember that “popping up” can take millions of years! Erosion of Earth’s surface rocks also helped expose the granitic rocks that make up Denali.
Granite is also very resistant to erosion. The forces of erosion, that is water, ice and wind, have a hard time wearing De-nali’s rock away. The rock pushes up faster than it is eroded, so Denali continues to grow. Subduction, uplift, and the lack of erosion have all contributed to Denali’s great height.
Weathering and Eroson: Forces that Tear Down Mountains
Even as the uplift of the Alaska Range continues, weathering and erosion are constantly working to tear it down. Weather and water, in the form of wind, rain, frost, streams, rivers and glaciers, have the power to turn mountains into molehills.
In brief, weathering crumbles rocks and minerals apart into smaller pieces. Erosion carries these pieces away by water, wind, glaciers, and gravity, often transporting the pieces for long distances. In Denali, ice is the predominant mechanism of erosion.
A Land Sculpted By Ice
In the high, frozen regions of the Alaska Range, snow and ice are the main forms of precipitation. In the past, most of the snow and ice remained behind; very little melting occurred. Snow and ice accumulated and got deeper and deeper, year after year, until the mass of ice that formed was so thick it compressed under its own weight. Gravity caused this ice to flow through stream valleys as glaciers. Glaciers are rivers of ice. The glaciers we see today in the park are increasingly small remnants of their former selves, but all around us we can see evidence of how they dominated the landscape. Dur-ing past ice ages, most recently about 10,000 years ago, glaciers covered the Alaska Range and much of Alaska in ice. All of south-central Alaska has been buried in ice numerous times, and the shape of the land in this area comes from the carving forces of glaciers and the debris they leave behind.
Glaciers are often fed by more snow and ice precipitating and accumulating at higher elevations. If ice builds up at its source, a glacier may flow at rates ranging from several feet per year to several feet per day. As a glacier flows downhill, it grinds away at its beds with tremendous force. It picks up rocks from its bed, grinding some to a fine powder called silt and by plucking up larger chunks. When the glacial ice melts, the silt is carried along in the meltwater to be deposited downstream as outwash. Streams flowing from melting glaciers are often milky-colored. The silt in the water is called glacial flour, and the silty water is described as glacial milk. The larger chunks get left behind as erratics or in unsorted deposits forming ridges or hills called moraines.
Erratics are rocks that are foreign to the surrounding terrain. They differ from the types of rock found where they are deposited.
The rocks embedded in glacial ice grind away at bedrock, forming the jagged ridges and deep U-shaped valleys found in the range. Large blocks of ice can be stranded in the moraines left behind by retreat-ing glaciers. When they finally melt, a water-filled depression known as a kettle lake develops. The carving action of ice forms many of the elongated lakes in the upper Susitna Valley to the south of Denali, and examination of a map reveals that they are all oriented in the direction that the ice was moving.
Acknowledgements and Contacts
This document exists thanks to the support of the Geological Society of America and GeoCorps America.
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Last updated: September 1, 2015