T I ME 
(in rn it I ion s of ye a rs) 
0 
 
0 
 
<! 
0: UJ 
 
-0 
0: UJ 
 
Q_ 
 
1\ u 
0 
 
QU ATER NAR Y ;- 
 
N 
 
0 z 
UJ 
 
TE RTI ARY 
 
u 
 
FORMS OF LIFE 
AGE OF MAN earliest man 1st apes. grasses 1st monk eys AGE OF MAMMALS 
 
100 - 
u 
0 
N 
0 
(/) 
UJ ~ 
 
CRE TACEOUS JURASSI C 
 
extinction of dinosaurs 1st sna k es 1st an giosperms 
(blooming plants) 
AGE OF REPTIL ES 
1st birds, mammals 
 
EVENTS IN GEORGIA 
Deposition of the Coastal Plain sediments, which is still occurring. 
 
200 - 
 
TRIASS IC 
 
1st Liinosaurs 
 
300 - 
 
PER M I A N PENNSYLVANIAN 
MISSISSIPPI AN 
 
1st frogs, eve rgr eens 
 
1st reptiles AGE OF AMPHIB IANS 
 
Erosion o f the Piedmont by strea ms, which is sti ll occurring. 
 
u 
 
400 
 
- 
 
0 
N 
 
0 
 
UJ 
 
...J 
 
<( 
c.. 
 
DEVONIAN SILURIAN ORDOVICI AN 
 
Et scale trees, ferns, amph ibians 
AGE OF F I SH ES 1st air breathing 
animals. land pl an ts 
1st fishes 
 
Upl i ft, folding and faulting of the rocks an d the fo r mation o f a mountain range in the Pi edmont . 
 
500 600 
 
CAM BRIAN 
 
1st hard-s hell ed inve rt ebrates 
 
Thro ughout the Paleozoic 
there was deposit ion of sediments w hich formed shales, sandstones, and gr e y w a c k e s . 
 
PRE CA MBRIAN 
 
multi -cellular l i f e fo r ms 
one -celled life forms 
 
GEOLOGIC TIME CHART 
 
Mod ;f;ed f r om l : 2,000,000 Geolog1c Map of Georgia 
 
 GEOLOGIC GUIDE TO SWEETWATER CREEK STATE PARK 
by Charlotte E. Abrams and Keith I. McConnell 
DEPARTMENT OF NAT URA L RESOURCES Joe D . Tanner Commissioner 
T HE GEO L OG IC A N D WATE R RESOURCES D IV ISI O N Sam M. Picker ing, State Geologist and Division Directo r ATLAN TA 1977 
 
  Table of Contents 
page Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 The creek, past and present . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 The land and the creek . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2 Geologic history . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 
Deposition . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 Metamorphism . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 Uplift and erosion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8 Geologic guide to the Factory Ruins Trail ........................ 14 Geologic guide to the Sweetwater Creek Trail .................... 21 Glossary . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 27 Acknowledgements . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29 
iii 
 
 Illustrations 
page Figure 1. Sweetwater Creek flood, April 1977 . . . . . . . . . . . . . . . . . . . . 2 
2. Block diagram . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 3. Map of the drainage basin of Sweetwater Creek . . . . . . . . . 5 4. Metamorphism, folding and erosion of the rocks . . . . . . . . . 7 5. Development of a thrust fault . . . . . . . . . . . . . . . . . . . . . . . . . . 9 6. Geologic trails map . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 7. Open pothole . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 8. Development of a pothole . . . . . . . . . . . . . . . . . . . . . . . . . . . 18 9. Scenic overlook . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20 10. Rock "benches" ..................................... 23 11. Refolded fold . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 12. Folded pegmatite .................................... 26 
iv 
 
 Tables 
page Table 1. The rocks at Sweetwater Creek State Park .............. 10 
v 
 
 Italicized words appear in the glossary. 
 
