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A simulated-color satellite image of Dallas and Fort Worth, Texas, taken by NASA's Landsat 7 satellite. The geology of the DFW Metroplex consists of gently tilted sediments of mostly Cretaceous age, which also obscures a much older geologic record.

Although the Ouachita Mountain roots are not visible in the DFW Metroplex since they are buried, they can still be recognized by boreholes and other data.In west Texas near Marathon, the mountain range makes an appearance to the surface, and is known as the Marathon Uplift.Online dating brings singles together who may never otherwise meet.It's a big world and the INTERRACIALPeople community wants to help you connect with singles in your area.Going from west to east in the DFW Metroplex and down towards the Gulf of Mexico, the strata gets progressively younger.

The Cretaceous sediments dip very gently (about 1°) to the east.Ancient folded mountains formed by the Ouachita orogeny existed in the eastern part of the Metroplex 300 million years ago.These ancient mountains were reduced by erosion and rifting associated with the opening of the Gulf of Mexico in Jurassic time and were buried beneath younger Cretaceous sediments.If you’re looking for a night on the town, a trip to Fort Worth is a straight shot on I-30 West, where you’ll have access to boutique shopping and galleries in the up and coming Magnolia area.The town of Roanoke may be small, but the great date potential is huge.It is a Class A clear-channel station, using a non-directional antenna.