text:
Dongfeng (missile)

The Dongfeng series, typically abbreviated as "DF missiles", are a family of short, medium, intermediate-range and intercontinental ballistic missiles operated by the Chinese People's Liberation Army Rocket Force (formerly the Second Artillery Corps).

History
After the signing of the Sino-Soviet Treaty of Friendship, Alliance and Mutual Assistance in 1950, the Soviet Union assisted China's military R&D with training, technical documentation, manufacturing equipment and licensed production of Soviet weapons. In the area of ballistic missiles, the Soviets transferred R-1 (SS-1), R-2 (SS-2) and R-11F technology to China. The first Chinese ballistic missiles were based on Soviet designs. Since then, China has made many advances in its ballistic missile and rocket technology. For instance, the space launch Long March rockets have their roots in the Dongfeng missiles.

Dongfeng 1 (SS-2)
The first of the Dongfeng missiles, the DF-1 (SS-2, codenamed '1059', initially 'DF-1', later the DF-3 ), was a licensed copy of the Soviet R-2 (SS-2 Sibling) short-range ballistic missile (SRBM), based on the German V-2 rocket. The DF-1 had a single RD-101 rocket engine, and used alcohol for fuel with liquid oxygen (LOX) as an oxidizer. The missile had maximum range of 550 km and a 500 kg payload. Limited numbers of DF-1 were produced in the 1960s, and have since been retired.

Dongfeng 2 (CSS-1)

The DF-2 (CSS-1) is China's first medium-range ballistic missile (MRBM), with a 1,250 km range and a 15-20 kt nuclear warhead. It received the western designation of CSS-1 (stands for "China Surface-to-Surface"). It was long noted by western observers that the DF-2 could be a copy of the Soviet R-5 Pobeda (SS-3 Shyster), as they have identical look, range, engine and payload. The entire documentation for R-5 had been delivered from Soviet Union to China in the late 1950s. But some western authors still attribute the design to Chinese specialists Xie Guangxuan, Liang Sili, Liu Chuanru, Liu Yuan, Lin Shuang, and Ren Xinmin. The first DF-2 failed in its launch test in 1962, leading to the improved DF-2A. The DF-2A was used to carry out China's test of a live warhead on a rocket on 27 October 1966 (detonated in the atmosphere above Lop Nor), and was in operational service from the late 1960s. All DF-2 were retired from active duty in the 1980s.

Dongfeng 3 (CSS-2)
The DF-3 (CSS-2) is often considered China's first "domestic" intermediate-range ballistic missile (IRBM). The common ICBM design was greatly influenced by the Soviet R-14 Chusovaya missile and the first stage engine itself was a direct copy of the С.2.1100/С.2.1150 La-350 booster engine developed by Aleksei Isaev at OKB-2 (NII-88). Design leadership has been attributed to both Tu Shou'e and Sun Jiadong. The missile was produced at Factory 211 (Capital Astronautics Co., [首都航天机械公司], also known as Capital Machine Shop, [首都机械厂]). The 2,500 km DF-3 was originally designed with a 2,000 kg payload to carry an atomic (later thermonuclear) warhead. A further improved DF-3A with 3,000 km range (~4,000 km with reduced payload) was developed in 1981, and exported to Saudi Arabia with a conventional high-explosive warhead. The DF-3's range of 2,810 km means it is just short of being able to target Guam, although the 2012 DOD report on China's military power states that they have a range of 3,300 km, which would be enough to target Guam. The 2013 Pentagon report on China's military power confirms the DF-3's 3,300 km range, and its maps show Guam being within the DF-3's range. All DF-3/DF-3A's were retired by the mid-2010s and replaced by the DF-21.

Dongfeng 4 (CSS-3)
The DF-4 (CSS-3) "Chingyu" is China's first two-stage ballistic missile, with 5,550-7,000 km range and 2,200 kg payload (3 Mt nuclear warhead). It was developed in late 1960s to provide strike capability against Moscow and Guam. The DF-4 missile also served as basis for China's first space launch vehicle, Chang Zheng 1 (Long March 1). Approx. 20 DF-4's remain in service, and are scheduled to be replaced by DF-31 by 2010–2015.

Dongfeng 5 (CSS-4)
The DF-5 (CSS-4) is an intercontinental ballistic missile (ICBM), designed to carry a 3 megaton (Mt) nuclear warhead to distance up to 12,000 km. The DF-5 is a silo-based, two-stage missile, and its rocket served as the basis for the space-launch vehicle Fengbao-Tempest (FB-1) used to launch satellites. The missile was developed in the 1960s, but did not enter service until 1981. An improved variant, the DF-5A, was produced in the mid 1990s with improved range (>13,000 km). Currently, an estimated 24-36 DF-5A's are in service as China's primary ICBM force. If the DF-5A is launched from the eastern part of the Qinghai province, it can reach cities like Los Angeles, Sacramento and San Francisco. If it is launched from the most eastern parts of northeastern provinces, it can cover all of the mainland of the United States.

Dongfeng 11 (CSS-7)
The DF-11 (CSS-7, also M-11 for export), is a road-mobile SRBM designed by Wang Zhenhua at the Sanjiang Missile Corporation (also known as the 066 Base) in the late 1970s. Unlike previous Chinese ballistic missiles, the DF-11 use solid fuel, which greatly reduces launch preparation time to around 15–30 minutes, while liquid-fuelled missiles such as the DF-5 require up to 2 hours of pre-launch preparation. The DF-11 has a range of 300 km and an 800 kg payload. An improved DF-11A version has increased range of >825 km. The range of the M-11 does not violate the limits set by the Missile Technology Control Regime (MTCR). Estimates on the number of DF-11s in service vary between 500 and 600.

Dongfeng 12 (CSS-X-15)
The DF-12 (CSS-X-15) is an SRBM formerly known as the M20. The change in designation signalled a shift in fielding to the Second Artillery Corps, making it possible the missile could be armed with a tactical nuclear warhead. Images of it bear a resemblance to the Russian 9K720 Iskander missile which, although not purchased by China from Russia, could have been acquired from former Soviet states. Like the Iskander, the DF-12 reportedly has built-in countermeasures including terminal maneuverability to survive against missile defense systems. Range is officially between 100-280 km, but given MTCR restrictions, actual maximum range may be up to 400-420 km. With guidance provided by inertial navigation and Beidou, accuracy is 30 meters CEP; since the missile is controlled throughout the entire flight path, it can be re-targeted mid-flight. The DF-12 is 7.815 m long, 0.75 m in diameter, has a take-off weight of 4010 kg, and an 880 lb warhead that can deliver cluster, high explosive fragmentation, penetration, or high-explosive incendiary payloads. They are fired from an 8×8 transporter erector launcher (TEL) that holds two missiles.

An anti-ship ballistic missile export variant of the M20, called A/MGG-20B (M20B), was unveiled at the 2018 Zhuhai Airshow.

Dongfeng 15 (CSS-6)
The DF-15 (CSS-6, also M-9 for export) was developed by the China Aerospace Science and Technology Corporation (CASC, previously known as the 5th Aerospace Academy)'s Academy of Rocket Motor Technology (ARMT, also known as the 4th Academy). The missile is a single-stage, solid-fuel SRBM with a 600 km range and a 500 kg payload. During the 1995-1996 Taiwan strait crisis, the PLA launched six DF-15's near Taiwan in a demonstration of the missile's capability. Although the DF-15 is marketed for export, its range would violate the Missile Technology Control Regime (MTCR) agreement, and thus no DF-15 has been exported to date. Approximately 300-350 DF-15's are in service with the PLA Rocket Force.

Dongfeng 16 (CSS-11)
The DF-16 (CSS-11) is a new-model missile that has a longer range than the DF-15 (between 800-1000 km). A Taiwan official announced on 16 March 2011 that Taiwan believed China had begun deploying the missiles. The DF-16 represents an increased threat to Taiwan because it is more difficult to intercept for anti-ballistic missiles systems such as the MIM-104 Patriot PAC-3. Due to its increased range, the missile has to climb to higher altitudes before descending, giving more time for gravity to accelerate it on re-entry, faster than a PAC-3 could effectively engage it. The DF-16 is an MRBM longer and wider than previous models with a 1,000-1,500 kg warhead and 5-10 meter accuracy. Its bi-conic warhead structure leaves room for potential growth to include specialized terminally guided and deep penetrating warheads. It is launched from a 10×10 wheeled TEL similar to that of the DF-21, but instead of a "cold launch" missile storage tube it uses a new protective "shell" to cover the missile. Nuclear capable.

The missile was shown to the public during the 2015 China Victory Day Parade in Beijing celebrating 70-year anniversary of the end of World War II.

Dongfeng 17
The DF-17 is a medium-range ballistic missile used to launch the DF-ZF hypersonic glide vehicle. The DF-ZF is armed with a conventional warhead, although US intelligence considers it to be nuclear capable as well. The system entered service in the second half of 2019.