 Introduction 
Sweetwater Creek, near Austell, Georgia, has served many purposes; it has served as a factory site, a local municipal water source, and as the local fishing and swimming hole. To the beaver that inhabit its banks Sweetwater Creek is home. Signs of their work are visible along the park trails. To the botanist the creek is an ideal place to study various plants unique to this area, and to the geologist it is a spot where the past is revealed in the rocks, and changes in the land's surface can be seen taking place day by day. 
The Creek, Past and Present 
The mill ruins within Sweetwater Creek State Park are the visible remains of a once prosperous factory and town. The Sweetwater Factory was one of several factories located on tributaries of the Chattahoochee River in the nineteenth century. These factories used the water of the local creeks to provide power for the factories' machinery. (See stop 3, Factory Ruins Trail.) During the Civil War the workers at the Sweetwater Factory produced cloth for Confederate uniforms until the Union army destroyed the factory and surrounding town leaving only the ruins that remain today. 
During this century Sweetwater Creek has provided water for several cities in this area of Georgia. Untill971, Austell used the creek for its water supply, and today the city of East Point still relies on Sweetwater Creek for its water. A pumping station is located downstream from the park where an average of 7Yz million gallons of water are pumped out of the creek each day for East Point residents. Although 7Yz million gallons may seem to be a considerable amount of water to remove from the creek, this amount is negligible when compared with Sweetwater Creek's average discharge of 299 million gallons per day. 
In recent years the land within the creek's drainage basin has undergone considerable development. Towns near the creek have grown and residential areas have increased in size and number. Some industries have also located along the creek or on its tributaries. Pavement and buildings now stand where trees and vegetation once were. Runoff of water into the creek after a rainfall has increased due to this decrease in vegetation or soil cover. As a result, recent flood levels along Sweetwater Creek are higher than in the past, because the channel ofthe creek can no longer hold the larger amounts of water it receives as runoff after a heavy rain. Flood waters generally recede within a day, but while flooding is at its peak, portions of the park trails are covered by water and the creek becomes a raging torrent. At this time the largest amount of erosion takes place. 
1 
 
 Figur e I. Sweetwat er Creek nood. Apr il 1977 
The Land and the Creek 
The drainage basin of Sweetwater Creek encompasses a n area of 246 square miles 637 sq . km. within the G eorgia Piedmont. The no rthern and southern sections of th e c reek are distinctly differe nt in c ha racte r The northe rn section of the creek flows quietly through a wide , ofte n swampy stream valley In the north ern section , from where it o ri ginates near New G eorgia, in Paulding County until it reac hes Aust e ll , Swee twa ter Creek flows in an eastward direc tio n . This eastward direc tion of fl ow is unusual for a m ajor stream in this p ar t of the Pie dmont a nd is du e to the influ e nce of a regional geologic structure known as the Aust e ii-Frolo na Anticlinorium , an up-warped fo ld composed of many smaller folds (fig. 2) The Aust e ii -F ro lona is higher in elevation th a n the surround ing rocks, preve ntin g Swee twa te r Creek from crossing the a nti c lino rium a nd forcing the c ree k to fl ow a round the nos e of the s tructur e. 
2 
 
 ~ 
 
- 
~- 
 
?:;:""- 
 
w 
 
~ 
 
r _&.~~~ ~- 
 
~L; Swootwo\"*AIIooto '\\ 
 
Figure 2. Block diagram. 
 
