View allAll Photos Tagged Include
On an errand to Fittleworth, so I chose to pause for a photo at the old bridge at Stopham.
Stopham Bridge is said to be the finest medieval bridge in Sussex. It was built in 1423 to replace an earlier (1309) wooden bridge across the River Arun. The central arch was raised in 1822 to allow masted ships access to the Wey and Arun canal further upriver. A replacement road bridge was built in the 1980s to take away heavy traffic.
www.nationaltransporttrust.org.uk/heritage-sites/heritage...
Includes 7 minifigures with assorted weapons and accessories: King Ulysses, 2 Ardun soldiers, Rothut, 2 Ustokal warriors, and an Ustokal archer
The Cowra War Cemetery includes markers for Australian WWII service personnel. These include those who died in training at the local Military Camp, and the four who were killed during the Breakout.
For the story , please visit: www.ursulasweeklywanders.com/history/war-and-pieces-cowra...
Another "lively" weather day. The harbour wall at Newhaven was taking a beating at high tide around lunchtime.
Bios
Eva Arce
Human rights activist and mother of Silvia Arce who disappeared in Juarez on March 11, 1998. Eva Arce's daughter vanished in March 1998 along with a friend, Griselda Mares. The Washington-based Inter-American Commission on Human Rights (IACHR) of the Organization of American States has accepted her case.
Cynthia Bejarano
Assistant Professor of Criminal Justice at New Mexico State University, Las Cruces, and activist. She spearheaded the “Justice for Women” Symposium in Las Cruces in March 2006. Her research interests include youth and justice; U.S. border studies and violence; and race, class, and gender issues within the criminal justice system. Professor Bejarano was involved with community-based groups in the metropolitan Phoenix area and hopes to build strong community advocacy in the New Mexico, Texas, and Chihuahua tri-state area. She is also co-founder of Amigos de las Mujeres de Juárez, a non-profit organization working to end the violence against women in Chihuahua, Mexico and the borderlands. She is currently working on an anthology with colleague Rosa-Linda Fregoso focusing on feminicides and sexual assaults against women throughout Latin America, with the tentative title Gender Terrorism: Feminicides in the Américas.
Ilder Andrés Betancourt
Ilder Betancourt will graduate with a Masters in Psychology this June from Stanford University. His research has focused on Latino gangs, specifically in Los Angeles and El Salvador. He has the unusual distinction of having written two honors theses. For his first honors thesis, entitled “Relative Deprivation Mediating Street Gang Appeal,” he constructed and conducted the experimental paradigm used with Latino youth subjects in the Pico Union area of Los Angeles, looking for gang association that occurs at the local level. For his second thesis, “From LA to El Salvador: Displaying Street Performance for the Self,” he conducted field research in El Salvador where he interviewed deported ex-gang members. He is currently teaching for the third year in a row a student-initiated course on Latino gangs in the Chicana/o Studies Program, CCSRE.
Lawrence D. Bobo
Lawrence D. Bobo is the Martin Luther King Jr. Centennial Professor at Stanford University. He is in the Sociology Department and also serves as Director of both CCSRE and the Program in African and African American Studies. Professor Bobo is an elected member of the National Academy of Science, a former Fellow of the Center for Advanced Study in the Behavioral Sciences, and former Visiting Scholar at the Russell Sage Foundation. His interests include race, ethnicity, politics, and social inequality. He is currently conducting research for the “Race, Crime, and Public Opinion” project.
Lydia Cacho
Journalist and writer, Lydia Cacho has published over 400 articles in Mexico, Spain, the United States and Canada. She is also the director of a crisis center for women and children who have been sexually abused in Cancun, Mexico. She recently received the 2007 Ginetta Sagan Award for Women’s and Children's Rights from Amnesty International for her work exposing a net of pederasts and child pornographers linked to powerful politicians and business people, as well as for her high-security shelter for victims of trafficking and violence in Cancun, Mexico. After her book Los demonios del Edén (The demons of Eden) was published, she received death threats and was kidnapped and incarcerated by the Mexican police. For 15 years she has researched, lectured, and published articles on violence against women in the State of Chihuahua and other parts of Mexico. She is an expert on issues concerning the corruption and impunity of the Mexican government. The Ginetta Sagan Award is given once a year to one woman in the world who stands out for her work on behalf of women’s and children’s rights. Lydia Cacho is the first Mexican to receive this prestigious award. She is also the author of the novel Muérdele el corazón (Bite his heart) based on the diary of a Mexican woman who dies of AIDS and is currently working on the book Trata y tráfico de mujeres en México (Trafficking in Persons: Women in Mexico).
Adriana Carmona
Human rights lawyer from the Centro de Derechos Humanos de las Mujeres (Center for Women's Human Rights) in Chihuahua City, Mexico. She has argued cases before the International Commission of Human Rights. She collaborates in the writing of reports for CEDAW and the United Nations in the area of human rights and feminicide. She is also a legislative advisor for the Congress of the State of Chihuahua and works with Justicia para Nuestras Hijas (Justice for Our Daughters), a non- government organization formed by relatives on behalf of the women who have disappeared or have been murdered in Juarez and Chihuahua, Mexico.
Carlos Castresana Fernández
Project Coordinator of the United Nations’ Office on Drugs & Crime, Mexican Regional Office. He is also Visiting Professor and Director of International Human Rights Programs at the University of San Francisco Center for Law and Global Justice. In 2003, he visited Ciudad Juarez as a UN Independent Commission Expert to participate in the review of the murder cases in the State of Chihuahua. In 2005, he was appointed Prosecutor of the Spanish Supreme Court. Professor Castresana authored the formal complaint and subsequent reports in the Argentina Case and the Pinochet Case before the Spanish Audiencia Nacional. Professor Castresana serves as an expert in international legal cooperation and other issues in Europe and Latin America. He received the National Human Rights Award in Spain in 1997, and was awarded an Honorary Doctoral Degree from Guadalajara University, Mexico in 2003. He received his law degree from the Complutense University, Madrid, Spain.
Lucha Castro
Human rights lawyer from the Centro de Derechos Humanos de las Mujeres (Center for Women’s Human Rights) in Chihuahua City, Mexico. She is also a legal advocate for Justicia para Nuestras Hijas (Justice for Our Daughters). She represents families of murdered women in the State of Chihuahua and also files the cases with the Inter-American Commission on Human Rights in Washington DC, a commission that accused the Mexican government of violating the rights of victims and their families.
Norma Cruz
Norma Cruz is an activist for women’s human rights in Guatemala. She began her struggle for justice in 1999 as the result of her own personal experience in the case of her daughter Claudia María who was a victim of sexual violence. Deeply upsetting Guatemalan society, she and her supporters refused to keep silent and made public a reality that affects thousands of Guatemalan female children. Alter a long and dehumanizing legal process, a conviction was achieved in July of 2002, shattering with it the wall of impunity. During this legal process, Norma Cruz and her daughter established the Fundación Sobrevivientes (Survivors Foundation) and began to support hundreds of women who endure violence and seek justice. In July 2006, the Foundation opened the Centro de Atención, providing legal and psychological aid for these women. The Center’s shelter offers protection for women who are victims of intra-family violence and sexual violence, and provides support for families of women who are murdered. Their struggle is directed at bringing impunity to a halt and ending feminicide in Guatemala. In June of 2005, Norma Cruz was officially nominated for the Nobel Peace Prize as part of the campaign “A Thousand Women for a Nobel Peace Prize.” In Killer’s Paradise, a new Canadian documentary focusing on feminicide in Guatemala, she analyzes the links between the murders of women and the civil war in Guatemala.
Paula Flores
An activist in the community of Lomas de Poleo in Ciudad Juarez, she is the mother of María Sagrario González Flores, who disappeared on March 11, 1998 in Juarez and was murdered in April, 1998. Her daughter is one of over 400 women who have been disappeared and slain in Juarez over the past 13 years. Paula Flores runs the María Sagrario Foundation, an organization that established the kindergarten Jardín de Niños Ma. Sagrario González Flores in Juarez.
Rosa-Linda Fregoso
Professor and Chair of Latin American and Latino Studies, and Feminist Studies, at the University of California, Santa Cruz. Rosa-Linda Fregoso received the second annual MLA Prize in United States Latina and Latino and Chicana and Chicano Literary and Cultural Studies for her book MeXicana Encounters: The Making of Social Identities on the Borderlands. Her interests include human rights, visual culture and and transnational feminist studies. Among her publications on feminicide is the recent article “’We Want Them Alive!’: The Politics and Culture of Human Rights.” Along with Cynthia Bejarano, she is co-editing a book tentatively entitled, Gender Terrorism: Feminicides in the Américas.
Judith Galarza
Mexican activist Judith Galarza Campos joined the struggle for human rights as a result of the forced disappearance of her sister Leticia Galarza Campos in 1978. From 1982 to 1996, she was President of the Independent Committee for Human Rights in Juarez. She was also President of the Association of Relatives of Missing Detainees (AFADM) from 1996 to 2000. Currently she is the Executive Secretary of the Latin American Federation of Associations of Relatives of Missing Detainees (FEDEFAM), headquartered in Venezuela. FEDEFAM provides assistance to families of “disappeared people” in all of Latin America. She has been a promoter of several family groups, among them the Association of Missing Children in Mexico in the 1980s. She is currently completing the degree of licenciatura in Education in Venezuela. On July 24th, she will be awarded the Theodor Häcker Prize in Esslingen, Germany. Häcker worked as a writer and translator during the Nazi period and was part of the Catholic resistance. First awarded in 1995, this prize is dedicated to persons who defend human rights "honorably, with special political valor.”
Marcela Lagarde
Maria Marcela Lagarde y de los Ríos is a Professor in the Graduate Program in Anthropology and Sociology as well as in the Degree Program in Gender and Development at the Universidad Nacional Autónoma de México (UNAM). She is also advisor to the Graduate Program in Gender Studies of the Guatemala Foundation and to the Program on Feminist Research at UNAM. She is the coordinator of the Casandra Workshops on feminist anthropology and advisor to the Gender Program of the Center for Interdisciplinary Research of UNAM. She is also the Secretary for the College of University Academics at UNAM, of which she became a member in 2002.
Marcela Lagarde is a major figure in Latin American feminism. She is the author of over one hundred articles and ten books. Her doctoral thesis, Los cautiverios de las mujeres: madresposas, monjas, putas, presas y locas (The captivities of women: mother-wives, nuns, prostitutes, prisoners and lunatics), has been reprinted a total of five times between 1990 and 2003. Her books examine topics such as the relationship between gender identity, feminism, human development and democracy; the relationship between ethnicity, gender and feminism; the theme of women’s power and autonomy; and feminist perspectives on love, self-concept, and the eve of the millennium.
Marcela Lagarde collaborates with feminist groups and women’s centers and institutes in Mexico, Latin America and Spain. She also works with organizations of international cooperation, labor unions and political parties focusing on women’s issues. She is a member of the Network of Researchers for the Life and Liberty of Women and other feminist networks. She is also a member of many editorial boards: of Hypatia, a collection of the Andalusian Institute for Women in Spain; of the journal Cuadernos Feministas, of the Editorial Series Diversidades Feministas published by the Center for Interdisciplinary Research at UNAM; and of the journal Pensamiento Iberoamericano, in Spain.
As to the topic that concerns us at this conference, it is Marcela Lagarde who coined the term “feminicide” to describe the situation in Juarez, Mexico. She has developed an analysis of what she calls “the politics of gender extermination” to examine the proliferation of violence in Mexico. Through her ideas, writings and activism, she wishes to leave an indelible mark on public policies.
Marcela Lagarde was a federal representative for the Partido de la Revolución Democrática (PRD) in the LIX Congress (2003-2006) and served as President of the Special Commission on Feminicide in the Republic of Mexico. It was the work of this Commission that disclosed that feminicide was not exclusive to Ciudad Juarez. Marcela Lagarde also promoted legislation establishing feminicide as a crime in the Federal Penal Code and helped pass the law Access to a Life Free of Violence for Women, which was established on February 2.
Marcela Lagarde is a member of the Mexican Academy on Human Rights (2006); of El Consejo Asesor del Centro de Formación Política Mujer y Ciudad, of the Diputación de Barcelona, España (2006); and of the Council to Prevent and Eradicate Discrimination in Mexico City (2006).
Among the many distinctions and honors Marcela Lagarde has received are the Maus Prize for the best doctoral thesis, the Medal of University Merit for 25 years of teaching at UNAM, and the Presea Águila Canacintra al Mérito Legislativo, awarded by the Cámara Nacional de la Industria de la Transformación in 2005. She also received the Omecíhuatl Medal in 2006. The Omecíhuatl Medal is awarded by the Women’s Institute of Mexico City to women who have distinguished themselves for their commitment, struggle and creativity and the defense of democracy. Also in 2006, she received the Hermila Galindo Prize from Mexico City’s Commission on Human Rights, for the defense of women’s human rights.
Miguel Méndez
Adelbert H. Sweet Professor of Law at Stanford University. After a litigation career in public interest law that included work for the Mexican American Legal Defense and Education Fund and California Rural Legal Assistance, Miguel Méndez entered academia and has become a foremost expert, scholar, and teacher in the field of evidence law. An author of leading works on the laws of evidence in California, he writes about reforms in the federal and California evidence codes and on emerging issues in state substantive criminal law. He is a consultant to the California Law Revision Commission, a board member at Public Advocates, Inc., and an elected member of the American Law Institute.
Miguel David Meza Argueta
Falsely accused on July 14, 2003 and held for the murder of Neyra Azucena Cervantes by the judicial authorities in the city of Chihuahua, Mexico. The falseness of this accusation and incarceration was established by reports from Amnesty International, news articles, and testimonies from relatives of the murdered woman, including her mother, Sra. Patti Cervantes, who is also David’s aunt. After proving that Mexican authorities tortured him, he was set free in June 2006.
Paula Moya
Associate Professor in the English Department at Stanford University, Paula Moya served for three years as Director of the Undergraduate Program in CCSRE and as Chair of its Comparative Studies major. Her interests are Chicana/o cultural studies and feminist theory, incorporating 19th and 20th century American literatures, post-colonial literature and literary and cultural theory. Her main theoretical concern centers on the relationship between a subject's social location and her identity, and seeks to interrogate the epistemic and political consequences of social identity. For the past five years, she has been actively involved with the Future of Minority Studies research project (FMS), facilitating discussions about the democratizing role of minority identity and participation in a multicultural society.
Elisabeth Mudimbe-Boyi
Professor of the French and Comparative Literature Departments and Director of the Program in Modern Thought and Literature at Stanford University. Her fields are 20th-century French literature and Francophone literature from Africa and the Caribbean. Her interests include cultural relations between Europe, Africa and the Caribbean; travel writing; history and memory in literature; literature, intellectuals and society; and women writers. She recently served on the Executive Council of the Modern Language Association, where she represented the field of French.
Marisela Ortiz
Marisela Ortiz is the Director of Nuestras Hijas de Regreso a Casa (Our Daughters on Their Way Back Home), a non-profit organization composed of mothers, family members and friends of murdered women in Ciudad Juarez, Mexico. A psychologist with a Masters degree in special education, she has taught at the Escuela Normal Superior de Chihuahua for the past 20 years, specializing in professional development. She continues to work with adolescents and also trains middle school teachers in her entire region.
David Palumbo-Liu
Professor of Comparative Literature, Director of the Undergraduate Program in CCSRE, and Chair of CCSRE’s Comparative Studies major at Stanford University. His fields of interest include social and cultural criticism; literary theory and criticism; and East Asian and Pacific Asian American studies. His current project addresses the role of contemporary humanistic literature with regard to the instruments and discourses of globalization, seeking to discover modes of affiliation and transnational ethical thinking. Professor Palumbo-Liu is most interested in issues regarding social theory, community, justice, globalization, and the specific role that literature and the humanities play in helping us address each of these areas.
