Earth Blocks: Modeling Geologic Events One Layer at a Time
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Absolute Time Radiometric Dating: the Source of the Dates on the Geologic Time Scale
Absolute Time Radiometric Dating: the source of the dates on the Geologic Time Scale Radiometric Dating • Actually a simple technique. • Only two measurements are needed: • 1. The parent:daughter ratio measured with a mass spectrometer. • 2. The decay constant measured by a scintillometer. Basis of the Technique • Radioactive elements “decay.” Decay occurs as an element changes to another element, e.g. uranium to lead. • The parent element is radioactive, the daughter element is stable. • The decay rate is constant. What is Radioactivity? • Radioactivity occurs when certain elements literally fall apart. • Usually protons and neutrons are emitted by the nucleus. • Sometimes an electron is emitted by the nucleus, which changes a neutron to a proton. • Sometimes an electron is captured. What causes radioactivity? • Carbon-14 is produced by cosmic ray bombardment of Nitrogen-14 in the atmosphere. • All other radioactive elements were produced by supernova explosions before our solar system formed. This is called explosive nucleosynthesis. Common Radioactive Elements, Parents and Daughters • Carbon-14, C14 Nitrogen-14, N14 • Uranium-235, U235 Lead-207, Pb207 • Potassium-40, K40 Argon-40, Ar40 • Uranium-238, U238 Lead-206, Pb206 • Rubidium-87, Rb87 Strontium-87, Sr87 Basis of the Technique • As the parent element decays, its amount decreases while the amount of the daughter element increases. This gives us a ratio of parent:daughter elements. • The decay rate is geometric rather than linear. Unaffected by heat or pressure. Key Term • Half-Life: the amount of time for half the atoms of a radioactive element to decay. Doesn’t matter how many atoms started, half will decay. -
Lithologic Description Checklist
GY480 Field Geology Lithologic Description Checklist When describing outcrops you should attempt to determine the following at the exposure: 1. Rock name and/or Formation name (Granite, Cap Mt. Limestone member, etc.) 2. Color or color variations at outcrop (pink granite, vari-colored shale, etc.) 3. Mineralogy (estimate percentages if possible; try to distinguish between primary and secondary minerals) 4. texture: size, shape and arrangement of mineral grains (aphanitic, rhyolite porphyry, idioblastic, porphyroblastic, grain-supported, coarse sandstone, foliated granite, etc.). 5. Primary features: crossbeds, ripple marks, sole marks, igneous flow foliation, pillow basalt, vesicular basalt, etc.) Examples of well-written descriptions Sandstone (quartz arenite): white and very pale orange, weathers light brown and moderate reddish brown; very fine grained; subangular; well-sorted; laminated; locally cross-bedded; bedding thickness as much as a foot (30 cm), mostly covered with rubble; forms steep, rounded slope. Bolsa Quartzite. Granite, light gray or light pink, usually deeply weathered to light brown. Typically coarse- grained, containing large phenocrysts of pale-pink orthoclase up to 3 inches (7.6 cm) long. Coarse-grained groundmass consists of pale-pink orthoclase, chalky plagioclase (albite or andesine), quartz, and books of black biotite. Probably underlies diabase and sedimentary formations in most of the region. Ruin Granite. Schist, light to dark gray, weathers brown to greenish-brown. Comprised of a variety of types from coarse-grained quartz-sericite schist to fine-grained quartz-sericite-chlorite schist. Low- grade metamorphism greenschist facies; higher-grade occurs locally. Relict bedding of sedimentary protolith is generally recognizable in outcrop; plunging overturned tight to isoclinal folding is pervasive. -
Chapter 8. Weathering, Sediment, & Soil
