65-566: The Logan Temple Barn was built in Logan, Utah in 1896–97 to house the animals belonging to members of the Church of Jesus Christ of Latter-day Saints working at or attending the nearby Logan Temple . It is unique as one of only two stone barns in the Cache Valley, where wood-frame barns prevailed. The temple barn fell into disuse after automobiles began to bring worshipers to the temple and
130-459: A " Gilbert-type" river delta over several thousand years. The Logan River later cut down through these sedimentary deposits following the draining of Lake Bonneville approximately 14,500 years ago. This created a low-lying area with very steep slopes that reach into the rest of town and to the Logan River bottomlands. To the west of Logan lie flatlands that contain both farmland and marshes. To
195-611: A change from low-amplitude glacial cycles with a dominant periodicity of 41,000 years to asymmetric high-amplitude cycles dominated by a periodicity of 100,000 years. However, a 2020 study concluded that ice age terminations might have been influenced by obliquity since the Mid-Pleistocene Transition, which caused stronger summers in the Northern Hemisphere . Glaciation in the Pleistocene
260-574: A deviation from today's annual mean temperature, taken as zero. This sort of graph is based on another isotope ratio versus time. Ratios are converted to a percentage difference from the ratio found in standard mean ocean water (SMOW). The graph in either form appears as a waveform with overtones . One half of a period is a Marine isotopic stage (MIS). It indicates a glacial (below zero) or an interglacial (above zero). Overtones are stadials or interstadials. According to this evidence, Earth experienced 102 MIS stages beginning at about 2.588 Ma BP in
325-421: A few regions had been studied and the names were relatively few. Today the geologists of different nations are taking more of an interest in Pleistocene glaciology. As a consequence, the number of names is expanding rapidly and will continue to expand. Many of the advances and stadials remain unnamed. Also, the terrestrial evidence for some of them has been erased or obscured by larger ones, but evidence remains from
390-538: A fort near the banks of the Logan River . They named their new community "Logan" for Ephraim Logan, an early fur trapper in the area. Logan was incorporated on January 17, 1866. Brigham Young College was founded here on August 6, 1877 (and closed in 1926), and Utah State University – then called the Agricultural College of Utah – was founded in 1888. Brigham Young College , a college run by
455-578: A team of Russian scientists in collaboration with Princeton University announced that they had brought two female nematodes frozen in permafrost , from around 42,000 years ago, back to life. The two nematodes, at the time, were the oldest confirmed living animals on the planet. The evolution of anatomically modern humans took place during the Pleistocene. At the beginning of the Pleistocene Paranthropus species were still present, as well as early human ancestors, but during
520-534: Is dominated by a central bearing wall supporting the wood framed floor and roof. The Logan Temple Barn was placed on the National Register of Historic Places on December 19, 1985. [REDACTED] Media related to Logan Temple Barn at Wikimedia Commons Logan, Utah Logan is a city in Cache County , Utah , United States. The 2020 census recorded the population was 52,778. Logan
585-781: Is estimated that, at maximum glacial extent, 30% of the Earth's surface was covered by ice. In addition, a zone of permafrost stretched southward from the edge of the glacial sheet, a few hundred kilometres in North America , and several hundred in Eurasia . The mean annual temperature at the edge of the ice was −6 °C (21 °F); at the edge of the permafrost, 0 °C (32 °F). Each glacial advance tied up huge volumes of water in continental ice sheets 1,500 to 3,000 metres (4,900–9,800 ft) thick, resulting in temporary sea-level drops of 100 metres (300 ft) or more over
650-507: Is in northern Utah, 47 miles (76 km) north of Ogden , on the Logan River . It is about 82 miles (132 km) north of Salt Lake City . According to the United States Census Bureau , the city has a total area of 18.5 square miles (48.0 km ), of which 18.0 square miles (46.5 km ) is land and 0.58 square miles (1.5 km ), or 3.16%, is water. The city lies near the eastern edge of Cache Valley on
715-459: Is no systematic correspondence between pluvials to glacials, however. Moreover, regional pluvials do not correspond to each other globally. For example, some have used the term "Riss pluvial" in Egyptian contexts. Any coincidence is an accident of regional factors. Only a few of the names for pluvials in restricted regions have been stratigraphically defined. The sum of transient factors acting at
