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James Lankford, (born 4 March 1968, Dallas, Texas, U.S.A.), American politician elected to U.S. Senate as a Republican in 2014, and began the next year’s representation of Oklahoma. He served in the U.S. House of Representatives (2011-2015).
In Texas, Lankford grew up. He studied high school at the University of Texas (B.A., 1990) and then went to the theological seminary of Southwestern Baptists. During that time, Lankford married (1992) and subsequently had two children with him and his wife Cindy. After his master’s degree in deities (1994), he moved his family to Oklahoma, where he worked for the Baptist General Convention, becoming director of both Student Ministries and Falls Creek Youth Camp. From 1995 until 2009, he served in these positions.
In 2010, Lankford entered electoral politics with a U.S. House of Representatives seat. He won first and subsequently defeated his Democratic opponent. He became recognised after gaining office in 2011 for his resistance to laws on arms control, taxes, environmental regulations and the government health insurance. In 2012, he was re-elected. Two years later, Lankford was elected to replace retired Tom Coburn for a special Senate election. He handily defeated a Tea Party contestant in first place and won the general election. Lankford continues to advance as a senator on conservative grounds.
The tenure of around 1/3 of the membership of the Senate expire every two years and the Chamber is named “the house that never dies.”
Each state is therefore equally represented, irrespective of size or population. In addition, the elections to the Senate were indirect until the Seventeenth Amendment of the Constitution (1913) by the state legislatures. Most of the west North Central Plains have red or tan-colored and sandy soils, but in the region there is also black clay. The highlands, to the west, have reddish clay loams, sandy loams and sands in dark brown. Reddish brown sandy soils in the mountains and grey brown to reddish brown clay soils in the lowlands are found in the Trans-Pecos region.
In accordance with the “advice and consent” provisions of Article II, section 2 of the Constitution the Senate has important powers: ratification of Treaties requires a two-thirds majority of all present Senators and a simple majority of important public appointments, such as members of the cabinet, ambassadors and Supreme Court judges, to be approved by simple majority. The Senate shall also adjudicate the procedures begun by the House of Representatives for the purpose of conviction by a two-thirds majority.
Each party elects a leader to co-ordinate Senate activity, usually a Senator of substantial significance in its own right. The leader of the largest party is known as the leader of the majority and the leader of the opposition as the leader of the minority. The leaders of the Senate also have a major role in the nomination of their party members to the Senate committees which evaluate and process legislation and have general oversight of government agencies and departments. The Vice President of the United States acts as Senate President, but can only vote if a tie exists. In the absence of the Vice President, the pro tempore president – normally the longest serving member of the governing party – is the Senate chairman.
Seventeen standing committees are typically organised around significant policy topics with staff, budgets and several subcommittees. The standing committees on appropriations, finance, government operations, external relations and the judiciary are essential. Thousands of proposals are referred to committees throughout each congressional session, however only a minority of the proposals are taken up by the commissions. The final text for a law is discussed in “mark-up” sessions, which can be open or closed. The committees hold hearings and call on witnesses to give evidence of the law before them. Select and special committees will also be established to conduct studies, investigate and report to the Senate on ageing, ethics, Indian affairs and intelligence.
The smaller membership of the Senate allows for wider discussion than the House of Representatives usually does. Three-fifths of the members (60 senators) must vote for cloture to check a filibuster—endless debate which obstructs legislative movement. (In 2013, the cloture rule of the Senate was re-interpreted to allow majority voting for the discussion on all presidential nominations except those of the Supreme Court and in 2017 the rule was also reinterpreted for nominations by the Supreme Court.) If the legislation under discussion would change the standing rules of the Senate, cloture can only be triggered when two-thirds of those present vote. The structure of party control in the Senate is less complex; the position chosen by the senators may be more important than (if any) the position expressed by the party.
The constitutional rules on Senate membership standards set a minimum age of 30 years, United States nationality for nine years, and domicile in the State of electing.In the grasslands and plains of west Texas, bluestem, grama, Indian grass, switch grass and buffalo grass grow. The natural trees of the Prairies and Cross Timbers are Oak, Pecan, Elm, Osage orange and Mesquite. The Edwards Plateau’s vegetation is made mainly of cedar, mesquite, yucca, cactus and few cypress islands.