Physical Geology, First University of Saskatchewan Edition is used under a CC BY-NC-SA 4.0 International License Read this book online at http://openpress.usask.ca/physicalgeology/ Chapter 8. Weathering, Sediment, & Soil Adapted by Karla Panchuk from Physical Geology by Steven Earle Figure 8.1 The Hoodoos, near Drumheller, Alberta, have formed from the differential weathering (weaker rock weathering faster than stronger rock) of sedimentary rock. Source: Steven Earle (2015) CC BY 4.0. Learning Objectives After reading this chapter and answering the review questions at the end, you should be able to: • Explain why rocks formed at depth in the crust are susceptible to weathering at the surface. • Describe the main processes of mechanical weathering, and the materials that are produced. • Describe the main processes of chemical weathering, and common chemical weathering products. • Explain the characteristics used to describe sediments, and what those characteristics can tell us about the origins of the sediments. • Discuss the relationships between weathering and soil formation, and the origins of soil horizons. • Describe and explain the distribution of Canadian soil types. • Explain how changing weathering rates affect the carbon cycle and the climate system. Chapter 8. Weathering, Sediment, & Soil 1 What Is Weathering? Weathering occurs when rock is exposed to the “weather” — to the forces and conditions that exist at Earth’s surface. Rocks that form deep within Earth experience relatively constant temperature, high pressure, have no contact with the atmosphere, and little or no interaction with moving water. Once overlying layers are eroded away and a rock is exposed at the surface, conditions change dramatically. -
Scientific Dating in Archaeology
SCIENTIFIC DATING IN ARCHAEOLOGY Tsuneto Nagatomo 1. AGE DETERMINATION IN ARCHAEOLOGY • Relative Age: stratigraphy, typology • Absolute Chronology: historical data • Age Determination by (natural) Scientific Methods: Numerical age (or chronometric age) Relative age 2. AGE DETERMINATION BY SCIENTIFIC METHODS 2-1. Numerical Methods • Radiometric Dating Methods Radioactive Isotope: radiocarbon, potassium-argon, argon-argon, uranium series Radiation Damage: fission track, luminescence, electron spin resonance • Non-Radiometric Dating Methods Chemical Change: amino acid, obsidian hydration 2-2. Relative Methods • Archaeomagnetism & palaeomagnetism, dendrochronology, fluorite 3. RADIOMETRIC METHODS 3-1. Radioactive Isotopes The dating clock is directly provided by radioactive decay: e.g. radiocarbon, potassium-argon, and the uranium-series. The number of a nuclide (Nt) at a certain time (t) decreases by decaying into its daughter nuclide. The number of a nuclide (dN) that decays within a short time (dt) is proportional to the total number of the nuclide at time (t) (Nt): d Nt /dt = -λNt (1) where λ: decay constant. Then, Nt is derived from (1) as Nt = N0 exp(-0.693t/T1/2) (2) …Where N0 is the number of the isotope at t = 0 and T1/2 is its half-life. Thus, the equation from this is: t = (T1/2/0.693)exp(N0/Nt) When the values of T1/2 and N0 are known, we get t by evaluating the value Nt. The radiocarbon technique is the typical one in which the decrease of the parent nuclide is the measure of dating. On the other hand, the decrease of the parent nuclide and increase of the daughter nuclide, or their ratio, is the measure of dating in potassium-argon and the uranium-series. -
Dating Techniques.Pdf
Dating Techniques Dating techniques in the Quaternary time range fall into three broad categories: • Methods that provide age estimates. • Methods that establish age-equivalence. • Relative age methods. 1 Dating Techniques Age Estimates: Radiometric dating techniques Are methods based in the radioactive properties of certain unstable chemical elements, from which atomic particles are emitted in order to achieve a more stable atomic form. 2 Dating Techniques Age Estimates: Radiometric dating techniques Application of the principle of radioactivity to geological dating requires that certain fundamental conditions be met. If an event is associated with the incorporation of a radioactive nuclide, then providing: (a) that none of the daughter nuclides are present in the initial stages and, (b) that none of the daughter nuclides are added to or lost from the materials to be dated, then the estimates of the age of that event can be obtained if the ration between parent and daughter nuclides can be established, and if the decay rate is known. 3 Dating Techniques Age Estimates: Radiometric dating techniques - Uranium-series dating 238Uranium, 235Uranium and 232Thorium all decay to stable lead isotopes through complex decay series of intermediate nuclides with widely differing half- lives. 4 Dating Techniques Age Estimates: Radiometric dating techniques - Uranium-series dating • Bone • Speleothems • Lacustrine deposits • Peat • Coral 5 Dating Techniques Age Estimates: Radiometric dating techniques - Thermoluminescence (TL) Electrons can be freed by heating and emit a characteristic emission of light which is proportional to the number of electrons trapped within the crystal lattice. Termed thermoluminescence. 6 Dating Techniques Age Estimates: Radiometric dating techniques - Thermoluminescence (TL) Applications: • archeological sample, especially pottery. -