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#1732787619318780-457: Is the county seat of Cache County and the principal city of the Logan metropolitan area , which includes Cache County and Franklin County, Idaho . The Logan metropolitan area contained 147,908 people as of the 2020 census. Logan is the location of the main campus of Utah State University . The town of Logan was founded in 1859 by settlers sent by Brigham Young to survey for the site of
845-592: The Ice Age ) is the geological epoch that lasted from c. 2.58 million to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations . Before a change was finally confirmed in 2009 by the International Union of Geological Sciences , the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of
910-659: The Alpine ice sheet on the Alps . Scattered domes stretched across Siberia and the Arctic shelf. The northern seas were ice-covered. South of the ice sheets large lakes accumulated because outlets were blocked and the cooler air slowed evaporation. When the Laurentide Ice Sheet retreated, north-central North America was completely covered by Lake Agassiz . Over a hundred basins, now dry or nearly so, were overflowing in
975-529: The ICS timescale, the Pleistocene is divided into four stages or ages , the Gelasian , Calabrian , Chibanian (previously the unofficial "Middle Pleistocene"), and Upper Pleistocene (unofficially the "Tarantian"). In addition to these international subdivisions, various regional subdivisions are often used. In 2009 the International Union of Geological Sciences (IUGS) confirmed a change in time period for
1040-657: The Isthmus of Panama , causing a faunal interchange between the two regions and changing ocean circulation patterns, with the onset of glaciation in the Northern Hemisphere occurring around 2.7 million years ago. During the Early Pleistocene (2.58–0.8 Ma), archaic humans of the genus Homo originated in Africa and spread throughout Afro-Eurasia . The end of the Early Pleistocene is marked by
1105-677: The Laurentide Ice Sheet . Charles Lyell introduced the term "Pleistocene" in 1839 to describe strata in Sicily that had at least 70% of their molluscan fauna still living today. This distinguished it from the older Pliocene Epoch , which Lyell had originally thought to be the youngest fossil rock layer. He constructed the name "Pleistocene" ('most new' or 'newest') from the Greek πλεῖστος ( pleīstos ) 'most' and καινός ( kainós ( Latinized as cænus ) 'new'). This contrasts with
1170-615: The Mid-Pleistocene Transition , with the cyclicity of glacial cycles changing from 41,000-year cycles to asymmetric 100,000-year cycles, making the climate variation more extreme. The Late Pleistocene witnessed the spread of modern humans outside of Africa as well as the extinction of all other human species. Humans also spread to the Australian continent and the Americas for the first time, co-incident with
1235-662: The Ruwenzori Range in east and central Africa were larger. Glaciers existed in the mountains of Ethiopia and to the west in the Atlas Mountains . In the northern hemisphere, many glaciers fused into one. The Cordilleran Ice Sheet covered the North American northwest; the east was covered by the Laurentide . The Fenno-Scandian ice sheet rested on northern Europe , including much of Great Britain;
1300-477: The last glacial period ended about 10,000 years ago. Over 11 major glacial events have been identified, as well as many minor glacial events. A major glacial event is a general glacial excursion, termed a "glacial." Glacials are separated by "interglacials". During a glacial, the glacier experiences minor advances and retreats. The minor excursion is a "stadial"; times between stadials are "interstadials". These events are defined differently in different regions of
1365-599: The woolly rhinoceros , various giraffids , such as the Sivatherium ; ground sloths , Irish elk , cave lions , cave bears , Gomphotheres , American lions , dire wolves , and short-faced bears , began late in the Pleistocene and continued into the Holocene. Neanderthals also became extinct during this period. At the end of the last ice age, cold-blooded animals, smaller mammals like wood mice , migratory birds, and swifter animals like whitetail deer had replaced
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#17327876193181430-689: The Cache Valley Area. There are numerous events at the Logan/Cache County Fairgrounds including fairs, rodeos, and demolition derbies. Nearby, the city of Logan runs an aquatic center and a skate park. During the winter season, the city operates an outdoor ice skating rink at Merlin Olsen Park (Central Park). The government of the city of Logan consists of the Executive Branch, led by an elected mayor;
