DEQ Geo. Web. Face. The animation above shows examples of some of the Geo. Web. Face map layers. Getting Started. When you access the Geo. Web. Face application what you need to do next is not intuitively obvious. Before you use the application it is recommended that you review the User Guide and or some of the other information listed below. The Geo. Web. Face website address changed to http www. CREG/images/Bench-mapping-group.jpg' alt='Top Economic Geology Programs' title='Top Economic Geology Programs' />The animation above shows examples of some of the GeoWebFace map layers. Getting Started. When you access the GeoWebFace application what you need to do next is not. The Ozarks, also referred to as the Ozark Mountains and Ozark Plateaus, is a physiographic region in the U. S. states of Arkansas, Missouri, Oklahoma, and Kansas. TOPTEN_TORONTO_POST01.jpg' alt='Top Economic Geology Programs' title='Top Economic Geology Programs' />Strategic Planning. The Beaches, Inlets and Ports Program planning staff is charged with updating and maintaining the Strategic Beach Management Plan SBMP and. Geo. Web. Face on July 6. Please make changes to your favorites or bookmarks. Geo. Web. Face User Guides. This is good starting point. It can be used online or downloaded and reviewed at your convenience. To access the illustrated documentation at    http www. Geo. Web. FaceUsersGuide3. The User Guide is accessible via the Help link in the bottom panel of the application. You can have the User Guide and the Geo. Web. Face application open at the same time. If you are using a tabbed browser you can move back and forth as needed. You can use the keyboard combination Alt Tab to switch back and forth as well. Alt Tab will cycle through all of the applications you have open at the time. Dont want a big thick manual  Listed below are some distillations and excerpts from the User Guide. This is the very briefest of references for the Geo. Web. Face.   No illustrations or explanations just 1 page. Geo. Web. Face0. DeskTopSummary3. This four page guide might be useful to keep on hand. Geo. Web. Face0. DeskTopGuide3. Want a little bit of explanation in your user guide  Then this might be it  not illustrated. Geo. Web. Face1. DeskTopBriefGuide3. This one sheet document explains what all the links are on the bottom banner. Geo. Web. FaceBottomBannerLinks3. If you are thinking about exporting data to Excel this will help you find what is where. Geo. Web. FaceResultsDataElements3. Here is where you can get more details and information about the more than ninety different layers that are available to use making a map to suit your needs. Geo. Web. FaceLayersandDescriptions3. Quick, what is the API county number for Saint Clair County Here is where you can look to find all of the codes. APItoCountyName3. Step by Step. These are written instructions that illustrates how to some aspect of the Geo. Web. Face. Find out if there are Oil and Gas wells around an addresshttp www. AppendixFindWellsbyAddress3. You can use Latitude and longitude to find a well or location. You can also get the latitude and longitude for any place in Michigan. Geo. Web. FaceFindaLocationbyLatitudeandLongitude3. If you know one or more of the well attributes Permit Number, API Number, Well Name, Company, Field etc. You can use a partial name which you can redefine if you get too many responses. Geo. Web. FaceFindOilGasWellInformationUsingWellAttributes3. Ever want to make your own geologic map  Here are instructions on how to do just that. The example is a starting point. You can easily change what is displayed and the area covered to suite your needs. AppendixHowtoMakeanEndMoraineMap4. Aquaman Full Movie 2013. Some hints for using FTP file transfer protocol to access and download larger amounts of data. Geo. Web. FaceUsingFTP3. Videos. Below are links to some videos that may help you get started. These are rough drafts and will be fine tuned in the future. Please refer to the Geo. Web. Face User Guide for more information and details on using the Geo. Web. Face. Geo. Web. Face Overview Video 1  headphones may be neededhttp www. XLXXqofk. 8 Geo. Web. Save Game Files Psp Iso. Face Overview Video 2http www. R6pr. 6Xf. LS Geo. Web. Face Oil and Gas Layershttp www. Nfk. Sa. EFkh Geo. Web. Face Oil and Gas Searcheshttp www. Wryn. Rh. Xi. Sfc. To view the videos in Internet Explorer Select and Copy the first video URL,Open Internet Explorer and maximize it to fill the screen upper right corner,Click the dropdown arrow next to the CHANGE ZOOM LEVEL Icon magnifying glass with 1. Paste the URL into the browser address bar then press the Enter key. Click the triangular play button that shows up in the middle of the video. Adjust the volume headphones may be needed. More Resources. This is what we want to see in GWF 2. What would make the application more useful for you   http www. Geo. Web. FaceWishList3. Get online access to Michigan oil and gas data. Firefoxhttp www. Geo. Web. FaceOnlineOilandGasDatabase3. Background. The free Geo. Web. Face provides a wide array of geologic information for natural resource management, educational and general