Fossil Forests of the Yellowstone National Park — Story, Setting & Ideas

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Knowlton, Frank Hall, 1860-1926 Project Gutenberg 2020 Not confirmed
Petrified forests; Paleobotany -- Yellowstone National Park; Trees, Fossil -- Yellowstone National Park Readers of public-domain and historical texts
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Words 10,584
Reading time 47 min
Text sections 2

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Knowlton's 1928 monograph examines Yellowstone's petrified forests through microscopic wood anatomy, identifying ten fossil species and explaining how volcanic eruptions preserved successive forest layers. The text balances scientific description with accessible explanations of growth rings, resin ducts, and medullary rays.
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UNITED STATES DEPARTMENT OF THE INTERIOR HUBERT WORK, SECRETARY

NATIONAL PARK SERVICE STEPHEN T. MATHER, DIRECTOR

FOSSIL FORESTS OF THE YELLOWSTONE NATIONAL PARK

UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON 1928

THE NATIONAL PARKS AT A GLANCE.

[Number, 19; total area, 11,817 square miles.]

National parks Location. Area in Distinctive characteristics. in order of square creation. miles.

Hot Springs Middle 1½ 46 hot springs possessing 1832 Arkansas. curative properties—Many hotels and boarding houses—20 bath-houses under public control. Yellowstone Northwestern 3,348 More geysers than in all rest 1872 Wyoming. of world together—Boiling springs—Mud volcanoes—Petrified forests—Grand Canyon of the Yellowstone, remarkable for gorgeous coloring—Large lakes—Many large streams and waterfalls—Vast wilderness, greatest wild bird and animal preserve in world—Exceptional trout fishing. Sequoia Middle 604 The Big Tree National 1890 eastern Park—Scores of sequoia trees 20 California. to 30 feet in diameter, thousands over 10 feet in diameter—Towering mountain ranges—Mount Whitney, highest peak in continental United States—Startling precipices—Cave of considerable size. Yosemite Middle 1,125 Valley of world-famed 1890 eastern beauty—Lofty cliffs—Romantic California. vistas—Many waterfalls of extraordinary height—3 groves of big trees—High Sierra—Waterwheel falls—Good trout fishing. General Grant Middle 4 Created to preserve the 1890 eastern celebrated General Grant Tree, California. 35 feet in diameter—6 miles from Sequoia National Park. Mount Rainier West central 325 Largest accessible single peak 1890 Washington. glacier system—28 glaciers, some of large size—48 square miles of glacier, 50 to 500 feet thick—Wonderful sub-alpine wild-flower fields. Crater Lake Southwestern 249 Lake of extraordinary blue in 1902 Oregon. crater of extinct volcano—Sides 1,000 feet high—Interesting lava formations—Fine fishing. Wind Cave South Dakota. 17 Cavern having many miles of 1903 galleries and numerous chambers containing peculiar formations. Platt Southern 1⅓ Many sulphur and other springs 1901 Oklahoma. possessing medicinal value. Sullys Hill North Dakota. 1⅕ Small park with woods, streams, 1904 and a lake—Is an important wild-animal preserve. Mesa Verde Southwestern 77 Most notable and best preserved 1906 Colorado. prehistoric cliff dwellings in United States, if not in the world. Glacier Northwestern 1,534 Rugged mountain region of 1910 Montana. unsurpassed Alpine character—250 glacier-fed lakes of romantic beauty—60 small glaciers—Precipices thousands of feet deep—Almost sensational scenery of marked individuality—Fine trout fishing. Rocky Mountain North middle 378 Heart of the Rockies—Snowy 1915 Colorado. range, peaks 11,000 to 14,250 feet altitude—Remarkable records of glacial period. Hawaii Hawaii. 242 Three separate areas—Kilauea 1916 and Mauna Loa on Hawaii, Haleakala on Maui. Lassen Volcanic Northern 124 Only active volcano in United 1916 California. States proper—Lassen Peak, 10,465 feet—Cinder Cone, 6,879 feet—Hot springs—Mud geysers. Mount McKinley South 2,645 Highest mountain in North 1917 central America—Rises higher above Alaska. surrounding country than any other mountain in the world. Grand Canyon North 1,009 The greatest example of erosion 1919 central and the most sublime spectacle Arizona. in the world. Lafayette Maine coast. 12 The group of granite mountains 1919 upon Mount Desert Island. Zion Southwestern 120 Magnificent gorge (Zion 1919 Utah. Canyon), depth from 1,500 to 2,500 feet, with precipitous walls—Of great beauty and scenic interest.