1495-593: The Church of Jesus Christ of Latter-day Saints , was located in Logan from 1878 to 1926. Its library and its papers were given to the Utah State University when it ceased operating. Logan's growth reflects settlement and post-war booms along with other changes incidental to conditions in the West. Logan grew to about 20,000 in the mid-1960s, and according to Census estimates, exceeded 50,000 in 2015. Logan
1560-569: The Early Pleistocene Gelasian . Early Pleistocene stages were shallow and frequent. The latest were the most intense and most widely spaced. By convention, stages are numbered from the Holocene, which is MIS1. Glacials receive an even number and interglacials receive an odd number. The first major glacial was MIS2-4 at about 85–11 ka BP. The largest glacials were 2, 6, 12, and 16. The warmest interglacials were 1, 5, 9 and 11. For matching of MIS numbers to named stages, see under
1625-409: The Earth's surface is cyclical: climate, ocean currents and other movements, wind currents, temperature, etc. The waveform response comes from the underlying cyclical motions of the planet, which eventually drag all the transients into harmony with them. The repeated glaciations of the Pleistocene were caused by the same factors. The Mid-Pleistocene Transition , approximately one million years ago, saw
1690-693: The Legislative Branch, led by a five-member city council; and the Judicial Branch, led by the city judge. Logan does not use districts for election purposes, as the mayor and council members are elected at-large . The current mayor of Logan, Holly H. Daines, was elected in November 2017. Current Logan City Council Members include Amy Z. Anderson, Mark A. Anderson, Mike Johnson, Ernesto Lopez, and Jeannie F. Simmonds. Alvin Crockett
1755-641: The Logan River Golf Course, the Logan/Cache County Fairgrounds, and the Logan Aquatic Center. Zootah at Willow Park is a small zoo in Logan's Willow Park, with a small collection of wild animals including monkeys, coyotes, bobcats, bald eagles, and land birds and ducks. Logan is the home of two full-length golf courses, the Logan River Golf Course and the Logan Golf and Country Club. Other golf courses are also found around
1820-649: The Logan metropolitan statistical area (MSA) ranked as the eighth highest in the United States for percentage of commuters who biked to work (3.3 percent). Logan is served by a local sales-tax-funded zero-fare bus system called the Cache Valley Transit District (CVTD), which incorporated the Logan Transit District (LTD) in 2007. The LTD system began in 1992 with six routes in Logan. Service outside of Logan began with
1885-479: The North American west. Lake Bonneville , for example, stood where Great Salt Lake now does. In Eurasia, large lakes developed as a result of the runoff from the glaciers. Rivers were larger, had a more copious flow, and were braided . African lakes were fuller, apparently from decreased evaporation. Deserts, on the other hand, were drier and more extensive. Rainfall was lower because of the decreases in oceanic and other evaporation. It has been estimated that during
1950-434: The Pleistocene to 2.58 Ma, results in the inclusion of all the recent repeated glaciations within the Pleistocene. Radiocarbon dating is considered to be inaccurate beyond around 50,000 years ago. Marine isotope stages (MIS) derived from Oxygen isotopes are often used for giving approximate dates. Pleistocene non-marine sediments are found primarily in fluvial deposits , lakebeds, slope and loess deposits as well as in
2015-496: The Pleistocene's overall climate could be characterised as a continuous El Niño with trade winds in the south Pacific weakening or heading east, warm air rising near Peru , warm water spreading from the west Pacific and the Indian Ocean to the east Pacific, and other El Niño markers. Pleistocene climate was marked by repeated glacial cycles in which continental glaciers pushed to the 40th parallel in some places. It
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2080-503: The Pleistocene, changing the start date from 1.806 to 2.588 million years BP, and accepted the base of the Gelasian as the base of the Pleistocene, namely the base of the Monte San Nicola GSSP . The start date has now been rounded down to 2.580 million years BP. The IUGS has yet to approve a type section , Global Boundary Stratotype Section and Point (GSSP), for the upper Pleistocene/Holocene boundary ( i.e.