 Sweetwater Creek State Park lies along the southern portion of the creek. At Austell the creek bends to flow in a southeastward direction until it enters the Chattahoochee River. The characteristics of the creek change as well as its direction as it encounters the resistant rocks of this area. Relief increases, the creek valley sides steepen, and falls and turbulence disrupt the previously tranquil creek. This section of Sweetwater Creek closely resembles a mountain stream. 
The Chattahoochee River flood plain lies within the Brevard Fault Zone at a lower elevation than the surrounding portion of the Piedmont. Sweetwater, as well as the other creeks that enter the river, is constantly downcutting in its effort to reach the lower elevation of the Chattahoochee River. From Austell to its junction with the Chattahoochee River, Sweetwater Creek drops 120 feet in elevation, 80 feet of which are inside the park. This change in gradient was an important factor in the choice of the Sweetwater Factory site. 
Before Sweetwater Creek enters the Brevard Fault Zone and the Chattahoochee River, it crosses a series of northeast-trending rock units. Some of these rocks, such as quartzites, are more resistant to erosion than the surrounding rocks. These quartz-rich rocks divert the creek at right angles to its southeastward direction of flow. Other rocks in the creek contain open joints and allow the creek to flow through these openings and across the rock units. This control of the creek's direction by the rocks and the structures within them gives Sweetwater Creek a rectangular drainage pattern. Rectangular drainage is characterized by right angle bends in a stream and its tributaries. The map of the drainage basin of Sweetwater Creek (Fig. 3) shows this drainage pattern. 
4 
 
 THE DRAINAGE BASIN OF SWEETWATER CREEK 
 
1 
 
o 0 
 
I 
 
2 
 
2 
 
3 
 
34 5 
 
4 Miles 6 Kiloll'leters 
 
N 
 
Axis of the / Austeii-Frolona Anticlinonum 
 
(}1 
 
I 
r__j '--1 
i i 
Figure 3. Map of the drainage basin of Sweetwater Creek. 
 
t~ 
 
 Geologic History 
This historical geology of Sweetwater Creek State Park can be separated into three periods. In order of occurrence these are: deposition of sediments, metamorphism and folding, and uplift and erosion (See Geologic Time Chart on inside of cover). 
Deposition The rock units presently exposed at the surface at Sweetwater Creek 
were originally deposited at least 450 million years ago as a series of sediments which formed rocks: shales, sandstones and greywackes (dark, impure sandstone). These sediments were deposited in an environment similar to that existing off the coast of Georgia today. Deposition occurred continuously in a slowly subsiding basin where older deposits were covered by younger ones and buried to depths of several miles (Fig. 4A). These sediments were later blanketed by basaltic lava flows which poured into the basin from volcanoes located near the basin's margins. As time passed thousands more feet of sediment were added to the basin, covering the lava flows. 
Metamorphism Deposition in the basin probably continued until approximately 450 million 
years before the present. Until this time the increasing weight of the sediment in the basin caused it to subside slowly allowing deposition to continue; now, however, the direction of the forces acting on the basin changed and the basin began to be compressed from the sides. Subsidence stopped and uplift began. Compression caused increases in the temperature and pressure acting on the rocks in the basin, which eventually led to a complete reforming of the rocks buried there. Increasing temperature recrystallized the minerals in the rocks to new minerals. During recrystallization the pressure applied to the rocks by the compressive forces caused the new minerals, primarily the micas, to be preferentially oriented. These minerals were oriented so that their broad, flat bases were all in the same position (Fig. 48). Because of this mineral orientation, the rock now breaks more easily along the layers of mica. This plane of weakness is termed foliation. Recrystallization of the minerals and the development of foliation changed the shales, sandstones, greywackes and basalts into mica schists, quartzites, metagreywackes and amphibolites respectively (defined in table 1, page 10 ). Metamorphism, the process whereby the rocks are altered under heat and pressure, also destroyed any fossil remains that may have been in the original rock units. 
Increasing pressure occurring deep within the earth's crust played two other significant roles in addition to the metamorphism of the rocks of Sweetwater 
6 
 
 Direction of the compressive forces. 
Sediments are deposited horizontally in a basin and covered by additional deposits. Under the weight of the overlying sediments they are consolidated into shales, sandstones and greywackes. Then compression and ' metamorphism of rocks within the basin begins. 
 
garnet 
 
Under the heat and pressure accompanying metamorphism the rocks are recrystallized into schists, gneisses and quartzites. The newly formed minerals are preferentially oriented to form foliation and the horizontal layers are compressed to form folds. 
 