Elena Poniatowska Amor
Journalist and novelist, Elena Poniatowska is one of Latin America's most distinguished and innovative living writers. Many of her works have been translated into English, including Querido Diego te abraza Quiela (Dear Diego), Hasta no verte, Jesús mío (Here's to You, Jesusa!); Nada, Nadie. Las voces del temblor (Nothing, Nobody: The Voices of the Mexican Earthquake); Tinísima; La noche de Tlatelolco. Testimonios de historia oral (Massacre in Mexico) and La piel del cielo (The Skin of the Sky). Translations of her work also exist in Polish, Danish, French, Dutch, Italian and German. Elena Poniatowska advocates for women and the poor in their struggle for social and economic justice, denounces the repression of that struggle, and blurs the boundaries between conventional literary forms.
Born in Paris, Elena Poniatowska is of Mexican and French descent. Her father was a Frenchman whose family was originally from Poland. She moved to Mexico in 1942 and began her work as a journalist at the newspaper Excelsior in 1953, where she published daily interviews during an entire year under the name "Hélene.'' She interviewed Diego Rivera, Octavio Paz, William Golding, Barry Goldwater, Dolores del Río, Cantinflas, María Félix, Juan Rulfo, and Linus Pauling, among others. From Excelsior she went to Novedades, where she drew an audience who followed her because of her unpredictable texts. She is a founder and a contributor of the leftist newspaper La Jornada, and continues to contribute to its pages.
In 1954 she published her first novel, Lilus Kikus. Chronicler of the 1985 earthquake and of the Chiapas conflict, she continues to meld her journalistic and literary work. She published Tinísima in 1992, a novel about the life of Tina Modotti, which was as successful as her novel Hasta no verte Jesús mío, about the life of a soldadera, or camp follower. Her next novel, La piel del cielo, won the Premio Alfaguara in 2001 and the prize for the best novel in Spanish awarded by the government of China. In 2004, Alfaguara published her novel El tren pasa primero, which brought to life the struggle of railroad workers and led to the reconstruction of railway stations in many parts of Mexico. During a 35-year period, she led a literary workshop that produced writers such as Silvia Molina, Guadalupe Loaeza y Rosa Nissan.
When Luis Echevarría, who had been Secretary of State during the massacre of 1968, was elected president, he awarded the Xavier Urrutia Literary Prize to Elena Poniatowska in 1971 for her book La noche de Tlatelolco. She rejected the prize asking who was going to award prizes to the dead.
She has been awarded many honorary doctoral degrees: by the University of Sinaloa, the University of Toluca, Columbia University and Manhattanville College in New York, Florida Atlantic University in Boca Raton, and the University of Pau in France. She is the only woman who has received the Mazatlán Prize in Literature on two occasions, and in 1979, she was the first woman to receive the National Prize for Journalism. In 1993, she was awarded a Guggenheim Fellowship and received the Gabriela Mistral Medal in Chile in 1997. She holds the rank of official in the French Legion of Honor, and in 2004 she received the Mary Moors Cabot Prize for Outstanding Work in Journalism. In 2006 the International Women’s Media Foundation awarded her the Courage in Journalism Lifetime Achievement Award. In addition to these she has received many other prizes and awards.
Elena Poniatowska dedicates a good part of her life to writing novels, short stories, poems, articles, interviews, prologues, and book presentations. She was married to Dr. Guillermo Haro, the founder of modern astronomy in Mexico. She has three children, the oldest of whom is a scientist, and ten grandchildren. She lives in Chimalistac with 13 canaries and an unending line of visitors.
Lourdes Portillo
Lourdes Portillo was born in Chihuahua, Mexico and moved to the United States in 1960. Her films focus on the representation of Latina/o identity, human rights, social justice and Latin American realities. An equally important aspect of her filmmaking is experimenting with the documentary form. Her most recent film, Señorita Extraviada (Missing young woman), released in 2002, is a documentary about the disappearance and death of young women in Juarez and the search for truth and justice by their families and human rights groups. It received a Special Jury Prize at the Sundance Film Festival, the Best Documentary Prize at the Havana International Film Festival, and the Néstor Almendros Prize at the Human Rights Watch Film Festival. It premiered on P.O.V. and received more than 20 prizes and awards around the world. The film inspired a number of governmental and non-governmental organizations such as Amnesty International to conduct intensive investigations into the disappearances and murders of women in Juárez. Lourdes Portillo made her first film, a dramatic short called After the Earthquake, in 1979. Some of the other documentary, dramatic, experimental and performance films and videos she has made are the Academy Award-nominated Las Madres: The Mothers of Plaza de Mayo (1986); La Ofrenda: The Days of the Dead (1988); Vida (1989); Columbus on Trial (1992); Mirrors of the Heart for the PBS series “Americas” (1993); The Devil Never Sleeps (1994); Sometimes My Feet Go Numb; 13 Days, a multi-media piece for a nationally toured play by the San Francisco Mime Troupe (1997); and Corpus (1999), a documentary about the late Tejana singer Selena.
Kris Samuelson
Professor in the Art and Art History Department at Stanford, where she is Director of the Film and Media Studies Program and the Documentary Film and Video MFA Program. She has also been a Professor in the Department of Communication, where she served as Chair from 2000-2003. Kris Samuelson has been an independent producer for twenty-eight years and was nominated for an Academy Award for her film Arthur and Lillie. She has received artist's fellowships from the NEA and the California Arts Council and is a member of the Academy of Motion Picture Arts and Sciences. From 1999-2006, Samuelson served on the Board of the Independent Television Service. Samuelson recently completed .Point 25, a multimedia concert and co-production with colleagues in Stockholm.
Rita Laura Segato
Professor of Anthropology at the University of Brasilia in Brazil, Rita Segato directs the National Research Council of Brazil’s research group on anthropology and human rights. She is also the project director for the non-government organization AGENDE, Ações em Gênero, Cidadania e Desenvolvimento ((Measures in Gender, Citizenship and Development). As part of her work on human rights, she was the co-author of the first affirmative action proposal for the inclusion of students of African and indigenous background in Brazilian higher education.
Her study on ethno-psychology and the construction of gender in the Yoruba religious tradition in Recife, Brazil was published in the book Santos e Daimones. O politeísmo afro-brasileiro e a tradição arquetipal (Saints and demons. African-Brazilian polytheism and the archetypal tradition), a second edition of which came out in 2005. A chapter from this book was translated and published as "Inventing Nature: Family, Sex and Gender In the Xango Cult" in 1997. Her essay “Gender, Politics, and Hybridism in the Transnationalization of the Yorùbá Culture” is included in the volume Òrìsà Devotion as World Religion to be published by the University of Wisconsin Press.
She has also carried out a comparative study of emerging political identities and multiculturalism within the United States, Brazil and Argentina. This study led to the publication in 2007 of the volume La Nación y sus Otros. Raza, etnicidad y diversidad religiosa en tiempos de Políticas de la Identidad (The nation and its Others: race, ethnicity and religious diversity in times of Identity Politics). Two of the articles included in this volume were published in English as "The Color-Blind Subject of Myth; or, Where to find Africa in the Nation" in 1998 and "Frontiers and Margins: The Untold Story of the Afro-Brazilian Religious Expansion to Argentina and Uruguay" in 1996.
Rita Segato carried out an extensive investigation among inmates convicted for sexual crimes in the city in which she resides, and published a book on gender and violence entitled Las estructuras elementales de la violencia (The elemental structures of violence) in 2003. In 2006 the Universidad del Claustro de Sor Juana published her essay “La escritura en el cuerpo de las mujeres asesinadas en Ciudad Juárez. Territorio, soberanía y crímenes de Segundo Estado” (Writing on the body of the murdered women of Juarez: Territory, sovereignty and crimes of the Second State). Her understanding of prison reality is the subject of her article “El sistema penal como pedagogía de la irresponsabilidad y el proyecto ‘habla preso: el derecho humano a la palabra en la cárcel’” (The penal system as a pedagogy of irresponsibility and the project prisoner talk: the right to speech in jail), accessible on the website of the Lozano Long Institute of Latin American Studies, University of Texas, Austin (http://lanic.utexas.edu/project/etext/llilas/cpa/spring03/culturaypaz/segato.pdf). Also part of this series of articles is “El color de la cárcel en América Latina. Apuntes sobre la colonialidad de la justicia en un continente en desconstrucción” (The color of jail in Latin America. Notes toward the coloniality of justice in a continent in the process of deconstruction).
Rita Segato is one of the most renowned experts on the subject of feminicide. Her most recent study is entitled “What is feminicide? Notes toward an Emerging Debate,” in which she argues that feminicide should be considered a special category of crimes against humanity in order to bring greater pressure on governments and international jurists to include it among the crimes prosecuted by the International Criminal Court of The Hague.
She has been an invited researcher at the Institute for Research in the Humanities of the University of Wisconsin-Madison and in the Department of Anthropology at Rice University in Houston, and a Visiting Professor at the Center for Latin American Studies at the University of Florida, Gainesville.
Irene Simmons
Artist, university educator, activist and creator of the art installation “ReDressing Injustice.” The “Redressing Injustice” project brings public awareness to the hundreds of unsolved murders perpetrated against women living in Juarez, Mexico. The installation features over 400 dresses hanging on pink crosses that commemorate the victims of feminicide and protest the absence of justice in Juarez. Creatively transformed dresses are continually added to this collaborative endeavor by community members in the areas where the installation is shown. The installation has been featured at political rallies, social justice forums, and memorial events both nationally and internationally since 2003.
Guadalupe Valdés
Bonnie Katz Tenenbaum Professor in the School of Education and Professor in the Spanish and Portuguese Department at Stanford University. She works in the areas of sociolinguistics and applied linguistics. Much of Guadalupe Valdés’ work has focused on the English-Spanish bilingualism of Latinas and Latinos in the United States and on discovering and describing how two languages are developed, used, and maintained by individuals who become bilingual in immigrant communities. Her interests include language diversity; bilinguals and bilingualism; heritage languages among minority populations; and the teaching of Spanish to Hispanic bilinguals and monolingual speakers of English.
Yvonne Yarbro-Bejarano
Professor in the Spanish and Portuguese Department and Chair of the Chicana/o Studies Program in CCSRE at Stanford University. Her interests include queer studies and feminist theories, and the confluence of race, gender and sexuality in cultural representations across a variety of media, especially with respect to imaginings of home, nation and family. Since 1994 she has been developing the digital archive Chicana Art, a database of images and information featuring women artists. She will offer a course on the films of Lourdes Portillo in Fall 2007.
Gwenda Yuzicappi
Standing Buffalo First Nation member and mother of 19-year-old missing Amber Redman, who disappeared in rural Saskatchewan, Canada on July 15, 2005. Her case was featured in "Stolen Sisters: Discrimination and Violence against Indigenous Women in Canada," a report released by Amnesty International that addresses the disproportionate number of First Nations women who have been abducted, and how these severe felonies have not been deemed a priority by numerous police forces.
Copyright 2007, Center for Comparative Studies in Race and Ethnicity, all rights reserved.
FEMINICIDE = SANCTIONED MURDER
gabbyjaws.blogspot.com/2024/12/still-crazy-for-christmas....
Tiffany Designs Eve Christmas Gown [Mesh] DEMO + Lara X
★★★ MESH XMAS GOWN ★★★
════════════════════════════════════════════════════
➣ Includes:
• Mesh Bra Bow
• Mesh Dress
• Mesh Gloves
• Mesh Fur
• Mesh Headbox
• Mesh Spine Decorations/lights
• Mesh Jewelry
• Glitter Emitter (white stars)
════════════════════════════════════════════════════
➣ Compatible with:
➠ LARA X
➠ MAITREYA
➠ LEGACY, Perky
➠ REBORN
➠ GENX, Curvy
➠ KUPRA
➠ ERIKA
════════════════════════════════════════════════════
★ Before buying, please try the free demo.
★ Thank you for shopping at ::TIFFANY DESIGNS:: !
☎ In world assistance if you need additional help - please contact LucyHope.
Tiffany Designs
LM: maps.secondlife.com/secondlife/Hilton%20Villas/232/207/22
MP: marketplace.secondlife.com/stores/139726?
NOVA Gigi group gift
LaraX
Schoenthal Monastery, first mentioned in 1145, includes one of the oldest churches in Switzerland. It is considered a showpiece of Romanesque architecture. Its western façade features ashlar masonry, a portal with a depiction of a lamb carrying a cross, and an arch supported by a lion baring its teeth on one side, and by a man on the other. The inscription on the arch reads: HIC EST RODO.
Of the murals on the inside of the church, a depiction of St. Christopher has been preserved above the gateway to the cloister dating from about 1310/20. Behind the eastern façade, fragments can be seen of an angel swinging a censer; these date from around 1430. The bell in the steeple was cast in Aarau in the 15th century. The deconsecrated monastery was used for various commercial purposes over a period of 500 years. As of 1986, the new owner had extensive renovations carried out in collaboration with the canton’s departments of archaeology and the preservation of historical monuments. The latter recommended using the traditional plaster made of slaked lime.
Includes teams from Estelline/Hendricks, Chamberlain, Milbank Area, Wall/Kadoka Area/Philip and Sisseton. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.
©2021 SDPB
Includes teams from Mitchell, Harrisburg, Watertown, Aberdeen Central. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.
©2021 SDPB
Includes the blanket tent, pallet mattress, milkcrate bench and camping stove. Bench has a guitar playing pose with music! Available in PG and Adult for 75L at The Sales Room! maps.secondlife.com/secondlife/MoonLand/180/33/22
More from Friday at the Goodwood Festival of Speed - the sculptured details of a Renault Grand Prix car/
Inverhuron is a community located in Bruce County within the Municipality of Kincardine in the Canadian province of Ontario. The community includes approximately 200 permanent residents and 400 seasonal cottagers. Inverhuron is located on the shore of Lake Huron, at the west end of County Road 15, just west of Highway 21 and the town of Tiverton. The village is located about halfway between Port Elgin and the town of Kincardine.
Inverhuron was first settled in the early 1840s. In 1851 Superintendent of Schools of Bruce County, William Gunn opened a general store and post office. Gunn quickly followed with a school and library. By the end of the decade Inverhuron boasted lime kilns, saw and grist mills, a quarry, numerous tradesmen including carpenters,and a blacksmith shop. During this time, Inverhuron had a peak population of around 500 people. A major shipping centre with three large grain warehouses was established in the 1870s.
Inverhuron's days of success came to an abrupt stop on April 13, 1882 when fire struck the grain warehouses and the pier. The community experienced a devastating financial loss and many of the businesses shut down or relocated elsewhere. Another fire struck the community again in 1887. After the second fire, Inverhuron was finished financially and physically.
- Inverhuron is the site of Bruce Power, the Bruce Nuclear Generating Station, the largest nuclear power facility in the world.
- Ontario's first commercial wind farm, called "Huron Wind" is located on the outskirts of Inverhuron. The wind farm consists of 5 wind turbines.
- from "Lovell's Gazetteer of the Dominion of Canada (1873)" - INVERHURON, a post village in Bruce County, Ontario, on Lake Huron, 23 miles from Southampton, it contains several saw and grist mills, 1 store and 2 hotels, and has a large grain trade. The Goderich and Saugeen steamers call here. The population in 1873 was 150.
- from "Lovell's Gazetteer of the Dominion of Canada (1908)" - INVERHURON, a post village in Bruce County, Ontario, on Lake Huron, 23 miles from Southampton, 9 miles from Kincardine, on the G.T.R. It contains 1 saw mill and 1 store. The population in 1908 was 75.
The Post Office at Inverhuron opened - 1 January 1854 and closed - 1 August 1873. It reopened - 1 July 1874 and closed - 30 December 1911. It reopened again as a summer office - 22 July 1931 and closed permanently - 1 April 1986.
/ INVERHURON / JUL 2 / 43 / ONT. / - split ring cancel.
----------------------------------------------------------------------------------------
Message on postcard reads: Dear Mrs. Lawson - I am having a wonderful time up at the lake. It has been quite chilly but is getting warmer. Elsie can add another post card to her collection now. Love, Barbara
Addressed to: Mrs. S. Lawson / 17 Chappell Street / Thorold, Ontario
★ PROMO ☆
♥ !creamSH! Dot Knit Tights ♥
Include: Maitreya applier, OMEGA applier and System tattoo layer.
