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Wednesday, March 23, 2022

Digital television

From Wikipedia, the free encyclopedia
 
A map depicting digital terrestrial television standards
 

Digital television (DTV) is the transmission of television signals using digital encoding, in contrast to the earlier analog television technology which used analog signals. At the time of its development it was considered an innovative advancement and represented the first significant evolution in television technology since color television in the 1950s. Modern digital television is transmitted in high-definition television (HDTV) with greater resolution than analog TV. It typically uses a widescreen aspect ratio (commonly 16:9) in contrast to the narrower format of analog TV. It makes more economical use of scarce radio spectrum space; it can transmit up to seven channels in the same bandwidth as a single analog channel, and provides many new features that analog television cannot. A transition from analog to digital broadcasting began around 2000. Different digital television broadcasting standards have been adopted in different parts of the world; below are the more widely used standards:

History

Background

Digital television's roots have been tied very closely to the availability of inexpensive, high performance computers. It was not until the 1990s that digital TV became a real possibility. Digital television was previously not practically feasible due to the impractically high bandwidth requirements of uncompressed digital video, requiring around 200 Mbit/s (25 MB/s) for a standard-definition television (SDTV) signal, and over 1 Gbit/s for high-definition television (HDTV).

Development

In the mid-1980s, Toshiba released a television set with digital capabilities, using integrated circuit chips such as a microprocessor to convert analog television broadcast signals to digital video signals, enabling features such as freezing pictures and showing two channels at once. In 1986, Sony and NEC Home Electronics announced their own similar TV sets with digital video capabilities. However, they still relied on analog TV broadcast signals, with true digital TV broadcasts not yet being available at the time.

A digital TV broadcast service was proposed in 1986 by Nippon Telegraph and Telephone (NTT) and the Ministry of Posts and Telecommunication (MPT) in Japan, where there were plans to develop an "Integrated Network System" service. However, it was not possible to practically implement such a digital TV service until the adoption of discrete cosine transform (DCT) video compression technology made it possible in the early 1990s.

In the mid-1980s, as Japanese consumer electronics firms forged ahead with the development of HDTV technology, and as the MUSE analog format was proposed by Japan's public broadcaster NHK as a worldwide standard, Japanese advancements were seen as pacesetters that threatened to eclipse U.S. electronics companies. Until June 1990, the Japanese MUSE standard—based on an analog system—was the front-runner among the more than 23 different technical concepts under consideration.

Between 1988 and 1991, several European organizations were working on DCT-based digital video coding standards for both SDTV and HDTV. The EU 256 project by the CMTT and ETSI, along with research by Italian broadcaster RAI, developed a DCT video codec that broadcast SDTV at 34 Mbit/s and near-studio-quality HDTV at about 70–140 Mbit/s. RAI demonstrated this with a 1990 FIFA World Cup broadcast in March 1990. An American company, General Instrument, also demonstrated the feasibility of a digital television signal in 1990. This led to the FCC being persuaded to delay its decision on an ATV standard until a digitally based standard could be developed.

In March 1990, when it became clear that a digital standard was feasible, the FCC made a number of critical decisions. First, the Commission declared that the new TV standard must be more than an enhanced analog signal, but be able to provide a genuine HDTV signal with at least twice the resolution of existing television images. Then, to ensure that viewers who did not wish to buy a new digital television set could continue to receive conventional television broadcasts, it dictated that the new ATV standard must be capable of being "simulcast" on different channels. The new ATV standard also allowed the new DTV signal to be based on entirely new design principles. Although incompatible with the existing NTSC standard, the new DTV standard would be able to incorporate many improvements.

The final standard adopted by the FCC did not require a single standard for scanning formats, aspect ratios, or lines of resolution. This outcome resulted from a dispute between the consumer electronics industry (joined by some broadcasters) and the computer industry (joined by the film industry and some public interest groups) over which of the two scanning processes—interlaced or progressive—is superior. Interlaced scanning, which is used in televisions worldwide, scans even-numbered lines first, then odd-numbered ones. Progressive scanning, which is the format used in computers, scans lines in sequences, from top to bottom. The computer industry argued that progressive scanning is superior because it does not "flicker" in the manner of interlaced scanning. It also argued that progressive scanning enables easier connections with the Internet, and is more cheaply converted to interlaced formats than vice versa. The film industry also supported progressive scanning because it offers a more efficient means of converting filmed programming into digital formats. For their part, the consumer electronics industry and broadcasters argued that interlaced scanning was the only technology that could transmit the highest quality pictures then (and currently) feasible, i.e., 1,080 lines per picture and 1,920 pixels per line. Broadcasters also favored interlaced scanning because their vast archive of interlaced programming is not readily compatible with a progressive format.

Inaugural launches

DirecTV in the U.S. launched the first commercial digital satellite platform in May 1994, using the Digital Satellite System (DSS) standard. Digital cable broadcasts were tested and launched in the U.S. in 1996 by TCI and Time Warner. The first digital terrestrial platform was launched in November 1998 as ONdigital in the United Kingdom, using the DVB-T standard.

Technical information

Formats and bandwidth

Comparison of image quality between ISDB-T (1080i broadcast, top) and NTSC (480i transmission, bottom)

Digital television supports many different picture formats defined by the broadcast television systems which are a combination of size and aspect ratio (width to height ratio).

With digital terrestrial television (DTT) broadcasting, the range of formats can be broadly divided into two categories: high-definition television (HDTV) for the transmission of high-definition video and standard-definition television (SDTV). These terms by themselves are not very precise, and many subtle intermediate cases exist.