Isotope Geochemistry I Lectures & Exercises
Tools and methods Geochronology Methods relying on the decay of naturally occurring radiogenic isotopes: Parent isotope Daughter isotope 1. Potassium-40 -> Argon-40 2. Rubidium-87 -> Strontium-87 3. Uranium-235 -> Lead-207 4. Uranium-238 -> Lead-206 5. Thorium-232 -> Lead-208 Radioactivity Natural and artificial radioactivity Natural radioactivity Isotopes that have been here since the earth formed: 238U, 235U, 232Th, 40K Isotopes produced by cosmic rays from the sun, i.e cosmogenic radionuclides: 14C, 10Be, 36Cl Synthetic radioisotopes Made in nuclear reactors when atoms are split (fission). Produced usinc cyclotrons, linear accererators... 39 39 K (n, p) Ar 19 18 The dawn of radiometric dating “U-Pb” method • Boltwood studied radioactive elements and found that Pb was always present in uranium and thorium ores. Pb must be the final product of the radioactive decay. • In 1907, he reasoned that since he knew the rate at which uranium breaks down (its half-life), he could use the proportion of lead in the uranium ores (chemical dating, isotopes not discovered yet) as a meter or clock. • His observations and calculations put Earth's age at 2.2 billion years. He accumulation method • Based on the fact that 235U, 238U and 232Th emit 7, 8 and 6 α-particles, resp. in their decay to Pb • U and Th concentration can be determined chemically and the current rate of He production can be calculated • The sample is heated to release He and the helium-retention age is calculated Radioactive decay half-lifes, T1/2 • if it is possible to determine the -
Datin History of Rock Chronometric/Radiometric G
Ed Planansky, Hay Springs, NE © 2008 DATIN HISTORY OF ROCK CHRONOMETRIC/RADIOMETRIC G Educational Objective: To help students become aware of dating techniques used to date very ancient (millions of years) to relatively recent (tens of thousands of years) events in geologic time. Target Audience: Any science or math class with adaptations for age groups and class setting. Questions To Be Answered: 1. What is the half-life of a radioactive isotope? 2. How can the half life of an isotope be used to date anything? 3. Which isotope dating method is most likely to give the most accurate dating of a sediment or specimen? 4. Given a hypothetical amount of material present in a sample compared to the amount that was present at formation be able to date events or sediments. HALF-LIFE Following World War I and the invention of a device called a mass spectrometer more than 200 isotopes of the 92 naturally occurring elements were found. Isotopes are atoms of elements that have the same atomic number but different atomic masses, they are the same element but have different weights because of different numbers of neutrons in the nucleus of the atom. Because the isotopes are essentially the same element they have the same chemical properties but have different physical properties. For the purposes of dating geologic times the property we are concerned with is radioactive decay. Each radioactive isotope decays, by emitting alpha or beta particles and becoming a new element many of which are stable and no longer decay. The time it takes for half of a sample to decay into new material(s) is called its half-life. -
ROCK OUTCROP SYSTEM Ros12 Southern Floristic Region Southern Bedrock Outcrop Dry, Open Lichen-Dominated Plant Communities on Areas of Exposed Bedrock