!cream spaghetti hair! will participate in SaNaRae 41 ROUND.
I will release Knit Tights Series.
!creamSH! Dot Knit Tights
!creamSH! Heart Knit Tights
!creamSH! Simple Knit Tights
Available on SaNaRae.
January 26th 7:00pm Open :
includes
*texture change menu
*silver and gold metal options
TP: maps.secondlife.com/secondlife/Heavens%20Gate/214/116/1001
⭐️ [Belantti] Getsby Set
Includes Lashes & Eye Shadow
Rigged for EvoX
NOW AT THE ANTHEM EVENT
📍: maps.secondlife.com/secondlife/Anthem/123/122/1109
⭐️ [Belamour] Lick em lippies
Comes with 8 beautiful lip shades!
Rigged for: EvoX
NOW AT THE LABEL EVENT
📍: maps.secondlife.com/secondlife/The%20Label/196/96/3060
⭐️ ASCENT - Eyelet Nose Gauges
Unisex, Unrigged, resizable by script
NOW AT THE ASTROPHE EVENT
Singapore National Day Parade
Singapore celebrated its first National Day as an independent nation in 1966, one year after Singapore's separation from Malaysia on 9 August 1965.
The first National Day Parade started in the morning at 9:00 a.m. that day. People came as early as 7:00 a.m. in order to get good vantage points. Singapore's first President, Mr Yusof bin Ishak and Singapore's first Prime Minister, Mr Lee Kuan Yew, were seated with members of the government at the grandstand on the steps of City Hall. When the parade began, 6 military contingents (including the Singapore Infantry Regiment, SPDF and the then Republic of Singapore Police), a mobile column from the SIR, and various schools and civil contingents marched past City Hall and then into the city streets. Three military bands accompanied the parade inspection and later the march past with military music. The Singapore Fire Brigade also took part in this first parade with its firetrucks included in the mobile column. Rounding it all was a massed lion and dragon dance performance from drum and dragon troupes nationwide.
The following year, the contingents increased to 76, including those of the then established Singapore Armed Forces, the RSP and more cultural groups, with the addition of more civil marching groups. The reason is partly due to the introduction of the National Service program in the military and police forces, and later extended to the Fire Brigade, later called the Singapore Fire Services in the 1970s. Street performances by various groups also debuted in that year's parade. The 1968 edition, although held on a rainy morning that surprised even the marching contingents and the dignitaries, saw the first ground performances on the Padang as the weather improved - a prelude to today's show performances. 1969's parade, the one where the Mobile Column made its first drivepast, commemorated the 150th year of the city's founding and had Princess Alexandra of the UK as principal guest.
On the August 9, 1970 NDP edition, the Flypast of the State Flag and the Republic of Singapore Air Force Flypast debuted. A combat simulation performance by Singapore Army personnel was one of the new highlights for that year.
The 1971 NDP was the first to include the iconic mobile parade floats from various organizations. Choirs also debuted on that year's edition.
The 1973 parade was held from the afternoon to early evening for the first time to attract more attendance from the public. The next year, colour broadcasts of the parade on television began.
The 1975 parades, held to celebrate Singapore's 10th year, were for the first time decentralized into 13 parade venues for more public participation. Almost all of them lasted for an hour and all of them even had route marches on the streets to the participating venues.
By the time the NDP was held at the National Stadium (for the first time) in 1976, the NDP Guard of Honour, composed of officers and personnel of the SAF and the Singapore Police Force made its first appearance, followed after the parade proper by the very first evening presentations by various groups, a prelude to future evening NDPs in 1980 and from 1984 onward. 1977's parade was a decentralized event like two years before (and like 1968's was damped by the rain) while 1978 would see the parade back at the Padang grounds. 1979's parade was yet another decentralized one, held in several high schools and sports stadiums nationwide.
The 1980 parade, held at the National Stadium, almost rained at the start, but the performances went on as planned as the weather improved later. This was the first parade in which the feu de joie of the Guard-of-Honour contingents made its inaugural appearance. 1981's NDP was the very first parade appearance of the then SPF Civil Defense Command, presently the Singapore Civil Defense Force, later combined with the SFS in 1989. (The SCDF of today showed itself for the first time in the 1982 NDP held in the Padang.) They were held in two decentralised venues, Jurong and Queenstown Sports Stadiums for further increase public attendance and participation in the celebrations. 1982's parade, back at the Padang site, featured more contingents and for the first time the mobile column drove past after the marchpast had concluded, thus making it a predecessor to the parades at the Padang from 1995 onward (every 5 years).
1983 would be the final year that the NDP was held in multiple venues.
The 1984 NDP, now back at the Padang, celebrated Singapore's Silver Jubilee of self-governance and included a bigger Mobile Column, the first appearance of the popular Silent Precision Drill Squad from the Singapore Armed Forces Military Police Command and the first true evening fireworks display (plus the debut of the very first NDP theme song) while NDP 1985 celebrated the nation's 20th year with more participants in the parade segment and in the show proper. The 1986 edition was the first true evening edition of the parade, and the first to use flashlights for audience use. 1987's parade, held at the Padang, was the first ever evening event held there and featured the first appearance of the massed military bands of the SAF. 1988 saw the card stunt feature being used for the first time during the National Stadium event and the 1989 edition, the first National Stadium daytime event, saw the debut of the nationally famous Red Lions parachute team and the daylight fireworks after 1966. The parade returned to the Padang in 1990 to honor the nation's silver jubilee year, which would turn out to be the last afternoon event ever to be held.
In 1997, for the first time, there was a National Education Show, where Primary 5 students watch NDP rehearsals.
The government set up the electronic voting ticketing system in 2003 in order to tackle the problem of overcrowding. Such ticketing system enables citizens to stand a chance at winning the tickets by registering their e-mail addresses or mobile numbers at the NDP website or phonelines.
Starting 2008, the NDP is also aired all over the Asia-Pacific region through Channel NewsAsia.
2009's NDP was the first ever edition to have an integrated show including the parade segment.
In 2014 Third Warrant Officer Shirley Ng became the first female Red Lion parachutist to jump at the NDP.[1][2]
2015's parade, even as all was planned for the parade to be at the Padang, will be the first ever parade to be held both there and at the Float at Marina Bay, breaking a parade tradition in the process. NDP 2015 is the first National Day Parade without the founding leader Lee Kuan Yew, who never missed a single National Day Parade since 1966, for whom he had died on 23 March 2015, within 8 months after attending the 2014 edition.
NDP editions
The venue of the parade is usually at the historical grounds of the Padang, where the declaration of Singapore's independence was held. Since the first parade in 1966, all the way to 1975, the venue was located in this central area to bring the parade closer to the people. In 1976, the parade was held for the first time at the newly completed National Stadium, where the much larger capacity allowed for more to view the parade live.
Although offering about 60,000 seats in the National Stadium, the demand for tickets remained high. Hence there were several attempts to decentralise the venue to bring the celebration closer to more Singaporeans. From 1975 to 1983, celebrations were alternated between a decentralised event and one centered at the Padang or stadium. From 1984, the parade was held twice at the stadium before being brought back to the Padang. This three-year cycle was repeated up to 1994.
From 1995, it was decided that the Padang would be used as the venue every five years. The Padang, although historically important, posed a greater logistical challenge and also offered fewer seats for spectators. The event and rehearsals also required the closing of surrounding roads. There was a need to construct temporary spectator stands around the field. The site remained, however, the only feasible venue for the mobile column, as the heavy vehicles could not be driven onto the stadium track. The Padang was used as the main performance venue for the 2005 parade, with fringe activities decentralised to Marina South, Jurong East, Yishun and Tampines.
Several alternate locations were mooted, including the utilisation of the Padang, which is physically bigger and less likely to disrupt daily functions in the city.
Parade being held at the Marina Bay Floating Stadium in 2007
On 16 October 2005, it was announced that that 2006 NDP would be held at the old stadium for the last time before moving to The Float at Marina Bay [1]. The 130 metre by 100 metre platform would be used for the next five years until the new stadium is completed. Although offering a seating capacity of only 27,000, which is less than National Stadium, there is a vast area for 150,000 extra spectators along the Marina Bay waterfront.
Since the 2000s (decade), every year's parade would revolve around a theme which would guide the planning of the parade and show.
After ten-year hiatus, the 2016 edition of NDP will return back to the new National Stadium
From a wander around the quaint thatched cottages of Amberley. There's a similarly traditional tea room there too.
5 hand held bracketed images combined in Photomatix
The present remains of the castle include work from about 1114 to about 1476. Created as a defence against the Welsh, the castle fell to the Welsh several times in the twelfth century. Later in its history, it was unsuccessfully besieged by forces of Owain Glyndŵr in 1403 with assistance from soldiers from France and Brittany who captured Kidwelly town. The castle was relieved by a Norman army after just three weeks. The gatehouse was extensively damaged and it was rebuilt on the instructions of King Henry V. It largely escaped involvement in the English Civil War.
The plan of the castle consists of a square inner bailey defended by four round towers, which overlook a semi-circular outer curtain wall on the landward side, with the massive gatehouse next to the river. The river prevents this from being a truly concentric plan, however a jutting tower protects the riverside walls, and the final plan is very strong.
Plan of Kidwelly Castle
The castle is relatively well-preserved, and is managed by Cadw.
The surrounding countryside is reputedly haunted by the headless ghost of Gwenllian ferch Gruffydd, wife of the Welsh prince Gruffydd ap Rhys, who was beheaded in 1136
Field Hockey action at Worthing Hockey Club at Angmering School. A win for Brighton & Hove 4ths over Worthing 2nds.
Action #14 for the treasure hunt
Romanian postcard by Casa Filmului Acin.
Mia Farrow (1945) is an American actress and activist who has built a remarkable film career spanning over six decades. She had her breakthrough on TV in the series Peyton Place (1965-1966). Her films include Rosemary's Baby ( 1968), The Great Gatsby (1974) and 13 films with Woody Allen. Farrow is also celebrated for her humanitarian work.
Mia Farrow was born Maria de Lourdes Villiers Farrow in 1945, in Los Angeles, California, USA. She grew up in a privileged Hollywood household as the third child and eldest daughter of Australian film director John Farrow and Irish actress Maureen O'Sullivan, who was famous for playing Jane in the classic Tarzan films. Her childhood godparents included the famous director George Cukor and journalist Louella Parsons. At the age of nine, she contracted polio, an illness that required her to be isolated during her recovery. A few years later, her eldest brother, Michael, sadly died in a plane crash at just 19 years old. These experiences had a big impact on her. Farrow started her career as a fashion model and appeared in a few small, uncredited film roles for her father, such as in John Paul Jones (John Farrow, 1959). Her big break came in the mid-1960s when she landed the role of Allison MacKenzie in the popular American television soap opera Peyton Place (1964-1966). Her performance made her a household name in the US and established her as a rising star, known for her 'hippie' look and vulnerability. After leaving Peyton Place and her short-lived, high-profile marriage to singer Frank Sinatra in the late 1960s, Farrow focused on her film career. Her most iconic and defining role came in the psychological horror film Rosemary's Baby (Roman Polanski, 1968). In this chilling film, she played a young, pregnant woman who suspects her neighbours are part of a satanic cult. Critic Roger Ebert: "The characters and the story transcend the plot. In most horror films, and indeed in most suspense films of the Alfred Hitchcock tradition, the characters are at the mercy of the plot. In this one, they emerge as human beings actually doing these things. A great deal of the credit for this achievement must go to Mia Farrow, as Rosemary, and Ruth Gordon, as Mrs. Castevet, the next-door neighbor. Here are two of the finest performances by actresses this year." Her performance earned her a BAFTA and a Golden Globe nomination for Best Actress. Throughout the 1970s, Farrow explored diverse roles in both theatre and film. She became the first American actress to join the prestigious Royal Shakespeare Company in London. Notable film appearances during this time included playing the beautiful but complex character of Daisy Buchanan in The Great Gatsby (Jack Clayton, 1974) opposite Robert Redford and a supporting role in the star-studded mystery film Death on the Nile (John Guillermin, 1978).
Mia Farrow's professional and personal life took a significant turn in the early 1980s when she began a long relationship with the writer and director Woody Allen. Over a decade, she became his muse and appeared in 13 of his films, showcasing her versatility and range. These collaborations are among her most celebrated works. Their first film together was the charming fantasy The Purple Rose of Cairo (Woody Allen, 1985), where she played a lonely waitress whose film hero steps off the screen. Critic Roger Ebert: "'Purple Rose' is delightful from beginning to end, not only because of the clarity and charm with which (Jeff) Daniels and Farrow explore the problems of their characters, but also because the movie is so intelligent. It’s not brainy or intellectual—no one in the whole movie speaks with more complexity than your average 1930s movie hero—but the movie is filled with wit and invention, and Allen trusts us to find the ironies, relish the contradictions, and figure things out for ourselves. " She also starred in the critically acclaimed comedy-drama Hannah and Her Sisters (Woody Allen, 1986), playing the central character, a dedicated, anxious woman. Other major roles in his films included Zelig (Woody Allen, 1983), a mockumentary about a man who can change his appearance to look like anyone around him; the comedy Broadway Danny Rose (Woody Allen, 1984), where she played a tough, gum-chewing mob widow; and the drama Crimes and Misdemeanors (Woody Allen, 1989). These roles solidified her reputation as one of the era's leading actresses, earning her more award nominations. The relationship with Allen ended in the early 1990s in a very public and painful scandal involving a custody battle over their children. This highly publicised period shifted some of the media's focus from her acting to her personal life and family. Beyond the screen, Farrow is perhaps even more well-known for her extensive humanitarian work. She has served as a UNICEF Goodwill Ambassador, travelling to war zones and areas affected by poverty and disease, particularly in Africa. Her efforts in places like Darfur and Chad have drawn international attention to crises and made her one of Time magazine's most influential people in the world in 2008. Farrow has a very large family, with 14 children in total, many of whom are adopted. She raised her family primarily in New York and Connecticut. Her memoir, 'What Falls Away', published in 1997, discusses her life journey, from her Hollywood childhood and the polio ward to her marriages and her struggle to protect her children during difficult times. In recent years, Farrow has continued to act occasionally, with supporting roles in films like the Horror remake The Omen (John Moore, 2006) and the comedy Be Kind Rewind (Michel Gondry, 2008). She also returned to the stage, earning a Tony Award nomination for her performance in the play 'The Roommate' on Broadway in 2025.
Sources: Roger Ebert (Roger Ebert.com), Alexis Soloski (New York Times), Britannica, Wikipedia (English, German and Dutch) and IMDb.
And, please check out our blog European Film Star Postcards.
include something (red) in the photograph .... It was pioneered by National Geographic photographers, who had subjects wear, or chose subjects who wore overly colorful clothes, (not necessarily red) though red was preferred as it rendered best on Kodachrome film.
------------------
HIT THE 'L' KEY FOR A BETTER VIEW! Thanks for the favs and comments. Much Appreciated.
-------------
All of my photographs are under copyright ©. None of these photographs may be reproduced and/or used in any way without my permission.
© VanveenJF Photography
Canyonlands National Park is an American national park located in southeastern Utah near the town of Moab. The park preserves a colorful landscape eroded into numerous canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964.
The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the combined rivers—the Green and Colorado—which carved two large canyons into the Colorado Plateau. While these areas share a primitive desert atmosphere, each retains its own character. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
In the early 1950s, Bates Wilson, then superintendent of Arches National Monument, began exploring the area to the south and west of Moab, Utah. After seeing what is now known as the Needles District of Canyonlands National Park, Wilson began advocating for the establishment of a new national park that would include the Needles. Additional explorations by Wilson and others expanded the areas proposed for inclusion into the new national park to include the confluence of Green and Colorado rivers, the Maze District, and Horseshoe Canyon.
In 1961, Secretary of the Interior Stewart Udall was scheduled to address a conference at Grand Canyon National Park. On his flight to the conference, he flew over the Confluence (where the Colorado and Green rivers meet). The view apparently sparked Udall's interest in Wilson's proposal for a new national park in that area and Udall began promoting the establishment of Canyonlands National Park.