Later, a second set of folds is produced, but the heat necessary for a recrystallization of the rocks is not present during this event. 
The crest of the fold is eroded away exposing the rocks in its core at the surface. 
Figure 4. Metamorphism, folding and erosion of the rocks. 
7 
 
 Creek State Park. These were folding and faulting of the rocks. Pressure resulting from compressive forces folded the rocks into a series of troughs and ridges giving the rocks a roller coaster appearance. Two separate periods of this folding are observed in the rocks at Sweetwater Creek with the first set of folds being refolded by a later set (Fig. 4C & photo page 25 ). Pressure also caused the rocks to break and be thrust up and over each other. This type of movement is called faulting (Fig. 5). Finally, both faulting and folding forced rock buried deep within the crust of the earth to be squeezed up towards the surface. This uplift led to the formation of a mountain range in the Piedmont of Georgia which may have been similar to the present Blue Ridge Mountains or even the Rocky Mountains in the western United States. Uplift and Erosion 
Uplift, folding and faulting of the rocks continued until approximately 250 million years ago when the compressive forces stopped. During and after uplift streams began to cut into and change the appearance of the newly emerging land surface. Dissolved organic acids carried by streams and groundwater caused the rock to decompose into sediments just as these processes are decomposing the rock at Sweetwater Creek State Park today. These sediments were carried by streams to the south towards what is now the Coastal Plain of Georgia. In fact, rock eroded from the Piedmont is the major source for the material making up the Coastal Plain sediments. Streams flowing southeastward eroded and changed the mountain range into the present rolling hills of Piedmont Georgia. Uplift and erosion exposed rocks in the Piedmont and at Sweetwater Creek that had once been several miles beneath the surface of the earth (Fig. 4D). 
8 
 
 Metamorphic rock was intruded by a pegmatite. 
The pegmatite was offset by a thrust fault. 
The rock was eroded. Erosion can continue until all signs of faulting are removed. 
Figure 5. Development of a thrust fault. 
9 
 
 THE ROCKS AT SWEETWATER CREEK STATE PARK 
 
NAME Mica schist 
Metagreywacke ,__. 
0 
Quartzite Amphibolite 
Pegmatite 
 
DESCRIPTION 
Biotite and muscovite mica, quartz and feldspar. Garnets are present in most of the schist units within the park. Some units also contain kyanite. 
Fine to medium grained quartz, biotite (black) mica, muscovite mica and feldspar. Layering can be distinguished. Some units contain smaller garnets. 
Quartz. Fairly uniform in texture. Becomes sugary with weathering. 
Medium-grained (black) hornblende, quartz and feldspar. Layered. Weathered rock is ochre in color. 
Coarse grained rock made up primarily of quartz and feldspar with some large flakes of mica. 
 
COLOR 
 
ORIGINAL ROCK 
 
Grey to silver with garnets appearing brown 
 
Shale 
 
Light to medium grey 
 
Greywacke 
 
Light brown 
Dark grey to black 
White with some pink 
 
Sandstone Basalt 
Injected, once molten rock 
 
 Scene at the end of the Factory Ruins Trail. II 
 
 GEORGE H. SPARKS RESERVOIR 
 
.0-0:::::=500-===>'000 
SCALE IN FEET 
 
EXPLANATION 
m METAGREYWACKE WITH SCHIST LAYERS 
QUARTZITE 
. AMPHIBOLITE 
. < PEGMATITE 
 
D 
 
mNORTH 
 
w....... SWEETWATER CREEK STATE PARK 
 
GEOLOGIC TRAILS GUIDE 
 
Figure 6. Geologic trails map. 
 
Geology by Keith I. McConnell and Chorloffe E. Abrams, 1977 
Base map by D. P Cox 
 
 Geologic Guide to the Factory Ruins Trail of Sweetwater Creek State Park 
 
Distance Between Stops 
00' 
1363' 
 
Total 00' 
1363' 
 
Leave the rest station and follow the trail that leads to the mill ruins. Upon reaching Sweetwater Creek, turn right on the Factory Ruins Trail. Take the first trail on the left. This trail leads to stop 1. 
 