One of several different HDTV formats that can be transmitted over DTV is: 1280 × 720 pixels in progressive scan mode (abbreviated 720p) or 1920 × 1080 pixels in interlaced video mode (1080i). Each of these uses a 16:9 aspect ratio. HDTV cannot be transmitted over analog television channels because of channel capacity issues.

SDTV, by comparison, may use one of several different formats taking the form of various aspect ratios depending on the technology used in the country of broadcast. In terms of rectangular pixels, NTSC countries can deliver a 640 × 480 resolution in 4:3 and 854 × 480 in 16:9, while PAL can give 768 × 576 in 4:3 and 1024 × 576 in 16:9. However, broadcasters may choose to reduce these resolutions to reduce bit rate (e.g., many DVB-T channels in the United Kingdom use a horizontal resolution of 544 or 704 pixels per line).

Each commercial broadcasting terrestrial television DTV channel in North America is permitted to be broadcast at a bit rate up to 19 megabits per second. However, the broadcaster does not need to use this entire bandwidth for just one broadcast channel. Instead the broadcast can use the channel to include PSIP and can also subdivide across several video subchannels (a.k.a. feeds) of varying quality and compression rates, including non-video datacasting services that allow one-way high-bit-rate streaming of data to computers like National Datacast.

A broadcaster may opt to use a standard-definition (SDTV) digital signal instead of an HDTV signal, because current convention allows the bandwidth of a DTV channel (or "multiplex") to be subdivided into multiple digital subchannels, (similar to what most FM radio stations offer with HD Radio), providing multiple feeds of entirely different television programming on the same channel. This ability to provide either a single HDTV feed or multiple lower-resolution feeds is often referred to as distributing one's "bit budget" or multicasting. This can sometimes be arranged automatically, using a statistical multiplexer (or "stat-mux"). With some implementations, image resolution may be less directly limited by bandwidth; for example in DVB-T, broadcasters can choose from several different modulation schemes, giving them the option to reduce the transmission bit rate and make reception easier for more distant or mobile viewers.

Receiving digital signal

There are several different ways to receive digital television. One of the oldest means of receiving DTV (and TV in general) is from terrestrial transmitters using an antenna (known as an aerial in some countries). This way is known as Digital terrestrial television (DTT). With DTT, viewers are limited to channels that have a terrestrial transmitter in range of their antenna.

Other ways have been devised to receive digital television. Among the most familiar to people are digital cable and digital satellite. In some countries where transmissions of TV signals are normally achieved by microwaves, digital MMDS is used. Other standards, such as Digital multimedia broadcasting (DMB) and DVB-H, have been devised to allow handheld devices such as mobile phones to receive TV signals. Another way is IPTV, that is receiving TV via Internet Protocol, relying on digital subscriber line (DSL) or optical cable line. Finally, an alternative way is to receive digital TV signals via the open Internet (Internet television), whether from a central streaming service or a P2P (peer-to-peer) system.

Some signals carry encryption and specify use conditions (such as "may not be recorded" or "may not be viewed on displays larger than 1 m in diagonal measure") backed up with the force of law under the World Intellectual Property Organization Copyright Treaty (WIPO Copyright Treaty) and national legislation implementing it, such as the U.S. Digital Millennium Copyright Act. Access to encrypted channels can be controlled by a removable smart card, for example via the Common Interface (DVB-CI) standard for Europe and via Point Of Deployment (POD) for IS or named differently CableCard.

Protection parameters for terrestrial DTV broadcasting

Digital television signals must not interfere with each other, and they must also coexist with analog television until it is phased out. The following table gives allowable signal-to-noise and signal-to-interference ratios for various interference scenarios. This table is a crucial regulatory tool for controlling the placement and power levels of stations. Digital TV is more tolerant of interference than analog TV, and this is the reason a smaller range of channels can carry an all-digital set of television stations.

System Parameters
(protection ratios)
Canada [13] USA [5] EBU [9, 12]
ITU-mode M3
Japan & Brazil [36, 37]
C/N for AWGN Channel +19.5 dB
(16.5 dB)
+15.19 dB +19.3 dB +19.2 dB
Co-Channel DTV into Analog TV +33.8 dB +34.44 dB +34 ~ 37 dB +38 dB
Co-Channel Analog TV into DTV +7.2 dB +1.81 dB +4 dB +4 dB
Co-Channel DTV into DTV +19.5 dB
(16.5 dB)
+15.27 dB +19 dB +19 dB
Lower Adjacent Channel DTV into Analog TV −16 dB −17.43 dB −5 ~ −11 dB −6 dB
Upper Adjacent Channel DTV into Analog TV −12 dB −11.95 dB −1 ~ −10 −5 dB
Lower Adjacent Channel Analog TV into DTV −48 dB −47.33 dB −34 ~ −37 dB −35 dB
Upper Adjacent Channel Analog TV into DTV −49 dB −48.71 dB −38 ~ −36 dB −37 dB
Lower Adjacent Channel DTV into DTV −27 dB −28 dB −30 dB −28 dB
Upper Adjacent Channel DTV into DTV −27 dB −26 dB −30 dB −29 dB

Interaction

People can interact with a DTV system in various ways. One can, for example, browse the electronic program guide. Modern DTV systems sometimes use a return path providing feedback from the end user to the broadcaster. This is possible with a coaxial or fiber optic cable, a dialup modem, or Internet connection but is not possible with a standard antenna.