Utah Senator Frank Moss first introduced legislation into Congress to create Canyonlands National Park. His legislation attempted to satisfy both nature preservationists' and commercial developers' interests. Over the next four years, his proposal was struck down, debated, revised, and reintroduced to Congress many times before being passed and signed into creation.
In September, 1964, after several years of debate, President Lyndon B. Johnson signed Pub.L. 88–590, which established Canyonlands National Park as a new national park. Bates Wilson became the first superintendent of the new park and is often referred to as the "Father of Canyonlands."
The Colorado River and Green River combine within the park, dividing it into three districts called the Island in the Sky, the Needles, and the Maze. The Colorado River flows through Cataract Canyon below its confluence with the Green River.
The Island in the Sky district is a broad and level mesa in the northern section of the park, between the Colorado and Green rivers. The district has many viewpoints overlooking the White Rim, a sandstone bench 1,200 feet (370 m) below the Island, and the rivers, which are another 1,000 feet (300 m) below the White Rim.
The Needles district is located south of the Island in the Sky, on the east side of the Colorado River. The district is named for the red and white banded rock pinnacles which are a major feature of the area. Various other naturally sculpted rock formations are also within this district, including grabens, potholes, and arches. Unlike Arches National Park, where many arches are accessible by short to moderate hikes, most of the arches in the Needles district lie in backcountry canyons, requiring long hikes or four-wheel drive trips to reach them.
The Ancestral Puebloans inhabited this area and some of their stone and mud dwellings are well-preserved, although the items and tools they used were mostly removed by looters. The Ancestral Puebloans also created rock art in the form of petroglyphs, most notably on Newspaper Rock along the Needles access road.
The Maze district is located west of the Colorado and Green rivers. The Maze is the least accessible section of the park, and one of the most remote and inaccessible areas of the United States.
A geographically detached section of the park located north of the Maze district, Horseshoe Canyon contains panels of rock art made by hunter-gatherers from the Late Archaic Period (2000-1000 BC) pre-dating the Ancestral Puebloans. Originally called Barrier Canyon, Horseshoe's artifacts, dwellings, pictographs, and murals are some of the oldest in America. The images depicting horses date from after 1540 AD, when the Spanish reintroduced horses to America.
Since the 1950s, scientists have been studying an area of 200 acres (81 ha) completely surrounded by cliffs. The cliffs have prevented cattle from ever grazing on the area's 62 acres (25 ha) of grassland. According to the scientists, the site may contain the largest undisturbed grassland in the Four Corners region. Studies have continued biannually since the mid-1990s. The area has been closed to the public since 1993 to maintain the nearly pristine environment.
Mammals that roam this park include black bears, coyotes, skunks, bats, elk, foxes, bobcats, badgers, ring-tailed cats, pronghorns, desert bighorn sheep, and cougars. Desert cottontails, kangaroo rats and mule deer are commonly seen by visitors.
At least 273 species of birds inhabit the park. A variety of hawks and eagles are found, including the Cooper's hawk, the northern goshawk, the sharp-shinned hawk, the red-tailed hawk, the golden and bald eagles, the rough-legged hawk, the Swainson's hawk, and the northern harrier. Several species of owls are found, including the great horned owl, the northern saw-whet owl, the western screech owl, and the Mexican spotted owl. Grebes, woodpeckers, ravens, herons, flycatchers, crows, bluebirds, wrens, warblers, blackbirds, orioles, goldfinches, swallows, sparrows, ducks, quail, grouse, pheasants, hummingbirds, falcons, gulls, and ospreys are some of the other birds that can be found.
Several reptiles can be found, including eleven species of lizards and eight species of snake (including the midget faded rattlesnake). The common kingsnake and prairie rattlesnake have been reported in the park, but not confirmed by the National Park Service.
The park is home to six confirmed amphibian species, including the red-spotted toad, Woodhouse's toad, American bullfrog, northern leopard frog, Great Basin spadefoot toad, and tiger salamander. The canyon tree frog was reported to be in the park in 2000, but was not confirmed during a study in 2004.
Canyonlands National Park contains a wide variety of plant life, including 11 cactus species,[34] 20 moss species, liverworts, grasses and wildflowers. Varieties of trees include netleaf hackberry, Russian olive, Utah juniper, pinyon pine, tamarisk, and Fremont's cottonwood. Shrubs include Mormon tea, blackbrush, four-wing saltbush, cliffrose, littleleaf mountain mahogany, and snakeweed
Cryptobiotic soil is the foundation of life in Canyonlands, providing nitrogen fixation and moisture for plant seeds. One footprint can destroy decades of growth.
According to the Köppen climate classification system, Canyonlands National Park has a cold semi-arid climate ("BSk"). The plant hardiness zones at the Island in the Sky and Needles District Visitor Centers are 7a with an average annual extreme minimum air temperature of 4.0 °F (-15.6 °C) and 2.9 °F (-16.2 °C), respectively.
The National Weather Service has maintained two cooperative weather stations in the park since June 1965. Official data documents the desert climate with less than 10 inches (250 millimetres) of annual rainfall, as well as hot, mostly dry summers and cold, occasionally wet winters. Snowfall is generally light during the winter.
The station in The Neck region reports an average January temperature of 29.6 °F and an average July temperature of 79.3 °F. Average July temperatures range from a high of 90.8 °F (32.7 °C) to a low of 67.9 °F (19.9 °C). There are an average of 45.7 days with highs of 90 °F (32 °C) or higher and an average of 117.3 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 105 °F (41 °C) on July 15, 2005, and the lowest recorded temperature was −13 °F (−25 °C) on February 6, 1989. Average annual precipitation is 9.33 inches (237 mm). There are an average of 59 days with measurable precipitation. The wettest year was 1984, with 13.66 in (347 mm), and the driest year was 1989, with 4.63 in (118 mm). The most precipitation in one month was 5.19 in (132 mm) in October 2006. The most precipitation in 24 hours was 1.76 in (45 mm) on April 9, 1978. Average annual snowfall is 22.8 in (58 cm). The most snowfall in one year was 47.4 in (120 cm) in 1975, and the most snowfall in one month was 27.0 in (69 cm) in January 1978.
The station in The Needles region reports an average January temperature of 29.7 °F and an average July temperature of 79.1 °F.[44] Average July temperatures range from a high of 95.4 °F (35.2 °C) to a low of 62.4 °F (16.9 °C). There are an average of 75.4 days with highs of 90 °F (32 °C) or higher and an average of 143.6 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 107 °F (42 °C) on July 13, 1971, and the lowest recorded temperature was −16 °F (−27 °C) on January 16, 1971. Average annual precipitation is 8.49 in (216 mm). There are an average of 56 days with measurable precipitation. The wettest year was 1969, with 11.19 in (284 mm), and the driest year was 1989, with 4.25 in (108 mm). The most precipitation in one month was 4.43 in (113 mm) in October 1972. The most precipitation in 24 hours was 1.56 in (40 mm) on September 17, 1999. Average annual snowfall is 14.4 in (37 cm). The most snowfall in one year was 39.3 in (100 cm) in 1975, and the most snowfall in one month was 24.0 in (61 cm) in March 1985.
National parks in the Western US are more affected by climate change than the country as a whole, and the National Park Service has begun research into how exactly this will effect the ecosystem of Canyonlands National Park and the surrounding areas and ways to protect the park for the future. The mean annual temperature of Canyonlands National Park increased by 2.6 °F (1.4 °C) from 1916 to 2018. It is predicted that if current warming trends continue, the average highs in the park during the summer will be over 100 °F (40 °C) by 2100. In addition to warming, the region has begun to see more severe and frequent droughts which causes native grass cover to decrease and a lower flow of the Colorado River. The flows of the Upper Colorado Basin have decreased by 300,000 acre⋅ft (370,000,000 m3) per year, which has led to a decreased amount of sediment carried by the river and rockier rapids which are more frequently impassable to rafters. The area has also begun to see an earlier spring, which will lead to changes in the timing of leaves and flowers blooming and migrational patterns of wildlife that could lead to food shortages for the wildlife, as well as a longer fire season.
The National Park Service is currently closely monitoring the impacts of climate change in Canyonlands National Park in order to create management strategies that will best help conserve the park's landscapes and ecosystems for the long term. Although the National Park Service's original goal was to preserve landscapes as they were before European colonization, they have now switched to a more adaptive management strategy with the ultimate goal of conserving the biodiversity of the park. The NPS is collaborating with other organizations including the US Geological Survey, local indigenous tribes, and nearby universities in order to create a management plan for the national park. Right now, there is a focus on research into which native plants will be most resistant to climate change so that the park can decide on what to prioritize in conservation efforts. The Canyonlands Natural History Association has been giving money to the US Geological Survey to fund this and other climate related research. They gave $30,000 in 2019 and $61,000 in 2020.
A subsiding basin and nearby uplifting mountain range (the Uncompahgre) existed in the area in Pennsylvanian time. Seawater trapped in the subsiding basin created thick evaporite deposits by Mid Pennsylvanian. This, along with eroded material from the nearby mountain range, became the Paradox Formation, itself a part of the Hermosa Group. Paradox salt beds started to flow later in the Pennsylvanian and probably continued to move until the end of the Jurassic. Some scientists believe Upheaval Dome was created from Paradox salt bed movement, creating a salt dome, but more modern studies show that the meteorite theory is more likely to be correct.
A warm shallow sea again flooded the region near the end of the Pennsylvanian. Fossil-rich limestones, sandstones, and shales of the gray-colored Honaker Trail Formation resulted. A period of erosion then ensued, creating a break in the geologic record called an unconformity. Early in the Permian an advancing sea laid down the Halgaito Shale. Coastal lowlands later returned to the area, forming the Elephant Canyon Formation.
Large alluvial fans filled the basin where it met the Uncompahgre Mountains, creating the Cutler red beds of iron-rich arkose sandstone. Underwater sand bars and sand dunes on the coast inter-fingered with the red beds and later became the white-colored cliff-forming Cedar Mesa Sandstone. Brightly colored oxidized muds were then deposited, forming the Organ Rock Shale. Coastal sand dunes and marine sand bars once again became dominant, creating the White Rim Sandstone.
A second unconformity was created after the Permian sea retreated. Flood plains on an expansive lowland covered the eroded surface and mud built up in tidal flats, creating the Moenkopi Formation. Erosion returned, forming a third unconformity. The Chinle Formation was then laid down on top of this eroded surface.
Increasingly dry climates dominated the Triassic. Therefore, sand in the form of sand dunes invaded and became the Wingate Sandstone. For a time climatic conditions became wetter and streams cut channels through the sand dunes, forming the Kayenta Formation. Arid conditions returned to the region with a vengeance; a large desert spread over much of western North America and later became the Navajo Sandstone. A fourth unconformity was created by a period of erosion.
Mud flats returned, forming the Carmel Formation, and the Entrada Sandstone was laid down next. A long period of erosion stripped away most of the San Rafael Group in the area, along with any formations that may have been laid down in the Cretaceous period.
The Laramide orogeny started to uplift the Rocky Mountains 70 million years ago and with it, the Canyonlands region. Erosion intensified and when the Colorado River Canyon reached the salt beds of the Paradox Formation the overlying strata extended toward the river canyon, forming features such as The Grabens. Increased precipitation during the ice ages of the Pleistocene quickened the rate of canyon excavation along with other erosion. Similar types of erosion are ongoing, but occur at a slower rate.
Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.
Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.
People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.
Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.
The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.
Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.
The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:
use of the bow and arrow while hunting,
building pithouse shelters,
growing maize and probably beans and squash,
building above ground granaries of adobe or stone,
creating and decorating low-fired pottery ware,
producing art, including jewelry and rock art such as petroglyphs and pictographs.
The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.
These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.
In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.
In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.
Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.
At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.
The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.
A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.
Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.
Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.
Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.
Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.
Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.
The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.
Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.
Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.
In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.
The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.
Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.
After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.
As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.
Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.
Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.
Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.
Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.
On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.
Main article: Latter Day Saint polygamy in the late-19th century
During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.
The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.
Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:
William Torrington in Carson City (then a part of Utah territory), 1859
Thomas Coleman (Black man) in Salt Lake City, 1866
3 unidentified men at Wahsatch, winter of 1868
A Black man in Uintah, 1869
Charles A. Benson in Logan, 1873
Ah Sing (Chinese man) in Corinne, 1874
Thomas Forrest in St. George, 1880
William Harvey (Black man) in Salt Lake City, 1883
John Murphy in Park City, 1883
George Segal (Japanese man) in Ogden, 1884
Joseph Fisher in Eureka, 1886
Robert Marshall (Black man) in Castle Gate, 1925
Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).
Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.
Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.
During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.
In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.
Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.
Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.
As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.
One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.
It is estimated that 1,450 soldiers from Utah were killed in the war.
Includes a colour hud with 6 options. Comes in sizes - Signature Gianni, Belleza Jake, Aesthetic, Slink, TMP, Adam & Classic
This lovely steamer includes,
1 3 Piece Steamer (6.5"W x 5.5H)
5 Gyoza (3")
3 Pork Buns (2" to 2.5")
2 Shiitake caps (2")
3 Carrots Slices (1.5")
2 Round Leaves (5.25")
3 Snow Peas (3")
Hand sewn except for underneath the mushroom caps and the patterns on the greens. Made from craft felt and stuffed with polyfil. Pork buns are white and gyozas are off white. Please handle them with care.
Wearable and rezzable, includes a texture hud with 33 textures for the Headphones plus a wooden stand to put them on.
(it's mod so all surfaces are tintable with face select)
-------------------------
-Headphones 1 prim
-Stand 1 prim
-Copy/Mod
-Original Mesh + Materials
Available @ Main Store:
maps.secondlife.com/secondlife/Neverdol/167/118/74
Marketplace:
Devils Tower (also known as Bear Lodge Butte) is a butte, possibly laccolithic, composed of igneous rock in the Bear Lodge Ranger District of the Black Hills, near Hulett and Sundance in Crook County, northeastern Wyoming, above the Belle Fourche River. It rises 1,267 feet (386 m) above the Belle Fourche River, standing 867 feet (265 m) from summit to base. The summit is 5,112 feet (1,559 m) above sea level.
Devils Tower was the first United States national monument, established on September 24, 1906 by President Theodore Roosevelt. The monument's boundary encloses an area of 1,347 acres (545 ha).
Native American names for the monolith include "Bear's House" or "Bear's Lodge" (or "Bear's Tipi", "Home of the Bear", "Bear's Lair"); Cheyenne, Lakota: Matȟó Thípila, Crow: Daxpitcheeaasáao ("Home of Bears"), "Aloft on a Rock" (Kiowa), "Tree Rock", "Great Gray Horn", and "Brown Buffalo Horn" (Lakota: Ptehé Ǧí).
The name "Devil's Tower" originated in 1875 during an expedition led by Colonel Richard Irving Dodge, when his interpreter reportedly misinterpreted a native name to mean "Bad God's Tower". All information signs in that area use the name "Devils Tower", following a geographic naming standard whereby the apostrophe is omitted.
In 2005, a proposal to recognize several Native American ties through the additional designation of the monolith as Bear Lodge National Historic Landmark were opposed by United States Representative Barbara Cubin, arguing that a "name change will harm the tourist trade and bring economic hardship to area communities". In November 2014, Arvol Looking Horse proposed renaming the geographical feature "Bear Lodge" and submitted the request to the United States Board on Geographic Names. A second proposal was submitted to request that the U.S. acknowledge what it described as the "offensive" mistake in keeping the current name and to rename the monument and sacred site Bear Lodge National Historic Landmark. The formal public comment period ended in fall 2015. Local state senator Ogden Driskill opposed the change. The name was not changed.
The landscape surrounding Devils Tower is composed mostly of sedimentary rocks. The oldest rocks visible in Devils Tower National Monument were laid down in a shallow sea during the Triassic.[citation needed] This dark red sandstone and maroon siltstone, interbedded with shale, can be seen along the Belle Fourche River. Oxidation of iron minerals causes the redness of the rocks. This rock layer is known as the Spearfish Formation. Above the Spearfish Formation is a thin band of white gypsum, called the Gypsum Springs Formation, Jurassic in age.[citation needed] Overlying this formation is the Sundance Formation. During the Paleocene Epoch, 56 to 66 million years ago, the Rocky Mountains and the Black Hills were uplifted.[citation needed] Magma rose through the crust, intruding into the existing sedimentary rock layers.