Stop 1: Garnet - mica schist 
 
The rock outcrop on your left before reaching the creek is a garnet - mica schist. The most interesting feature of this rock is the garnets. Garnet is a common rock-forming mineral in the Georgia Piedmont. Most of the garnets here are small, reddish-brown and "wart-like." On closer examination of the rock, a second, flattened type of garnet can also be seen. 
 
In some parts of the United States, garnets are mined for use as gemstones or abrasives. However, garnets found here have little or no commercial value because they lack the size, form, and quality necessary for such uses. 
 
3' 
 
1366' From Stop 1 walk toward the creek along 
 
the same trail to Stop 2. 
 
Stop 2: Joint control of stream flow. 
 
At this stop the creek turns almost 90 and begins to flow nearly perpendicular to the strike. Until this point, stream flow was moving in the direction of the foliation (see page 6 of general geology). Here, most joints have the same orientation and control stream flow by providing natural channels for the water to cross the strike of the rocks. Several joints can be 
seen in the rocks present at this stop. 
 
524' 
 
1890' Return to the main trail and continue 
 
downstream to the marked trail on your 
 
left. Follow this side trail to the Creek. 
 
14 
 
 Stop 3: Natural Dam 
 
The rock spanning the creek at this point was a major factor in the site selection of the millway entrance. This rock provides a natural base for a dam to divert water into the millway. It also marks the beginning of a major increase in the slope of the stream. This change in stream level, or gradient, allowed the mill, located downstream, to be at a lower level than the entrance to the millway. This difference in the level of the millway entrance and the mill provided the slope necessary to generate the water energy to turn the mill wheel. 
 
858' Stop 4: Foliation 
 
2748' 
 
Return to the main trail and proceed to stop 4. Note the presence of amphibolite along the trail. A short distance along the. trail on the right is a spring which is fed by underground water passing through joints in the rock beneath the ground surface. 
 
The rock exposed at this stop shows weathering along foliation planes in a metagreywacke. The almost horizontal ridges in the rock are formed by erosion along the foliation. While all rock in Sweetwater Creek State Park, except the pegmatites, shows a foliation, this rock is one of the better examples of foliation. 
 
Another structural feature visible at this stop is the small joint in the middle of the rock. 
 
89' 
 
2837' 
 
Stop 5: Millway Wall 
 
Stops 5 and 6 are off the main trail on the path that leads through the millway to the left. From stop 4 proceed to the left into the millway towards the mill. 
 
This stop shows the millway wall which was partially constructed from rock quarried from the surrounding rock units. The marks made by quarrying equipment can be seen on some of the rocks in the wall. These marks are the cylindrical holes on the rock sides. 
 
Foliation played an important part in the quarrying operation. By splitting along the foliation quarrying was made easier, enabling the builders to provide rocks that had at least two regular smooth, flat surfaces. 
 
15 
 
 Joints, although not as common as foliation, were also used as an aid in quarrying. In the construction of the wall, the builders used a combination of joints and foliation to form rectangular blocks. 
 
Joints also played another role in the millway wall. As you continue through the millway, observe how the builders used the joint surfaces of the large rock outcrops to your right as part of the millway wall. This portion of the wall is formed by natural joint surfaces. 
 
176' 
 
3016' Continue along the millway to the second 
 
opening in the wall on the left. The features 
 
of stop 6 are visible from the top of the wall. 
 
Stop 6: Pothole and joints 
 
In the stream directly in front of you there are examples of 1) a well developed pothole and 2) welldeveloped joints. 
 
Potholes are erosional features usually. found in the rock in fast moving streams. These circular depressions in rocks are formed by the grinding action of trapped sand and gravel being swirled around by the strong currents within the creek (Fig. 8). Starting points for potholes are usually niches or breaks in the rock, such as poorly developed joints or along foliation planes, where the water flow becomes disturbed and begins to swirl and erode. The pothole shown at this stop was initiated along a poorly developed joint. 
 