Dongfeng 21 (CSS-5)
The DF-21 (CSS-5) is a two-stage, solid-fuel MRBM developed by the 2nd Aerospace Academy (now China Changfeng Mechanics and Electronics Technology Academy) in late 1970s. It was the first solid-fuelled ballistic missile deployed by the Second Artillery Corp. The missile carries a single 500 kt nuclear warhead, with up to 2,500 km range. The DF-21 also served as the basis for the submarine-launched ballistic missile (SLBM) JL-1 (CSS-N-3), used on the Xia-class SSBN. In 1996, an improved variant, the DF-21A, was introduced. As of 2010, 60-80 DF-21/DF-21A were estimated to be in service; this number may have increased since then. Sources say Saudi Arabia bought a DF-21 in 2007.

The latest variant, the DF-21D, has a maximum range exceeding 1,450 kilometres (900 mi; 780 nmi) according to the U.S. National Air and Space Intelligence Center. It is hailed as the world's first anti-ship ballistic missile (ASBM) system, capable of targeting a moving carrier strike group from long-range, land-based mobile launchers. The DF-21D is thought to employ maneuverable reentry vehicles (MaRVs) with a terminal guidance system. It may have been tested in 2005–2006, and the launch of the Jianbing-5/YaoGan-1 and Jianbing-6/YaoGan-2 satellites offering targeting information from synthetic aperture radar (SAR) and visual imaging respectively.

Dongfeng 25
The DF-25 was a mobile-launch, two-stage, solid-fuel IRBM with a range of 3,200 km. Development was allegedly cancelled in 1996. The U.S. Department of Defense in its 2013 report to Congress on China's military developments made no mention of the DF-25 as a missile in service.

Dongfeng 26

The DF-26C is an IRBM with a range of at least 5,000 km, far enough to reach U.S. naval bases in Guam. Few details are known, but it is believed to be solid-fuelled and road-mobile, allowing it to be stored in underground bunkers and fired at short notice, hence difficult to counter. It is possible that the DF-26C is a follow-up version of the DF-21. Possible warheads include conventional, nuclear or even maneuverable anti-ship and hypersonic glide warheads.

Dongfeng 27
The DF-27 is a long-range ballistic missile that is in development as of 2021, with a range of 5,000 km to 8,000 km.

Dongfeng 31 (CSS-10)
The DF-31 (CSS-10) is China's newest road-mobile, solid-fuel ICBM developed by the 4th Aerospace Academy (now ARMT). The DF-31 has range of 8,000+ km, and can carry a single 1,000 kt warhead, or up to three 20-150 kt MIRV warheads. An improved version, the DF-31A, has range of 11,000+ km, far enough to reach Los Angeles from Beijing. The DF-31 was developed to replace many of China's older ballistic missiles, and served as basis to the new JL-2 (CSS-NX-4/CSS-NX-5) SLBM. In 2009, approx. 30 DF-31/DF-31A are estimated to be in service; it is possible this number may have increased since then. 12 were displayed at the 2009 military parade in Beijing commemorating the 60th anniversary of the PRC's founding.

The DF-31AG uses a mobile launcher with improved mobility. It made its first official public appearance in the 2017 PLA Day Parade.

Dongfeng 41 (CSS-20)
The DF-41 (CSS-20), capable of being armed with ten or twelve MIRV warheads, is China's newest addition to its nuclear arsenal. With an estimated range between 12,000 - 15,000 km, it is believed to surpass the range of the US's LGM-30 Minuteman ICBM to become the world's longest range missile.

title: Dongfeng (missile)


text:
Jefferson County, New York

Jefferson County is a county on the northern border of the U.S. state of New York. As of the 2020 census, the population was 116,721. Its county seat is Watertown. The county is named after Thomas Jefferson, third President of the United States of America. It is adjacent to Lake Ontario, southeast from the Canada–US border of Ontario. The county is part of the North Country region of the state.

Jefferson County comprises the Watertown-Fort Drum, NY Metropolitan Statistical Area. The popularity of the area as a summer tourist destination results in a dramatic increase of population during that season.

In 2014, it elected Colleen M. O'Neill as the first woman county sheriff in the state. She had served with the New York State Police for 32 years.

The United States Army's 10th Mountain Division is based at Fort Drum. The base had a total population of nearly 13,000 according to the 2010 census.

History
When counties were established in the Province of New York in 1683, the present Jefferson County was part of Albany County. This was an enormous county, including the northern part of New York State as well as all of the present State of Vermont and, in theory, extending westward to the Pacific Ocean. This county was reduced in size on July 3, 1766, by the creation of Cumberland County, and further on March 16, 1770, by the creation of Gloucester County, both containing territory now in Vermont.

On March 12, 1772, what was left of Albany County was split into three parts, one remaining under the name Albany County. One of the other pieces, Tryon County, contained the western portion (and thus, since no western boundary was specified, theoretically still extended west to the Pacific). The eastern boundary of Tryon County was approximately 5 mi west of the present city of Schenectady, and the county included the western part of the Adirondack Mountains and the area west of the West Branch of the Delaware River. The area then designated as Tryon County now includes 37 counties of New York State. The county was named for William Tryon, colonial governor of New York.

In the years subsequent to 1776, most of the Loyalists in Tryon County fled to Canada. In 1784, following the peace treaty that ended the American Revolutionary War, the name of Tryon County was changed to Montgomery County to honor the general, Richard Montgomery, who had captured several places in Canada and died attempting to capture the city of Quebec, replacing the name of the hated British governor.

In 1789, the size of Montgomery County was reduced by the creation of Ontario County from Montgomery. The area split off from Montgomery County was much larger than the present county, as it was later divided to form the present Allegany, Cattaraugus, Chautauqua, Erie, Genesee, Livingston, Monroe, Niagara, Orleans, Steuben, Wyoming, Yates, and parts of Schuyler and Wayne counties.

Jefferson County is part of Macomb's Purchase of 1791.

In 1791, Herkimer County was one of three counties split off from Montgomery (the other two being Otsego, and Tioga County). This was much larger than the present county, however, and was reduced by a number of subsequent splits. The first one of these, in 1794, produced Onondaga County. This county was larger than the current Onondaga County, including the present Cayuga and Cortland Counties, and part of Oswego County.

Oneida County (as well as a part of Chenango County), was split off from Herkimer County in 1798.

Jefferson County was split off from Oneida County in 1805. In 1817, Carleton Island, captured from the British in the War of 1812, was annexed to the county. During the late eighteenth and nineteenth centuries, the county was largely developed for agriculture.

By the early 20th centuries, Watertown was a city with the highest per capita number of millionaires in the United States. Local industrialists had made early fortunes from industries driven by water power. Mills were established along the falls of the Black River from the first half of the nineteenth century.

In 2019, Jefferson County and much of the rest of the North Country was identified as one of the most politically tolerant communities in America, according to an analysis by PredictWise.

Geography
According to the U.S. Census Bureau, the county has an area of 1857 sqmi, of which 1269 sqmi is land and 589 sqmi (32%) is water. It is the fourth-largest county in New York by area.

Jefferson County is in New York State's northern lobe, adjacent to the area where the Saint Lawrence River exits Lake Ontario. It is northeast of Syracuse, and northwest of Utica. The county is at the international border with Canada.

The Black River, which empties into Lake Ontario, is an important waterway in the county. Part of the Tug Hill Plateau is in the southern part of the county. The county contains part of the Thousand Islands in the St. Lawrence River, including such large islands as Carleton Island, Grindstone Island, and Wellesley Island.

Adjacent counties

 * St. Lawrence County – northeast
 * Lewis County – southeast
 * Oswego County – southwest
 * Leeds and Grenville United Counties, Ontario – north
 * Frontenac County, Ontario – northwest

Major highways

 * [[Image:I-81.svg|20px]] Interstate 81
 * [[Image:I-781 (long).svg|22px]] Interstate 781
 * [[Image:US 11.svg|20px]] U.S. Route 11
 * [[Image:NY-3.svg|20px]] New York State Route 3
 * [[Image:NY-3A.svg|20px]] New York State Route 3A
 * [[Image:NY-12.svg|20px]] New York State Route 12
 * [[Image:NY-12E.svg|22px]] New York State Route 12E
 * [[Image:NY-12F.svg|22px]] New York State Route 12F
 * [[Image:NY-26.svg|20px]] New York State Route 26
 * [[Image:NY-37.svg|20px]] New York State Route 37
 * [[Image:NY-180.svg|22px]] New York State Route 180

2000 census
As of the census of 2000, there were 111,738 people, 40,068 households, and 28,127 families residing in the county. The population density was 88 pd/sqmi. There were 54,070 housing units at an average density of 42 /mi2. The county's racial makeup was 88.71% White, 5.83% Black or African American, 0.53% Native American, 0.92% Asian, 0.14% Pacific Islander, 2.05% from other races, and 1.82% from two or more races. 4.19% of the population were Hispanic or Latino of any race. 93.2% spoke English and 3.5% Spanish as their first language.

