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This website is organized into two parts: 1) Ogallala Maps & Data and 2) Texas Maps. The Ogallala Maps & Data section contains aquifer information for forty-one Texas counties for a nineteen year study period from 1990 to 2008.The Ogallala Aquifer extends from the northern United States into the Texas Panhandle and West Texas and is the primary source of water within the District. The aquifer consists of sands, gravel, silts, and clay sediments that were deposited as part of ancient river systems approximately three to six million years ago during the Neogene ... That’s what’s happening right now in western Kansas where some farmers aren’t able to get enough water for their crops from wells fed by the Ogallala Aquifer, which underlies portions of eight states, stretching for nearly 175,000 square miles from South Dakota to Texas. It’s part of the High Plains Aquifer system that sits below one of ...But according to the Fourth National Climate Assessment (NCA4), producers are extracting water faster than it is being replenished, which means that parts of the Ogallala Aquifer should be considered a nonrenewable resource. This map shows changes in Ogallala water levels from the period before the aquifer was tapped to 2015.Explore what happens when the Ogallala aquifer runs out of water. Physical/Cultural Setting. The High Plains aquifer underlies 174,000 mi 2 in parts of eight States—Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. The area that overlies the aquifer occupies part of the Great Plains Physiographic Province; the extent of the Great Plains Physiographic Province and High ... much of the western Ogallala aquifer was never very productive because it is too thin and commonly discontinuous. Based on the limited data, water levels appear to be changing only slightly there. Map 1—Map and wells of saturated thickness in feet for the 2010s decade.Ogallala Formation and saturated material of Quaternary Age in hydraulic connection with the Ogallala Formation. The High Plains aquifer is commonly referred to as the Ogallala aquifer. The High Plains aquifer is similar to a rigid sponge, partially saturated with water. The aquifer is composed of clay, silt, sand,Spatial and temporal water-level variations in the Texas portion of the Ogallala Aquifer. January 2016; Natural Hazards 80(1 ... (using dendrograms and heat maps) resulted in the formation of ...Aug 26, 2020 · Map showing the location of the Ogallala aquifer — Credit: USGS (United States Geological Survey) Geology and recharge. The primary water-bearing unit in this high plains aquifer is the Miocene ... Monsoons affect people both in both positive and negative ways. In India and Southeast Asia, people rely on rain from monsoons to fertilize crops, fill aquifers and wells, and power hydroelectric facilities.The aquifer is slowly being pumped dry. Water wells, for instance, have dropped more than 61 meters (200 feet) in the Texas Panhandle. Though the trend line is downward, not all regions are equally affected. As the map shows, there are peaks and valleys of saturation. Some areas have a few decades of water left, some more.Ogallala Aquifer. These layers show the spatial variability in the saturated thickness and saturated thickness change on the Great Plains. Web Map by ttucgst. Last …Mar 22, 2019 · The Ogallala aquifer median dissolved-solids concentration layer shows points where groundwater-quality data were collected and indicate that most of the western part of the study area has dissolved solids that are less than or equal to 1000 milligrams per liter; and higher dissolved solids are present in the eastern part of the study area. The Ogallala, or High Plains, Aquifer is a porous body of complex sediments and sedimentary rock formations that conducts groundwater and yields significant quantities of water to wells and springs. The principal sediments and rocks of the aquifer range in age from 33 million years old to sediments being deposited today, but the majority is less …Overview. The Ogallala Aquifer lies beneath 111 million acres of land in Wyoming, South Dakota, Nebraska, Kansas, Colorado, Oklahoma, Texas, and New …There are at least seven major aquifer systems in Nebraska. By far, the High Plains/Ogallala aquifer is the largest in terms of volume of water in storage and withdrawals for irrigation. Several secondary aquifers exist in areas outside of the High Plains aquifer, providing water for irrigation, municipal supplies, and domestic use in parts of far western and far eastern Nebraska. The Ogallala Aquifer is up to 1,000 feet deep in some places. However, the average depth is estimated to be between 100 and 300 feet below the surface. In some areas, the water table can reach depths of 500 feet or more. The aquifer contains deposits of both fresh and salty water. In most places, the upper layer is composed of fresh water ... The Ogallala Aquifer extends from the northern United States into the Texas Panhandle and West Texas and is the primary source of water within the District. The aquifer consists of sands, gravel, silts, and clay sediments that were deposited as part of ancient river systems approximately three to six million years ago during the Neogene ...

The High Plains Water-Level Monitoring Study (HPWLMS) is the USGS's response to a directive from Congress to report on water-level changes in the High Plains [Ogallala] aquifer . Figure 1. Location map showing the …Maps are important to locate important places, study and compare different locations and even predict the weather. There are many different types of maps, including floor plans, topographical maps and weather maps.There are at least seven major aquifer systems in Nebraska. By far, the High Plains/Ogallala aquifer is the largest in terms of volume of water in storage and withdrawals for irrigation. Several secondary aquifers exist in areas outside of the High Plains aquifer, providing water for irrigation, municipal supplies, and domestic use in parts of far western and far eastern Nebraska. Sep 11, 2017 · The Dakota aquifer (formally called the Maha Aquifer) is by far the largest of these secondary aquifers, supplying all of the water to more than 3,400 wells in eastern Nebraska. Seventy-five percent of these wells are domestic, although in places the aquifer is capable of supplying a sufficient volume of water for irrigation and commercial use.

The water table, the upper boundary of the High Plains aquifer, ranges in altitude from about 6,000 to 1,200 feet above NGVD 29. A contour map of the water table shows groundwater flow direction is generally from west to east and locally toward streams ( figure 9 ). The average groundwater flow velocity in the High Plains aquifer is about 1 ...much of the western Ogallala aquifer was never very productive because it is too thin and commonly discontinuous. Based on the limited data, water levels appear to be changing only slightly there. Map 1—Map and wells of saturated thickness in feet for the 2010s decade. Areas of zero saturation have developed since the 1950s.Location-based services are becoming increasingly popular as businesses look for ways to better serve their customers. Live view maps offer a number of benefits that can help you improve your location-based services.…

Reader Q&A - also see RECOMMENDED ARTICLES & FAQs. Jan 10, 2023 · This map shows how much the aquifer has decli. Possible cause: Map: The Ogallala Aquifer – A Freshwater Bonanza in Decline - Circle of Blue.