As you look toward the opposite bank of the stream, you can see many joints and their influence on the creek. The water finds the open joints much easier to flow along and to erode down through than the less open foliation. 
 
54' 
 
3067' Continue along the millway until you reach 
 
the main trail. Stop at the first corner of 
 
the mill ruins near the archway. This is 
 
stop 7. 
 
Stop 7: Augen 
Rocks used for the mill base are primarily metagreywacke, and amphibolite. Both of these rocks are found locally, but no abandoned quarry, necessary for the large amount of rock used, has been found as a source for these rocks. An interesting feature in the rocks used for the base is the presence of large elliptically shaped feldspars (white). The distinctive appearance given 
 
16 
 
 by these elliptical feldspars within the rock is termed "augen" (German for "eyes"). A good example of the augen is found in the bottom cornerstone of the mill. There, a series of augen is visible within a band of feldspar in the rock. 
 
693 ' 
 
3760' Continue along the main trail behind the 
 
mill. As you pass behind the mill note the 
 
well-developed joints in the rock on your 
 
right. As you near the creek you can ob- 
 
serve two large blocks of rock on the 
 
opposite bank that have fallen down the 
 
hill side. These blocks are an indication 
 
that the stream is widening its channel, 
 
and therefore is undercutting the rocks 
 
along the banks. 
 
Figur ~ 7. Open pothole 
17 
 
 Pebbles transported by the water are caught in a depression in the rock. This depression can be at the intersection of two joints, in the nose of a fold, or where less resistant material has been eroded from the rock unit. 
Pebbles are circulated in the depression by the force of the water. Abrasion resulting from the grinding of the pebbles deepens the depression. 
With the passage of time abrasion continues and the pothole deepens even more. As the pebbles become abraded to smaller grains of sand new pebbles are constantly being introduced. 
Finally, the downstream side of the pothole may become eroded away, leaving an open pothole as seen in the photograph on page 17. 
Figure 8. Development of the pothole shown in figure 7. 
18 
 
 Stop 8: Pegmatite 
The lighter colored rock near the bank of the creek is called pegmatite. As you look diagonally across the creek in an upstream direction, you can see that the pegmatite extends across the width of the creek. The darker rock on either side of the pegmatite is metagreywacke. Joints are poorly developed or are not present in the pegmatite. The pegmatite was injected as a hot liquid into the metagreywacke after metamorphism, and therefore, lacks the foliation present in the metagreywackes. It also has much larger crystals than the metagreywacke because it cooled slowly. The lack of uniformity with the surrounding rocks caused the pegmatites to react differently than the metagreywackes to the joint forming stresses, resulting in a lack of joints in the pegmatites. Sweetwater Creek begins to bend at this point due to the influence of the pegmatites within the stream. As the creek bends, it once more flows at near right angles to the joints and parallel to the foliation. Further south, the creek bends again to flow through the joint openings. 
19 
 
 Figure 9. Scenic overlook. 
20 
 
 we 
 
Geologic Guide to the Sweetwater Creek Trail 
 
Leave the rest station area and follow the Factory Ruins Trail downhill to the Creek. Turn left at the creek and follow the trail to the bridge. 
 
As you cross the bridge notice the flat, sandy areas on either side of the creek. These areas are part of the creek's floodplain. A floodplain is a relatively flat area adjacent to a stream (creek or river) that is frequently covered by water during periods of flooding. A stream in flood has the capacity to carry more and larger sediment within its channel due to a higher water velocity. As the stream overflows its banks the velocity of the overflow water decreases and some of the stream's sediment load is deposited adjacent to the stream. The flat sandy areas on either side of the bridge are examples of deposition on the flood plain. 
 
Length from the bridge 
 
Between points 
 
Total 
 
00' 
 
00' 
 
68' 
 
68' 
 
Continue across the bridge to stop 1. 
 