2145-805: The Pleistocene, the East Antarctic Ice Sheet thinned by at least 500 meters, and that thinning since the Last Glacial Maximum is less than 50 meters and probably started after ca 14 ka. During the 2.5 million years of the Pleistocene, numerous cold phases called glacials ( Quaternary ice age ), or significant advances of continental ice sheets, in Europe and North America, occurred at intervals of approximately 40,000 to 100,000 years. The long glacial periods were separated by more temperate and shorter interglacials which lasted about 10,000–15,000 years. The last cold episode of
2210-411: The Pleistocene, the plates upon which they sit probably having moved no more than 100 km (62 mi) relative to each other since the beginning of the period. In glacial periods, the sea level would drop by up to 120 m (390 ft) lower than today during peak glaciation, exposing large areas of the present continental shelf as dry land. According to Mark Lynas (through collected data),
2275-706: The appearance of Homo sapiens about 300,000 years ago. Artifacts associated with modern human behavior are unambiguously attested starting 40,000–50,000 years ago. According to mitochondrial timing techniques, modern humans migrated from Africa after the Riss glaciation in the Middle Palaeolithic during the Eemian Stage , spreading all over the ice-free world during the late Pleistocene. A 2005 study posits that humans in this migration interbred with archaic human forms already outside of Africa by
2340-527: The articles for those names. Both marine and continental faunas were essentially modern but with many more large land mammals such as Mammoths , Mastodons , Diprotodons , Smilodons , tigers , lions , Aurochs , short-faced bears , giant sloths , species within Gigantopithecus and others. Isolated landmasses such as Australia , Madagascar , New Zealand and islands in the Pacific saw
2405-405: The campus of Utah State University, Bear River Charter School (K-6th), and Fast Forward Charter High School. InTech Collegiate Academy (often known simply as InTech) is located in Logan and is a STEM focused, early college high school partnered with Utah State University. Logan River Academy is an adolescent residential treatment center that operates in the southern end of Logan. In 2009,
2470-1002: The city was $ 13,765. About 12.6% of families and 22.7% of the population were below the poverty line , including 15.6% of those under age 18 and 6.4% of those age 65 or over. Logan has a wide diversity of economic sectors with a focus on education, manufacturing and processing, medical services, agriculture, and retail businesses. The city's largest employer is Utah State University and Space Dynamics Laboratory with other major employers including ICON Health & Fitness (IFIT), Campbell Scientific, Cache Valley Bank, Conservice, Cache County School District , Cytiva , Entegris , Gossner Foods , Intermountain Health , JBS USA , Lee’s Marketplace, Logan Regional Hospital , Logan City School District , Pepperidge Farm , RR Donnelley , Thermo Fisher Scientific , TTM Technologies , S&S – Sansei Technologies , and Schreiber Foods . Attractions and events include: Logan's Parks and Recreation department runs
2535-618: The entire surface of the Earth. During interglacial times, such as at present, drowned coastlines were common, mitigated by isostatic or other emergent motion of some regions. The effects of glaciation were global. Antarctica was ice-bound throughout the Pleistocene as well as the preceding Pliocene. The Andes were covered in the south by the Patagonian ice cap. There were glaciers in New Zealand and Tasmania . The current decaying glaciers of Mount Kenya , Mount Kilimanjaro , and
2600-782: The evolution of large birds and even reptiles such as the Elephant bird , moa , Haast's eagle , Quinkana , Megalania and Meiolania . The severe climatic changes during the Ice Age had major impacts on the fauna and flora. With each advance of the ice, large areas of the continents became depopulated, and plants and animals retreating southwards in front of the advancing glacier faced tremendous stress. The most severe stress resulted from drastic climatic changes, reduced living space, and curtailed food supply. A major extinction event of large mammals ( megafauna ), which included mammoths , mastodons , saber-toothed cats , glyptodons ,
2665-444: The extinction of most large-bodied animals in these regions. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, with the sea levels being up to 120 metres (390 ft) lower than present at peak glaciation, allowing the connection of Asia and North America via Beringia and the covering of most of northern North America by
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2730-641: The formation of CVTD in 2001. The system has 16 routes that serve Logan and the adjacent cities of North Logan and River Heights . These include a northern route that reaches north to Richmond , and a southern route that serves the southern suburbs and Hyrum . There is also a five-time daily connection to Lewiston and Preston, Idaho . The public general aviation airport is Logan-Cache Airport . It features flight instruction, and private charter flights. Pleistocene The Pleistocene ( / ˈ p l aɪ s t ə ˌ s iː n , - s t oʊ -/ PLY -stə-seen, -stoh- ; referred to colloquially as