Some of these systems support video on demand using a communication channel localized to a neighborhood rather than a city (terrestrial) or an even larger area (satellite).

1-segment broadcasting

1seg (1-segment) is a special form of ISDB. Each channel is further divided into 13 segments. The 12 segments of them are allocated for HDTV and remaining segment, the 13th, is used for narrow-band receivers such as mobile television or cell phone.

Timeline of transition

Comparison of analog vs digital

DTV has several advantages over analog TV, the most significant being that digital channels take up less bandwidth, and the bandwidth needs are continuously variable, at a corresponding reduction in image quality depending on the level of compression as well as the resolution of the transmitted image. This means that digital broadcasters can provide more digital channels in the same space, provide high-definition television service, or provide other non-television services such as multimedia or interactivity. DTV also permits special services such as multiplexing (more than one program on the same channel), electronic program guides and additional languages (spoken or subtitled). The sale of non-television services may provide an additional revenue source.

Digital and analog signals react to interference differently. For example, common problems with analog television include ghosting of images, noise from weak signals, and many other potential problems which degrade the quality of the image and sound, although the program material may still be watchable. With digital television, the audio and video must be synchronized digitally, so reception of the digital signal must be very nearly complete; otherwise, neither audio nor video will be usable. Short of this complete failure, "blocky" video is seen when the digital signal experiences interference.

Analog TV began with monophonic sound, and later developed multichannel television sound with two independent audio signal channels. DTV allows up to 5 audio signal channels plus a subwoofer bass channel, with broadcasts similar in quality to movie theaters and DVDs.

Digital TV signals require less transmission power than analog TV signals to be broadcast and received satisfactorily.

Compression artifacts, picture quality monitoring, and allocated bandwidth

DTV images have some picture defects that are not present on analog television or motion picture cinema, because of present-day limitations of bit rate and compression algorithms such as MPEG-2. This defect is sometimes referred to as "mosquito noise".

Because of the way the human visual system works, defects in an image that are localized to particular features of the image or that come and go are more perceptible than defects that are uniform and constant. However, the DTV system is designed to take advantage of other limitations of the human visual system to help mask these flaws, e.g. by allowing more compression artifacts during fast motion where the eye cannot track and resolve them as easily and, conversely, minimizing artifacts in still backgrounds that may be closely examined in a scene (since time allows).

Broadcast, cable, satellite, and Internet DTV operators control the picture quality of television signal encodes using sophisticated, neuroscience-based algorithms, such as the structural similarity (SSIM) video quality measurement tool, which was accorded each of its inventors a Primetime Emmy because of its global use. Another tool, called Visual Information Fidelity (VIF), is a top-performing algorithm at the core of the Netflix VMAF video quality monitoring system, which accounts for about 35% of all U.S. bandwidth consumption.

Effects of poor reception

Changes in signal reception from factors such as degrading antenna connections or changing weather conditions may gradually reduce the quality of analog TV. The nature of digital TV results in a perfectly decodable video initially, until the receiving equipment starts picking up interference that overpowers the desired signal or if the signal is too weak to decode. Some equipment will show a garbled picture with significant damage, while other devices may go directly from perfectly decodable video to no video at all or lock up. This phenomenon is known as the digital cliff effect.

Block error may occur when transmission is done with compressed images. A block error in a single frame often results in black boxes in several subsequent frames, making viewing difficult.

For remote locations, distant channels that, as analog signals, were previously usable in a snowy and degraded state may, as digital signals, be perfectly decodable or may become completely unavailable. The use of higher frequencies will add to these problems, especially in cases where a clear line-of-sight from the receiving antenna to the transmitter is not available, because usually higher frequency signals can't pass through obstacles as easily.

Effect on old analog technology

Television sets with only analog tuners cannot decode digital transmissions. When analog broadcasting over the air ceases, users of sets with analog-only tuners may use other sources of programming (e.g. cable, recorded media) or may purchase set-top converter boxes to tune in the digital signals. In the United States, a government-sponsored coupon was available to offset the cost of an external converter box. Analog switch-off (of full-power stations) took place on December 11, 2006 in The Netherlands, June 12, 2009 in the United States for full-power stations, and later for Class-A Stations on September 1, 2016, July 24, 2011 in Japan, August 31, 2011 in Canada, February 13, 2012 in Arab states, May 1, 2012 in Germany, October 24, 2012 in the United Kingdom and Ireland, October 31, 2012 in selected Indian cities, and December 10, 2013 in Australia. Completion of analog switch-off is scheduled for December 31, 2017 in the whole of India, December 2018 in Costa Rica and around 2020 for the Philippines.

Disappearance of TV-audio receivers

Prior to the conversion to digital TV, analog television broadcast audio for TV channels on a separate FM carrier signal from the video signal. This FM audio signal could be heard using standard radios equipped with the appropriate tuning circuits.

However, after the transition of many countries to digital TV, no portable radio manufacturer has yet developed an alternative method for portable radios to play just the audio signal of digital TV channels; DTV radio is not the same thing.

Environmental issues

The adoption of a broadcast standard incompatible with existing analog receivers has created the problem of large numbers of analog receivers being discarded during digital television transition. One superintendent of public works was quoted in 2009 saying; "some of the studies I’ve read in the trade magazines say up to a quarter of American households could be throwing a TV out in the next two years following the regulation change". In 2009, an estimated 99 million analog TV receivers were sitting unused in homes in the US alone and, while some obsolete receivers are being retrofitted with converters, many more are simply dumped in landfills where they represent a source of toxic metals such as lead as well as lesser amounts of materials such as barium, cadmium and chromium.

