View of Ouachita Mountains from Hot Springs Mountain Tower, Hot Springs National Park, Arkansas (Looking North)
The deciduous trees had just begun to blossom, so the mix between pine and hardwood was very stark.
Overlooking the Ouachita Mountains from Hot Springs Mountain Tower, Hot Springs National Park, Hot Springs, Arkansas.
The Ouachita Mountains are a mountain range located in west central Arkansas, southeastern Oklahoma and north-east Texas. The range's subterranean roots may extend as far as central Texas, or beyond it to the current location of the Marathon Uplift. Along with the Ozark Mountains, the Ouachita Mountains form the US Interior Highlands, the only major mountainous region between the Rocky Mountains and the Appalachian Mountains. The highest peak in the Ouachitas is Mount Magazine in west-central Arkansas.
The Ouachita Mountains contain the Ouachita National Forest, Hot Springs National Park and Lake Ouachita as well as numerous state parks and scenic byways. They also contain the Ouachita National Recreation Trail, a 223-mile long hiking trail through the heart of the mountains. The trail runs from Talimena State Park in Oklahoma to Pinnacle Mountain State Park, near Little Rock, Arkansas. It is a well maintained, premier trail for hikers, backpackers, and mountain bikers (for only selected parts of the trail).
The Ouachita Mountains are a physiographic section of the larger Ouachita province (which includes both the Ouachita Mountains and the Arkansas Valley), which in turn is part of the larger Interior Highlands physiographic division.
The Ouachita Mountains are fold mountains like the Appalachian Mountains to the east, and were originally part of that range. During the Pennsylvanian part of the Carboniferous period, about 300 million years ago, the coastline of the Gulf of Mexico ran through the central parts of Arkansas. As the South American plate drifted northward, a subduction zone was created in this region. The South American oceanic crust was forced underneath the less-dense North American continental crust. Geologists call this collision the Ouachita orogeny. The collision buckled the continental crust, producing the fold mountains we call the Ouachitas. At one time the Ouachita Mountains were very similar in height to the current elevations of the Rocky Mountains. Because of the Ouachitas' age, the craggy tops have eroded away leaving the low formations that used to be the heart of the mountains.
Unlike most other mountain ranges in the United States, the Ouachitas run east and west rather than north and south. Also, Ouachitas are distinctive in that volcanism, metamorphism, and intrusions are notably absent throughout most of the system.
The Ouachitas are noted for quartz crystal deposits around the Mount Ida area and for renowned Arkansas novaculite whetstones. This quartz was formed during the Ouachita orogeny, as folded rocks cracked and allowed fluids from deep in the Earth to fill the cracks.
The Ouachita Mountain area of Arkansas is dominated by Cambrian through Pennsylvanian clastic sediments, with the lower Collier formation in the core of the range and the Atoka formation on the flanks. The Atoka Formation, formed in the Pennsylvanian Period, is a sequence of marine, mostly tan to gray silty sandstones and grayish-black shales. Some rare calcareous beds and siliceous shales are known. The Collier sequence is composed of gray to black, lustrous shale containing occasional thin beds of dense, black, and intensely fractured chert. An interval of bluish-gray, dense to spary, thin-bedded limestone may be present. Near its top, the limestone is conglomeratic and pelletoidal, in part, with pebbles and cobbles of limestone, chert, meta-arkose, and quartz. It was formed during the Late Cambrian.
The mountains are known to contain at least 15 endemic plant species (i.e. plants that occur nowhere else). These include Sabatia arkansana, Valerianella nuttallii, Liatris compacta and Quercus acerifolia.
The mountains were home to the Ouachita tribe, for which they were named. Later French explorers translated the name to its present spelling. The first recorded exploration was in 1541 by Hernando de Soto. Later, in 1804, President Jefferson sent William Dunbar and Dr. George Hunter to the area after the Louisiana Purchase. Hot Springs National Park became one of the nation's first parks in 1832. The Battle of Devil's Backbone was fought here at the ridge of the same name in 1863. In August 1990, the Forest Service discontinued clear-cutting as the primary tool for harvesting and regenerating short leaf, pine and hardwood forests on the Ouachita National Forest.
View from Scenic Mountain Drive up Hot Springs Mountain in Hot Springs National Park, Hot Springs, Arkansas.
Hot Springs is the 10th most populous city in the U.S. state of Arkansas, the county seat of Garland County, and the principal city of the Hot Springs Metropolitan Statistical Area encompassing all of Garland County. According to 2008 Census Bureau estimates, the population of the city was 39,467.
Hot Springs is traditionally best known for the natural spring water that gives it its name, flowing out of the ground at a temperature of 147 degrees Fahrenheit (64 degrees C). Hot Springs National Park is the oldest federal reserve in the USA, and the tourist trade brought by the famous springs make it a very successful spa town.
The city takes its name from the natural thermal water that flows from 47 springs on the western slope of Hot Springs Mountain in the historic downtown district of the city. About a million gallons of 143-degree water flow from the springs each day. The rate of flow is not affected by fluctuations in the rainfall in the area. Studies by National Park Service scientists have determined through carbon dating that the water that reaches the surface in Hot Springs fell as rainfall in an as-yet undetermined watershed 4,000 years earlier. The water percolates very slowly down through the earth’s surface until it reaches superheated areas deep in the crust and then rushes rapidly to the surface to emerge from the 47 hot springs.
A small channel of hot spring water known as Hot Springs Creek runs under ground from an area near Park Avenue to Bath House Row.