21.9% were of English, 14.1% Irish, 12.8% German, 8.5% French and 8.5% Italian ancestry according to the 2010 American Community Survey.

There were 40,068 households, of which 37.20% had children under the age of 18 living with them, 55.60% were married couples living together, 10.40% had a female householder with no husband present, and 29.80% were non-families. 24.40% of all households were made up of individuals, and 10.10% had someone living alone who was 65 years of age or older. The average household size was 2.58 and the average family size was 3.07.

26.50% of the county's population was under age 18, 11.80% was from age 18 to 24, 31.30% was from age 25 to 44, 19.10% was from age 45 to 64, and 11.30% were age 65 or older. The median age was 32 years. For every 100 females there were 107.30 males. For every 100 females age 18 and over, there were 108.50 males.

The county's median household income was $34,006, and the median family income was $39,296. Males had a median income of $28,727 versus $21,787 for females. The county's per capita income was $16,202. About 10.00% of families and 13.30% of the population were below the poverty line, including 16.80% of those under age 18 and 9.20% of those age 65 or over.

Education
Jefferson Community College in Watertown provides higher education within the county.

Larger Settlements
† - County Seat

†† - Former Village

Towns

 * Adams
 * Alexandria
 * Antwerp
 * Brownville
 * Cape Vincent
 * Champion
 * Clayton
 * Ellisburg
 * Henderson
 * Hounsfield
 * Le Ray
 * Lorraine
 * Lyme
 * Orleans
 * Pamelia
 * Philadelphia
 * Rodman
 * Rutland
 * Theresa
 * Watertown
 * Wilna
 * Worth

Hamlet

 * Sanfords Four Corners

Government and politics
Legislative authority is vested in the county Board of Legislators, which consists of 15 members each elected from single member districts for two-year terms. As of 2018, there are 14 Republicans and 1 Democrat.

Jefferson County is reliably Republican. Since 1884, Democrats only carried the county twice, in 1964 and in 1996.

 * }

Law enforcement
the sheriff is Colleen M. O'Neill. O'Neill is the first female sheriff elected in the state, and was first elected in 2014.

In 2012, the Sheriff's Office was the subject of three unrelated sexual harassment lawsuits by a female deputy and two other women.

Sites of interest

 * Antique Boat Museum
 * Boldt Castle
 * Burnham Point State Park
 * Canoe-Picnic Point State Park
 * Cape Vincent
 * Carleton Island
 * Cedar Point State Park
 * Clayton
 * Dewolf Point State Park
 * Duffy Fairgrounds
 * Fairview Manor
 * Fort Drum
 * Grass Point State Park
 * Grenadier Island
 * Grindstone Island Upper Schoolhouse
 * National Register of Historic Places listings in Jefferson County, New York
 * Orleans
 * Paddock Arcade
 * Paddock Mansion
 * Public Square Historic District
 * Roswell P. Flower Memorial Library
 * Sackets Harbor
 * Sackets Harbor Battlefield State Historic Site
 * Thousand Islands
 * Thousand Islands National Park
 * Tibbetts Point Lighthouse
 * Union Hotel (Sackets Harbor, New York)
 * Watertown
 * Wellesley Island State Park
 * Thousand Islands Arts Center

license: Creative Commons - Attribution Share-Alike - https://creativecommons.org/licenses/by-sa/4.0/

title: Jefferson County, New York


text:
Herkimer County, New York

Herkimer County is a county in the U.S. state of New York. As of the 2020 census, the population was 60,139. Its county seat is Herkimer. The county was created in 1791 north of the Mohawk River out of part of Montgomery County. It is named after General Nicholas Herkimer, who died from battle wounds in 1777 after taking part in the Battle of Oriskany during the Revolutionary War.

Herkimer County is part of the Utica–Rome Metropolitan Statistical Area and the Mohawk Valley region.

History
In 1791, Herkimer County was created as one of three counties split off from Montgomery (the other two being Otsego and Tioga counties) as New York State was developed after the American Revolutionary War. Its area was much larger than the present county, however, and was reduced subsequently as more counties were organized.

Part of Herkimer County was included in the Macomb's Purchase of 1791, during the wide-scale sale of public lands after the state forced Iroquois tribes allied with the British during the war to cede their territory. Suddenly the state was selling 5 e6acre of land in upstate, central and western New York.

In 1794, Onondaga County was split off from Herkimer County. This county was larger than the current Onondaga County, and included the present Cayuga, Cortland, and part of Oswego counties.

In 1798, portions of Herkimer and Tioga counties were taken to form Chenango County.

Another part of Herkimer was split off to form Oneida County. It was then larger than the current Oneida County, including the present Jefferson, Lewis, and part of Oswego counties.

In 1802, parts of Herkimer, Clinton and Montgomery counties were combined to form the new St. Lawrence County.

The rural economy was first based on general agriculture and then wheat, but after the opening of the Erie Canal, Herkimer farmers found that they could not compete with grain farmers to the west. By the mid-19th century, they had begun to specialize in dairy farming and created a cheese industry that supplied the New York City market, among others.

During the American Civil War, Herkimer contributed five companies to the 34th New York Volunteer Infantry Regiment, leading to the unit's nickname "The Herkimer Regiment".

The Herkimer County Jail, constructed in 1834, was used to hold the murderer Chester Gillette before his trial at the Herkimer County Courthouse. The jail is now disused, except for tours by the Herkimer County Historical Society.

The Herkimer County shootings took place in 2013, killing five people.

Geography
According to the U.S. Census Bureau, the county has a total area of 1458 sqmi, of which 1411 sqmi is land and 46 sqmi (3.2%) is water.

Adjacent counties

 * St. Lawrence County - north
 * Hamilton County - northeast
 * Fulton County - east
 * Montgomery County - southeast
 * Otsego County - south
 * Oneida County - west
 * Lewis County - northwest

Herkimer County is in central New York State, northwest of Albany, and east of Syracuse. The northern part of the county is in the Adirondack Park. The Mohawk River flows across the southern part of the county. Herkimer County is larger than the State of Rhode Island

2000 census
As of the census of 2000, there were 64,427 people, 25,734 households, and 17,113 families residing in the county. The population density was 46 PD/sqmi. There were 32,026 housing units at an average density of 23 /mi2. The racial makeup of the county was 97.83% White, 0.51% Black or African American, 0.22% Native American, 0.41% Asian, 0.02% Pacific Islander, 0.18% from other races, and 0.84% from two or more races. 0.90% of the population were Hispanic or Latino of any race. 20.6% were of Italian, 16.3% German, 13.9% Irish, 9.3% English, 7.7% Polish, 6.2% American and 5.2% French ancestry according to Census 2000. 95.2% spoke English, 1.2% Spanish and 1.1% Italian as their first language.

There were 25,734 households, out of which 30.60% had children under the age of 18 living with them, 51.20% were married couples living together, 10.30% had a female householder with no husband present, and 33.50% were non-families. 27.60% of all households were made up of individuals, and 13.70% had someone living alone who was 65 years of age or older. The average household size was 2.46 and the average family size was 2.99.

In the county, the population was spread out, with 24.40% under the age of 18, 8.30% from 18 to 24, 26.60% from 25 to 44, 24.00% from 45 to 64, and 16.80% who were 65 years of age or older. The median age was 39 years. For every 100 females there were 94.20 males. For every 100 females age 18 and over, there were 91.70 males.

The median income for a household in the county was $32,924, and the median income for a family was $40,570. Males had a median income of $29,908 versus $21,518 for females. The per capita income for the county was $16,141. About 8.90% of families and 12.50% of the population were below the poverty line, including 15.60% of those under age 18 and 10.40% of those age 65 or over.

Government and politics

 * }

Herkimer County is one of the most Republican counties in New York. Since 1884, it has voted for a Democratic presidential candidate only three times, with vote splitting due to a third-party candidate playing a role in two of those races. Since 2022, the entire county is within New York's 21st congressional district, presently held by Republican Elise Stefanik.

The Herkimer County Legislature consists of 17 members, each elected from single-member districts. the county legislature is almost entirely Republican: the single Democratic legislator also ran on the Conservative Party line.

Economy
Herkimer County is known for producing unusually clear, doubly terminated quartz crystals, marketed as Herkimer diamonds.

Ilion in Herkimer County has one of two production sites of the Remington Arms Company, where many of the company's firearms are produced.

Education
Herkimer County Community College is located in the Village of Herkimer.