According to one campaign group, a CRT computer monitor or TV contains an average of 8 pounds (3.6 kg) of lead. According to another source, the lead in glass of a CRT varies from 1.08 lb to 11.28 lb, depending on screen size and type, but the lead is in the form of "stable and immobile" lead oxide mixed into the glass. It is claimed that the lead can have long-term negative effects on the environment if dumped as landfill. However, the glass envelope can be recycled at suitably equipped facilities. Other portions of the receiver may be subject to disposal as hazardous material.

Local restrictions on disposal of these materials vary widely; in some cases second-hand stores have refused to accept working color television receivers for resale due to the increasing costs of disposing of unsold TVs. Those thrift stores which are still accepting donated TVs have reported significant increases in good-condition working used television receivers abandoned by viewers who often expect them not to work after digital transition.

In Michigan in 2009, one recycler estimated that as many as one household in four would dispose of or recycle a TV set in the following year. The digital television transition, migration to high-definition television receivers and the replacement of CRTs with flatscreens are all factors in the increasing number of discarded analog CRT-based television receivers.

Tuesday, March 22, 2022

History of paleontology in the United States

Exhuming the First American Mastodon, oil on canvas by Charles Willson Peale (1806).

The history of paleontology in the United States refers to the developments and discoveries regarding fossils found within or by people from the United States of America. Local paleontology began informally with Native Americans, who have been familiar with fossils for thousands of years. They both told myths about them and applied them to practical purposes. African slaves also contributed their knowledge; the first reasonably accurate recorded identification of vertebrate fossils in the new world was made by slaves on a South Carolina plantation who recognized the elephant affinities of mammoth molars uncovered there in 1725. The first major fossil discovery to attract the attention of formally trained scientists were the Ice Age fossils of Kentucky's Big Bone Lick. These fossils were studied by eminent intellectuals like France's George Cuvier and local statesmen and frontiersman like Daniel Boone, Benjamin Franklin, William Henry Harrison, Thomas Jefferson, and George Washington. By the end of the 18th century possible dinosaur fossils had already been found.

By the beginning of the 19th, their fossil footprints definitely had. Later in the century as more dinosaur fossils were uncovered eminent paleontologists Edward Drinker Cope and Othniel Charles Marsh were embroiled in a bitter rivalry to collect the most fossils and name the most new prehistoric species. Early in the 20th century major finds continued, like the Ice Age mammals of the La Brea Tar Pits, the Oligocene bonebeds of South Dakota, and the Triassic bonebeds of New Mexico. Mid-to-late twentieth century discoveries in the United States triggered the Dinosaur Renaissance as the discovery of the bird-like Deinonychus overturned misguided notions of dinosaurs as plodding lizard-like animals, cemented their sophisticated physiology and relationship with birds. Other notable finds include Maiasaura, which provided early evidence for parental care in dinosaurs and "Seismosaurus" the largest known dinosaur.

Indigenous interpretations

Fossils of large Ice Age birds like Teratornis may have inspired Native American Thunderbird legends.

The indigenous people of the United States interpreted the fossil record through a mythological lens. Some of the tactics they used to understand the fossil record were nevertheless similar to scientific approaches. Native American fossil legends often derived from observation and rational speculation based on fossil finds. The indigenous people of the United States also frequently attempted to verify and modify interpretations of the fossil record in order to make sense of new discoveries. Although imperfect, Native American oral histories can preserve accurate information for extended periods of time. Since contact with Europeans, the ensuing epidemics, colonial violence, the Indian Wars, and forced displacement of Native peoples to reservations has resulted in the loss of much of their fossil-related culture.[2] According to folklorist Adrienne Mayor, a common theme in indigenous American fossil legends is "the eternal struggle for natural balance among earth, water and sky forces". Indigenous fossil legends also frequently show motifs resembling major themes in scientific paleontology like deep time, extinction, change over time and relationships between different life forms. Fossils have been used by Native Americans for evidence about the past, healing, personal protection, and trade. Fossil sites were often chosen as the setting of vision quests. Modern Comanche in Oklahoma still use dinosaur and mammoth bones for medicinal purposes.

18th century

George Cuvier's illustration comparing the lower jaw of a wooly mammoth (above) and an Indian elephant (below).

The first reasonably correct identification of a vertebrate fossil in North America was made in 1725, at a South Carolina plantation called Stono. There slaves had uncovered several large fossil teeth while digging in a swamp. The slaves unanimously identified the teeth as elephant molars, which they would have recognized from life in Africa. In the early 19th century, Georges Cuvier authored an 1806 translated account of the discovery at Stono. He remarked that the African slaves understood the similarity between mammoth remains and elephants before European naturalists.

The first major vertebrate fossil discovery in North America to attract the attention of formally trainer scientists occurred just a few decades later. In July 1739 a French military expedition comprising 123 French soldiers and 319 Native American warriors left Quebec under the command of Charles III Le Moyne (2nd Baron Charles de Longueuil) to help defend New Orleans from the Chickasaw, who were attacking the city on behalf of England. While on their journey down the Ohio River towards the Mississippi, they camped in what is now Kentucky. Some of the expedition's Native members formed a hunting party and embarked to acquire that evening's meal. When they returned that evening their canoes were laden with massive fossils including long tusks, massive teeth, and a thighbone almost as tall as a person. The source of their fossils was the site now known as Big Bone Lick.