Texas, United States of America member state. In 1845 it became the 28th state of the union. Texas occupies the south-central region of the country and is the largest state in area except for Alaska. The State stretches from north to south around 1.000 miles (1.600 km) and from east to west about the same amount.
Water has numerous boundaries. The rough path of the Red River covers the eastern two-thirds of Texas with Oklahoma in the north, while the rest of the northern border covers the north, forming a parallel in the west of this state. The Sabine River forms most of the east border of Louisiana and is also bordered by Arkansas by land. The Gulf of Mexico has a crown-shaped shoreline to the southeast, while the river Grande has a narrow channel that separates Texas from Mexico to the southwest. New Mexico is located in the west. Austin is the capital in the south-central region of the State.
Texas’ size and diversity are visible in almost every element of its physical characteristics, economics, history and cultural life. For over a century, Texas was part of the Spanish Empire. From 1821 until 1836, it was part of the fledgling country of Mexico, then became independent, having a short-lived existence before joining the Union. Texas’ reputation was raw and lawless when it gave up its autonomy and became a state. While Texas is still strongly identified with their cowboy legacy, the state image of Texas dramatically changed during the twentieth century. Texas is known today for its great agricultural wealth, the major production of oil and natural gas, industry, finance and enormous urban centres, promoting cosmopolitan cultural life, and seemingly endless high prairies and devotional areas.
The state name comes from the term Caddo thecas, which means “allies” or “friends.” (The Spanish name tejas or texas was spelt and used to denote the territory in which this indigenous group inhabited.) Texas is usually divided into East and West however the dividing line is uncertain. But, generally speaking, East Texas has a moist environment with cotton and ties to the Old South, whereas West Texas is dry and famous for its cattle ranching and its affinity with the West. Area 268,597 miles square (695,662 square km). 25.145.561 people; (2019 est.) 28.995.881.
The coast of Texas consists of a succession of broad regions, from the lush and densely populated coastal plains in the southeast to the western and northwestern highlands and mountains. It stretches inland from the Gulf Coast, from around two-fifths of the state land, up to a height of approximately 1.000 feet (300 metres). These flat low meadows spread inside to form a fertile crescent which is well adapted to agriculture and livestock rearing. Near the shore there is a lot of marshy, nearly swampy area except that it is drained by man-made systems.
The coastal plains culminate in the Escarpment balconies, where tremors have taken place. The area stretches north-west of this fault into the Texas Hill country and into the Edwards Plateau tablelands to the south, and the North Central Plains to the north. The entire region fluctuates between between 750 and 2,500 feet (200 to 750 metres) above sea level, and the basic economy is agriculture and animals. There are modest industry and leisure places in Hill Country.
The Amarillo Subdivision of the North Plains depends on grain, ranching, petroleum and minor industry. The subdivision of South Plains, with Lubbock as its main city, contains wide subterranean reservoirs for irrigated cotton farming on a massive scale.
The Caprock Escarpment stands on the west side of the north central plains, a rock protrusion stretching roughly 200 miles north and south (320 km). Furthermore, the third largest region in Texas, the High Plains country, and the Trans-Pecos region, to the south.
Many legends of Texas weather and Texas cowboy came out of the High Plains territory of West Texas. Sandstorms are typical on these areas. Many large flat riparian beds stay dry most of the year in the region, but for flash floods they can become sluiceways. The flat, dry landscape called Llano Estacado (“Staked plain”) lies in this region. According to the tale, the Spanish expedition from New Spain (Mexico), lead by Francisco Vázquez de Coronado in the mid-16th century, established stakes as guides for the return trip. Even Americans hesitated to go through these countries.
The most robust country is to the west of the Pecos River. From the rocky mountains, the mountains of Guadalupe lead to the nation of Big Bend, whose name is from a bend in the Rio Grande region. The highest summit in Texas is the Guadalupe Peak, which stands at an altitude of 8,749 feet. In the Big Bend National Park, most of the native roughness of the terrain is conserved.
The Rio Grande is the most important river in Texas. It spans from its source in the Rocky Mountains of Colorado to the Gulf of Mexico approximately 1,900 miles (3,060 km), and its segment in Texas defines the border between the United States and Mexico. The Brazos (1,280 km [2,060 km], the longest river in Texas), as well as the Sabine River, the Trine River and the Red River, last of which covers a substantial part of the Texas-Oklahoma border.