Airport
The following public use airport is located in the county:
 * Frankfort-Highland Airport (6B4) – Frankfort

Rail
Passenger rail service by Amtrak is available at Utica, nearby to the west of the county. Up to the latter 1950s, New York Central Railroad trains such as the North Shore Limited (New York-Chicago) made stops at Little Falls. Until 1965, the New York Central operated passenger trains through Thendara in the upper part of the county.

Roads
Interstate 90, as part of the New York State Thruway, runs east–west through the lower part of the county, as does New York State Route 5. State Route 28 runs north–south through the county.

Towns

 * Columbia
 * Danube
 * Fairfield
 * Frankfort
 * German Flatts
 * Herkimer
 * Litchfield
 * Little Falls
 * Manheim
 * Newport
 * Norway
 * Ohio
 * Russia
 * Salisbury
 * Schuyler
 * Stark
 * Warren
 * Webb
 * Winfield

Hamlets

 * Beaver River
 * Jordanville
 * Newville

title: Herkimer County, New York


text:
Treaty of Belgrade

The Treaty of Belgrade, also known as the Belgrade Peace, was the peace treaty signed on September 18, 1739 in Belgrade, Habsburg Kingdom of Serbia (today Serbia), by the Ottoman Empire on one side and the Habsburg monarchy on the other, that ended the Austro–Turkish War (1737–39). It also recognized Circassia, particularly its eastern half Kabardia, as an independent nation for the first time by the European countries.

Treaty
This treaty ended the hostilities of the five-year Austro-Russian–Turkish War (1735–39), in which the Habsburgs joined Imperial Russia in its fight against the Ottomans. Austria was defeated by the Turks at Grocka and signed a separate treaty in Belgrade with the Ottoman Empire on August 21, probably being alarmed at the prospect of Russian military success. With the Treaty of Belgrade, the Habsburgs ceded the Kingdom of Serbia with Belgrade, the southern part of the Banat of Temeswar and northern Bosnia to the Ottomans, and the Banat of Craiova (Oltenia), gained by the Treaty of Passarowitz in 1718, to Wallachia (an Ottoman subject), and set the demarcation line to the rivers Sava and Danube. The Habsburg withdrawal forced Russia to accept peace at the Russo-Turkish War, 1735-1739 with the Treaty of Niš, whereby it was allowed to build a port at Azov, gaining a foothold on the Black Sea.

The Treaty of Belgrade effectively ended the autonomy of Kingdom of Serbia which had existed since 1718. This territory would await the next Habsburg-Ottoman war to be temporarily again included into the Habsburg monarchy in 1788 with the help of Koča Anđelković.

The treaty is also notable for being one of the last international treaties to be written in Latin.

The treaty recognized Circassia, particularly its eastern half Kabardia, as an independent nation for the first time by the European countries.

title: Treaty of Belgrade


text:
Peak District

The Peak District is an upland area in central-northern England, at the southern end of the Pennines. Mostly in Derbyshire, it extends into Cheshire, Greater Manchester, Staffordshire, West Yorkshire and South Yorkshire. It is subdivided into the Dark Peak, moorland dominated by gritstone, and the White Peak, a limestone area with valleys and gorges. The Dark Peak forms an arc on the north, east and west of the district, and the White Peak covers central and southern areas. The highest point is Kinder Scout (2087 ft). Most of the area is within the Peak District National Park, a protected landscape designated in 1951.

A 2021 report states that "the Park’s own population numbers around 40,000 and supports an estimated 18,000 jobs, predominantly through farming, manufacturing and, inevitably, tourism".

The area has been inhabited since the Mesolithic era, and was largely agricultural until mining arose in the Middle Ages. During the Industrial Revolution several cotton mills were constructed in the area's valleys by Richard Arkwright. As mining declined, quarrying grew. Tourism came with the railways, spurred by the landscape, spa towns and Castleton's show caves.

Geography
The Peak District forms the southern extremity of the Pennines. Much of it is upland above 1000 ft, its highest point being Kinder Scout at 2087 ft. Despite its name, the landscape has fewer sharp peaks than rounded hills, plateaus, valleys, limestone gorges and gritstone escarpments (the "edges"). The mostly rural area is surrounded by conurbations and large urban areas, including Manchester, Huddersfield, Sheffield, Derby and Stoke-on-Trent.

The national park has formal boundaries. It covers most of the Dark Peak and White Peak, but the wider Peak District is less well defined. The Dark Peak is largely uninhabited moorland and gritstone escarpments in the northern Peak District and its eastern and western margins. It encloses the central and southern White Peak, which is where most settlements, farmland and limestone gorges are found. Three of Natural England's National Character Areas (NCAs) cover parts of it. The Dark Peak NCA includes the northern and eastern parts of the Dark Peak and the White Peak NCA most of the White Peak. The western margins of the Dark Peak are in the South West Peak NCA, where farmland and pastured valleys are found with gritstone edges and moorland. Outside the park, the wider Peak District often includes the area approximately between Disley and Sterndale Moor, encompassing Buxton and the Peak Dale corridor. It may also include some of the outer fringes and foothills, such as the Churnet and lower Derwent Valleys. The region is mostly surrounded by lowlands with gritstone moorlands of the South Pennines to the north, separated approximately by the Tame Valley, Standedge and Holme Valley.

The national park covers 555 sqmi, including most of the region in Derbyshire and extends into Staffordshire, Cheshire, Greater Manchester and South and West Yorkshire. Its northern limit is on a track near Deer Hill in Meltham; its southernmost point is on the A52 road near Ashbourne. The boundaries were drawn to exclude built-up and industrial areas; in particular Buxton and the quarries at the end of the Peak Dale corridor are surrounded on three sides by the park. Bakewell and many villages are in the national park, as is much of the rural west of Sheffield. In 2010 it became the fifth largest national park in England and Wales. In the UK, designation as a national park means that planning and other functions are provided by a national park authority, with additional restrictions that enhance protection from inappropriate development. Land within this national park as in others is in a mix of public and private ownership.

The National Trust, a charity that conserves historic and natural landscapes, owns about 12 per cent of the land in the national park. Its three estates (High Peak, White Peak and Longshaw) include ecologically or geologically significant areas at Bleaklow, Derwent Edge, Hope Woodlands, Kinder Scout, the Manifold valley, Mam Tor, Dovedale, Milldale and Winnats Pass. The park authority owns around 5 per cent; other major landowners include several water companies.

Settlements
Bakewell is the largest settlement and only town in the national park and the site of the National Park Authority offices. Its five-arched bridge over the River Wye dates from the 13th century. Castleton is the centre of production of a semi-precious mineral, Blue John. Eyam village is known for a self-imposed quarantine during the Black Death. Edale is the southern end of the Pennine Way, a 268-mile national trail which traverses most of the Pennines and ends at Kirk Yetholm in the Scottish border. The park also contains the highest village in the United Kingdom, Flash, at 1519 ft. Other villages in the park include Hathersage, Hartington, Ilam and Tideswell.

The towns of Glossop, Chapel-en-le-Frith, Buxton, Macclesfield, Leek, Ashbourne, Matlock and Chesterfield are on the national park's fringes. The spa town of Buxton was built up by the Dukes of Devonshire as a genteel health resort in the 18th century while the spa at Matlock Bath, in the River Derwent valley, was popularised in Victorian times. Hayfield is at the foot of Kinder Scout, the area's highest summit. Other towns and villages fringing the park include Whaley Bridge, Hadfield, Tintwistle, Darley Dale and Wirksworth in Derbyshire, Stocksbridge in South Yorkshire and Marsden and Holmfirth in West Yorkshire.

Rivers, reservoirs and canals
Several rivers have sources on the moorland plateaux of the Dark Peak and the high ridges of the White Peak. Many rivers in the Dark Peak and outer fringes were dammed to create reservoirs for supplying drinking water. Streams were dammed to provide headwater for water driven mills; weirs were built for the same purpose. The reservoirs of the Longdendale Chain were completed in February 1877 to provide compensation water, ensuring a continuous flow in the River Etherow, which was essential for local industry and provided drinking water for Manchester. In a report for the Manchester Corporation, John Frederick Bateman wrote in 1846:

"Within ten or twelve miles of Manchester, and six or seven miles from the existing reservoirs at Gorton, there is this tract of mountain land abounding with springs of the purest quality. Its physical and geological features offer such peculiar features for the collection, storage and supply of water for the use of the towns in the plains below that I am surprised that they have been overlooked."

The western Peak District is drained by the Etherow, the Goyt and the Tame, all tributaries of the River Mersey. The north-east is drained by tributaries of the River Don. Of the tributaries of the River Trent draining south and east, the River Derwent is the most prominent. It rises on Bleaklow just east of Glossop and flows through the Upper Derwent Valley, where it is constrained by the Howden, Derwent and Ladybower reservoirs. The reservoirs of the Upper Derwent Valley were built from the early to mid-20th century to supply drinking water to the East Midlands and South Yorkshire.

