Bedrock Geology


However, this geologic record is disrupted by several prolonged gaps of time, called unconformities, when no rocks formed or when rocks that formed during an earlier time were later eroded away. Figure 1 below shows a representation of geologic time intervals, from the Earth's beginning at about 4.6 billion years ago to present day. The areas shaded in gray portray the age of the major bedrock units found in Minnesota, while the white areas represent unconformities, the time intervals missing from Minnesota's geologic record. Only a small percentage of geologic time is preserved in the bedrock geology of Minnesota.

Geologic time scale. The gray areas represent the age of rocks present in Minnesota.
Figure 1. Geologic time scale. Areas shaded in gray portray the age of the major rock units found in Minnesota. The white areas represent unconformities, the time intervals missing from Minnesota's geologic record. The three main portions of bedrock geologic time in Minnesota are highlighted in red: Precambrian, Paleozoic, and Mesozoic (modified from Southwick and Lusardi, 1997, fig. 5).

Overall, the bedrock geology of Minnesota can be subdivided into three general categories based on geologic time. From oldest to youngest, these categories are the Precambrian, Paleozoic, and Mesozoic (highlighted in red on the geologic time scale in Figure 1).

Sources:
(1) Morey, G.B., and Dahlberg, H., 1995, Geology of Minnesota: A Guide for Teachers: State of Minnesota, Department of Natural Resources, Fifth Printing, 34 p.
(2) Southwick, D.L., and Lusardi, B.A., 1997, Minnesota at a Glance: Geologic Time: Minnesota Geological Survey. Revised June, 2017 by E.L. Dengler.


Precambrian Geology

Have you ever admired the cliffs along the North Shore of Lake Superior, fished off a smooth outcrop in the Boundary Waters Canoe Area, overlooked one of the immense iron mines on the Mesabi range, or noticed the abundant knobby outcrops within the Minnesota River Valley (Figs. 2, 3, 4 and 5)? If so, you were looking through windows of younger material into the very old bedrock, commonly referred to as "ledge-rock", that underlies all of Minnesota. Minnesota is situated at the southern edge of the Canadian Shield—the nucleus of the continent of North America that formed during Precambrian time. This period of time encompasses about 88% of Earth's history. Geologists consider Precambrian time to have begun with the formation of planet Earth about 4,600 million years ago and to have ended about 541 million years ago, when organisms with hard parts, such as shells, first appeared. The rocks formed in Minnesota during this enormous span of time record a complicated geologic history that involved volcanoes, ocean islands, mountain chains, and unstable geologic conditions that were very different from the Minnesota of today.

View along the North Shore of the Split Rock Lighthouse built atop a cliff of Precambrian volcanic rocks.
Photo credit
Andrew J. Retzler
Figure 2. View along the North Shore of the Split Rock Lighthouse built atop an intrusion of Precambrian anorthosite.
An iron mine along the Mesabi Iron Range.
Photo credit
Mark A. Jirsa
Figure 3. An iron mine along the Mesabi Iron Range.
Precambrian bedrock outcrop along Snowbank Lake in the Boundary Waters Canoe Area Wilderness.
Photo credit
Mark A. Jirsa
Figure 4. Precambrian bedrock outcrop along Snowbank Lake in the Boundary Waters Canoe Area Wilderness.
Knobby Sioux Quartzite outcrop near the Minnesota River Valley region.
Photo credit
Mark A. Jirsa
Figure 5. Knobby Sioux Quartzite outcrop near the Minnesota River Valley region.

The mountains and other features of the various Precambrian landscapes were slowly eroded to low relief over many millions of years. Most of the Precambrian rocks now exposed in Minnesota's flat terrain originally were much deeper in the earth; they record processes and conditions that existed beneath landscapes long since removed by erosion. Geologists can reconstruct the conditions that existed within the ancient Precambrian crust of the Earth through studies of these formerly deep-seated rocks now exposed at the surface. Presently, these deeply-eroded Precambrian rocks are mostly covered by younger sedimentary rocks, or by a thick blanket of glacially-deposited clay, sand, and gravel. However, they do appear at the surface here and there in northeastern, east-central, and southwestern Minnesota.

Collectively, Precambrian rocks of Minnesota encompass metamorphic, igneous, and sedimentary rocks. Examples include gneiss, greenstone, granite, graywacke, iron formation, schist, basalt, gabbro, and anorthosite. Even some of the oldest rocks in the world can be found in the Precambrian rocks of the Minnesota River valley—up to 3.5 billion years old!

Written by T.J. Boerboom, 1994, Minnesota at a Glance: Precambrian Geology: Minnesota Geological Survey; modified for web by A.J. Retzler, June 2020.


Paleozoic Geology

Imagine a sandy, tropical seashore extending across southern Minnesota—part of a vast, shallow sea that covers much of North America. The sandstone, shale and calcareous rock layers exposed across much of southeastern Minnesota (Figs. 6 and 7) are a geologic record of such conditions that existed hundreds of millions of years ago, during the Early Paleozoic.

Distribution of Paleozoic rocks in southeastern Minnesota. Time periods shown in italics are not represented by rocks in Minnesota.
Figure 6. Distribution of Paleozoic rocks in southeastern Minnesota. Line of cross section A-A' corresponds to Figure 2. Time periods shown in italics are not represented by rocks in Minnesota (modified from Runkel, 2000, fig. 1).
Schematic cross section of bedrock from west to east across southeastern Minnesota. The bedrock consists of sedimentary rock layers composed of sandstone, shale, and carbonate rocks such as limestone. Location of cross section is shown on Figure 1.
Figure 7. Schematic cross section of bedrock from west to east across southeastern Minnesota. The bedrock consists of sedimentary rock layers composed of sandstone, shale, and carbonate rocks such as limestone. Location of cross section is shown on Figure 1 (modified from Runkel, 2000, fig. 2). [Click image to see larger version]

Although many people are not aware of the geologic history of the Paleozoic bedrock in Minnesota, the rocks are familiar to anyone who has travelled in southeastern Minnesota. The bluffs along the St. Croix, Minnesota and Mississippi rivers, and their tributaries, are composed of layers of Paleozoic-aged rock such as the St. Peter Sandstone (Fig. 8) and the Prairie du Chien Group (Fig. 9). Paleozoic rocks lie beneath glacial deposits across much of southeastern Minnesota, from as far north as Taylors Falls, southwest to Mankato. They extend southward into Iowa and eastward into Wisconsin.