interests. Additional programs are not needed but can be added to suit individual needs. It can be accessed by anyone, at anytime, anywhere the web is available. This is one of the largest publically accessible record sets in Michigan over 1. GB of files with 7. To help make information easy to find GIS tools work with a comprehensive database. The intelligent links between maps data and records make this application powerful yet easy to use. Information includes oil and gas well data and files, mining and related geographic information. Maps can be built on a road map, aerial photograph or topographic map base. The over sixty layers many specific to this application of map information include Glacial Geology, Structural Geology, Outcrops, Bedrock Geology, Gravity, Magnetics, Shaded Relief, Hillshade, Water Falls, Wetlands Inventory, Town, Range and Section, State Ownership, State Mineral Leases, Federal Lands, and National Forests. The Geo. Web. Face allows users to view, on a Michigan map, information about non renewable geological resource activities regulated under Part 6. Oil and Gas Rules and Regulations, Part 6. Mineral Wells, Part 6. Mine Reclamation, Part 6. Nonferrous Metallic Mining, Part 6. Coal Mines, and Part 6. Sand Dune Mining. The Geo. Web. Face provides web and FTP access to over 1. GB of digital files and information from the OOGM Oil and Gas database. With the Geo. Web. Face you can locate oil and gas wells and mining sites, and can display associated geologic information as well as a variety of land use information. This is one of the largest public facing document access applications in Michigan. System Requirements. In order to use the Geo. Web. Face you need access to the Internet. The Geo. Web. Face was designed and tested using Microsoft Internet Explorer 8. Other contemporary web browsers can be used. However, some screens may look differently and some procedures may need to be modified. The speed at which maps are drawn or refreshed is in part a function of the speed of your internet connection and the computer equipment you are using. Some selections, like a number of oil and gas wells, may take a moment or two to gather the data and display it. The speed of FTP transfers is likewise a function of system resources and configuration as well as the number of users accessing the server. Contact Us. If you have any questions, comments, contributions or concerns please contact us. Feel free to make suggestions for additions, report omissions or errors and or provide examples to help expand the usefulness of the Geo. Web. Face.   Use whichever communication method you prefer. Send mail to the Geo. Web. Face Team at   Geo. Web. Face Team. Michigan Department of Environmental Quality. Office of Oil, Gas, and Minerals. P. O. Box 3. 02. 56   Lansing, MI 4. Geo. Web. Face Team at  DEQ Geo. Web. Face michigan. Ozarks Wikipedia. The Saint Francois Mountains, viewed here from Knob Lick Mountain, are the exposed geologic core of the Ozarks. Elevation map of the Ozarks. The Ozarks, also referred to as the Ozark Mountains and Ozark Plateaus, is a physiographic region in the U. S. states of Arkansas, Missouri, Oklahoma, and Kansas. The Ozarks cover a significant portion of northern Arkansas and southern Missouri, extending from Interstate 4. Arkansas to the south and western suburbs of St. Louis. Small parts of the Ozarks extend into northeastern Oklahoma and extreme southeastern Kansas. Though often referred to as the Ozark Mountains, the region is technically the Ozark Plateaus. There are, however, two mountain ranges within the Ozarks the Boston Mountains of Arkansas and St. Francois Mountains of Missouri. Buffalo Lookout, the highest point in the Ozarks, is located in the Boston Mountains. Geologically, the area is a broad dome with the exposed core in the St. Francois Mountains. The Ozarks cover nearly 4. Appalachians and Rockies. Together with the Ouachita Mountains, the area is known as the U. S. Interior Highlands. EtymologyeditOzarks is a toponym believed to be derived as a linguistic corruption of the French abbreviation aux Arcs short for aux Arkansas, or ofat Arkansas in English1 in the decades prior to the French and Indian War, aux Arkansas originally referring to the trading post at Arkansas Post, located in wooded Arkansas Delta lowland area above the confluence of the Arkansas River with the Mississippi River. Arkansas seems to be the French version of what the Illinois tribe further up the Mississippi called the Quapaw, who lived in eastern Arkansas in the area of the trading post. Eventually, the term came to refer to all Ozark Plateau drainage into the Arkansas and Missouri Rivers. An alternative origin for the name Ozark involves the French term aux arcs. In the later 1. 