Stop 1: Kyanite 
 
The rock outcropping in the road is mica schist. This schist contains kyanite, a mineral that is commercially important to Georgia. On close examination of the rock at this stop, kyanite is visible as the bluishgrey, bladed mineral. It is characterized by its ability to be scratched with a knife in a direction parallel to its long axis, and irs resistance to scratching along its short axis. Kyanite is formed under high temperatures and pressures. Its presence is used by geologists as an indication of the intensity of metamorphism that has occurred in an area. 
 
Kyanite is mined at Graves Mountain in Lincoln County, Georgia. Its stability at high temperatures allows it to be used as a refractory (a material that resists the action of heat and chemical agents). Kyanite is also altered to a synthetic mineral termed mullite which is used in ceramics, in particular as the ceramic insulator on spark plugs. 
 
21 
 
 732' 
 
800' Continue along the trail to stop 2. As you 
 
walk along the trail you may notice debris 
 
left in the branches of trees and shrubs by 
 
high water. This material was left from one 
 
of Sweetwater Creek's periodic floods. 
 
Stop 2: Quartzite 
 
The rock at the water's edge near the trail is quartzite. Because of its high quartz content the quartzite is more resistant to erosion by the creek than the surrounding metagreywackes and mica schists. Here the quartzite deflects the water flow causing the creek to bend and flow parallel to the foliation of the rocks (see page 6 of general geology). The creek continues in this new direction until the water reaches a point where it has been able to erode through the quartzite; there the creek returns to its earlier direction. The quartzite is the first evidence within the park that the rock units control or influence the direction of Sweetwater Creek. This control of the creek by the rocks is called lithologic control. 
 
1567' 
 
2447' 
 
Continue on the main trail to the first trail on your right. Follow this side trail to the creek. 
 
Stop 3: Natural Dam 
 
At this stop the park visitor gets a better view of the natural dam and millway entrance described in stop 3 of the Factory Ruins trail. As you can see very little additional construction was needed for the natural dam to divert some of the creek's flow into the millway. 
 
Downstream from this point the slope of the creek channel begins to steepen. Another term for this slope is gradient. The increased gradient of Sweetwater Creek results in an increase in the water velocity of the creek. Turbulence also increases as the creek channel becomes more rocky and full of obstacles which disturb the water flow. The water no longer flows smoothly but becomes disrupted and forms eddies within the creek. The churning water is more erosive than the quiet, uninterrupted stream flow, enabling the creek to gradually cut through and remove rock lying within its channel. 
 
321' 
 
2768' Return to the main trail and proceed to 
 
the second side trail to your right. Follow 
 
441' 
 
3209' this trail to stop 4. 
 
22 
 
 Figure 10. Rock "benches". 
Stop 4: Rock "benches" Vis ible down s trea m fro m this s top are a series o f roc k "benc hes" ex tending across th e cree k. These "benches" are formed by d iffere nti al erosio n of the 
rock by the cree k. By differe ntial eros io n we mean so me roc k becomes ero ded and carried away fas ter than other roc k due to a diffe rence in roc k compos itio n. S ome o f the roc k has been removed leav ing ridges o r benches o f resistant roc k in th e cree k. The roc k be nc hes fo rm s hoals within the cree k inhibiting the water fl ow and causin g tur bulence. As the water fl ow becomes mo re int erru pted by th ese barri ers, c hurnin g current s (as disc ussed in stop 3) increase the rate o f erosio n within th e cree k. 
23 
 
 171' 
 
3380' Continue along the side trail to stop 5. On 
 
the hill to your left are several large out- 
 
crops of metagreywacke. Over a period of 
 
millions of years, Sweetwater Creek has 
 
eroded down to its present level exposing 
 
the outcrops on your left. The trail be 
 
comes more difficult from this point on 
 
and should be taken with caution. 
 