2795-414: The glacial range, which have their own glacial history depending on latitude, terrain and climate. There is a general correspondence between glacials in different regions. Investigators often interchange the names if the glacial geology of a region is in the process of being defined. However, it is generally incorrect to apply the name of a glacial in one region to another. For most of the 20th century, only
2860-450: The historical terminology was established. Corresponding to the terms glacial and interglacial, the terms pluvial and interpluvial are in use (Latin: pluvia , rain). A pluvial is a warmer period of increased rainfall; an interpluvial is of decreased rainfall. Formerly a pluvial was thought to correspond to a glacial in regions not iced, and in some cases it does. Rainfall is cyclical also. Pluvials and interpluvials are widespread. There
2925-445: The immediately preceding Pliocene ("newer", from πλείων ( pleíōn , "more") and kainós ) and the immediately subsequent Holocene ("wholly new" or "entirely new", from ὅλος ( hólos , "whole") and kainós ) epoch , which extends to the present time. The Pleistocene has been dated from 2.580 million (±0.005) to 11,700 years BP with the end date expressed in radiocarbon years as 10,000 carbon-14 years BP. It covers most of
2990-622: The large amounts of material moved about by glaciers. Less common are cave deposits, travertines and volcanic deposits (lavas, ashes). Pleistocene marine deposits are found primarily in shallow marine basins mostly (but with important exceptions) in areas within a few tens of kilometres of the modern shoreline. In a few geologically active areas such as the Southern California coast, Pleistocene marine deposits may be found at elevations of several hundred metres. The modern continents were essentially at their present positions during
3055-540: The latest period of repeated glaciation , up to and including the Younger Dryas cold spell. The end of the Younger Dryas has been dated to about 9700 BCE (11,700 calendar years BP). The end of the Younger Dryas is the official start of the current Holocene Epoch . Although it is considered an epoch, the Holocene is not significantly different from previous interglacial intervals within the Pleistocene. In
3120-470: The lower Palaeolithic they disappeared, and the only hominin species found in fossilic records is Homo erectus for much of the Pleistocene. Acheulean lithics appear along with Homo erectus , some 1.8 million years ago, replacing the more primitive Oldowan industry used by A. garhi and by the earliest species of Homo . The Middle Paleolithic saw more varied speciation within Homo , including
3185-478: The megafauna and migrated north. Late Pleistocene bighorn sheep were more slender and had longer legs than their descendants today. Scientists believe that the change in predator fauna after the late Pleistocene extinctions resulted in a change of body shape as the species adapted for increased power rather than speed. The extinctions hardly affected Africa but were especially severe in North America where native horses and camels were wiped out. In July 2018,
3250-527: The north and south of Logan are rapidly growing residential suburbs. Logan has a humid continental climate ( Köppen : Dsa ) with very warm though usually dry summers and cold winters with moderate snowfall. Precipitation tends to be heaviest in the spring months. Like other areas in northern Utah, during mid-winter, high-pressure systems often situate themselves over Cache Valley, leading to strong temperature inversions. These temperature inversions trap cold air and pollutants and allow thick smog to accumulate in
3315-478: The period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology . The name is a combination of Ancient Greek πλεῖστος ( pleîstos ) 'most' and καινός ( kainós ; Latinized as cænus ) 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by
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#17327876193183380-435: The population. As of the 2000 Census there were 13,902 households counted in Logan, out of which 33.4% had children under the age of 18 living with them, 55.1% were married couples living together, 7.7% had a female householder with no husband present, and 34.0% were non-families. 17.9% of all households were made up of individuals, and 5.7% had someone living alone who was 65 years of age or older. The average household size
3445-417: The ratio of O to O (two isotopes of oxygen ) by mass (measured by a mass spectrometer ) present in the calcite of oceanic core samples is used as a diagnostic of ancient ocean temperature change and therefore of climate change. Cold oceans are richer in O , which is included in the tests of the microorganisms ( foraminifera ) contributing the calcite. A more recent version of
3510-461: The recent period of repeated glaciations. The name Plio-Pleistocene has, in the past, been used to mean the last ice age. Formerly, the boundary between the two epochs was drawn at the time when the foraminiferal species Hyalinea baltica first appeared in the marine section at La Castella, Calabria, Italy. However, the revised definition of the Quaternary , by pushing back the start date of