ROCK OUTCROP SYSTEM ROs12 Southern Floristic Region Southern Bedrock Outcrop Dry, open lichen-dominated plant communities on areas of exposed bedrock. Woody vegetation is sparse, and vascular plants are restricted to crevices, shallow soil deposits, and rainwater pools. Vegetation Structure & Composition Description is based on summary of vegetation plot data (relevés), plant species lists, and field notes from surveys of approximately 50 bedrock outcrops. • Lichen and bryophyte cover is high. On exposed bedrock, crustose and foliose lichens predominate. Species include Can- delariella vitellina, Lecanora muralis, Rhi- zocarpon disporum, Dimelaena oreina, Xanthoparmelia cumberlandia, Xanthopar- melia plittii, Acarospora americana, Physcia subtilis, and Dermatocarpon miniatum. On bedrock margins and along crevices, fruti- cose species such as Cladonia pyxidata are present with the more abundant crustose and foliose species. Common bryophytes on exposed rock include Schistidium and Grim- mia species, and, along crevices, Ceratodon purpureus, Weissia controversa, and Tortula species. Mosses often form carpets in shallow rainwater-collecting bedrock hollows. • Herbaceous plant cover is sparse to patchy (5–50%); characteristic species in crevices and areas with shallow soil (< 1in [3cm] deep), where plant biomass is low, include small-flowered fameflower (Talinum parviflorum), brittle prickly pear (Opuntia fragilis), rock spikemoss (Selaginella rupestris), rusty woodsia (Woodsia ilvensis), false pennyroyal (Isanthus brachiatus), slender knotweed -
Chapter 9 Generally Have Cold Ocean Currents Flowing from the Checkpoint 9.1 Examine the Photos
Geog 106LRS - Prof. Fischer Name ______Answer Key__ Chapter 9 generally have cold ocean currents flowing from the Checkpoint 9.1 Examine the photos. Both images poles toward the equator, of which the California show granite outcrops in the Sierra Nevada current is an example. Much of California is made of Mountains, California. Which outcrop contains accreted terranes from subduction zones that have pressure release cracks? Explain your existed along the coast over the last 200 million years choice. or so. a) Outcrop A b) Outcrop B Checkpoint 9.6 Weathering Analogies Matrix Many simple occurrences in our daily lives are Pressure release joints result in onion-skin-like similar to geologic processes. The following table exfoliation. contains some everyday events that you may have experienced. Match these actions to specific Checkpoint 9.2 Outcrops of granite are examined weathering processes. Complete the table by placing in California at similar elevations in the interior of the an “X” in the columns on the right-hand side where state more than 100 kilometers (63 miles) from the appropriate. For each characteristic in the Pacific Ocean and in outcrops along the coast. The left-hand column write in whether it is analogous granites have identical compositions and textures. On (similar) to physical, chemical, or biological the basis of the following information, which granite weathering. outcrop would weather most rapidly? Characteristic a) Outcrop A; located at coast, contains fractures Paint on house gradually disappears __________C spaced -
A Walk Back in Time the Ruth Canstein Yablonsky Self-Guided Geology Trail
The cross section below shows the rocks of the Watchung Reservation and surrounding area, revealing the relative positions of the lava flows that erupted in this region and the sedimentary rock layers between them. A Walk Back in Time The Ruth Canstein Yablonsky Self-Guided Geology Trail click here to view on a smart phone NOTES Trailside Nature & Science Center 452 New Providence Road, Mountainside, NJ A SERVICE OF THE UNION COUNTY BOARD OF UNION COUNTY (908) 789-3670 CHOSEN FREEHOLDERS We’re Connected to You! The Ruth Canstein Yablonsky Glossary basalt a fine-grained, dark-colored Mesozoic a span of geologic time from Self-Guided Geology Trail igneous rock. approximately 225 million years ago to 71 million years This booklet will act as a guide for a short hike to interpret the geological history bedrock solid rock found in the same area as it was formed. ago, and divided into of the Watchung Reservation. The trail is about one mile long, and all the stops smaller units called Triassic, described in this booklet are marked with corresponding numbers on the trail. beds layers of sedimentary rock. Jurassic and Cretaceous. conglomerate sedimentary rock made of oxidation a chemical reaction “Watchung” is a Lenape word meaning “high hill”. The Watchung Mountains have an rounded pebbles cemented combining with oxygen. elevation of about 600 feet above sea level. As you travel southeast, these high hills are the together by a mineral last rise before the gently rolling lowland that extends from Rt. 22 through appropriately substance (matrix) . Pangaea supercontinent that broke named towns like Westfield and Plainfield to the Jersey shore. -