Devils Tower is composed of a porphyritic phonolite (left), and close-up view of the columns (right)
Geologists Carpenter and Russell studied Devils Tower in the late 19th century and came to the conclusion that it was formed by an igneous intrusion. In 1907, geologists Nelson Horatio Darton and C. C. O'Harra (of the South Dakota School of Mines) theorized that Devils Tower must be an eroded remnant of a laccolith.
The igneous material that forms the Tower is a phonolite porphyry intruded about 40.5 million years ago, a light to dark-gray or greenish-gray igneous rock with conspicuous crystals of white feldspar. As the magma cooled, hexagonal columns formed (though sometimes 4-, 5-, and 7-sided columns were possible), up to 20 feet (6.1 m) wide and 600 feet (180 m) tall.
As rain and snow continue to erode the sedimentary rocks surrounding the Tower's base, more of Devils Tower will be exposed. Nonetheless, the exposed portions of the Tower still experience certain amounts of erosion. Cracks along the columns are subject to water and ice erosion. Portions, or even entire columns, of rock at Devils Tower are continually breaking off and falling. Piles of broken columns, boulders, small rocks, and stones, called scree, lie at the base of the tower, indicating that it was once wider than it is today.
The geologically-related Missouri Buttes are located 3.5 mi (5.6 km) northwest of Devils Tower.
According to the traditional Indigenous beliefs of the Kiowa and Lakota, a group of girls went out to play and were spotted by several giant bears, who began to chase them. In an effort to escape the bears, the girls climbed atop a rock, fell to their knees, and prayed to the Great Spirit to save them. Hearing their prayers, the Great Spirit made the rock rise from the ground towards the heavens so that the bears could not reach the girls. The bears, in an effort to climb the rock, left deep claw marks in the sides, which had become too steep to climb. Those are the marks which appear today on the sides of Devils Tower. When the girls reached the sky, they were turned into the stars of the Pleiades.
Another version tells that two Sioux boys wandered far from their village when Mato the bear, a huge creature that had claws the size of tipi poles, spotted them, and wanted to eat them for breakfast. He was almost upon them when the boys prayed to Wakan Tanka the Creator to help them. They rose up on a huge rock, while Mato tried to get up from every side, leaving huge scratch marks as he did. Finally, he sauntered off, disappointed and discouraged. The bear came to rest east of the Black Hills at what is now Bear Butte. Wanblee, the eagle, helped the boys off the rock and back to their village. A painting depicting this legend by artist Herbert A. Collins hangs over the fireplace in the visitor center at Devils Tower.
In a Cheyenne version of the story, the giant bear pursues the girls and kills most of them. Two sisters escape back to their home with the bear still tracking them. They tell two boys that the bear can only be killed with an arrow shot through the underside of its foot. The boys have the sisters lead the bear to Devils Tower and trick it into thinking they have climbed the rock. The boys attempt to shoot the bear through the foot while it repeatedly attempts to climb up and slides back down leaving more claw marks each time. The bear was finally scared off when an arrow came very close to its left foot. This last arrow continued to go up and never came down.
Wooden Leg, a Northern Cheyenne, related another legend told to him by an old man as they were traveling together past the Devils Tower around 1866–1868. An Indigenous man decided to sleep at the base of Bear Lodge next to a buffalo head. In the morning he found that both he and the buffalo head had been transported to the top of the rock by the Great Medicine with no way down. He spent another day and night on the rock with no food or water. After he had prayed all day and then gone to sleep, he awoke to find that the Great Medicine had brought him back down to the ground, but left the buffalo head at the top near the edge. Wooden Leg maintained that the buffalo head was clearly visible through the old man's spyglass. At the time, the tower had never been climbed and a buffalo head at the top was otherwise inexplicable.
The buffalo head gives this story special significance for the Northern Cheyenne. All the Cheyenne maintained in their camps a sacred teepee to the Great Medicine containing the tribal sacred objects. In the case of the Northern Cheyenne, the sacred object was a buffalo head.
N. Scott Momaday (Kiowa) was given the name Tsoai-talee (Rock Tree Boy) by Pohd-lohk, a Kiowa elder, linking the child to the Devils Tower bear myth. To reinforce this mythic connection, his parents took him there. Momaday incorporated the bear myth as unifying subtext into his 1989 novel The Ancient Child.
The Bighorn Mountains are a mountain range in northern Wyoming and southern Montana in the United States, forming a northwest-trending spur from the Rocky Mountains extending approximately 200 mi (320 km) northward on the Great Plains. They are separated from the Absaroka Range, which lie on the main branch of the Rockies to the west, by the Bighorn Basin. Much of the land is contained within the Bighorn National Forest.
The Bighorns were uplifted during the Laramide orogeny beginning approximately 70 million years ago. They consist of over 9,000 ft (2,700 m) of sedimentary rock strata laid down before mountain-building began: the predominantly marine and near-shore sedimentary layers range from the Cambrian through the Lower Cretaceous, and are often rich in fossils. There is an unconformity where Silurian strata were exposed to erosion and are missing. The granite bedrock below these sedimentary layers is now exposed along the crest of the Bighorns. The precambrian formations contain some of the oldest rocks in the world, at 3.25 billion years old. Following the uplift, large volumes of sediments, rich in early Tertiary fossils, were deposited in the adjoining basins. The ice ages of the Pleistocene led to extensive glaciation. Though many cirques, U-shaped valleys and glacial lakes can be found in the mountain range, the only remaining active glacier is the Cloud Peak Glacier, which is on the east slope of Cloud Peak.
Geologist N.H. Darton with the U.S. Geological Survey produced one of the earliest studies of geology in the area, drawn from field research from 1901-1905.
Despite extensive prospecting in the Bighorns, no major deposits of precious metals have been found to date. Brief gold rushes of placer deposits occurred at Bald Mountain City and Porcupine Creek, and in Big Goose Canyon. The lack of precious metals helped stave off development and settlement in the mountains, in contrast to the Colorado Rockies.
The Madison limestone aquifer provides a significant source of groundwater for the town of Dayton. Limestone karst formations throughout the range contain many fissures and cracks that have developed into extensive cave systems, including Tongue River Cave, and the caves adjacent to Medicine Mountain. The Natural Trap Cave on the west slope of the Bighorns contains numerous remains of prehistoric mammals.
The highest peaks within the Bighorns are located in Wyoming in the 1.12×106-acre (4,500 km2) Bighorn National Forest. Two peaks rise to over 13,000 feet (3,960 m): Cloud Peak (13,175 ft, 4013 m) and Black Tooth Mountain (13,005 ft, 3964 m). There are a dozen more that rise to over 12,000 feet (3,650 m). From the east the mountains present a vertical relief of over 8,000 feet (2,450 m), rising abruptly from the plains. Overall, the Bighorns are more rounded than their sister mountain ranges to the west.
The Cloud Peak Wilderness is the centerpiece of a roadless block of land around 189,000 acres in size. The Wilderness is surrounded by acreage of U.S National Forest as well as Bureau of Land Management, state, and some private land. Most of the Cloud Peak Wilderness is above the tree line; the National Forest lands surrounding it are lower in elevation and covered in coniferous forests. Mule deer, elk, moose, black bear, and mountain lion are found throughout the area.
Two more large roadless areas remained in the Bighorns as of 1992. It is unknown whether these areas have since been reduced in size by road-building and other development. Both areas straddle the Montana-Wyoming state line, in the northern part of the range. One area, north of U.S. Route 14A and containing the headwaters of the Little Bighorn River, is 155,000 acres of National Forest land. This little-known region features subalpine terrain cut by steep canyons. Pronghorn inhabit the area, as it includes a portion of the Great Plains. What little human use it receives is from hunters and fishermen. The second roadless area is located mainly on the Crow Indian Reservation in Montana; its 144,000 acres also includes 34,000 acres of Devil's Canyon on the Bighorn N.F. in Wyoming. In this part of the range, semidesert prairie is cut by steep canyons leading to Yellowtail Reservoir, and high, Douglas-fir cloaked ridges top out at over 9,000'. Colorful rock formations are common. Rocky Mountain juniper and limber pine are scattered on lower elevations, and wildlife includes pronghorn, rattlesnake, golden eagle, ferruginous hawk, and mule deer. The Crow Indians manage a wild bison herd on this portion of the Bighorns. The Crow lands are a sacred area, and thus are off-limits to non-tribal members.
The three highways traversing the Bighorns are designated Scenic Byways by the US Forest Service and the State of Wyoming. These include U.S. Routes 14, 14A, and 16.
The high elevation of the Bighorns results in condensation of air and significant yearly snowfall, creating a highland oasis of moisture towering over the otherwise arid plains that surround the range in all directions. The melting snow feeds many rivers through the summer months. The range is the location of the headwaters of the Little Bighorn, Tongue, and Powder rivers.
Bighorn Canyon National Recreation Area consists of approximately 120,000 acres (490 km2) within the Bighorn Mountains. It includes Bighorn Lake, a reservoir damming the Bighorn River.
In 2015, a sudden, huge 'gash' was found in Wyoming's Big Horn Mountains. The Wyoming Geological Survey studied the area and determined that "The Crack" may be the result of an "apparent active landslide" in the southern end of the Big Horn Mountains.
The Bighorns provided important resources for ancestral indigenous people, including plants, migratory big game, rock shelters, tepee poles, and stone for tools. American Indian trails crisscrossed the range, while the canyons provided important winter shelters. Stone game blinds in the high country were used by pedestrian hunters to kill migratory big game animals with atlatl-propelled spears or bows. The northern Bighorns and the Tongue River drainage were formerly a significant summer range for migratory bison that wintered in either the Bighorn Basin and the Powder River/Tongue River/Little Bighorn River drainages. The southern Bighorns, particularly in the Middle Fork of the Powder River, contained an important American Indian trail adjacent to a bison migration corridor. The Wilson Price Hunt expedition of Astorians noted in 1811 that the bison dung was so dense in this area that it resembled a "continuous barnyard" for several miles. Hunt noticed Shoshone and Crow Indians in the area. The Medicine Wheel on the northern end of the Bighorns is an important sacred site built by ancestral tribes that is still used in present-day American Indian ceremonies.
Ancestors of the Shoshone Tribe likely had the longest continuous association with the Bighorns, potentially dating back 1,000 years or more. Stone artifacts found in the Absaroka Range farther west are known to have originated in the Bighorns, suggesting ancestral movement between the two ranges.
The Apsalooke or Crow tribe located in this region about 300–400 years ago after discovering the sacred tobacco plant growing in the Bighorn Mountains below Cloud Peak. This ended a multi-generational sojourn that began near Devils Lake, North Dakota, where a leader named No Vitals received a vision to seek the tobacco. The Crow chief Arapooish gave a speech in the 1830s showing that his people were fully aware of the migratory behaviors of bighorn sheep and deer, which spent summer on high-elevation summer range in the Bighorns and other mountain ranges.
Cheyenne, Arapaho, and Lakota use of the Bighorns region mostly dates to the period after 1800, when they made incursions into traditional Shoshone and Crow territory. Of the Cheyenne, Arapaho and Lakota, the Arapaho had longest history on the east slope of the Rocky Mountains in a region spanning from the Yellowstone River to the Arkansas River, which included the Bighorns. The Cheyenne and Lakota were originally agricultural tribes based on rivers of the Great Plains and the Midwest. By the 1860s and 1870s, the Lakota showed a knowledge of the ancestral trail systems in the Bighorn Mountains, particularly in incidents like the Sibley Fight
Wyoming is a landlocked state in the Mountain West subregion of the Western United States. It borders Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in 2020, Wyoming is the least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is Cheyenne, which had an estimated population of 63,957 in 2018.
Wyoming's western half consists mostly of the ranges and rangelands of the Rocky Mountains; its eastern half consists of high-elevation prairie, and is referred to as the High Plains. Wyoming's climate is semi-arid in some parts and continental in others, making it drier and windier overall than other states, with greater temperature extremes. The federal government owns just under half of Wyoming's land, generally protecting it for public uses. The state ranks sixth in the amount of land—-and fifth in the proportion of its land—-that is owned by the federal government. Its federal lands include two national parks (Grand Teton and Yellowstone), two national recreation areas, two national monuments, and several national forests, as well as historic sites, fish hatcheries, and wildlife refuges.
Indigenous peoples inhabited the region for thousands of years. Historic and currently federally recognized tribes include the Arapaho, Crow, Lakota, and Shoshone. Part of the land that is now Wyoming came under American sovereignty via the Louisiana Purchase, part via the Oregon Treaty, and, lastly, via the Mexican Cession. With the opening of the Oregon Trail, the Mormon Trail, and the California Trail, vast numbers of pioneers travelled through parts of the state that had once been traversed mainly by fur trappers, and this spurred the establishment of forts, such as Fort Laramie, that today serve as population centers. The Transcontinental Railroad supplanted the wagon trails in 1867 with a route through southern Wyoming, bringing new settlers and the establishment of founding towns, including the state capital of Cheyenne. On March 27, 1890, Wyoming became the union's 44th state.
Farming and ranching, and the attendant range wars, feature prominently in the state's history. Today, Wyoming's economy is largely based on tourism and the extraction of minerals such as coal, natural gas, oil, and trona. Its agricultural commodities include barley, hay, livestock, sugar beets, wheat, and wool.
Wyoming was the first state to allow women the right to vote (not counting New Jersey, which had allowed it until 1807), and the right to assume elected office, as well as the first state to elect a female governor. In honor of this part of its history, its most common nickname is "The Equality State" and its official state motto is "Equal Rights".[1] It is among the least religious states in the country,[15] and is known for having a political culture that leans towards libertarian conservatism.[16] The Republican presidential nominee has carried the state in every election since 1968.
There is evidence of prehistoric human habitation in the region known today as the U.S. state of Wyoming stretching back roughly 13,000 years. Stone projectile points associated with the Clovis, Folsom and Plano cultures have been discovered throughout Wyoming. Evidence from what is now Yellowstone National Park indicates the presence of vast continental trading networks since around 1,000 years ago.
The Union Pacific Railroad played a central role in the European colonization of the area. Wyoming would become a U.S. territory in 1868. It was the first state to grant women the right to vote in 1869 (although it was then still a territory). Wyoming would become a U.S. state on July 10, 1890, as the 44th state.
There is evidence of prehistoric human habitation in the region known today as the U.S. state of Wyoming stretching back roughly 13,000 years. Stone projectile points associated with the Clovis, Folsom and Plano cultures have been discovered throughout Wyoming. In the Big Horn Mountains there is a medicine wheel that has not yet been dated accurately due to disruption of the site prior to the two archaeological excavations of 1958 and 1978. However, the Big Horn Medicine Wheel's design of twenty-eight spokes is similar to the Majorville Medicine Wheel in Canada that has been dated at 3200 BCE (5200 years ago) by careful stratification of known artifact types. Throughout the Bighorn Mountains, south to Medicine Lodge Creek, artifacts of occupation date back 10,000 years. Large ceremonial blades chipped from obsidian rock formations in what is now Yellowstone National Park to the west of the Bighorns, have been found in the Hopewell burial mounds of Southern Ohio, indicative of vast continental trading networks since around 1000 years ago.[1] When White explorers first entered the region, they encountered numerous American Indian tribes including the Arapaho, Bannock, Blackfeet, Cheyenne, Crow, Gros Ventre, Kiowa, Nez Perce, Sioux, Shoshone and Ute.