The rivers Noe and the Wye are tributaries. The River Manifold and River Dove in the south-west, whose sources are on Axe Edge Moor, flow into the Trent. The River Dane flows into the River Weaver in Cheshire.

There are no canals in the national park, although the Standedge Tunnels on the Huddersfield Narrow Canal run underneath the extreme north of it. Outside the park, waters from the Dark Peak feed the Macclesfield, Ashton, and Huddersfield Narrow Canals and waters from the White Peak fed the Cromford Canal. The Peak Forest Canal brought lime from the quarries at Dove Holes for the construction industry. It terminated at Bugsworth Basin and the journey was completed using the Peak Forest Tramway.

The Cromford Canal, from Cromford to the Erewash Canal, served lead mines at Wirksworth and Sir Richard Arkwright's cotton mills. The Caldon Canal from Froghall was built to transport limestone from quarries at Cauldon Low for the iron industry and flints for the pottery industry.

Climate
Most of the area is over 1000 ft above sea level, in the centre of the country at a latitude of 53°N, bringing relatively high annual rainfall averaging 40.35 in in 1999. The Dark Peak tends to receive more rainfall than the White Peak, as it is higher. The higher rainfall does not affect the temperature, which averages the same as the rest of England and Wales at 10.3 °C.

In the 1970s, the Dark Peak regularly had more than 70 days of snowfall. Since then the number has fallen. The hills still see long periods of continuous snow cover in some winters. Snow in mid-December 2009 on some hill summits created some snow patches that lasted until May 2010. In the same winter, the A635 (Saddleworth Moor) and A57 (Snake Pass) were closed due to snow for almost a month. Frost cover is seen for 20–30 per cent of the winter on moorland in the Dark Peak and 10 per cent in the White Peak.

The Moorland Indicators of Climate Change Initiative was set up in 2008 to collect data in the area. Students investigated the interaction between people and the moorlands and their effect on climate change, to discover whether the moorlands are a net carbon sink or source, based on the fact that Britain's upland areas contain a major global carbon store in the form of peat. Human interaction in terms of direct erosion and fire, with the effects of global warming, are the main variables they considered.

Geology
The Peak District is formed almost wholly of sedimentary rocks of the Carboniferous period. They make up the carboniferous limestone overlying gritstone, and the coal measures that occur only on the margins and infrequent outcrops of igneous rocks, including lavas, tuffs and volcanic vent agglomerates. The general geological structure is that of a broad dome, whose western margins have been intensely faulted and folded. Uplift and erosion have sliced the top off the Derbyshire Dome to reveal a concentric outcrop pattern with coal-measured rocks on the eastern and western margins, carboniferous limestone at the core and rocks of millstone grit between them. The southern edge of the Derbyshire dome is overlain by sandstones of Triassic age, though they barely impinge on the National Park. The White Peak forms a central and southern section with carboniferous limestone found at or near the surface. The Dark Peak to the north, east and west is marked by millstone grit outcrops and broad swathes of moorland.

Earth movements after the Carboniferous period resulted in the up-doming of the area and, particularly in the west, the folding of the rock strata along north–south axes. The region was raised in a north–south line which resulted in the dome-like shape and the shales and sandstones were worn away until limestone was exposed. At the end of this period, the Earth's crust sank here which led to the area being covered by sea, depositing a variety of new rocks. Some time after its deposition, mineral veins were formed in the limestone. The veins and rakes have been mined for lead since Roman times. The Peak District was iced over in at least one of the ice ages of the last two million years, probably the Anglian glaciation of some 450,000 years ago, as shown by patches of glacial till or boulder clay found across the area. It was not iced over in the last glacial period, which peaked about 20,000–22,000 years ago. A mix of Irish Sea and Lake District ice abutted its western margins. Glacial meltwaters eroded a complex of sinuous channels along this margin of the district. Glacial meltwaters contributed to the formation and development of many caves in the limestone area. Remains of wild animal herds roaming the area have been found in several caves.

Various rock-types beneath the soil strongly influence the landscape; they determine the type of vegetation and ultimately the type of animal inhabiting the area. Limestone has fissures and is soluble in water, so that rivers could carve deep, narrow valleys. These often find routes underground, creating cave systems. Millstone grit is insoluble but porous, absorbing water that seeps through the grits, until it meets the less porous shales beneath, creating springs where it reaches the surface. The shales are friable and easily attacked by frost, forming areas vulnerable to landslides, as on Mam Tor.

Ecology
The gritstone and shale of the Dark Peak supports heather moorland and blanket bog, with rough sheep pasture and grouse shooting as the main land uses, though parts are also farmed, especially the South West Peak NCA. The limestone plateaus of the White Peak are more intensively farmed, with mainly dairy usage of improved pastures. Woodland forms some 8 per cent of the Peak National Park. Natural broad-leaved woodland appears in the steep dales of the White Peak and cloughs of the Dark Peak. Reservoir margins often have coniferous plantations.

Flora
White Peak habitats include calcareous grassland, ash woodlands and rock outcrops for lime-loving species. They include early purple orchid (Orchis mascula), dark-red helleborine (Epipactis atrorubens) and fly orchid (Ophrys insectifera), common rockrose (Helianthemum nummularium), spring cinquefoil (Helianthemum nummularium) and grass of parnassus (Parnassia palustris). Lead rakes, the spoil heaps of ancient mining activity, form another distinctive White Peak habitat, supporting a range of rare metallophyte plants, including spring sandwort (Minuartia verna; also known as leadwort), alpine pennycress (Thlaspi caerulescens) and mountain pansy (Viola lutea).

Two endemic vascular plants are found nowhere else in the world: Derby hawkweed (Hieracium naviense), found only in Winnats Pass, is a native perennial of limestone cliffs discovered by J. N. Mills in 1966 and described as a new species in 1968; and leek-coloured hawkweed (H. subprasinifolium), which was believed extinct until rediscovered on banks beside the Monsal Trail in Chee Dale in 2017. The endemic Derbyshire feather moss (Thamnobryum angustifolium) occurs in one Derbyshire limestone dale, its sole world location intentionally kept confidential; the colony covers about 3 m2 of a rock face with small subsidiary colonies nearby.

Jacob's-ladder (Polemonium caeruleum), a rarish species characteristic of limestone dales in the White Peak, has been Derbyshire's county flower since 2002. It grows on grassland, light woodland, screes and rock ledges, and by streams in Lathkill, Wolfscote, Taddington, Wye Dale and other dales. Pollen evidence from peat bogs shows it was widespread throughout Britain just after the last ice age. Much planted in gardens from where it has established itself in other parts of the area, as a native it is restricted to the White Peak and the Yorkshire Dales.

The Dark Peak heathlands, bogs, gritstone edges and acid grasslands contain relatively few species; heather (Calluna vulgaris), crowberry (Empetrum nigrum), bilberry (Vaccinium myrtillus) and hare's-tail cotton grass (Eriophorum vaginatum) dominate the high moors. After decades of decline due to pollution, Sphagnum mosses are returning, with species such as S. cuspidatum particularly dominant.

Mammals
Most Peak District mammals are generalists and widespread across the UK, but the mountain hares on heather moorland in the Dark Peak form the only wild population in England. They were reintroduced in the Victorian era for sporting purposes. A feral population of red-necked wallabies lived around The Roaches from the 1940s onwards, but may now be extinct. Red deer herds, assumed to be derived from animals escaped from deer parks at Lyme Park and Chatsworth, are established in the upper reaches of the Goyt valley and on the moors above Baslow, and a herd on Wharncliffe Crags outside the national park north of Sheffield may derive from hunting stock of Wharncliffe Chase. Biodiversity action plans have been prepared for mountain hare, brown hare, brown long-eared bat, dormouse, harvest mouse, hedgehog, noctule bat, otter, pine marten, polecat, soprano pipistrelle and water vole. The status of the pine marten is unclear, though confirmed sightings have occurred in recent decades in Derbyshire and north Staffordshire and a specimen from an introduced Welsh population was found dead outside the national park on a road between Ripley and Belper in 2018.

Birds
As with mammals, many Peak bird species are widespread generalists. The Dark Peak moors still support breeding populations of several upland specialists, such as twite, short-eared owl, golden plover, dunlin, ring ouzel, northern wheatear and merlin. The populations of twite and golden plover are the southernmost confirmed breeding populations in England, and the Peak District Moors Special Protection Area (SPA) is a European designation for its populations of merlin, golden plover and short-eared owl. The Peak District lacks the concentrations of breeding waders found further north in the Pennines, though the moors and their fringes accommodate breeding curlew and lapwing, and less noticeable wading birds such as dunlin and snipe.