In 1913 there were just 8 major lakes or reservoirs in Texas; around 200 by the beginning of the 21st century, many of which were developed to retain water from regular droughts. Others in Hill Country, notably the 85-mile (137-km) Highland Lakes series, are popular for leisure.
The abundant fertility of the land lured initial settlers to Texas. Much of the land was deteriorated by waste in the 19th and early 20th centuries, but since the 1930s, federal and state governments have made great progress in promoting soil conservation in the state.
The varieties of Texas soil vary enormously. In the Piney Woods region of East Texas, a grey and tan topsoil is usually 2 metres (0.6 metres) apart from the red subsoil. The soil is in black clay or loam over the upper and middle coasts of Texas, with lighter coloured sandy soil on coastal islands, bars or spits. The soil in the southern part of Texas is sandy like in the eastern part of Texas, although it is less eroded and leached.
The Blackland Prairie, a stretch of fertile black clay to the west of the Piney Woods, extends southwesterly from the Red River to San Antonio. The ground in the Greater Prairie region to the west of the Blackland Prairie is rockier and more erosion resistant.
A light-colored, somewhat acidic sandy loam soil forest zone, the Cross Timbers extends over the meadows of Northern Texas, enclosing a part of the Great Prairie. In the central state of Llano Basin, red sandy and black clay soils are found. The Edwards plateau features a thin, rocky, calcareous soil.
Most of the west North Central Plains have red or tan-colored and sandy soils, but in the region there is also black clay. The highlands, to the west, have reddish clay loams, sandy loams and sands in dark brown. Reddish brown sandy soils in the mountains and grey brown to reddish brown clay soils in the lowlands are found in the Trans-Pecos region.
Virtually all weather conditions in Texas are known to occur. January temperatures in the Rio Grande valley were known to be registered throughout the 1990s F (about 32 °C) and during the same month snowstorm roads shut in the state of Panhandle. The Gulf coast area near Houston has average annual precipitation temperatures of approximately 45 inches (1100 mm) at a low 70s F (approximately 21°C) while that of Panhandle averages less than 20 inches (500 mm) of rain in a low 60s F area (approximately 16°C). The driest area is Trans-Pecos, and the southeast is the west. Southern places rarely have frigid weather. Snow is unusual in Brownsville, the southernmost city of Texas yet the northwest portion of the state has an annual average of roughly 23 inches (580 mm).
The Texas Gulf Coast is particularly prone to storms. The deadliest hurricane struck the area was in 1900 when over 8,000 people were killed and Galveston Island flooded. Hurricane Audrey (June 1957), Hurricane Carla (September 1961), Tropical Storm Allison (June 2001), Hurricane Ike (September 2008), and Hurricane Harvey also were destructive striking hurricanes in Texas (August 2017).
A wide range of vegetation is discovered in Texas due to variances in precipitation and soil types. The majority of commercial timber in East Texas is native longleaf, shortleaf and loblolly pine. A belt of postoak, blackjack oak, elm, pecan and walnut grows west of Piney Woods. The Texas coast is covered with marsh and salt grass, with bluestem and tall grasses extending inland a little further.
In the grasslands and plains of west Texas, bluestem, grama, Indian grass, switch grass and buffalo grass grow. The natural trees of the Prairies and Cross Timbers are Oak, Pecan, Elm, Osage orange and Mesquite. The Edwards Plateau’s vegetation is made mainly of cedar, mesquite, yucca, cactus and few cypress islands.
Desert plants comprise much of the Trans-Pecos region’s vegetation. In the upper mountains of the area, pine pines, ponderous pines, spruce, cedars, and oak thrive. Originally, the terrain south of San Antonio was a brushland, with mesquita, little live and after oak, prickly pear cactus, bluestem and bunch grass. Much of this original vegetation was replaced by agriculture.
(1)Full Name: James Lankford
(2)Nickname: James Lankford
(3)Born: 4 March 1968
(4)Father: Linda Joyce Lankford
(5)Mother: James Wesley Lankford
(6)Sister: Not Available
(7)Brother: Not Available
(8)Marital Status: Married
(10)Birth Sign: Pisces
(12)Religion: Not Available
(13)Height: Not Available
(14)School: Not Available
(15)Highest Qualifications: Not Available
(16)Hobbies: Not Available
(17)Address: Dallas, Texas, U.S
(18)Contact Number: 202-224-5754
(19)Email ID: Not Available