Outcrop of the St. Peter Sandstone (at base), Glenwood Shale (next unit above in section), and Platteville Limestone (top unit in section) along the Mississippi River bluff.
Photo credit
Andrew J. Retzler
Figure 8. Outcrop of the St. Peter Sandstone (at base), Glenwood Shale (next unit above in section), and Platteville Limestone (top unit in section) along the Mississippi River bluff.
Roadcut of Prairie du Chien Group dolostone east of the City of Oronoco in Olmsted County.
Photo credit
Andrew J. Retzler
Figure 9. Roadcut of Prairie du Chien Group dolostone east of the City of Oronoco in Olmsted County.

Paleozoic bedrock layers are sedimentary in origin. They are composed of particles of pre-existing rocks or minerals, or are precipitated by living organisms or chemical processes. Sedimentary rocks are deposited by the accumulation of these particles into layers, or beds. Small grains are dropped by wind or settle in water to form sandstone and shale. Elements such as calcium, magnesium, and iron, precipitate from seawater to form limestone or dolostone.

The next time you drive through southeastern Minnesota, take note of the varied rock formations exposed in the river bluffs and along the side of the road. Remember that these rocks record what the world was like hundreds of millions of years ago when a shallow tropical sea existed right here in Minnesota and across much of central North America.

Written by A.C. Runkel, 2000, Minnesota at a Glance: Ancient tropical seas - Paleozoic history of southeastern Minnesota: Minnesota Geological Survey; revised by A.C. Runkel, June 2002; modified for web by A.J. Retzler, June 2020.


Mesozoic Geology

Rocks of Mesozoic age in Minnesota tell the story of two major marine trangressions (or sea level rises): one during the Jurassic Period (roughly 200 million years ago) and one during the Cretaceous Period (roughly 100 million years ago).

The poorly understood Jurassic rocks are known only from drill core samples in the far northwestern corner of the state (Fig. 10). They include shale, limestone, dolostone, sandstone and siltstone possibly deposited within streams, lakes, and other marginal-marine environments as a sea over much of North Dakota and other western states slowly advanced eastward.

Statewide distribution of Mesozoic rocks in Minnesota.
Figure 10. Distribution of Mesozoic rocks in Minnesota.

The Cretaceous rocks form a nearly continuous blanket covering the Paleozoic and Precambrian rocks throughout the western half of Minnesota and numerous, small outliers in the eastern half of the state (Fig. 10). These rocks consist primarily of weathered residuum and overlying sedimentary rocks of conglomerate, sandstone, mudstone, shale, marl, and minor limestone. The residuum, which spans both the western and eastern half of the state, developed during a long period of weathering and erosion from sometime after the Middle Devonian (roughly 370 million years ago) to the Late Cretaceous (roughly 100 million years ago), after which the overlying sedimentary rocks were deposited.

The Cretaceous sedimentary rocks formed within a transitional marine and nonmarine environment along the eastern shoreline of a large inland sea, known as the Western Interior Seaway, that once split North America into two landmasses. Fossilized shark teeth, snails, clams, ammonites, fish bones and even crocodile parts are known from the marine and marginal-marine deposits in southwestern and northeastern Minnesota, while fossilized leaf impressions and pollen have been identified in some of the nonmarine deposits in the southeast (Fig. 11).

Cretaceous fossil ammonite from a core sample drilled in Rock County, Minnesota.
Figure 11. Cretaceous fossil ammonite from a core sample drilled in Rock County, Minnesota.

Sources:
(1) Webers, G.F. and Austin, G.S., 1972, Field trip guide book for Paleozoic and Mesozoic rocks of southeastern Minnesota: Minnesota Geological Survey Guidebook 4, 91 p.
(2) Sloan, R.E., 1964, The Cretaceous System in Minnesota: Minnesota Geological Survey Report of Investigations 5, 64 p.
(3) Setterholm, D.R., 1994, The Cretaceous rocks of southwestern Minnesota: Reconstructions of a marine to nonmarine transition along the eastern margin of the Western Interior Seaway, in Shurr, G.W., Ludvigson, G.A., and Hammond, R.H., eds., Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin: Boulder, Colorado, Geological Society of America Special Paper 287.
(4) Jirsa, M.A., Runkel, A.C., and Chandler, V.W., 1994, Bedrock geologic map of northwestern Minnesota: Minnesota Geological Survey Miscellaneous Map Series M-80, 1:250,000.


Featured Map

S-21 Geologic Map of Minnesota: Bedrock Geology


Click here to open the web map in a new window.

Above is the web map version of S-21 Geologic Map of Minnesota: Bedrock Geology published in 2011. It portrays our current geologic understanding of the temporal and geographic distribution of units within major Precambrian terranes and of the Phanerozoic strata (Paleozoic and Mesozoic bedrock). The western part of the mapped Precambrian terrane is inferred largely from geophysical maps, anchored locally by drilling. In many places, contacts are drawn between units of the same or similar apparent rock type (and same unit label); these are recognized as geometrically distinct, though geophysically or lithologically similar. Click here to download the publication version.