Global Geologic Maps Are Tectonic Speedometers— Rates of Rock Cycling from Area-Age Frequencies
Global geologic maps are tectonic speedometers— Rates of rock cycling from area-age frequencies Bruce H. Wilkinson1†, Brandon J. McElroy2, Stephen E. Kesler3, Shanan E. Peters4, and Edward D. Rothman3 1Department of Earth Sciences, Syracuse University, Syracuse, New York 13244, USA 2Department of Geological Sciences, Jackson School of Geosciences, University of Texas, Austin, Texas 78712, USA 3Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA 4Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706, USA ABSTRACT the Earth’s surface, age-frequency distribu- lion years suggested by map age-frequencies tions for plutonic and metamorphic rocks are the same as would be anticipated on the Relations among ages and present areas of exhibit lognormal relations, with modes at basis of hundreds of published rates of ero- exposure of volcanic, sedimentary, plutonic, ca. 154 and 697 Ma, respectively. A dearth sional uplift and exhumation determined by and metamorphic rock units (lithosomes) of younger exposures of plutonic and meta- more conventional geochronometers. This record a complex interplay between depths morphic rocks refl ects the fact that these agreement suggests that geologic maps serve and rates of formation, rates of subsequent rock types form at depth, and some duration as effective deep-time speedometers for the tectonic subsidence and burial, and/or rates of tectonism is therefore required for their geologic rock cycle. of uplift and erosion. Thus, they potentially exposure. Increasing modal ages, from Qua- serve as effi cient deep-time geologic speed- ternary for volcanic and sedimentary succes- INTRODUCTION ometers, providing quantitative insight into sions, to early Mesozoic for intrusive rocks, rates of material transfer among the principal to Neoproterozoic for metamorphic rocks, Since the fi rst complete geologic map of Eng- rock reservoirs—processes central to the rock demonstrate that greater amounts of geologic land, Wales, and Scotland was scribed and pub- cycle. -
Magnetic Minerals As Recorders of Weathering, Diagenesis, And
Earth and Planetary Science Letters 452 (2016) 15–26 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Magnetic minerals as recorders of weathering, diagenesis, and paleoclimate: A core–outcrop comparison of Paleocene–Eocene paleosols in the Bighorn Basin, WY, USA ∗ Daniel P. Maxbauer a,b, , Joshua M. Feinberg a,b, David L. Fox b, William C. Clyde c a Institute for Rock Magnetism, University of Minnesota, Minneapolis, MN, USA b Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA c Department of Earth Sciences, University of New Hampshire, Durham, NH, USA a r t i c l e i n f o a b s t r a c t Article history: Magnetic minerals in paleosols hold important clues to the environmental conditions in which the Received 17 February 2016 original soil formed. However, efforts to quantify parameters such as mean annual precipitation (MAP) Received in revised form 15 July 2016 using magnetic properties are still in their infancy. Here, we test the idea that diagenetic processes and Accepted 17 July 2016 surficial weathering affect the magnetic minerals preserved in paleosols, particularly in pre-Quaternary Available online 4 August 2016 systems that have received far less attention compared to more recent soils and paleosols. We evaluate Editor: H. Stoll the magnetic properties of non-loessic paleosols across the Paleocene–Eocene Thermal Maximum (a Keywords: short-term global warming episode that occurred at 55.5 Ma) in the Bighorn Basin, WY. We compare weathering data from nine paleosol layers sampled from outcrop, each of which has been exposed to surficial diagenesis weathering, to the equivalent paleosols sampled from drill core, all of which are preserved below environmental magnetism a pervasive surficial weathering front and are presumed to be unweathered.