Europeans may have ventured into the northern sections of the state in the 18th century. Most of the southern part of modern-day Wyoming was nominally claimed by Spain and Mexico until the 1830s, but they had no presence. John Colter, a member of the Lewis and Clark Expedition, was probably the first American to enter the region in 1807.[8] His reports of thermal activity in the Yellowstone area were considered at the time to be fictional. Robert Stuart and a party of five men returning from Astoria, Oregon discovered South Pass in 1812. The route was later followed by the Oregon Trail. In 1850, Jim Bridger located what is now known as Bridger Pass, which was later used by both the Union Pacific Railroad in 1868, and in the 20th century by Interstate 80. Bridger also explored the Yellowstone region and like Colter, most of his reports on that region of the state were considered at the time to be tall tales. During the early 19th century, fur trappers known as mountain men flocked to the mountains of western Wyoming in search of beaver. In 1824, the first mountain man rendezvous was held in Wyoming. The gatherings continued annually until 1840, with the majority of them held within Wyoming territory.
The route later known as the Oregon Trail was already in regular use by traders and explorers in the early 1830s. The trail snakes across Wyoming, entering the state on the eastern border near the present day town of Torrington following the North Platte River to the current town of Casper. It then crosses South Pass, and exits on the western side of the state near Cokeville. In 1847, Mormon emigrants blazed the Mormon Trail, which mirrors the Oregon Trail, but splits off at South Pass and continues south to Fort Bridger and into Utah. Over 350,000 emigrants followed these trails to destinations in Utah, California and Oregon between 1840 and 1859. In 1859, gold was discovered in Montana, drawing miners north along the Bozeman and Bridger trails through the Powder River Country and Big Horn Basin respectively.
The influx of emigrants and settlers into the state led to further encounters with the native people there, and settler military presence along the trails increased; military posts such as Fort Laramie were established. In 1851, representatives from the United States and American Indian nations signed the first Treaty of Fort Laramie in hopes of ensuring peace and the safety of settlers on the trails. While the 1850s were subsequently quiet, tensions rose again after settlers increasingly encroached upon lands promised to the tribes in the region. This was the case after settlers, in 1864, blazed the Bozeman Trail through the hunting grounds of the Powder River Country, which the United States had promised to the tribes in the 1851 treaty. As encounters between settlers and natives grew more serious in 1865, Major General Grenville M. Dodge ordered the first Powder River Expedition to attempt to quell the violence. The expedition ended in the Battle of the Tongue River against the Arapaho. In the following year, the fighting escalated into Red Cloud's War, which was the first major military conflict between the United States and the Wyoming Indian tribes. The second Treaty of Fort Laramie in 1868 ended the war by closing the Powder River Country to whites. Violation of this treaty by miners in the Black Hills led to the Black Hills War in 1876, which was fought mainly along the border of Wyoming and Montana.
In 1866, Nelson Story Sr. drove approximately 1000 head of Texas Longhorns to Montana through Wyoming along the Bozeman Trail—the first major cattle drive from Texas into Montana. The Wyoming Stock Growers Association is a historic American cattle organization created in 1873. The Association was started among Wyoming cattle ranchers to standardize and organize the cattle industry, but quickly grew into a political force that has been called "the de facto territorial government" of Wyoming's organization into early statehood, and wielded great influence throughout the Western United States. The association is still active to this day, but it is best known for its rich history and is perhaps most famous for its role in Wyoming's Johnson County War. In 1892 the Johnson County War, also known as the War on Powder River and the Wyoming Range War, took place in Johnson, Natrona and Converse County, Wyoming. It was fought between small settling ranchers against larger established ranchers in the Powder River Country and culminated in a lengthy shootout between local ranchers, a band of hired killers, and a sheriff's posse, eventually requiring the intervention of the United States Cavalry on the orders of President Benjamin Harrison. The events have since become a highly mythologized and symbolic story of the Wild West, and over the years variations of the storyline have come to include some of the west's most famous historical figures and gunslingers. The storyline and its variations have served as the basis for numerous popular novels, films, and television shows.
In 1870, roughly three-eights of Wyoming's population was foreign born, coming primarily from Ireland, Germany and England. The Union Pacific Railroad played a central role in the settlement of Wyoming. The land was good for cattle ranches, but without transportation it was too far for a cattle drive. The UP railroad companies had large land grants that were used to back the borrowings from New York and London that financed construction. UP was anxious to locate settlers upon the land as soon as possible, so there would be a steady outflow of cattle, and a steady inflow of manufactured items purchased by the ranchers. UP also built towns that were needed to service the railroad itself, with dining halls for passengers, construction crews, repair shops and housing for train crews. The towns attracted cattle drives and cowboys.
The UP reached the town of Cheyenne, which later became the state capital, in 1867. The railroad eventually spanned the entire state, boosting the population, and creating some of Wyoming's largest cities, such as Laramie, Rock Springs and Evanston. The railroad needed coal, which was discovered in quantity in the southwestern part of the state, especially around Rock Springs In 1885, a murderous riot known as the Rock Springs Massacre broke out when white miners drove out Chinese miners employed by the Union Pacific Coal Company in Rock Springs.
The name "Wyoming" was used by Representative J. M. Ashley of Ohio, who introduced the Ashley Bill to Congress to provide a "temporary government for the territory of Wyoming". The name was made famous by the 1809 poem Gertrude of Wyoming by Thomas Campbll. "Wyoming" is derived from the Delaware (Munsee) name xwé:wamənk, meaning "at the big river flat", originally applied to the Wyoming Valley in Pennsylvania.
After the arrival of the railroad, the population began to grow steadily in the Wyoming Territory, which was established on July 25, 1868. Unlike Colorado to the south, Wyoming never experienced a rapid population boom in the 19th century from any major mineral discoveries such as gold or silver.
Inclusion of women's suffrage in the Wyoming constitution was debated in the constitutional convention, but ultimately accepted. The constitution was mostly borrowed from those of other states, but also included an article making all the water in Wyoming property of the state. Wyoming overcame the obstacles of low population and of being the only territory in the U.S. giving women the right to vote, and the United States admitted Wyoming into the Union as the 44th state on July 10, 1890.
In 1869, Wyoming territory granted women the right to vote, becoming the first U.S. state to extend suffrage to women. Wyoming was also the home of many other firsts for U.S. women in politics. The first time women served on a jury was in Wyoming (Laramie in 1870). Wyoming had the first female court bailiff (Mary Atkinson, Laramie, in 1870), and the country's first female justice of the peace (Esther Hobart Morris, South Pass City, in 1870). Wyoming became the first state in the Union to elect a female governor, Nellie Tayloe Ross, who was elected in 1924 and took office in January 1925.
Following on the reports of men like Colter and Bridger, a number of organized expeditions were undertaken in northwestern Wyoming. The Cook–Folsom–Peterson Expedition in 1869 and the Washburn-Langford-Doane Expedition in 1870 confirmed the stories of the mountain men. In 1871, Ferdinand Vandeveer Hayden led a formal geological survey of the area, the result of which ultimately convinced Congress to set aside the region. Yellowstone National Park became the world's first National Park in 1872. In August 1886, the U.S. Army was given administration of the park. In 1917, administration of the park was transferred to the new National Park Service. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than 1,000 archaeological sites. Most of Yellowstone National Park is located in Wyoming.
Wyoming is also home to the nation's first national monument (Devils Tower created in 1906), and the first national forest (Shoshone National Forest created in 1891).
The Homestead Act of 1862 attracted many new farmers and ranchers to Wyoming, where they congregated along the fertile banks of the rivers. Most of the land in Wyoming in the 2nd half of the 19th century was in the public domain and so was open for both homesteading and open range for grazing cattle. As individual ranchers moved into the state, they became at odds with the larger ranches for control of the range and water sources. Tensions rose to a boiling point in April 1892 as an armed conflict known as the Johnson County War, fought between the large cattle operators and smaller ranchers and homesteaders. The increased number of settlers also brought with them merchants, as well as outlaws. A number of notable outlaws of the time started their careers in Wyoming, including Butch Cassidy and Harry Longabaugh, both of whom were incarcerated in Wyoming as young men.[25] A remote area in Johnson County, Wyoming known as the Hole-in-the-Wall was a well known hideout for a loose association of outlaw gangs known as the Hole in the Wall Gang. It was used from the 1860s through the early 20th century by outlaws operating throughout Wyoming.
Precious metals were never discovered in great quantities, though a small amount of gold was discovered near South Pass prompting a small rush in the 1860s. Coal was discovered early and has been mined extensively through the state. Union Pacific Railroad ran several coal mines in the southern part of the state to supply the railroad. In 1885 tensions at a Union Pacific mine in Rock Springs resulted in the Rock Springs massacre, one of the largest race riots in U.S. history. Oil is also plentiful throughout the state. In 1924, irregularities over the allocation of naval reserves near Casper resulted in the Teapot Dome Scandal. Natural gas, bentonite and uranium have also been mined through the state's history.
One exception is the copper mines in Carbon County west of Encampment. The Ferris-Haggarty Mine Site supplied copper for the electrification of the world in the late 1800s and early 1900s.
After 1890, Wyoming pageants and parades, as well as school courses, increasingly told a nostalgic story of Wyoming as rooted in the frontier West. During the 1940s, Wyoming millionaire William R. Coe made large contributions to the American studies programs at Yale University and at the University of Wyoming. Coe wished to celebrate the values of the Western United States in order to meet the threat of communism.
Includes all 10 company commanders (includes 1 in terminator armour, 1 with jump pack and 1 on a bike) along with the high commander, master of the apothecarion, master of the forge, chief librarian and high chaplain all using a variety of models and kits.
A clear sky, so a chance to "see" Comet A3. It was very faint. I couldn't actually see it with my naked eyes. During the shoot, Elon Musk's Starlink train came over.
The new REBIRTH RoX head series include features never seen before in other heads.
In addition to common features like HD layers, RoX heads innovate with features like :
- Brand new FX layers to play with amazing effects or create your owns with the devkit inworld.
- Moods that include original and customizable sound FX with your own sounds (devkit available in the store).
- Animations synchronized with the smile FX for an even more realistic effects.
- Revolutionary "2kBOM" skins with realistic FULL 2048 px rendering and easy to design with an evoX compatibility (devkit available in the store and on rebirth-sl.com/).
- Themed heads with cross-compatibility content for all other RoX heads to create an original collection and mix styles.
- 2 neck versions of the head to fit most bodies, male or female. RoX head are easy to shape and very versatile, so you can build a female or male avatar with each head.
- RoX packs contain an unprecedented quantity of items to spend hours in customization.
Locations:
French Touch event
maps.secondlife.com/secondlife/Scheveningen/232/226/23
Rebirth Heads Store
maps.secondlife.com/secondlife/REBIRTH%20Forever/47/79/21
Info about hair, earrings and dress on my Blog:
tillyopaline3.wixsite.com/tilly-opaline/post/rebirth-rox-...
Action from the Brighton Speed Trials on Madeira Drive - Arguable the World's Oldest Motor race, which began in 1905. This Giulia Sprint GT caught my eye, for obvious reasons.
Santa Fe EMD CF7 locomotive # 2649, rebuilt from EMD F7 locomotive # 262C, includes dynamic brakes on the long hood of wrecked GP7B locomotive # 2788A, is seen leading a four unit set of freight designated F7's, while hauling a manifest freight train at an unknown location, 1970. Locomotive # 2649 was the only CF7 conversion locomotive to include dynamic brakes, because the other 232 converted CF7 locomotives had new Cleburne Shop built long hoods installed. These converted CF7 locomotives were used for many years after the covered wagons vanished. Many other roads including Amtrak wound up with some ex-Santa Fe CF7's. The location appears like it may be entrance or exit tracks at a railroad yard. Photo courtesy of Sylvain Assez's railroad photo collection. Sylvain is an active French railway locomotive engineer.
The name of the photographer that took this photo is unknown.
Copyright Disclaimer under Section 107 of the Copyright Act of 1976, allowance is made for “fair use” for the purposes such as criticism, comment, news reporting, teaching, scholarship, and research. Fair use is a use permitted by copyright statute that might otherwise be infringing. Non-profit, educational or personal use tips the balance in favor of fair use.
The London Ambulance Service historic collection includes a number of classic ambulances available for hire at events, and for film and television work. The ambulances have been maintained in their original condition and still have all of the equipment used from when they were in service.
Designed and built by the coachbuilder Wadham Stringer in Waterlooville, Hampshire, this vehicle was first registered with London Ambulance Service (LAS) on 19th August 1967. This type was brought in to replace the Morris LD Wandsworth, a design unique to the capital and produced in the London County Council’s workshops between 1958 and 1966.
The London Ambulance Service operated about 215 of these vehicles between 1965 and 1978.
Unlike its predecessor, the Wandsworth, they also served in different ambulance services across the UK. Although it used the same Morris LD chassis it was a little more refined with fully opening windows, better controls and a connecting door between the driver’s cab at the front and the patient’s compartment at the rear.
One of the major improvements was the use of a removable ‘trolley bed’ type stretcher on wheels. Previously all patients had to be carried on either a chair or a stretcher made of wooden poles and canvas. Variations of the wheeled trolley bed pioneered on the Morris Wadham have become a standard feature on modern ambulances.
As well as the traditional bell, two tone horns were fitted as standard on this model. The bell was retained in case the ambulance had to respond to an emergency call in the City of London where the use of two tone sirens was forbidden at the time.
Unusually, this was one of only six Wadham Stringer ambulances to be built with a single rear door rather than the standard twin doors.
For More info contact:
Communications Department
London Ambulance Service NHS Trust
220 Waterloo Road
London SE1 8SD
Phone: 020 7783 2286
Includes left and right leg braces
click to resize
leg scar tatoos
please try demo cause some people have fat legs
kthx
OH AND might not fit guys unless theyre really girly
Snowdonia, or Eryri is a mountainous region and national park in North Wales. It contains all 15 mountains in Wales over 3000 feet high, including the country's highest, Snowdon (Yr Wyddfa), which is 1,085 metres (3,560 ft) tall. These peaks are all part of the Snowdon, Glyderau, and Carneddau ranges in the north of the region. The shorter Moelwynion and Moel Hebog ranges lie immediately to the south.
The national park has an area of 823 square miles (2,130 km2) (the fourth-largest in the UK), and covers most of central and southern Gwynedd and the western part of Conwy County Borough. This is much larger than the area traditionally considered Snowdonia, and in addition to the five ranges above includes the Rhinogydd, Cadair Idris, and Aran ranges and the Dyfi Hills. It also includes most of the coast between Porthmadog and Aberdyfi. The park was the first of the three national parks of Wales to be designated, in October 1951, and the third in the UK after the Peak District and Lake District, which were established in April and May 1951 respectively. The park received 3.89 million visitors in 2015.
The name Snowdon means 'snow hill' and is derived from the Old English elements snāw and dūn, the latter meaning 'hill'. Snowdonia is simply taken from the name of the mountain.
The origins of Eryri are less clear. Two popular interpretations are that the name is related to eryr, 'eagle', and that it means 'highlands' and is related to the Latin oriri ('to rise'). Although eryri is not any direct form of the word eryr in the meaning 'eagle', it is a plural form of eryr in the meaning 'upland'.
Before the boundaries of the national park were designated, "Snowdonia" was generally used to refer to a smaller upland area of northern Gwynedd centred on the Snowdon massif. The national park covers an area more than twice that size, extending south into the Meirionnydd area.
This difference is apparent in books published before 1951. In George Borrow's 1907 Wild Wales he states that "Snowdon or Eryri is no single hill, but a mountainous region, the loftiest part of which is called Y Wyddfa", making a distinction between the summit of the mountain and the surrounding massif. The Mountains of Snowdonia by H. Carr & G. Lister (1925) defines "Eryri" as "composed of the two cantrefs of Arfon and Arllechwedd, and the two commotes of Nant Conwy and Eifionydd", which corresponds to Caernarfonshire with the exception of southwest Llŷn and the Creuddyn Peninsula. In Snowdonia: The National Park of North Wales (1949), F. J. North states that "When the Committee delineated provisional boundaries, they included areas some distance beyond Snowdonia proper".
Snowdonia National Park, also known as Eryri National Park in English and Parc Cenedlaethol Eryri in Welsh, was established in October 1951. It was the third national park in the United Kingdom, following the Peak District and Lake District in April and May of the same year. It covers 827 square miles (2,140 km2) in the counties of Gwynedd and Conwy, and has 37 miles (60 km) of coastline.