Near the end of 1740, Baron Charles de Longueuil departed from New Orleans to France, carrying with him fossils from Big Bone Lick. Longueuil left the remains at the Cabinet du Roi. This Cabinet du Roi (not to be confused with the administration personnel cabinet of the same name) was a collection of curiosities stored in the chateau of the king's botanical garden (which is nowadays the Jardin des plantes, in Paris, main seat of the French National Museum of Natural History). These fossils were first speculated on by eminent French scientists like Jean-Etienne Guettard and Georges Cuvier. A few years later, in 1762, Louis Daubenton read his paper before the French Royal Academy of Science showing that the bones and tusks belonged to an elephant-like species and that the teeth belonged to some kind of carnivorous hippopotamus. In fact the teeth belonged to the same individual, in the present day identified as an American mastodon (Mammut americanum).

In 1767 George Crogan (an Indian agent) sent several fossils from Big Bone Lick to Benjamin Franklin. Benjamin Franklin wrote back to express his amazement that the tusks resembled those of an elephant, yet the molars resembled those of a carnivorous animal. Franklin also wondered at the fact that the elephant-like fossils of Big Bone Lick were found in places so much colder than places modern elephants live. He speculated that maybe earth was in a different position in the past and its climate correspondingly different. Soon after the fossils attracted the attention of other major American figures like George Washington, Thomas Jefferson, Daniel Boone, William Henry Harrison, and James Taylor. The mammoth quickly became a symbol of American patriotism and equality with the Old World.

One of the earliest notable events in American dinosaur paleontology occurred on October 5, 1787. Caspar Wistar and Timothy Matlack gave a presentation to the American Philosophical Society in Philadelphia regarding "'a large thigh bone'" from some mysterious ancient creature found in Late Cretaceous rocks near Woodbury Creek, New Jersey. Modern scientist suspect this bone was actually a metatarsal from a duck-billed dinosaur, which are known from the same sediments.

19th century

A negative footprint of Grallator showing skin impressions.

Among the earliest major fossil discoveries in America occurred in Massachusetts during the spring of 1802. At that time a boy uncovered a piece of reddish sandstone with bird-like three toed footprints while ploughing on his father's farm in South Hadley. This was the first recorded dinosaur footprint discovery in North America. A short while later, Lewis and Clark expedition of 1804 through 1806 made several fossil discoveries along its journey, including the first documented fossils from what is now North Dakota. However, only a fish jawbone from Iowa remains of the fossils they collected along the way. Another significant, but unrelated event from the early 19th century was the 1817 organization of the Lyceum of Natural History of New York by Samuel L. Mitchill. In 1869 the American Museum of Natural History was organized out of the Lyceum.

During the Late 1830s Increase Allen Lapham found a variety of fossils in great abundance in some rocky hills near Milwaukee. Lapham sent a sizable sampling of the local fossils to James Hall of New York in 1846. Hall began researching the area and in 1862 recognized the local reefs for what they were. The Silurian-aged reefs of the Milwaukee area were the first Paleozoic reefs in the world to be described for the scientific literature.

In 1835 another major dinosaur track find occurred in Massachusetts. The town of Greenfield was paving its streets when residents noticed fossil footprints on the sandstone slabs that resembled turkey tracks. These rocks were taken from what would turn out to be the most productive dinosaur tracksite in the Connecticut Valley. Later that year, word of the find reached Amherst College geology professor Edward Hitchcock. Hitchcock spent the rest of the summer traveling through the Connecticut Valley examining the fossil footprints. The next year Hitchcock wrote a scientific paper on the fossil footprints of the Connecticut Valley. He thought the tracks were made by giant birds. In 1858, Hitchcock published again on the Connecticut Valley fossil footprints and still thought of them as bird tracks.

In 1842, fossils were found on a plantation owned by a man named Judge Creagh. Local doctors identified the fossils as belonging to an ancient marine reptile, and called it Basilosaurus. However, some of the fossils were shipped to Sir Richard Owen in England. After examining the remains Owen realized the bones actually belonged to a whale, rather than a reptile. Herman Melville's narrator Ishmael gives an account of the discovery in chapters 104–105 of Moby-Dick (1851).

In 1853 the Pacific Railroad Exploration survey became the first to document Arizona's petrified forest. In 1900 the United States Geological Survey dedicated a report to the petrified forest and encouraged swift action to preserve the spectacular fossils before curiosity seekers removed them all. In 1906, protective action was taken and Petrified Forest officially became a national monument.

Benjamin Waterhouse Hawkins' mounted Hadrosaurus, the first mounted dinosaur skeleton in the world.

In 1858 the United States was home to the world's first "reasonably complete" dinosaur skeleton. A member of the Academy of Natural Sciences named William Foulke heard about fossil bones that had been found on a local farm while spending the summer in Haddonfield. That fall Foulke hired a team to reopen the marl pit the bones had been taken from. Roughly 10 feet down they found bones. Paleontologist Joseph Leidy later formally described the fossils. He interpreted the fossils as the remains of a bipedal amphibious reptile that had been swept out to sea by the river it lived alongside. Leidy called the creature Hadrosaurus foulkii after Foulke. A decade later, in 1868 Leidy worked with artist Benjamin Waterhouse Hawkins to mount Hadrosaurus foulkii for the Academy of Natural Sciences of Philadelphia. This became both the first mounted dinosaur skeleton ever mounted for public display but also one of the most popular exhibits in the history of the Academy. Estimates have the Hadrosaurus exhibit as increasing the number of visitors by up to 50%.