THE FOSSIL FORESTS OF THE YELLOWSTONE NATIONAL PARK.

By F. H. Knowlton, _United States Geological Survey._

The opening pages of Knowlton's monograph immediately establish its dual identity: a government-park-service bulletin and a technical paleobotanical report. The table of national parks, with Yellowstone's entry noting 'Petrified forests' among its features, frames the fossil forests as one attraction among many. Yet Knowlton quickly narrows focus, moving from park overview to microscopic wood anatomy. The first excerpt shows him describing thin sections of fossil redwood (Sequoia magnifica) at 100 diameters magnification, explaining how growth rings record seasonal moisture availability. This shift from scenic wonder to cellular detail sets the tone for the entire work.

From Park Brochure to Laboratory Report

The monograph's opening pages serve as a gateway between two readerships. The National Park Service table lists Yellowstone's area as 3,348 square miles and mentions 'Petrified forests' alongside geysers and the Grand Canyon. But Knowlton, a professional paleobotanist, quickly leaves the tourist's perspective behind. By the second excerpt, he is describing transverse sections of Pityoxylon amethystinum at 100 diameters, noting resin ducts filled with 'pitch.' The reader must adjust from expecting scenic description to following technical wood anatomy. Knowlton aids this transition by defining terms as he goes: medullary rays are 'little plates of cells that connect pith and bark.' The shift is deliberate—the fossil forests are not just curiosities but subjects for scientific investigation.

Reading the Evidence in Wood Cells

Knowlton's method relies on microscopic examination of thin sections. He presents four figures (12–15) showing transverse, tangential, and longitudinal cuts of fossil woods. Each reveals different structures: growth rings, resin ducts, medullary rays, and vessels. The descriptions are precise: in Pityoxylon amethystinum, growth rings are so broad that 'it is impossible to show a complete one.' In the laurel (Laurinoxylon pulchrum), wood cells are 'relatively much smaller and shorter,' and medullary rays appear in 'several irregular rows.' Knowlton uses these comparisons to distinguish coniferous from deciduous wood. The reader learns to see the fossils not as stone logs but as preserved cellular architecture, where each feature—a resin duct, a ray, a vessel—carries information about the living tree.

Ten Species from Thin Slices

After detailing the microscopic criteria, Knowlton enumerates the species identified: three conifers (including Sequoia magnifica and two pines) and seven dicotyledons (laurel, aromatic bay, sycamores, buckthorn, oaks). He notes that conifers make up 'fully 95 per cent of all the trunks,' attributing this to their original abundance and slower decay. The list is presented as a straightforward catalog, but it implies a larger story: the fossil forests preserve a mixed woodland, dominated by redwood and pine, with scattered hardwoods. Knowlton does not speculate on climate or ecology beyond noting favorable preservation conditions. The reader is left to infer that these ten species represent only a fraction of the original forest, filtered through the biases of preservation and discovery.

What the Excerpts Leave Unseen

The provided excerpts cover only the opening and a portion of the species discussion. Missing are Knowlton's explanations of how the forests were buried by volcanic eruptions, the stratigraphy of multiple fossil layers, and the geological history that created the park's petrified trees. The excerpts also omit any illustrations beyond the figure captions. Readers should expect the full text to expand on the processes of petrification and the sequence of eruptions that preserved successive forests. Knowlton's tone remains factual throughout the excerpts, but the incomplete record means the broader narrative—how these trees grew, died, and became stone—must be pieced together from the full monograph.

Knowlton's monograph rewards a patient reader willing to follow technical descriptions of wood anatomy. The excerpts show a scientist at work, building identifications from thin sections and growth rings. To get the most from this text, read the figure captions carefully—they carry essential observations. And remember that the fossil forests are not a single petrified grove but a series of buried woodlands, each layer telling a different chapter of Yellowstone's volcanic past.

Reading about Yellowstone’s petrified rings, I remembered a girlhood summer tracing the veins of an oak leaf, puzzling over its intricate skeleton. That patient ache to understand something old and silent returned in Knowlton's pages, much like it did years ago with Wayside and woodland trees — Reading Companion. Both books felt like quiet conversations with the living past.

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