7th and early 1. French cartographers mapped the Arkansas and Mississippi Rivers. The large, top most arc or bend in this part of the Arkansas River was referred to as the aux arcsthe top or most northern arc in the whole of the lower Arkansas. Travelers arriving by boat would disembark at this top bend of the river to explore the Ozarks the town of Ozark, Arkansas is located on the north bank at this location. Other possible derivations include aux arcs meaning landof the arches5 in reference to the dozens of natural bridges formed by erosion and collapsed caves in the Ozark region. These include Clifty Hollow Natural Bridge actually a series of arches in Missouri,6 and Alum Cove in the Ozark St. Francis National Forest. It is even suggested aux arcs is an abbreviation of aux arcs en ciel, French for toward the rainbows which are a common sight in the mountainous regions. After the Louisiana Purchase, American travelers in the region referred to various features of the upland areas using the term Ozark, such as Ozark Mountains and Ozark forests. By the early 2. 0th century, the Ozarks had become a generic term. Physiographic subregionseditThe Ozarks consist of five physiographic subregions Karst features such as springs,9losing streams, sinkholes and caves are common in the limestones of the Springfield Plateau and abundant in the dolostone bedrock of the Salem Plateau and Boston Mountains. Missouri is known as The Cave State with over 6. Ozark counties. 1. The Ozark Plateaus aquifer system affects groundwater movement in all areas except the igneous core of the St. Francois Mountains. Geographic features include limestone and dolomite glades, which are rocky, desert like area on hilltops. Kept open by periodic fires that limit growth of grasses and forbs in shallow soil, glades are home to collared lizards, tarantulas, scorpions, cacti and other species more typical of the desert southwest. The Boston Mountains contain the highest elevations of the Ozarks with peaks over 2,5. Appalachian and Rocky Mountains. The Ouachita Mountains to the south rise a few hundred feet higher, but are not geographically associated with the Ozarks. The Boston Mountains portion of the Ozarks extends north of the Arkansas River Valley 2. Springfield and Salem Plateau to the north of the White River. Summits can reach elevations of just over 2,5. Turner Ward Knob is the highest named peak. Located in western Newton County, Arkansas, its elevation is 2,4. Nearby, five unnamed peaks have elevations at or slightly above 2,5. Drainage is primarily to the White River, with the exception of the Illinois River, although there also is considerable drainage from the south slopes of the Boston Mountains to the Arkansas River. Major streams of this type include Lee Creek, Frog Bayou, Mulberry River, Spadra Creek, Big Piney Creek, Little Piney Creek, Illinois Bayou, Point Remove Creek, and Cadron Creek. Many Ozark waterways have their headwaters in the uplands of the Boston formation, including the Buffalo, Kings, Mulberry, Little Red and White rivers. Topography is mostly gently rolling in the Springfield and Salem Plateaus, whereas the Saint Francois Mountains are more rugged. Although the Springfield formations surface is primarily Mississippian limestone and chert, the Salem Plateau is older Ordovician dolostones, limestones, and sandstones. Both are rife with karst topography and form long, flat plains. The formations are separated by steep escarpments that dramatically interrupt the rolling hills. Although much of the Springfield Plateau has been denuded of the surface layers of the Boston Mountains, large remnants of these younger layers are present throughout the southern end of the formation, possibly suggesting a peneplain process. The Springfield Plateau drains through wide, mature streams ultimately feeding the White River. GeologyeditThe Saint Francois Mountains in the northeastern Ozarks are the eroded remnants of an ancient range which form the geological core of the highland dome. The igneous and volcanic rocks of the Saint Francois Mountains are the exposed remains of a Proterozoic mountain range hundreds of millions of years old. The remaining hills are the exposed portion of an extensive terrane the Spavinaw terrane in part of granitic and rhyolitic rocks dating from 1. Ohio to western Oklahoma. The core of the range existed as an island in the Paleozoic seas. Reef complexes occur in the sedimentary layers surrounding this ancient island. These flanking reefs were points of concentration for later ore bearing fluids which formed the rich lead zinc ores that have been and continue to be mined in the area. The igneous and volcanic rocks extend at depth under the relatively thin veneer of Paleozoic sedimentary rocks and form the basal crust of the entire region. Grey dolomite laid down c. St. Francois Mountains. A major unconformity in the region attests that the Ozarks was above sea level for several hundred million years from the time of the volcanism in the Precambrian until the mid Cambrian with an erosionally produced relief of up to 1. The seas encroached during the late Cambrian producing the Lamotte Sandstone, 2. Coral reefs formed around the granite and rhyolite islands in this Cambrian sea. This carbonate formation, the Bonneterre now mostly dolomite, is exposed around the St. Francis mountains, but extends in the subsurface throughout the Ozarks and reaches a thickness of 4. The Bonneterre is overlain by 5. Elvins Group and the Potosi and Eminence Formations.