Stop 5: Falls and Cave 
Located in the stream directly below you is a large block of rock that has been dislodged by the water flow. The strong force of the water flipped the block over during a period of high water when the stream had the large amount of energy necessary for such movements. Separation from the surrounding rock occurred along joints at both ends of the block and along the rock's foliation on its underside. 
The cave-like opening in the outcrop of metagreywacke behind you results from a process called undercutting. Through time Sweetwater Creek has been gradually erocling and cutting down to this level to form the present stream valley. This rock has been undercut by the creek, and material the rock once rested on has been removed. Gravity has caused the exposed underside of the rock to break off along planes of weakness (foliation) forming the opening. 
A scenic overlook is on the hill above you, and provides the best view of the creek. Across the creek from the overlook are the Factory Ruins. Upstream you can see the benches of rock described in stop 4 and the beginning of the creek's gradient change (stop 3). Below you, the creek drops sharply (approx. 6') at the falls where it flows parallel to the joints. Further downstream, observe how the creek bends to flow at a right angle to the joints and parallel to the foliation. 
 
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 Numrous folds are visible in the rocks of Sweetwater Creek State Park. The best examples of these are located at Sweetwater Falls on the East Ridge Trail. Figures 11 and 12 show two types of folds found there. The East Ridge T rail is rougher than most in the park, but the scenery at its end makes the trip worthwhile for the more adventurous park visitor. 
Figu re II. Refolded fo ld in a metagreywacke. T he rocks of Sweetwater C r eek State Park exhibit two sepa rate pe r iods of folding. In the photo th e limbs o f the first fo ld have been folded by a second episode o f fo lding (see F ig. 4C ). 
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 Figu re 12. Folded pegmat ite in a metagreywacke. Th e pegma tite was injected into th e meta greywacke before folding and was folded along wit h the surrounding rock . 
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 Glossary 
These definitions are paraphrased from the following sources: 
(1) Gary, Margaret, et al (eds.): Glossary of Geology, Washington: American Geological Institute, 1974. 
(2) Fairbridge, Rhodes W., (ed.); The Encyclopedia of Geomorphology; Encyclopedia of Earth Sciences Series, Volume III, New York: Rheinhold Book Corporation, 1968. 
(3) Gilluly, James, et al; Principles of Geology, San Francisco: W. H. Freeman and Company, 1968. 
anticlinorium - a convex upward fold of regional extent composed of smaller folds. (1) 
Brevard Fault Zone - a zone of intense faulting that extends from northwestern North Carolina to the Fall Line in Alabama. 
crust - the outer shell of the earth (1) 
differential erosion - erosion that occurs at irregular or varying rates, caused by the differences in the resistance and hardness of rocks. Softer and weaker rocks are rapidly worn away while harder and more resistant rocks remain to form ridges, hills, or mountains. (1) 
discharge - the amount of water passing a given point in a specific amount of time. 
drainage basin - region (or area) drained by a particular stream or river and its tributaries. (2) 
fault - a fracture in the rock along which movement has occurred. (3) 
feldspar - a closely related group of minerals which owe their importance to the fact that they are the most abundant of all minerals. (3) 
foliation - thin layering in metamorphic rocks which is due to the parallel orientation of its minerals. (3) 
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 gradient- ... (b) a part of a surface feature that slopes upward or downward; a slope, as of a stream channel. ... (1) 
joint - a fracture or break in a rock along which no movement has taken place. (1) 
lithology - (a) the description of rocks.... (b) the physical character of a rock. ... (1) 
metamorphism - the transformation of rocks by heat, pressure and chemically active fluids to which they were subjected after deep burial. (3) 
organic acids - acids derived from organic material. recrystallization - the formation of new minerals in a rock .... under the 
influence of metamorphism.... (1) relief - ... (b) the vertical difference in elevation between the hilltops... and 
the lowlands... of a given region.... (1) runoff - that portion of rainfall which makes its way into a stream.... (1) strike - the direction or trend of a rock unit. (1) tributary- (a) a stream... joining or flowing into a larger stream (at any point 
along its course) .... (1) 
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 .. 
The authors extend their thanks to Randy Powers, Superintendent of Sweetwater Creek State Park at the time of this report, and Jake Ingram of the Office of Planning and Research for their encouragement, cooperation, and assistance on this project. 
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