Commercial driven grouse shooting occurs on the heather moorlands of the Dark Peak, where the red grouse population is maintained by gamekeepers employed by shooting estates. A population of black grouse became extinct in 2000, but reintroduction was attempted in 2003. Quarries and rock outcrops provide nest sites for peregrine falcon and common raven. Ravens and common buzzards are increasingly found as their British range expands eastwards, perhaps because of general reductions in persecution. Illegal persecution has limited populations of rare raptors such as Eurasian goshawk, peregrine and hen harrier. Following the RSPB's publication of Peak Malpractice, a 2006 report highlighting wildlife crime, the Peak District Bird of Prey Initiative was set up in 2011 by conservationists and shooting bodies to try to boost populations of birds of prey. The park authorities expressed disappointment at the limited results and the RSPB withdrew from the partnership in January 2018 citing continued efforts by the Moorland Association and National Gamekeepers’ Organisation which together had "frustrated any possibility of progress" on the issue.

Fast-flowing rivers attract specialists such as grey wagtail, dipper, common sandpiper, mandarin duck and goosander. Wooded and semi-wooded areas attract redstart, pied flycatcher, wood warbler and tree pipit, and coniferous plantations house siskin and common crossbill. Upland reservoirs in the Dark Peak are generally oligotrophic and attract few birds, but lower-lying reservoirs on the southern fringes such as Carsington Water and Ogston Reservoir regularly attract rare migrants and wintering rarities such as various waders, wildfowl, gulls and terns. The area is regularly overflown by wintering populations of pink-footed geese moving between East Anglia and Morecambe Bay.

Dipper, golden plover, hen harrier, merlin and short-eared owl are local biodiversity action plan priority species.

Fossil records show that the Peak District was once inhabited by an eclectic mix of species, many of them no longer found in Britain, such as alpine swift, demoiselle crane and long-legged buzzard. Species lost from the Peak District through human activity include hazel grouse, capercaillie and golden eagle.

Other taxa
Amphibians and reptiles such as common lizards, grass snakes, great crested newts and slow worms are found in the district. The eastern moors are a stronghold for adders.

Native fish in the Peak District include Atlantic salmon, brown trout, European eel, bullhead, brook lamprey and grayling. A possibly unique population of "wild" rainbow trout survives on the Derbyshire Wye, following their introduction at the turn of the 20th century.

Butterflies in the region include the dingy skipper, brown argus, small blue and white-letter hairstreak. Moths include the anomalous, broom moth, dot moth, garden dart, mouse moth and white ermine. Other invertebrates include the bilberry bumblebee, broad groove-head spider, mole cricket, northern yellow splinter, shining guest ant, violet oil beetle and white-clawed crayfish.

National Park
The Peak District National Park was the first national park to be designated in the United Kingdom, on 17 April 1951 (following the National Parks and Access to the Countryside Act of 1949 and a resulting public enquiry to establish its boundary). It was one of ten parks created in the 1950s in the wake of the 1945 Dower Report and 1947 Hobhouse Report, which recommended the creation of national parks in England and Wales. The park has an area of 1438 km2 and receives approximately 13 million visitors each year. 90% of the national park is privately owned, with the largest single owner being the National Trust (12%).

The national park is governed by the Peak District National Park Authority, which was established under the 1995 Environment Act, replacing the Peak Park Planning Board. The authority has 30 members, 14 appointed by the Secretary of State for Environment, Food, and Rural Affairs and 16 appointed by the local authorities covered by the park. The local authorities and the number of members they appoint are as follows:

History
The Peak has been inhabited from the earliest periods of human activity, as shown by finds of Mesolithic flint artefacts and palaeo-environmental evidence from caves in Dovedale and elsewhere. Signs of Neolithic activity include monumental earthworks or barrows such as the one at Margery Hill.

The Bronze Age saw the area well populated and farmed. Evidence remains in henges such as Arbor Low near Youlgreave and the Nine Ladies stone circle at Stanton Moor. In the same period and into the Iron Age, hill forts such as Mam Tor's were created. The Romans drew on the area's rich mineral veins, exporting lead from the Buxton area along well-used routes. Buxton was a Roman settlement known as "Aquae Arnemetiae" for its spring.

Theories on how the name Peak derived cite the Pecsaetan or peaklanders, an Anglo-Saxon tribe inhabiting the central and northern parts of the area from the 6th century CE, when it belonged to the Anglian kingdom of Mercia. Barrows from the Anglo-Saxon period are present, including Benty Grange, where the eponymous helmet was found.

Mining and quarrying
In medieval and early modern times the area was mainly agricultural, with sheep farming, rather than arable the main activity in upland holdings. From the 16th century, the mineral and geological wealth became increasingly significant. Not only lead, but coal, fluorite, copper from Ecton Mines, zinc, iron, manganese and silver have been mined. Celia Fiennes, describing a journey through the Peak in 1697, wrote of: "...Craggy hills Whose Bowells are full of mines of all kinds off Black and white and veined Marbles, and some have mines of Copper, others tinn and Leaden mines, in wch is a great deale of silver."

Coal measures occur on the Peak's western and eastern fringes. Evidence of past workings can be found from Glossop to The Roaches, and from Stocksbridge to Baslow. The coal measures in the east are at the western edge of the South Yorkshire Coalfield. Those in the west are part of the Cheshire section of the Lancashire Coalfield. Mining started in medieval times, was at its most productive in the 18th and early 19th centuries, and continued into the early 20th century. The earliest mining took place around outcrops, where miners followed the seams deeper into the hillsides. At Goyt's Moss and Axe Edge, deep seams were worked and steam engines raised the coal and dewatered the mines. Coal from the east was used in lead smelting and from the west for lime burning.

Lead mining peaked in the 17th and 18th centuries; high concentrations were found in the area from this period, along with peat on Kinder Scout, suggesting that lead smelting occurred. Lead mining declined from the mid-19th century – the last major mine closed in 1939. Lead is a by-product of fluorite, baryte and calcite mining. Bell pits were sunk to access ore that lay close to the surface.

Fluorite or fluorspar is called Blue John locally, its name possibly from the French bleu et jaune describing its colour. Blue John is scarce and now only a few hundred kilograms are mined each year for ornamental and lapidary use. The Blue John Cavern in Castleton is a show cave. Small-scale mining takes place in Treak Cliff Cavern.

Industrial limestone quarrying to make soda ash started around Buxton in 1874. In 1926 the operation of the Buxton lime industry became part of ICI. Large-scale limestone and gritstone quarrying flourished as lead mining declined, and is an important if contentious industry. Of the twelve large limestone quarries in operation, Tunstead is one of the largest in Europe. Total limestone output was substantial: at the 1990 peak, 8.5 million tonnes was produced.

Textiles
Textiles have been exported for hundreds of years. In the 14th century, the area traded in unprocessed wool. There were several skilled hand spinners and weavers in the area. By the 1780s, Richard Arkwright had developed machinery to produce textiles faster and to a higher standard. The early Arkwright mills were of light construction, narrow, about 9 ft wide and low, the ceiling height being only 6 to 8 ft and lit by daylight. The new machines were powered by water wheels. The Peak was the ideal location, with its rivers and humid atmosphere. The local pool of labour was quickly exhausted and Litton Mill and Cressbrook Mill in Millers Dale brought in children as young as four from the workhouses of London as apprentices.

As technology advanced, narrow valleys proved unsuited to larger steam-driven mills, but Derbyshire mills remained to trade in finishing and niche products. Glossop benefited from the textile industry. Its economy was tied to a spinning and weaving tradition that evolved from developments in textile manufacture during the Industrial Revolution. Until the First World War, Glossop was the headquarters of the largest textile printworks in the world, but after the Wall Street crash its product lines became vulnerable and the industry declined.

Modern history
The Kinder Trespass in 1932 was a landmark in the campaign for open access to moorland in Britain and eventually led to the formation of Britain's national parks. Before the trespass, open moorland was closed to all. Moorland estates were the private property of landed gentry who used them for only 12 days a year and were guarded by their gamekeepers. The Peak District National Park became the United Kingdom's first national park on 17 April 1951. Campaigner Ethel Haythornthwaite played an important part in the development of the national park. The first long-distance footpath in the United Kingdom was the Pennine Way, which opened in 1965 and starts at the Nags Head Inn, in Grindsbook Booth, part of Edale village.

The Peak & Northern Footpaths Society (PNFS) was formed in 1894 to monitor, protect, and improve the footpath network of the Peak District and surrounding areas. The organisation is the oldest existing regional footpath society in the UK.

Saddleworth Moor and Wessenden, above Meltham, gained notoriety after the Moors murders in the 1960s.

Economy
Agriculture remains a significant sector for the park. A Park District report stated that in 2019, over 87% of the Peak District was being farmed. Another report, updated in 2023, added this information: "Farming is also one of the largest contributors to the park’s economy employing over 3500 people, which makes up 18.5% of total employment in the national park. That is understandable, since as of 2019, over 87% of the Peak District was being farmed. A State of the Park report indicated that in 2019, "at least 1 in 3 businesses in the Peak District [were] in the agricultural, forestry and fishing industries".

