Most of the precipitation is around the Gulf Coastal region near Austin and Galveston Island because that is the farthest point of southeast in Texas. Most of the Great Plains will not get nearly as much rain as the Gulf Coastal region because the elevation is a bit higher. The Mountains and Basins region will get little if not no rain at all because of the elevation of that region. The population in North Central is higher than most regions because of the few major cities we have and the growing cities. The regions Gulf Coastal and Great Plains are related because the weather is alike and the population of both regions are close together. The Great Plains and the Mountains and Basins are close related because the Great Plains has big hills
With defining the Texas climate I began with the northernmost area of land being the panhandle. Where within this region, the panhandle exhibits a Continental Steepe climate where there are “large variations in the magnitude of ranges in [both] daily temperature extremes and irregularly spaced rainfall”. Due to physical influences of North Texas such as its proximity to mountain barriers which subsequently blocks “moist air from oceans from reaching the steppe” the area results in a region that experiences low humidity in its air quality in the high plain area of the state. The
Although bout the New England and Chesapeake region were both settles by Americans, the regions were split due to some differences, but, they also shared similarities. During the 1700's the colonial era, colonies, began as one distinct region, yet, as time progressed, due to differences, such as a more fertile land in the New England colony, , the region broke into two different societies.
The Piedmont is the middle region it is between the Coastal Plain and the Mountain Region.
Two English groups came for better lives, yet they had different reasons to settle; therefore developing two completely different societies. This is what developed the different characteristics between the New England and the Chesapeake region.
The New England Chesapeake regions were settled largely by people of English origin, but by 1700, they became two very different societies. They developed differently, mostly because of the way that the English colonists obeyed their religion, and the manner in which they conducted politics. Although the colonists both originated from England, both groups had their reasons for venturing to the New World.
The 17th century saw the foundation and expansion of nearly all of Britain’s colonies on the Atlantic seaboard. This time saw the development of two distinct regions in this New World: the northern New England and the southern Chesapeake Bay region. Both regions attempted to recreate some aspects of English economy, society, and religion in their settlements, but they only did so to the extent which they felt fit for their new way of life. As such, the Chesapeake and New England regions, in the 17th century, developed similarities through their English heritage, but distinct differences as they pursued different goals and adapted to the specific demands of their unique environment. Both regions’ economic system were centered around providing
Despite the population of settlers in New England and the Chesapeake region being mostly English emigrants, the regions evolved very differently. The difference in development between New England and the Chesapeake region occurred as a result of the differences in economies, religious views, and senses of unity.
Some landmarks are mammoth cave and Florida everglades. There are landforms in the southeast are plains, mountains, and caves. Some climates are hurricanes, tornados, rain storms, sunny days, warm days. Some natural resources are tomatoes, oranges, rice, sugarcanes, grape- fruit, tobacco, peanuts, coal, peaches, and cotton.
Looking at these figures actually shows a grim picture there is 53,187 people in the county estimated to have
This is because wealthy Germans received land grants in some of the most fertile regions of Texas, but they did not know how to farm this soil, and the majority of them did not support the ideas of slavery. These wealthy families would send letters back to Germany and Bohemia telling about how great Texas is, comparing the climate to that of Sicily in Southern Italy, telling that the soil was lush and fertile, and that the game and available food was abundant. This was done in hopes that Germans and Bohemians that were sick of the overpopulation of their home country would take the opportunity to farm these fertile foreign
The Eastern Cottontail (Sylvilagus floridanus) is a mammal that lives throughout the eastern parts of Texas, according to The Mammals of Texas. The Desert Cottontail (Sylvilagus audubonii) is also a rabbit native to Texas. The Desert Cottontail lives in the uplands of Texas on the western half of the state, says The Mammals of Texas. Of the two, the Eastern Cottontail is the most common. A close relative of these cottontails is the New England Cottontail. The Desert Cottontail and the Eastern Cottontail have both evolved from the New England Cottontail to survive in their environments. Although the Desert Cottontail and the Eastern Cottontail are very similar, they also have differences.
The climate of the interior plains is continental, which basically means that the climate is relatively dry with extremely hot summers and cold winters. The weather is very diverse and may change quickly without warning. In the North of the physiographic region, the winters are long and the summers are short and cool whereas in the South, the the winters are harsh with little precipitation and long summers. Although the humid weather and the flat lands create an ideal place to grow crops like wheat and corn, the growing season itself is quite short, even in the southern region due to the lack of precipitation needed for diversified crops to flourish. The flat prairies east to the Rockies is a meeting ground for Arctic, Pacific and
The Piedmont is a plateau region located in the eastern periphery of the Appalachian region and the eastern United States, which extends from New Jersey in the north to central Alabama in the South. According to the article “Piedmont (United States)” on Wikipedia, The Free Encyclopedia, this region includes 80,000 thousand square miles of relatively small rolling hills that vary in elevation between 200 and 1,000 feet above sea level. This area varies in width like it is 300 miles wide in North Carolina but extremely narrow in New Jersey (“Piedmont (United States),” n.d.). Also, the elevation around the northeastern states such as New Jersey, southeastern Pennsylvania, central Maryland, and northern Virginia are between 100-400 feet above sea
The city's of Chicago, Cleveland and Omaha were on the same longitude. Chicago and Cleveland had around the same amount of rainfall expect for Omaha and it was higher in average fall than the two. In temperature Omaha was the coldest out of Chicago and Cleveland. The reason why Omaha, Neb has the most rainfall and temperature was because it is father away from the equator than the others, which is why Latitude effects the temperature, rainfall and many more things with that location.
Analyzing the precipitation graph we see that there are very minimal similarities on the temperature graph. There is an obvious difference in the volume of precipitation, the trend seen in this graph is specific to the Hot Springs, AR location, over a 15 year period there is a large amount of precipitation in the area. Big Sky, MT has a trend of very little precipitation except in 2005 where there was an unforeseen amount of precipitation. Big Sky shows a very consistent and even graph, while Hot Springs is much more unstable. This graph provides a strong case for Big Sky, MT as there is very little precipitation compared to Hot Springs, AR.