The year after the Hadrosaurus's fossils were first identified, 1859, state agricultural chemist Philip T. Tyson found the first documented dinosaur fossils of the Arundel Formation in an iron pit at Bladensburg, Maryland. The discovery consisted of two fossil teeth. Tyson took the dinosaur teeth to a local doctor named Christopher Johnston. Johnston cut thin sections of one tooth to examine it under a microscope. Johnson named the teeth Astrodon. In 1865 Joseph Leidy formally named the species Astrodon johnstoni after Christopher Johnston. This represents the first formal naming of a sauropod species in North America.

Two years later a chance find would bring instant fame to the fossils of the John Day region of Oregon. In 1861, a company of soldiers arrived in Oregon's Fort Dalles after visiting the Crooked River region brought back fossil bones and teeth, among which was a well-preserved rhinoceros jaw. The pastor of the fort's Congregational church, Thomas Condon, happened to be a paleontology enthusiast. In 1862, some soldiers were dispatched with supplies to Harney Valley. Condon went along with them and prospected for fossils when the troops passed back through the Crooked River area. He went fossil collecting again in 1863 and found rich fossil deposits north of Picture Gorge in the John Day River Valley. He realized that he had stumbled on a find of major scientific importance. Since he himself had no scientific qualifications or references to use in identifying fossils, Condon sent some fossils to O. C. Marsh of Yale University. Marsh replied with a request for Condon to guide and expedition to the area in which he found the fossils. Condon obliged and over the ensuing years a series of fossil hunting expeditions ventured into the John Day fossil beds.

An early painting of Laelaps/Dryptosaurus by Charles R. Knight.

Later, 1866 dinosaur remains were found in a marl pit near Barnsboro owned by the Wet Jersey Marl Company. He called it Laelaps aquilunguis. Also that year, Cope gave Othniel Charles Marsh a tour of the marl pit where Laelaps was found. While there, Marsh secretly made arrangements with some of the workers for them to send any fossils they find to him at the Yale Peabody Museum instead of to Cope at the Academy of Natural Sciences of Philadelphia. This may have been the "first shot" of the Bone Wars, a bitter long-running feud between the two scientists.

The next year a United States army surgeon named Dr. Theophilus Turner found a nearly complete plesiosaur skeleton in what is now Logan County while stationed at Fort Wallace. This was the first plesiosaur specimen of this caliber found in all of North America. Dr. Turner gave some of the vertebrae to a member of the Union Pacific railroad survey, John LeConte. He in turn gave the bones to paleontologist Edward Drinker Cope, who identified them as the remains of a very large plesiosaur. Cope wrote a letter to Dr. Turner requesting that he send him the remainder of the skeleton. Turner obliged and in mid-March 1868 Cope received the remainder of the fossils. Within two weeks of receiving the specimen, Cope made a presentation at the March 24th meeting of the Academy of Natural Sciences in Philadelphia. He named the creature Elasmosaurus platyurus, although in his hasty work he mistakenly reconstructed it with its head at the end of the tail instead of its neck.

In 1869, excavation started at Gilboa Forest, an extraordinary collection of Devonian plants regarded as one of the first forests to ever exist. Excavation of the Gilboa petrified forest continued on into the early twentieth century, but by 1921 on-site field work had completed.

The next year, O. C. Marsh led a paleontological expedition into the western United States on behalf of Yale University. Late that November they visited the area around Fort Wallace. Among the fossils found by Marsh's crew in western Kansas were the far ends of two pterosaur wing metacarpals. These were the first scientifically documented fossils of the pterosaur that would later be named Pteranodon. This formal naming occurred six years later, in 1876.

In 1874 March's rival, Cope arrived at New Mexico accompanying the G. M. Wheeler Survey. While in the area he found the first known Eocene mammal from the southwestern United States, Coryphodon. In total he discovered about 90 species. This was a major boon to his reputation as his research was foundational to understanding that interval of American geologic history.

Around March 1877 a man named Oramel Lucas discovered sauropod bones in a valley called Garden Park located a few miles north of Canon City, Colorado. He wrote to both Cope and O. C. Marsh, the famous rival paleontologists of the bone wars to alert them about his discovery. Although Marsh never responded, Cope did, and Oramel Lucas and his brother Ira began digging up local fossils and sending them to Cope. By August of the same year, Cope had formally named the new species excavated by the Lucas brothers Camarasaurus supremus. Later, a crew working on behalf of O. C. Marsh under Mudge and Williston started a quarry nearby. They made several important finds like the new species Allosaurus fragilis and Diplodocus longus. Following the initial excavations in the quarry field work stopped until 1883. That year brothers Marshall and Henry Felch reopened excavations there, again on behalf of O. C. Marsh. They worked for five years collecting many dinosaurs already known from the formation, but also the new species Ceratosaurus nasicornis.