Tourism in the park and Derbyshire was negatively affected by the pandemic but according to a September 2022 report, this sector is a major industry in the "Peak District and Derbyshire, attracting 45 million visitors annually, generating an output of £2.5 billion into the economy and supporting 31,000 jobs. (Data are not available for the park area only.)

Other sources of employment for park residents according to a 2009 report: Manufacturing (19%) and quarrying (12%) are also important. The cement works at Hope is the largest single employer in the park. Limestone is the most important mineral quarried, mainly for roads and cement; shale is extracted for cement at Hope, and several gritstone quarries are worked for building stone. Lead mining is no longer economic, but fluorite, baryte and calcite are extracted from lead veins and small-scale Blue John mining occurs at Castleton.

The springs at Buxton and Ashbourne are exploited for bottled mineral water and many plantations are managed for timber. Other manufacturing includes David Mellor's cutlery factory in Hathersage, Ferodo brake linings in Chapel-en-le-Frith and electronic equipment in Castleton.

Tourism
De Mirabilibus Pecci or The Seven Wonders of the Peak by Thomas Hobbes was an early touring description published in 1636. Much scorn was poured on the seven wonders by visitors, including Daniel Defoe, who called the moors by Chatsworth "a waste and houling wilderness" and scorned particularly Peak Cavern near Castleton, known as the "Devil's Arse". Visitor numbers did not rise until the Victorian era, when railways provided access and cultural appreciation of the Picturesque and Romantic developed. John Mawe's Mineralogy of Derbyshire (1802) and William Adam's Gem of the Peak (1843) raised interest in the area's unique geology.

A tradition of public access and outdoor recreation grew up in what is a natural hinterland and rural escape for the people of industrial Manchester and Sheffield, and remains a valuable resource in a largely post-industrial economy. In a 2005 survey of visitors, 85 per cent of respondents cited "scenery and landscape" as a draw.

Buxton
Buxton became a spa through its geothermal spring, which rises at a constant temperature of 28 °C. It was settled by the Romans around 78 CE, then known as Aquae Arnemetiae – the spa of the goddess of the grove. Bess of Hardwick and her husband the Earl of Shrewsbury "took the waters" in 1569, bringing Mary, Queen of Scots there in 1573. The town largely grew in importance in the late 18th century when it was developed by the 5th Duke of Devonshire in style of the spa of Bath.

A resurgence in the 18th century attracted Dr Erasmus Darwin and Josiah Wedgwood, who were drawn by the reputed healing properties of the waters. The railway reached Buxton in 1863. Buxton's notable buildings are The Crescent (1780–1784), modelled by John Carr on Bath's Royal Crescent, the Devonshire (1780–1789), the Natural Baths, and the Pump Room by Henry Currey. The Pavilion Gardens opened in 1871. Buxton Opera House was designed by Frank Matcham in 1903.

Historic buildings
Historic buildings in the park include Chatsworth House, seat of the Dukes of Devonshire and among Britain's finest stately homes; the medieval Haddon Hall, seat of the Dukes of Rutland; and Lyme Park, an Elizabethan manor house transformed by an Italianate front. Other historic buildings in the park include Eyam Hall, Ilam Hall and Tissington Hall. Many villages and towns have fine parish churches, including the 14th-century Church of St John the Baptist at Tideswell, sometimes dubbed the "Cathedral of the Peak", and the 12th-century Church of St Nicholas at High Bradfield. 'Little John's Grave' is in the churchyard at Hathersage. Peveril Castle, overlooking Castleton, was built by the Normans.

Museums and attractions
Inside the park, Eyam Museum has displays on the village's history during the Black Death. Castleton has four show caves; Peak Cavern, Blue John, Treak Cliff and Speedwell. In the outer fringes, the area's industrial heritage is represented by the mining museum at Matlock Bath, with the Temple Lead Mine, the Derwent Valley Mills World Heritage Site and Brindley Water Mill at Leek. Preserved railways such as the Peak Rail, Ecclesbourne Valley and Churnet Valley lines, the National Tramway Museum at Crich and the Cromford Canal chart the area's transport history. Matlock Bath also has the show caves and mines of the Heights of Abraham, which can be reached by cable car, and the Gulliver's Kingdom theme park. Buxton has an opera house and theatre, museum and art gallery and Poole's Cavern show cave. Other attractions in the fringes include the Alton Towers theme park and the Peak Wildlife Park. Well dressing ceremonies are held in many villages in the spring and summer months, a tradition said to date from pagan times. Other local customs include Castleton Garland Day and Ashbourne's Royal Shrovetide Football, played annually since the 12th century. Buxton hosts two opera festivals, the Buxton Festival and the International Gilbert and Sullivan Festival, and the Buxton Festival Fringe, and the Peak Literary Festival is held at various locations twice a year. Peak District food specialities include the dessert Bakewell pudding, very different from the nationally available Bakewell tart, and the famous cheese Stilton and other local cheeses are produced in the village of Hartington.

Activities
An extensive network of public footpaths and long-distance trails of over 1800 mi in total and large open-access areas are available for hillwalking and hiking. The Pennine Way traverses the Dark Peak from Edale to the park's northern boundary just south of Standedge. Bridleways are used by mountain bikers, as well as horse riders. The Tissington Trail and High Peak Trail, which reuse former railway lines, are well used by walkers, horse riders and cyclists. The Peak District Boundary Walk is a circular 190 mi walking trail around the national park.

Several old rail routes were converted into multi-purpose cycle trails. After the Woodhead Line closed between Hadfield and Penistone, some of the trackbed was used for the Longdendale Trail section of the Trans Pennine Trail between Hadfield and Woodhead. The Manchester, Buxton, Matlock and Midlands Junction Railway between Rowsley and Buxton contributed to the Monsal Trail. The trackbed of the Cromford and High Peak Railway is open as the High Peak Trail. The Tissington Trail uses another disused rail line between Buxton and Ashbourne, while the Manifold Way follows the old line of the Leek and Manifold Valley Light Railway between Waterhouses and Hulme End.

Local authorities run cycle hire centres at Ashbourne, Parsley Hay, Middleton Top, the Upper Derwent Valley and Hulme End. Wheelchair access is possible at several places on the ex-railway trails, and cycle hire centres offer vehicles adapted to wheelchair users. A project to make footpaths more accessible to less-agile walkers has replaced stiles with gates.

Gritstone outcrops at Stanage Edge and The Roaches, are recognised as some of the finest rock climbing sites in the world. Limestone is more unstable but provides many testing climbs. Thor's Cave was explored in the early 1950s by Joe Brown and others. Eleven limestone routes there are listed by the BMC, ranging in grade from Very Severe to E7, and several more have been claimed since the guidebook's publication; a few routes are bolted.

Caving takes place in the natural caves, potholes and old mine workings found in the limestone of the White Peak. Peak Cavern, the largest and most important cave system, is even linked to the Speedwell system at Winnats. The largest potholes are Eldon Hole and Nettle Pot. Many old mine workings were often extensions of natural cave systems. They can be found at Castleton, Winnats, Matlock, Stoney Middleton, Eyam, Monyash and Buxton.

Reservoirs such as Torside Reservoir, Damflask Reservoir, Carsington Water and Rudyard Lake are centres for water sports, including sailing, fishing and canoeing. Other activities include air sports such as hang gliding and paragliding, birdwatching, fell running, off-roading, and orienteering.

Roads
The first roads constructed by the Romans may have followed existing tracks. The Roman network linked the settlements and forts of Aquae Arnemetiae (Buxton), Chesterfield, Ardotalia (Glossop), Navio (Brough and Shatton) and beyond. Parts of the modern A515 and A53 roads, south of Buxton, are believed to follow the routes of Roman roads.

Packhorse routes crossed the Peak in the Middle Ages and some paved causeways, such as the Long Causeway along Stanage Edge, date from that period. No highways appear on Christopher Saxton's 1579 map of Derbyshire. Bridge-building improved the transport network.

Journey times fell with the introduction of turnpike roads from 1731, but the ride from Sheffield to Manchester in 1800 still took 16 hours, prompting Samuel Taylor Coleridge to remark that "a tortoise could outgallop us!" From about 1815, better quality turnpike roads were built. The Snake Pass, part of the A57, was built under the direction of Thomas Telford between 1819 and 1821.

The main roads in the Peak District are:
 * The A57 between Sheffield and Manchester;
 * The A628, Woodhead Pass, between Barnsley and Manchester, via Longdendale;
 * The A6 from Derby to Manchester via Buxton;
 * The Cat and Fiddle Road from Macclesfield to Buxton; and
 * In the north, the A635 from Manchester to Barnsley.

Roads and lanes are often congested and parking is problematic in towns and villages, especially in summer. A congestion charge was proposed in 2005, but was rejected.