The park is governed by the Snowdonia National Park Authority, which has 18 members: 9 appointed by Gwynedd, 3 by Conwy, and 6 by the Welsh Government to represent the national interest. The authority's main offices are at Penrhyndeudraeth.
The park authority used Snowdonia and Snowdon when referring to the national park and mountain in English until February 2023, when it resolved to primarily use the Welsh names, Eryri and Yr Wyddfa. There will be a transitional period of approximately two years in which the authority will continue to use the English names in parentheses — for example "Yr Wyddfa (Snowdon)" — where the context requires.
Unlike national parks in other countries, national parks in the UK are made up of both public and private lands under a central planning authority. The makeup of land ownership in the national park is as follows:
More than 26,000 people live within the park, of whom 58.6% could speak Welsh in 2011. While most of the land is either open or mountainous land, there is a significant amount of agricultural activity within the park.
The national park does not include the town of Blaenau Ffestiniog, which forms a unique non-designated enclave within the park boundaries. The town was deliberately excluded from the park when it was established because of its slate quarrying industry. The boundaries of the Peak District National Park exclude the town of Buxton and its adjacent limestone quarries for a similar reason.
The geology of Snowdonia is key to the area's character. Glaciation during a succession of ice ages, has carved from a heavily faulted and folded succession of sedimentary and igneous rocks, a distinctive rocky landscape. The last ice age ended only just over 11,500 years ago, leaving a legacy of features attractive to visitors but which have also played a part in the development of geological science and continue to provide a focus for educational visits. Visiting Cwm Idwal in 1841 Charles Darwin realised that the landscape was the product of glaciation. The bedrock dates largely from the Cambrian and Ordovician periods with intrusions of Ordovician and Silurian age associated with the Caledonian Orogeny. There are smaller areas of Silurian age sedimentary rocks in the south and northeast and of Cenozoic era strata on the Cardigan Bay coast though the latter are concealed by more recent deposits. Low grade metamorphism of Cambrian and Ordovician mudstones has resulted in the slates, the extraction of which once formed the mainstay of the area's economy.
The principal ranges of the traditional Snowdonia are the Snowdon massif itself, the Glyderau, the Carneddau, the Moelwynion and the Moel Hebog range. All of Wales' 3000ft mountains are to be found within the first three of these massifs and are most popular with visitors. To their south within the wider national park are the Rhinogydd and the Cadair Idris and Aran Fawddwy ranges. Besides these well-defined areas are a host of mountains which are less readily grouped though various guidebook writers have assigned them into groups such as the 'Arenigs', the 'Tarrens' and the 'Dyfi hills'.
Snowdon's summit at 1085 metres (3560 feet) is the highest in Wales and the highest in Britain south of the Scottish Highlands. At 905 metres (2970 feet) Aran Fawddwy is the highest in Wales outside of northern Snowdonia; Cadair Idris, at 893 metres (2930 feet), is next in line.
Rivers draining the area empty directly into Cardigan Bay are typically short and steep. From north to south they include the Glaslyn and Dwyryd which share a common estuary, the Mawddach and its tributaries the Wnion and the Eden, the smaller Dysynni and on the park's southern margin the Dyfi. A series of rivers drain to the north coast. Largest of these is the Conwy on the park's eastern margin which along with the Ogwen drains into Conwy Bay. Further west the Seiont and Gwyrfai empty into the western end of the Menai Strait. A part of the east of the national park is within the upper Dee (Dyfrydwy) catchment and includes Bala Lake, the largest natural waterbody in Wales. A fuller list of the rivers and tributaries within the area is found at List of rivers of Wales.
There are few natural waterbodies of any size in Wales; Snowdonia is home to most. Besides Bala Lake, a few lakes occupy glacial troughs including Llyn Padarn and Llyn Peris at Llanberis and Tal-y-llyn Lake south of Cadair Idris. Llyn Dinas, Llyn Gwynant, and Llyn Cwellyn to the south and west of Snowdon feature in this category as do Llyn Cowlyd and Llyn Ogwen on the margins of the Carneddau. There are numerous small lakes occupying glacial cirques owing to the former intensity of glacial action in Snowdonia. Known generically as tarns, examples include Llyn Llydaw, Glaslyn and Llyn Du'r Arddu on Snowdon, Llyn Idwal within the Glyderau and Llyn Cau on Cadair Idris.
There are two large wholly man-made bodies of water in the area, Llyn Celyn and Llyn Trawsfynydd whilst numerous of the natural lakes have had their levels artificially raised to different degrees. Marchlyn Mawr reservoir and Ffestiniog Power Station's Llyn Stwlan are two cases where natural tarns have been dammed as part of pumped storage hydro-electric schemes. A fuller list of the lakes within the area is found at List of lakes of Wales. In 2023, the park standardised its Welsh language lake names, to be also used in English.
The national park meets the Irish Sea coast within Cardigan Bay between the Dovey estuary in the south and the Dwyryd estuary. The larger part of that frontage is characterised by dune systems, the largest of which are Morfa Dyffryn and Morfa Harlech. These two locations have two of the largest sand/shingle spits in Wales. The major indentations of the Dovey, the Mawddach and Dwyryd estuaries, have large expanses of intertidal sands and coastal marsh which are especially important for wildlife: see #Natural history. The northern tip of the national park extends to the north coast of Wales at Penmaen-bach Point, west of Conwy, where precipitous cliffs have led to the road and railway negotiating the spot in tunnels.
There are only three towns within the park boundary, though there are several more immediately beyond it. Dolgellau is the most populous followed by Bala on the eastern boundary and then Harlech overlooking Tremadog Bay. More populous than these is the town of Blaenau Ffestiniog, which is within an exclave, that is to say it is surrounded by the national park but excluded from it, whilst the towns of Tywyn and Barmouth on the Cardigan Bay coast are within coastal exclaves. Llanrwst in the east, Machynlleth in the south and Porthmadog and Penrhyndeudraeth in the west are immediately beyond the boundary but still identified with the park; indeed the last of these hosts the headquarters of the Snowdonia National Park Authority. Similarly the local economies of the towns of Conwy, Bethesda, and Llanberis in the north are inseparably linked to the national park as they provide multiple visitor services. The lower terminus of the Snowdon Mountain Railway is at Llanberis. Though adjacent to it, Llanfairfechan and Penmaenmawr are less obviously linked to the park.
There are numerous smaller settlements within the national park: prominent amongst these are the eastern 'gateway' village of Betws-y-Coed, Aberdyfi on the Dovey (Dyfi) estuary and the small village of Beddgelert each of which attract large numbers of visitors. Other sizeable villages are Llanuwchllyn at the southwest end of Bala Lake (Llyn Tegid), Dyffryn Ardudwy, Corris, Trawsfynydd, Llanbedr, Trefriw and Dolwyddelan.
Six primary routes serve Snowdonia, the busiest of which is the A55, a dual carriageway which runs along the north coast and provides strategic road access to the northern part of the national park. The most important north–south route within the park is the A470 running from the A55 south past Betws-y-Coed to Blaenau Ffestiniog to Dolgellau. It exits the park a few miles to the southeast near Mallwyd. From Dolgellau, the A494 runs to Bala whilst the A487 connects with Machynlleth. The A487 loops around the northwest of the park from Bangor via Caernarfon to Porthmadog before turning in land to meet the A470 east of Maentwrog. The A5 was built as a mail coach road by Thomas Telford between London and Holyhead; it enters the park near Pentrefoelas and leaves it near Bethesda. Other A class roads provide more local links; the A493 down the Dovey valley from Machynlleth and up the coast to Tywyn then back up the Mawddach valley to Dolgellau, the A496 from Dolgellau down the north side of the Mawddach to Barmouth then north up the coast via Harlech to Maentwrog. The A4212 connecting Bala with Trawsfynydd is relatively modern having been laid out in the 1960s in connection with the construction of Llyn Celyn. Three further roads thread their often twisting and narrow way through the northern mountains; A4085 links Penrhyndeudraeth with Caernarfon, the A4086 links Capel Curig with Caernarfon via Llanberis and the A498 links Tremadog with the A4086 at Pen-y-Gwryd. Other roads of note include that from Llanuwchllyn up Cwm Cynllwyd to Dinas Mawddwy via the 545 metre (1788') high pass of Bwlch y Groes, the second highest tarmacked public road in Wales and the minor road running northwest and west from Llanuwchllyn towards Bronaber via the 531 metre (1742') high pass of Bwlch Pen-feidiog.
The double track North Wales Coast Line passes along the northern boundary of the park between Conwy and Bangor briefly entering it at Penmaen-bach Point where it is in tunnel. Stations serve the communities of Conwy, Penmaenmawr, Llanfairfechan and Bangor. The single-track Conwy Valley Line runs south from Llandudno Junction, entering the park north of Betws-y-coed which is served by a station then west up the Lledr valley by way of further stations at Pont-y-pant, Dolwyddelan and Roman Bridge. After passing through a tunnel the passenger line now terminates at Blaenau Ffestiniog railway station. Prior to 1961 the route continued as the Bala and Ffestiniog Railway via Trawsfynydd to Bala joining another former route along the Dee valley which ran southwest via Dolgellau to join the still extant coastal Cambrian Line south of Barmouth. The Pwllheli branch of the Cambrian Line splits from the Aberystwyth branch at Dovey Junction and continues via stations at Aberdovey, Tywyn, Tonfanau, Llwyngwril, Fairbourne and Morfa Mawddach to Barmouth where it crosses the Mawddach estuary by the Grade II* listed wooden Barmouth Bridge, a structure which also provides for walkers and cyclists. Further stations serve Llanaber, Tal-y-bont, Dyffryn Ardudwy, Llanbedr, Pensarn and Llandanwg before reaching Harlech. Tygwyn, Talsarnau and Llandecwyn stations are the last before the line exits the park as it crosses the Dwyryd estuary via Pont Briwet and turns westwards bound for Pwllheli via Penrhyndeudraeth, Porthmadog and Criccieth.
Many sections of dismantled railway are now used by walking and cycling routes and are described elsewhere. The Bala Lake Railway is a heritage railway which has been established along a section of the former mainline route between Bala and Llanuwchllyn. Other heritage railways occupy sections of former mineral lines, often narrow gauge and are described in a separate section.
The national park is served by a growing bus network, branded Sherpa'r Wyddfa (formerly Snowdon Sherpa). Together with the TrawsCymru network of buses this provides a car-free option to tourists and locals wishing to travel across the National Park.
The network was relaunched in July 2022 with a new brand, Sherpa'r Wyddfa, to reflect the National Park's new push for the promotion of Welsh place names. As such the publicity and websites for the newly branded service only use these Welsh names, even for English language users.
Snowdonia is one of the wettest parts of the United Kingdom; Crib Goch in Snowdonia is the wettest spot in the United Kingdom, with an average rainfall of 4,473 millimetres (176.1 in) a year over the 30-year period prior to the mid-2000s. (There is a rainfall gauge at 713 metres, 2340' on the slopes below Crib Goch.)
The earliest evidence for human occupation of the area dates from around 4000–3000 BCE with extensive traces of prehistoric field systems evident in the landscape. Within these are traces of irregular enclosures and hut circles. There are burial chambers of Neolithic and Bronze Age such as Bryn Cader Faner and Iron Age hillforts such as Bryn y Castell near Ffestiniog.
The region was finally conquered by the Romans by AD 77–78. Remains of Roman marching camps and practice camps are evident. There was a Roman fort and amphitheatre at Tomen y Mur. Roads are known to have connected with Segontium (Caernarfon) and Deva Victrix (Chester) and include the northern reaches of Sarn Helen.
There are numerous memorial stones of Early Christian affinity dating from the post-Roman period. The post-Roman hillfort of Dinas Emrys also dates to this time. Churches were introduced to the region in the 5th and 6th centuries. Llywelyn the Great and Llywelyn ap Gruffudd had various stone castles constructed to protect their borders and trade routes. Edward I built several castles around the margins including those at Harlech and Conwy for military and administrative reasons. Most are now protected within a World Heritage Site. Some of Snowdonia's many stone walls date back to this period too. In the Middle Ages, the title Prince of Wales and Lord of Snowdonia (Tywysog Cymru ac Arglwydd Eryri) was used by Llywelyn ap Gruffudd; his grandfather Llywelyn Fawr used the title Prince of north Wales and Lord of Snowdonia.
The 18th century saw the start of industrial exploitation of the area's resources, assisted by the appearance in the late part of the century of turnpike trusts making it more accessible. The engineer Thomas Telford left a legacy of road and railway construction in and around Snowdonia. A new harbour at Porthmadog linked to slate quarries at Ffestiniog via a narrow gauge railway. At its peak in the 19th century the slate industry employed around 12,000 men. A further 1000 were employed in stone quarrying at Graiglwyd and Penmaenmawr. Mining for copper, iron and gold was undertaken during the 18th and 19th centuries, leaving a legacy of mine and mill ruins today. Ruins of the gold industry are found at Cefn Coch on the Dolmelynllyn estate.
The Snowdonia Society is a registered charity formed in 1967; it is a voluntary group of people with an interest in the area and its protection.
Amory Lovins led the successful 1970s opposition to stop Rio Tinto digging up the area for a massive mine.
The park's entire coastline is a Special Area of Conservation, which runs from the Llŷn Peninsula down the mid-Wales coast, the latter containing valuable sand dune systems.
The park's natural forests are of the mixed deciduous type, the commonest tree being the Welsh oak. Birch, ash, mountain-ash and hazel are also common. The park also contains some large (planted) coniferous forested areas such as Gwydir Forest near Betws-y-Coed, although some areas, once harvested, are now increasingly being allowed to regrow naturally.
Northern Snowdonia is the only place in Britain where the Snowdon lily (Gagea serotina), an arctic–alpine plant, is found and the only place in the world where the Snowdonia hawkweed Hieracium snowdoniense grows.
One of the major problems facing the park in recent years has been the growth of Rhododendron ponticum. This fast-growing invasive species has a tendency to take over and stifle native species. It can form massive towering growths and has a companion fungus that grows on its roots producing toxins that are poisonous to any local flora and fauna for a seven-year period after the Rhododendron infestations have been eradicated. As a result, there are a number of desolate landscapes.
Mammals in the park include otters, polecats, feral goats, and pine martens. Birds include raven, red-billed chough, peregrine, osprey, merlin and the red kite. The rainbow-coloured Snowdon beetle (Chrysolina cerealis) is only found in northern Snowdonia.
Snowdonia has a particularly high number of protected sites in respect of its diverse ecology; nearly 20% of its total area is protected by UK and European law. Half of that area was set aside by the government under the European Habitats Directive as a Special Area of Conservation. There are a large number of Sites of special scientific interest (or 'SSSIs'), designated both for fauna and flora but also in some cases for geology. Nineteen of these sites are managed as national nature reserves by Natural Resources Wales. The park also contains twelve Special Areas of Conservation (or 'SACs'), three Special Protection Areas (or 'SPAs') and three Ramsar sites. Some are wholly within the park boundaries, others straddle it to various degrees.
There are numerous SSSIs within the park, the most extensive of which are Snowdonia, Migneint-Arenig-Dduallt, Morfa Harlech, Rhinog, Berwyn, Cadair Idris, Llyn Tegid, Aber Mawddach / Mawddach Estuary, Dyfi, Morfa Dyffryn, Moel Hebog, Coedydd Dyffryn Ffestiniog and Coedydd Nanmor.
The following NNRs are either wholly or partly within the park: Allt y Benglog, Y Berwyn (in multiple parts), Cader Idris, Ceunant Llennyrch, Coed Camlyn, Coed Cymerau, Coed Dolgarrog, Coed Ganllwyd, Coed Gorswen, Coed Tremadog, Coedydd Aber, Coedydd Maentwrog (in 2 parts), Coed y Rhygen, Cwm Glas Crafnant, Cwm Idwal, Hafod Garregog, Morfa Harlech, Rhinog and Snowdon.