Beginning in 1877, the plentiful dinosaur remains preserved in Wyoming came to the attention of scientists. Three men played a pivotal early role in bringing scientific attention to the area's dinosaurs. These were Colorado School of Mines professor Arthur Lakes, teacher O. Lucas, and Union Pacific Railroad foreman William H. Reed. In March 1877, Reed noticed fossil limbs and vertebrae at Como Bluff. He spent several weeks collecting fossils with foreman William E. Carlin. In July, O. C. Marsh was informed of Reed and Carlin's fossil discoveries. Marsh hired both of them to acquire more local fossils for him. They continued collecting into early 1878, uncovering several Camarasaurus specimens, one being a new species, Camarasaurus grandis. Nearby they made another significant find, Dryolestes priscus, the first Jurassic mammal known from North America. From 1877 to 1878 Princeton also sent a massive expedition to Wyoming. Major participants included Henry Fairfield Osborn, W. E. Scott, and Thomas Speer. Also around this time, Samuel W. Williston began periodic excavations.

Late in 1877, Marsh's scientific rival Edward Drinker Cope heard that fossils had been found at Como Bluff. He quickly dispatched his own fossil hunters into the area. Reed described his struggles to keep Cope's men away from his own hunting grounds in regular correspondence with Marsh. William Carlin quit working for Marsh and ended up joining Cope's efforts in the region. Since Carlin was in charge of the railway's station house he used his influence to keep Reed out. Marsh hired additional help for Reed, but none of his workers stayed on the job long term. Reed was essentially on his own by the spring of 1879, working hectically at excavating several quarries at once to recover the fossils before Cope's men. In the middle of May that same year Marsh directed Arthur Lakes to leave the Morrison, Colorado area and assist Reed at Como Bluff. The partnership would be fruitful that year and several major discoveries happened. They found a ninth site early in July that would be the most productive of any fossil site in the Morrison Formation.

In September, they made another major discovery. By the end of the month, they had identified a new species of sauropod, Brontosaurus excelsus, that would end up mounted in the Yale Peabody Museum. This species has since been reclassified as Apatosaurus excelsus. In September they found a thirteenth quarry that produced more dinosaur skeletons than any of the others. Camptosaurus and Stegosaurus were the most common. New dinosaurs found here included Camarasaurus lentus, Camptosaurus dispar, and Coelurus fragilis. By June 1889, fieldwork at Como Bluff had concluded after twelve years. Marsh's fieldwork in the area uncovered the greatest abundance of Jurassic fossils known in the world at the time. By the 1918 conclusion of Samuel W. Williston's work in Wyoming hundreds of tons of dinosaur bones had been recovered from Wyoming rocks.

A major Cenozoic fossil find also happened in 1877. That year, a scout and rancher named Captain James H. Cook found a Miocene bonebed in Sioux County, Nebraska now known as the Agate Springs Quarries. These rich deposits are so dense with bones that single forty foot slab of sandstone preserved more than 4300 bones from at least 1700 individual animals. The total number of fossils preserved here may number in the millions. The tiny rhinoceras Diceratherium cooki composed about one quarter of the remains in the Agate Springs beds. This was the first paleontological discovery to attract public attention to the fossils of Nebraska.

In late 1887 Othniel Charles Marsh sent John Bell Hatcher to look for dinosaur remains in the Arundel Clay. While on this expedition, Hatcher found a fossiliferous iron mine on a farm near Muikirk, Maryland. Hatcher's excavation continued uncovering dinosaur fossils into the next year. Hatcher recovered hundreds of bones and teeth, which helped the region between Maryland and Washington D.C. become known as Dinosaur Alley.

20th century

Between 1906 and 1916 hundreds of thousands of Pleistocene fossils were uncovered in central Los Angeles. Just a few years after the La Brea tar pits were found, in 1908, paleontologist Earl Douglass was excavating fossils in Utah on behalf of the Carnegie Museum of Natural History. The director of the museum visited Douglass's camp that year and suggested that Douglass search for Jurassic dinosaur fossils in the Uinta Mountains north of his camp. Douglass agreed and they set off to the Uinta Mountains the next day. They found so many fossils that Douglas built a home near the Green River and his family moved in from Pittsburgh. He spent the rest of his career in the area excavating fossils. Among the local finds were Allosaurus, Apatosaurus, Barosaurus, Camarasaurus, Camptosaurus, Diplodocus, Dryosaurus, Stegosaurus. In 1915 US president Woodrow Wilson declared the quarry and surrounding land Dinosaur National Monument in order to protect it from settlement. Between 1909 and 1923 millions of tons of rocks and fossils had been excavated from the Dinosaur National Monument area.

In 1909 in paleontology Massachusetts paleontologist Mignon Talbot became the first woman elected to the Paleontological Society. In an unrelated east coast discovery of 1912, workers digging in a cave for a railroad construction project near Cumberland, Maryland in Allegany County uncovered many fossils in the course of their labor. However, eventually the scientific significance of the fossils was realized and paleontologist J. W. Gidley conducted fieldwork at the cave between 1912 and 1915. By 1938 report more than 50 different kinds of animals had been identified among the fossils.

Norman Ross preparing the skeleton of a baby Brachyceratops for exhibition in 1921.

In 1938, Barnum Brown of the American Museum of Natural History sent Roland T. Bird to Texas in search of dinosaur trackways reportedly uncovered by local moonshiners. At the town of Glen Rose local residents guided him to carnivorous dinosaur tracks preserved along the Paluxy River. While he was cleaning mud from these footprints, he noticed another kind of footprint, apparently left by a long-necked sauropod dinosaur. In 1940, Bird resumed his Texas fieldwork with the help of paleontologists from the Survey and labor employed by the Works Progress Administration.