Waterways
Cromford Canal opened in 1794 to carry coal, lead and iron ore to the Erewash Canal. It closed in 1944. The canals and turnpike roads had to compete with the railways after 1825.

Railways

The first railway, the Cromford and High Peak Railway from High Peak Junction to Whaley Bridge, was an industrial line. Passenger services followed, including the Woodhead Line (Sheffield to Manchester, via Longdendale) and the Manchester, Buxton, Matlock and Midlands Junction Railway. Several railways succumbed to the Beeching Axe in the 1960s, including passenger services on the Woodhead line. Freight services continued until the line was finally closed in 1981; much of the route has been converted to shared-use paths on the Trans Pennine Trail.

Passenger train services currently operate along the following lines:
 * The Hope Valley line between Sheffield, New Mills Central and Manchester Piccadilly, stopping at stations including Hathersage, Hope and Edale;
 * The Derwent Valley line between Derby and Matlock;
 * The Buxton line between Manchester Piccadilly, Stockport and Buxton;
 * The Glossop line, linking Glossop and Hadfield with Manchester Piccadilly, along the remaining stub of the Woodhead line;
 * The Huddersfield line from Manchester to Huddersfield, via Marsden.

Buses and coaches
Coach services provide access to Matlock, Bakewell and Buxton from Derby, Nottingham and Manchester through TransPeak and National Express.

There are regular buses from Sheffield, Glossop, Stoke, Leek and Chesterfield.

In rural areas, minibuses operate from towns to smaller villages.

Air
The nearest airports are Manchester and East Midlands.

Cycling
Cycle England invested £1.25 million in building and improving cycle routes in the national park for leisure and commuting.

Conservation issues
The proximity of the Peak to conurbations and urban areas (some 20 million people live within an hour's drive) poses challenges for the area. The park authority, National Trust and other landowners try to keep the upland landscape accessible for recreation while protecting it from intensive farming, erosion and visitor pressures. Tension exists between the needs of conservation, of 38,000 residents, and of millions who visit.

The uneven distribution of visits creates stresses. Dovedale alone receives about two million visitors a year. Other much visited areas include Bakewell, Castleton and the Hope Valley, Chatsworth, Hartington and the reservoirs of the Upper Derwent Valley. Over 60 per cent of visits occur between May and September, with Sunday the busiest day.

Footpath users in the more popular walking areas have contributed to serious erosion problems, particularly on the fragile peat moorlands. The use of some paths by mountain bikers is believed to have exacerbated the problem. Measures to contain the damage include diversion of the official route of the Pennine Way out of Edale, which now goes via Jacob's Ladder rather than following the Grindsbrook, and surfacing moorland footpaths with expensive natural stone. Some rights of way have been damaged by legal and illegal use by off-road vehicles such as 4×4s and trail bikes. Campaigners have sought to reduce their impact.

Large-scale limestone quarrying is contentious. Most mineral extraction licences were issued by national government for 90 years in the 1950s and remain legally binding. The park authority has a policy of considering applications for new quarries and licence renewal in the park in terms of the local and national need for the mineral and how unique the source is, in conjunction with the effects on traffic, residents and the environment. Some licences have not been renewed; the RMC Aggregates quarry at Eldon Hill closed in 1999 and was landscaped. Proposals from Stancliffe Stone Ltd to reopen dormant gritstone quarries at Stanton Moor in 1999 became a test case, contested by ecological protesters and residents on the grounds that this would threaten Bronze Age remains at the Nine Ladies Stone Circle and damage the natural landscape. In 2007, negotiations took place to relocate the development to Dale View quarry in a less sensitive area.

From the 1990s onwards there has been an intensification in management of the upland moors for driven grouse shooting. This has involved an increase in the use of rotational burning and predator control. Both practices can be controversial and have led to calls for greater controls over the activities of moorland owners. The Birds of Prey Initiative has worked to link conservation groups with landowners, to improve the prospects for predatory birds in the Peak District. This has led to improvement in the numbers of breeding birds of prey, but overall numbers remain low. The RSPB withdrew support for the scheme in 2018, citing the continued and illegal persecution of raptors by commercial grouse shooting estates, represented within the Initiative by the Moorland Association and National Gamekeepers' Organisation.

The grasslands of the White Peak plateau have been improved for intensive farm and food production. The result has been that most of this grassland is of little value to nature conservation, often with only one grass species present. The best areas that remain are the steep sides of limestone valleys. These have international importance, but are fragmented, which makes them vulnerable to loss. Biodiversity within Britain's national parks has generally fared no better than that in the wider countryside, with similar rates of decline in species numbers. One reason may be that their powers are directed primarily at preventing intrusive development to protect the aesthetic and historic appearance of the park, rather than at land management.

The upland moors of the south Pennines suffered some of the worst ecological degradation of any extensive habitat in the UK. This is due mainly to a history of industrial pollution from neighbouring towns during the industrial revolution, worsened by wild fires and erosion. Work to restore this habitat got underway in the 21st century. While progress has been made, there is more to do to make it a sustainable, functioning ecosystem. The significance of the habitat degradation is compounded by its being a source of atmospheric carbon dioxide that contributes to climate change through global warming.

In literature and arts
The landscapes of the Peak have inspired writers for centuries. Various places have been identified by Ralph Elliott and others as locations in the 14th-century poem Sir Gawain and the Green Knight; Lud's Church is thought to be the Green Chapel.

Key scenes in Jane Austen's 1813 novel Pride and Prejudice are set in the Peak. Peveril of the Peak (1823) by Sir Walter Scott is a historical novel set at Peveril Castle, Castleton, in the reign of Charles II. William Wordsworth was a frequent visitor to Matlock; the Peak inspired several of his poems, including an 1830 sonnet to Chatsworth House. The village of Morton in Charlotte Brontë's 1847 novel Jane Eyre is based on Hathersage, where Brontë stayed in 1845; Thornfield Hall may have been inspired by nearby North Lees Hall. Snowfield in George Eliot's novel Adam Bede (1859) is thought to be based on Wirksworth, where her uncle managed a mill; Ellastone (as Hayslope) and Ashbourne (as Oakbourne) also feature.

Beatrix Potter, author of Peter Rabbit, visited her uncle Edmund Potter at his printworks in Dinting Vale. She copied cloth samples from his pattern book for her characters. Mrs Tiggywinkle's shawl, in The Tale of Mrs. Tiggy-Winkle, is based on pattern number 222714.

Children's author Alison Uttley (1884–1976) was born at Cromford; her novel A Traveller in Time, set in Dethick, recounts the Babington Plot to free Mary, Queen of Scots, from imprisonment. Crichton Porteous (1901–1991) set several books in Peak locations; Toad Hole, Lucky Columbell and Broken River take place in the Derwent Valley. Geraldine Brooks's first novel, Year of Wonders (2001), blends fact and fiction in the story of the plague village of Eyam. Eyam also inspired Children of Winter by children's novelist Berlie Doherty, who has set several other works in the Peak, including Deep Secret, based on the drowning of the villages of Derwent and Ashopton by the Ladybower Reservoir, and Blue John, inspired by the cavern at Castleton.

Many works of crime and horror have been set in the Peak. The Terror of Blue John Gap by Sir Arthur Conan Doyle (1859–1930) recounts terrible events at the Blue John mines. Sherlock Holmes investigates the kidnapping of a child in The Adventure of the Priory School. Many horror stories by local author Robert Murray Gilchrist feature Peak settings. Stephen Booth has set a crime-fiction series in real and imagined Peak locations, while In Pursuit of the Proper Sinner, an Inspector Lynley mystery by Elizabeth George, is set on the fictional Calder Moor. Another local author who sets crime novels there is Sarah Ward.

Other writers and poets who lived in or visited the Peak include Samuel Johnson, William Congreve, Anna Seward, Jean-Jacques Rousseau, Lord Byron, Thomas Moore, Richard Furness, D. H. Lawrence, Vera Brittain, Richmal Crompton and Nat Gould. The landscapes and historic houses are popular settings for film and television. The classic 1955 film The Dam Busters was filmed at the Upper Derwent Valley reservoirs, where practice flights for the bombing raids on the Ruhr dams had been made during the Second World War.

In adaptations of Pride and Prejudice, Longnor has featured as Lambton, and Lyme Park and Chatsworth House have stood in for Pemberley. Haddon Hall doubled as Thornfield Hall in two adaptations of Jane Eyre and has appeared in several films, including Elizabeth, The Princess Bride and The Other Boleyn Girl. The television medical drama Peak Practice set in the fictional village of Cardale was filmed in Crich, Matlock and other Peak locations. The world's longest-running sitcom, Last of the Summer Wine, was filmed in Holmfirth and the surrounding Holme Valley. The psychological thriller Dead Man's Shoes was filmed in 2003 in and around Matlock, Bonsall, Darley Dale, Tansley and Riber, and featured Riber Castle.

title: Peak District