3575-407: The sampling process makes use of modern glacial ice cores. Although less rich in O than seawater, the snow that fell on the glacier year by year nevertheless contained O and O in a ratio that depended on the mean annual temperature. Temperature and climate change are cyclical when plotted on a graph of temperature versus time. Temperature coordinates are given in the form of
3640-649: The sole factor responsible for the variations in climate since they explain neither the long-term cooling trend over the Plio-Pleistocene nor the millennial variations in the Greenland Ice Cores known as Dansgaard-Oeschger events and Heinrich events. Milankovitch pacing seems to best explain glaciation events with periodicity of 100,000, 40,000, and 20,000 years. Such a pattern seems to fit the information on climate change found in oxygen isotope cores. In oxygen isotope ratio analysis, variations in
3705-421: The study of cyclical climate changes. The glacials in the following tables show historical usages, are a simplification of a much more complex cycle of variation in climate and terrain, and are generally no longer used. These names have been abandoned in favour of numeric data because many of the correlations were found to be either inexact or incorrect and more than four major glacials have been recognised since
3770-648: The upper boundary). The proposed section is the North Greenland Ice Core Project ice core 75° 06' N 42° 18' W. The lower boundary of the Pleistocene Series is formally defined magnetostratigraphically as the base of the Matuyama (C2r) chronozone , isotopic stage 103. Above this point there are notable extinctions of the calcareous nannofossils : Discoaster pentaradiatus and Discoaster surculus . The Pleistocene covers
3835-517: The valley about three percent of the time. This reduces the air quality to unhealthy levels and can result in the worst air pollution levels in the U.S. During the 2020 census, there were 52,778 people. The population was counted at 48,174 in the 2010 census. The racial makeup of the city in 2010 was 83.9% White , 1.0% African American , 1.0% Native American , 3.3% Asian , 0.5% Pacific Islander , 8.0% from other races , and 2.3% from two or more races. Hispanic or Latino of any race were 13.9% of
3900-470: The western slopes of the Bear River Mountains . Mount Logan rises to an elevation of 9,710 feet (2,960 m) immediately to the east, and south of Logan Canyon . The eastern portions of the city are constructed on top of shelf-like "benches", late Pleistocene sedimentary deposits created by the glacially fed Logan River feeding into the northern stretches of Lake Bonneville , building
3965-459: Was 2.92 and the average family size was 3.2. In the city, the population was spread out, with The median age was 24 years. For every 100 females, there were 92.1 males. For every 100 females age 18 and over, there were 89.5 males. As of the 2000 Census the median income for a household in the city was $ 30,778, and the median income for a family was $ 33,784. Males had a median income of $ 27,304 versus $ 19,687 for females. The per capita income for
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#17327876193184030-543: Was a series of glacials and interglacials, stadials and interstadials, mirroring periodic climate changes. The main factor at work in climate cycling is now believed to be Milankovitch cycles . These are periodic variations in regional and planetary solar radiation reaching the Earth caused by several repeating changes in the Earth's motion. The effects of Milankovitch cycles were enhanced by various positive feedbacks related to increases in atmospheric carbon dioxide concentrations and Earth's albedo. Milankovitch cycles cannot be
4095-426: Was added to the top by its first private owner. The front and rear elevations have double doors to the ground floor, and there is an original doorway on the east side. Two more openings on the east and west sides were added in 1919 using concrete lintels in lieu of the original openings' stone arches and lintels. There is a hayloft door on the eastern side and several old and new window openings on all sides. The interior
4160-589: Was sold in 1919, becoming an automobile repair shop. The owner at the time was Thomas B. Budge, who owned the Utah-Idaho Hospital across the street, later the William Budge Memorial Hospital. During the 1980s a conversion to apartment use was proposed but not pursued. The Logan Temple Barn is a 36-foot (11 m) by 36-foot (11 m) square two-story stone structure with a pyramidal wood single roof. A pigeon-house cupola
4225-701: Was the city's first mayor, elected on March 5, 1866. Other previous mayors include Craig Petersen (2014-2018) and Randy Watts (2006-2014). Logan residents are served by two public school districts; primarily Logan City School District , but also Cache County School District for certain neighborhoods. There are eight public schools in the Logan City School District: six elementary schools, one middle school, and one high school, Logan High School . The Cache County School District has four high schools outside Logan in other cities. Charter schools include Edith Bowen Laboratory School (K-6th), located on
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