Later, in 1940, the South Dakota School of Mines and Technology collaborated with National Geographic on an expedition into the badlands of South Dakota. They uncovered tons of fossils from at least 175 different species of Oligocene life. The fossils were taken to the South Dakota School of Mines in Rapid City. Among the mammal discoveries were the remains of rhinoceroses, tapirs, three-toed horses, pig-like animals, and rodents. In 1947 another major dinosaur discovery took place. An American Museum field party led by Edwin Harris Colbert found a bonebed including the skeletons of more than 1,000 Coelophysis at Ghost Ranch. Later, in 1953 University of New Mexico graduate student William Chenoweth found three important sites where dinosaurs were preserved in Morrison Formation rocks. He found a fragmentary Allosaurus, sauropods, and Stegosaurus.

Theropod and sauropod tracks under water in the Paluxy River.

The famous Montanan Tertiary deposits of the Ruby Valley basin were also first studied in 1947. The early research was performed by Dr. Herman F. Becker on behalf of the New York Botanical Garden. These deposits from the southwestern part of the state are one of the best sources of plant and insect fossils in North America. In 1959 Becker's Ruby Valley excavations uncovered about 5,000 specimens of more than two hundred species of plants, insects, and fishes. Invertebrate finds included ants, bees, beetles, earwigs, caddis flies, crane flies, damsel flies, lantern flies, may flies, grasshoppers, leaf hoppers, mosquitoes, snails, and wasps. Vertebrate remains included feathers, and, once in a while, a bird.

During the late 1950s Francis Tully found a fossil he could not identify at the strip mines near Braidwood, Illinois. He took the specimen to Chicago's Field Museum of Natural History. Researchers at the museum couldn't identify it either, and the specimen became known as Mr. Tully's monster. In 1966, Eugene Richardson, the Curator of Fossil Invertebrates of the Field Museum formally named the Tully monster Tullimonstrum gregarium in honor of Tully.

The bird-like dinosaur Deinonychus instigated the Dinosaur Renaissance.

In 1964, John Ostrom led an expedition that included his student Robert T. Bakker into the south-central part of Montana. The rocks they prospected were of the Cloverly Formation, dating back to the Early Cretaceous. Among their finds were the first documented remains of a small carnivorous dinosaur that would be named Deinonychus antirrhopus. This discovery helped ignite the Dinosaur Renaissance. It exhibited important anatomical similarities to birds that helped scientists shed antiquated ideas interpreting dinosaurs as "overgrown lizards".

In Spring, 1965 a major discovery of Devonian fossils occurred in Cuyahoga County. A collaboration between the state Highway Department, Ohio Bureau of Public Roads and the Cleveland Museum of Natural History led by the Smithsonian's David Dunkle uncovered as many as 50,000 fish fossils from a construction site. By the ensuing November 120 or more different species had been found there, with half previously unknown to science. That same year, in an unrelated development, the Florissant fossil beds of Colorado were proposed as a potential federal preserve.

The hadrosaur Maisaura may have cared for its young.

In 1978 paleontologist Bill Clemens alerted fellow paleontologists Jack Horner and Bob Makela to the presence of unidentified dinosaur fossils in Bynum, Montana. Horner visited the town and recognized the remains as belonging to a duck-billed dinosaur. While in town the owner of a local rock shop, Marion Brandvold, showed him some tiny bones. Horner identified them as baby duck-bill bones. Horner also knew that this was an important find and convinced Brandvold to donate her fossils to a museum. She obliged and gave them to Princeton University. Horner's team prospected in the area where Brandvold found the baby hadrosaur fossils. Their effort paid off with the discovery of the first scientifically documented dinosaur eggs of the Western Hemisphere and a new kind of duck-bill, Maiasaura peeblesorum.

The next year, 1979, two hikers found a series of gigantic articulated vertebrae fossils near San Ysidro. They reported the remains to David Gilette of the New Mexico Museum of Natural History. Gillette led an expedition into the region and used cutting edge technology to locate the remains while they were still entombed in sandstone. The team excavated a massive quarry and gradually recovered a significant portion of the rear half of a diplodocid sauropod dinosaur. In 1991 this dinosaur was formally described as the new genus Seismosaurus and estimated to be the longest dinosaur known to science at 52 meters (171 feet) long.

21st century

More recently, in the 2000s, Seismosaurus was found to be the same as Diplodocus, a previously known dinosaur of similar age from the western United States. Dinosaur fossils continue to be found in new locations within the United States. It was not until 2004 that any dinosaur fossils were reported from Louisiana. Currently, within the United States, dinosaur fossils are known from Alabama, Alaska, Arizona, Arkansas, California, Colorado, Connecticut, Delaware, Georgia, Idaho, Iowa, Kansas, Louisiana, Maryland, Massachusetts, Minnesota, Mississippi, Missouri, Montana, Nebraska, Nevada, New Jersey, New Mexico, New York, North Carolina, North Dakota, Oklahoma, Pennsylvania, South Carolina, South Dakota, Tennessee, Texas, Utah, Virginia, Washington, D.C., Washington and Wyoming, but not in Florida, Hawaii, Illinois, Indiana, Kentucky, Maine, Michigan, New Hampshire, Ohio, Oregon, Rhode Island, Vermont, West Virginia, or Wisconsin. Washington is the latest state to have found their first dinosaur bone, it was recovered in 2012 but was not publicly identified until May 21, 2015. Some states contain rocks of the appropriate type and age to preserve dinosaur fossils, so the list of states with known dinosaur fossils is likely to increase in the future.

Distance education

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