The twelve SACs are as follows: Snowdonia SAC which covers much of the Carneddau, Glyderau, and the Snowdon massif, Afon Gwyrfai a Llyn Cwellyn, Corsydd Eifionydd / Eifionydd Fens (north of Garndolbenmaen), the Coedydd Derw a Safleoedd Ystlumod Meirion / Meirionydd Oakwoods and Bat Sites - a series of sites between Tremadog, Trawsfynydd, and Ffestiniog and Beddgelert and extending up the Gwynant. It also includes many of the oakwoods of the Mawddach and its tributaries. Afon Eden – Cors Goch Trawsfynydd, Rhinog, Cadair Idris (in 2 parts), Migneint-Arenig-Dduallt, River Dee and Afon Dyfrdwy a Llyn Tegid (Wales), Mwyngloddiau Fforest Gwydir / Gwydyr Forest Mines (north of Betws-y-Coed) and a part of the Berwyn a Mynyddoedd De Clwyd / Berwyn and South Clwyd Mountains SAC. The Pen Llyn a'r Sarnau / Lleyn Peninsula and the Sarnau SAC covers the entire Cardigan Bay coastline of the park and the sea area and extends above the high water mark at Morfa Harlech, Mochras and around the Dovey and Mawddach estuaries.
The three SPAs are Dovey Estuary / Aber Dyfi (of which a part is within the park), Berwyn (of which a part is within the park) and Migneint-Arenig-Dduallt.
The three designated Ramsar sites are the Dyfi Biosphere (Cors Fochno and Dyfi), Cwm Idwal and Llyn Tegid (Bala Lake).
The area's economy was traditionally centred upon farming and from the early 19th century increasingly on mining and quarrying. Tourism has become an increasingly significant part of Snowdonia's economy during the 20th and 21st centuries.
The extensive farming of sheep remains central to Snowdonia's farming economy.
Significant sections of the park were afforested during the 20th century for timber production. Major conifer plantations include Dyfi Forest, Coed y Brenin Forest between Dolgellau and Trawsfynydd, Penllyn Forest south of Bala, Beddgelert Forest and Gwydyr (or Gwydir) Forest near Betws-y-Coed which is managed as a forest park by Natural Resources Wales.
The region was once the most important producer of slate in the world. Some production continues but at a much reduced level from its peak. The park boundaries are drawn such that much of the landscape affected by slate quarrying and mining lies immediately outside of the designated area.
Construction of a nuclear power station beside Llyn Trawsfynydd began in 1959 with the first power produced in 1965. The site was operational until 1991 though it continues as an employer during its decommissioning phase. Pumped storage hydroelectric schemes are in operation at Llanberis and Ffestiniog.
Research indicates that there were 3.67 million visitors to Snowdonia National Park in 2013, with approximately 9.74 million tourist days spent in the park during that year. Total tourist expenditure was £433.6 million in 2013.
Many of the hikers in the area concentrate on Snowdon itself. It is regarded as a fine mountain, but at times gets very crowded; in addition the Snowdon Mountain Railway runs to the summit.
The other high mountains with their boulder-strewn summits as well as Tryfan, one of the few mountains in the UK south of Scotland whose ascent needs hands as well as feet are also very popular. However, there are also some spectacular walks in Snowdonia on the lower mountains, and they tend to be relatively unfrequented. Among hikers' favourites are Y Garn (east of Llanberis) along the ridge to Elidir Fawr; Mynydd Tal-y-Mignedd (west of Snowdon) along the Nantlle Ridge to Mynydd Drws-y-Coed; Moelwyn Mawr (west of Blaenau Ffestiniog); and Pen Llithrig y Wrach north of Capel Curig. Further south are Y Llethr in the Rhinogydd, and Cadair Idris near Dolgellau.
The park has 1,479 miles (2,380 km) of public footpaths, 164 miles (264 km) of public bridleways, and 46 miles (74 km) of other public rights of way. A large part of the park is also covered by right to roam laws.
The Wales Coast Path runs within the park between Machynlleth and Penrhyndeudraeth, save for short sections of coast in the vicinity of Tywyn and Barmouth which are excluded from the park. It touches the park boundary again at Penmaen-bach Point on the north coast. An inland alternative exists between Llanfairfechan and Conwy, wholly within the park. The North Wales Path, which predates the WCP, enters the park north of Bethesda and follows a route broadly parallel to the north coast visiting Aber Falls and the Sychnant Pass before exiting the park on the descent from Conwy Mountain. The Cambrian Way is a long-distance trail between Cardiff and Conwy that stays almost entirely within the national park from Mallwyd northwards. It was officially recognised in 2019, and is now depicted on Ordnance Survey maps.
The use of the English names for the area has been divisive, with an increase in protests against their use since 2020; these led to the national park authority deciding to use Welsh names as far as legally possible in November 2022. An early example of pressure to deprecate Snowdon and Snowdonia was a 2003 campaign by Cymuned, inspired by campaigns to refer to Ayers Rock as Uluru and Mount Everest as Qomolangma.
In 2020 an e-petition calling for the removal of the English names was put forward to the Senedd, but rejected as responsibility lies with the national park authority. In 2021 an e-petition on the same topic attracted more than 5,300 signatures and was presented to the national park authority.
On 28 April 2021 Gwynedd councillor John Pughe Roberts put forward a motion to use the Welsh names exclusively, calling this a "question of respect for the Welsh language". The motion was not considered and delayed, as the national park authority already appointed a "Welsh Place Names Task and Finish Group" to investigate the issue. The park authority however cannot compel other bodies and/or individuals to stop using the English names, with the proposals facing some criticism.
In May 2021, following the dismissal of the motion, YouGov conducted a poll on Snowdon's name. 60% of Welsh adults supported the English name Snowdon, compared to 30% wanting the Welsh name Yr Wyddfa. Separating by language, 59% of Welsh speakers preferred the Welsh name, but 37% of these still wanted Snowdon to be used as well. 69% of non-Welsh speakers firmly supported Snowdon as the Mountain's name. The proposals to rename Snowdon are usually accompanied with proposals to rename Snowdonia.
On 16 November 2022, Members of the Snowdonia National Park Authority committee voted to use the Welsh names Yr Wyddfa and Eryri to refer to the mountain and the national park, rather than the English names, in materials produced by the authority. The national park authority described the decision as "decisive action" and the authority's head of culture heritage stated that Welsh place names were part of the area's "special qualities" and that other public bodies, English-language press and filming companies have used the Welsh-language names. Before the decision the park had already prioritised the Welsh names by using them first and giving the English names in parentheses. The name "Snowdonia" cannot be abandoned entirely, as it is set in law and so must be used in statutory documents. The authority announced a review of the authority's branding in 2023 to adapt to the new approach to Welsh place names.
Gwynedd is a county in the north-west of Wales. It borders Anglesey across the Menai Strait to the north, Conwy, Denbighshire, and Powys to the east, Ceredigion over the Dyfi estuary to the south, and the Irish Sea to the west. The city of Bangor is the largest settlement, and the administrative centre is Caernarfon. The preserved county of Gwynedd, which is used for ceremonial purposes, includes the Isle of Anglesey.
Gwynedd is the second largest county in Wales but sparsely populated, with an area of 979 square miles (2,540 km2) and a population of 117,400. After Bangor (18,322), the largest settlements are Caernarfon (9,852), Bethesda (4,735), and Pwllheli (4,076). The county has the highest percentage of Welsh speakers in Wales, at 64.4%, and is considered a heartland of the language.
The geography of Gwynedd is mountainous, with a long coastline to the west. Much of the county is covered by Snowdonia National Park (Eryri), which contains Wales's highest mountain, Snowdon (Yr Wyddfa; 3,560 feet, 1,090 m). To the west, the Llŷn Peninsula is flatter and renowned for its scenic coastline, part of which is protected by the Llŷn AONB. Gwynedd also contains several of Wales's largest lakes and reservoirs, including the largest, Bala Lake (Llyn Tegid).
The area which is now the county has played a prominent part in the history of Wales. It formed part of the core of the Kingdom of Gwynedd and the native Principality of Wales, which under the House of Aberffraw remained independent from the Kingdom of England until Edward I's conquest between 1277 and 1283. Edward built the castles at Caernarfon and Harlech, which form part of the Castles and Town Walls of King Edward in Gwynedd World Heritage Site. During the Industrial Revolution the slate industry rapidly developed; in the late nineteenth century the neighbouring Penrhyn and Dinorwic quarries were the largest in the world, and the Slate Landscape of Northwest Wales is now a World Heritage Site. Gwynedd covers the majority of the historic counties of Caernarfonshire and Merionethshire.
In the past, historians such as J. E. Lloyd assumed that the Celtic source of the word Gwynedd meant 'collection of tribes' – the same root as the Irish fine, meaning 'tribe'. Further, a connection is recognised between the name and the Irish Féni, an early ethnonym for the Irish themselves, related to fían, 'company of hunting and fighting men, company of warriors under a leader'. Perhaps *u̯en-, u̯enə ('strive, hope, wish') is the Indo-European stem. The Irish settled in NW Wales, and in Dyfed, at the end of the Roman era. Venedotia was the Latin form, and in Penmachno there is a memorial stone from c. AD 500 which reads: Cantiori Hic Iacit Venedotis ('Here lies Cantiorix, citizen of Gwynedd'). The name was retained by the Brythons when the kingdom of Gwynedd was formed in the 5th century, and it remained until the invasion of Edward I. This historical name was revived when the new county was formed in 1974.
Gwynedd was an independent kingdom from the end of the Roman period until the 13th century, when it was conquered by England. The modern Gwynedd was one of eight Welsh counties created on 1 April 1974 under the Local Government Act 1972. It covered the entirety of the historic counties of Anglesey and Caernarfonshire, and all of Merionethshire apart from Edeirnion Rural District (which went to Clwyd); and also a few parishes of Denbighshire: Llanrwst, Llansanffraid Glan Conwy, Eglwysbach, Llanddoged, Llanrwst and Tir Ifan.
The county was divided into five districts: Aberconwy, Arfon, Dwyfor, Meirionnydd and Anglesey.
The Local Government (Wales) Act 1994 abolished the 1974 county (and the five districts) on 1 April 1996, and its area was divided: the Isle of Anglesey became an independent unitary authority, and Aberconwy (which included the former Denbighshire parishes) passed to the new Conwy County Borough. The remainder of the county was constituted as a principal area, with the name Caernarfonshire and Merionethshire, as it covers most of the areas of those two historic counties. As one of its first actions, the Council renamed itself Gwynedd on 2 April 1996. The present Gwynedd local government area is governed by Gwynedd Council. As a unitary authority, the modern entity no longer has any districts, but Arfon, Dwyfor and Meirionnydd remain as area committees.
The pre-1996 boundaries were retained as a preserved county for a few purposes such as the Lieutenancy. In 2003, the boundary with Clwyd was adjusted to match the modern local government boundary, so that the preserved county now covers the two local government areas of Gwynedd and Anglesey. Conwy county borough is now entirely within Clwyd.
A Gwynedd Constabulary was formed in 1950 by the merger of the Anglesey, Caernarfonshire and Merionethshire forces. A further amalgamation took place in the 1960s when Gwynedd Constabulary was merged with the Flintshire and Denbighshire county forces, retaining the name Gwynedd. In one proposal for local government reform in Wales, Gwynedd had been proposed as a name for a local authority covering all of north Wales, but the scheme as enacted divided this area between Gwynedd and Clwyd. To prevent confusion, the Gwynedd Constabulary was therefore renamed the North Wales Police.
The Snowdonia National Park was formed in 1951. After the 1974 local authority reorganisation, the park fell entirely within the boundaries of Gwynedd, and was run as a department of Gwynedd County Council. After the 1996 local government reorganisation, part of the park fell under Conwy County Borough, and the park's administration separated from the Gwynedd council. Gwynedd Council still appoints nine of the eighteen members of the Snowdonia National Park Authority; Conwy County Borough Council appoints three; and the Welsh Government appoints the remaining six.
There has been considerable inwards migration to Gwynedd, particularly from England. According to the 2021 census, 66.6% of residents had been born in Wales whilst 27.1% were born in England.
The county has a mixed economy. An important part of the economy is based on tourism: many visitors are attracted by the many beaches and the mountains. A significant part of the county lies within the Snowdonia National Park, which extends from the north coast down to the district of Meirionnydd in the south. But tourism provides seasonal employment and thus there is a shortage of jobs in the winter.
Agriculture is less important than in the past, especially in terms of the number of people who earn their living on the land, but it remains an important element of the economy.
The most important of the traditional industries is the slate industry, but these days only a small percentage of workers earn their living in the slate quarries.
Industries which have developed more recently include TV and sound studios: the record company Sain has its HQ in the county.
The education sector is also very important for the local economy, including Bangor University and Further Education colleges, Coleg Meirion-Dwyfor and Coleg Menai, both now part of Grŵp Llandrillo Menai.
The proportion of respondents in the 2011 census who said they could speak Welsh.
Gwynedd has the highest proportion of people in Wales who can speak Welsh. According to the 2021 census, 64.4% of the population aged three and over stated that they could speak Welsh,[7] while 64.4% noted that they could speak Welsh in the 2011 census.
It is estimated that 83% of the county's Welsh-speakers are fluent, the highest percentage of all counties in Wales.[9] The age group with the highest proportion of Welsh speakers in Gwynedd were those between ages 5–15, of whom 92.3% stated that they could speak Welsh in 2011.
The proportion of Welsh speakers in Gwynedd declined between 1991 and 2001,[10] from 72.1% to 68.7%, even though the proportion of Welsh speakers in Wales as a whole increased during that decade to 20.5%.
The Annual Population Survey estimated that as of March 2023, 77.0% of those in Gwynedd aged three years and above could speak Welsh.
Notable people
Leslie Bonnet (1902–1985), RAF officer, writer; originated the Welsh Harlequin duck in Criccieth
Sir Dave Brailsford (born 1964), cycling coach; grew up in Deiniolen, near Caernarfon
Duffy (born 1984), singer, songwriter and actress; born in Bangor, Gwynedd
Edward II of England (1284–1327), born in Caernarfon Castle
Elin Fflur (born 1984), singer-songwriter, TV and radio presenter; went to Bangor University
Bryn Fôn (born 1954), actor and singer-songwriter; born in Llanllyfni, Caernarfonshire.
Wayne Hennessey (born 1987), football goalkeeper with 108 caps for Wales; born in Bangor, Gwynedd
John Jones (c. 1530 – 1598), a Franciscan friar, Roman Catholic priest and martyr; born at Clynnog
Sir Love Jones-Parry, 1st Baronet (1832–1891), landowner and politician, co-founder of the Y Wladfa settlement in Patagonia
T. E. Lawrence (1888–1935), archaeologist, army officer and inspiration for Lawrence of Arabia, born in Tremadog
David Lloyd George (1863–1945), statesman and Prime Minister; lived in Llanystumdwy from infancy
Sasha (born 1969), disc jockey, born in Bangor, Gwynedd
Sir Bryn Terfel (born 1965), bass-baritone opera and concert singer from Pant Glas
Sir Clough Williams-Ellis (1883–1978), architect of Portmeirion
Owain Fôn Williams, (born 1987), footballer with 443 club caps; born and raised in Penygroes, Gwynedd.
Hedd Wyn (1887–1917), poet from the village of Trawsfynydd; killed in WWI
One of my photographs is include in the permanent exhibition at this mini-museum.
The Diving Bell is the first project in Dublin Port’s plan to create a ‘distributed museum’ of attractions across the Dublin docklands and into Dublin Port to preserve the port’s industrial heritage and history.
The Diving Bell was designed by the port engineer Bindon Blood Stoney (1828 to 1907) and built by Grendon and Co., Drogheda. It was delivered to the Port in 1866, entered service in 1871 and was used in the building of the Port’s quay walls until 1958. Stoney was a prodigious engineer and among his achievements were the building of the Boyne Viaduct in Drogheda, the construction of O’Connell Bridge and the building of many of the Port’s quay walls including Sir John Rogerson’s Quay and North Wall Quay Extension.
The Diving Bell was used in the building of the Port’s quay walls from the Victorian era right up until almost the 1960s. It was a ground-breaking piece of engineering innovation in its day.