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    • The Natural History & Fossils Record of Houston County, GA
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  • 1: Georgia's Oldest Fossils; Archaeocyathids, At 513 Million Years Old
  • 2: Trilobites; 500 Million Years Ago
    • 2A; Murray County Stromatolites
    • 2B; A Trilobite Nest in Georgia
  • 3: Geologic Time
  • 4: Our Oldest Vertebrate?
  • 5: Georgia Before the Dinosaurs
    • 5A; Georgia’s Pennsylvanian Plant Fossils
    • 5B: Carpentertypus durhami, Georgia’s Giant Insect, 315 Million Years Ago
  • 6: 200 Million Years Ago
    • 6A: Birth of the Atlantic Ocean
  • 7: Cretaceous Georgia, Dinosaurs & more
    • 7A: Georgias Pterosaur
    • 7C: Coelecanths
    • 7B: So Many Sharks
    • 7D: Xiphactinus vetus
    • 7E: Side-necked turtles
    • 7F: Marine Reptiles
    • 7G: Dinosaurs in Georgia
    • 7I; The Blufftown Formation
    • 7L: Bill Montante's Mega "Gator" Tooth Discovery
    • 7K: The Pio Nono Formation
    • 7J: The Eutaw Formation
    • 7H: Deinosuchus schwimmeri in Recognition of Dr. David Schwimmer
  • 8: Suwannee Current, Gulf Trough, & Bridgeboro Limestone
  • 9: The Clayton Formation Report; By Hank Josey
    • 9A: The Georgia Turtle
  • 10: The Eocene; Georgia's Oldest Mammals
    • 10A: The Origins of Whales
  • 11: A Whale For Georgia
  • 12: Basilosaurids; The First Modern Whales
    • 12A: Basilosaurus cetoides
    • 12B: Basilotritus
    • 12C: Cynthiacetus (Revised)
    • 12D: Chrysocetus
    • 12E: The Redmond Mandible of Albany Ga
    • 12F; Houston County, GA Basilosaurus to the Smithsonian
  • 13: Ziggy and The Museum of Arts & Sciences, Macon, GA
  • 14: Late Eocene
    • 14A: Eocene Fossils & Stratigraphy
    • 14B; Fossils, Impacts, & Tektites Dating the Clinchfield Formation
    • 14C: The Tivola Limestone
    • 14D: Twiggs Clay Vertebrates
    • 14F; Sandersville Limestone, By Hank Josey
    • 14E: Ocmulgee Formation Vertebrates
    • 14I: Dating Late Eocene Sediments
    • 14J: Georgia's Tektites; Georgiaites
    • 14K; Shell Bluff; Georgia's Most Historic Paleontology Site
    • 14L; Taylors Bluff, Paleo Paddling the Ocmulgee River
    • 14M; Eocene Terrestrial Mammals From Gordon, GA
    • 14N: Fossil Ridge, A Stratigraphic Study in Oaky Woods Wildlife Management Area
    • 14O; Georgia's First Entelodont
    • 14P: Historic Rich Hill
    • 14Q; Bibb County's Christy Hill, Clinchfield Formation Hilltop
  • 15: Early Oligocene
    • 15A: The Marianna Limestone
    • 15B; The Glendon Limestone
    • 15C: Undiffereniated Oligocene Residuum
    • 15D; Brissus bridgeboroensis; A New Echinoid Species From Georgia’s Bridgeboro Limestone
    • 15E: The Curious Steinkern Sea Biscuits of Red Dog Farm Road
    • 15F: Early Oligocene Gordian Knot
  • 16: Bonaire GA Entelodont
  • 17: The Whale Eating Shark
  • 18: Miocene Epoch; 23.3 to 5.3 Million Years Ago
    • 18A; Miocene Terrestrial Vertebrates
    • 18B; Paul Fell, Rockhouse Cave
    • 18C: The Marks Head Formation
    • 18D: Miocene Terrestrial Vertebrates of the Marks Head Formation
    • 18E: The Statenville Formation
    • 18F: South Georgia’s Dugong Metaxytherium calvertense
  • 19: Pliocene Epoch; 5.3 to 2.5 Million years Ago
    • 19A: Two Small Primitive Horses from Taylor County Advance the Science of Georgia Geology
  • 20: The Ice Ages; Pleistocene & Holocene Epochs
    • 20A; Clark Quarry's Mammoths & Bison
    • 20B: Pleistocene Vertebrate List
    • 20C: Georgia’s Eolian Dunes
    • 20D: Georgia’s Carolina Bays
    • 20E: Late Pleistocene Significant Events
    • 20F: Southeastern Thermal Enclave
    • 20G; Diamond Back Terrapins
    • 20H; A Kaolin Mine Beaver Dam
    • 20I; Pleistocene Vertebrate Fossils On Georgia’s Piedmont
    • 20J; Watkins Quarry Pleistocene Vertebrates, Glynn County, GA
  • *NEW* 20K: Pleistocene Vertebrates from Coastal Georgia
  • 21: Humans in Georgia
  • 22: Geology of the Coastal Plain, 1911
    • 22A: 1911 Cretaceous Fossil Locations
    • 22B: 1911 Eocene Fossil Locations
  • 23: Coastal GA Locations (1957)
  • 24: Needed; The Georgia Geologic Survey
  • Building This Site
    • Origins Of This Site
    • Contributing Artists
    • Black & White Sketches


​14P: Historic Rich Hill
Crawford County, GA


By Thomas Thurman
Filed: 10/May/2021
​

Picture
Brilliant Red Sand &
Abundant Fish Teeth.
“Brilliant red sand capping the hill…” is a quote from the 1911 report of Rich Hill in Crawford County, Georgia. This sand, stained by iron oxidation, is certainly interesting but a bit further down in the 1911 description you encounter; “…Fish teeth are also abundant in places.” (1) Abundant fish teeth suggest shark teeth.​
Preservation?​
Rich Hill in Crawford County is unquestionably historic. But recently a question was asked if it’s worthy of preservation? That’s a different matter. The problem is, there is surprisingly little in the way of research over the site in 30 years and many in the Earth science community have simply forgotten about it. ​
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​To my knowledge the last serious, professional-level fieldwork at Rich Hill was performed during a 1991 field trip of the Georgia Geologic Society led by Paul Huddlestun and John Hetrick. Two superb field researchers, scientists, and invertebrate paleontologists. However the real focus of their 1991 fieldwork was identifying, dating and describing the surrounding Cretaceous & Paleocene sediments. Old sand and clay hills which had never been properly surveyed. The fossil rich Eocene deposits of Rich Hill sit like a young island surrounded by older deposits. (6)

So is there sufficient public or scientific support for preservation? We simply need more information. There are several invertebrate faunal list, or species lists, for Rich Hill, but no follow-up or additional work on shark teeth or other vertebrate fossils, show up in the literature. 
1911
In 1911 Otto Veatch and Llyod W. Stephenson published an extensive geologic survey of Georgia’s Coastal Plain. To my knowledge this is the earliest mention of Rich Hill and its fossils. Veatch and Stephenson were working together as a joint project of the Georgia Geologic Survey and the USGS performing an initial assessment of the Coastal Plain’s paleontology and geologic resources. Rich Hill stands about 20 air miles southwest of Macon and is one of the northernmost fossil beds on the Coastal Plain. It is a natural first stop for researchers travelling south from Atlanta.  
At just over 700 feet above sea level Rich Hill is the highest point in the immediate area. A drive along Highway 42 follows rolling hills and gifts some dramatic outcrops and  sweeping views as it wanders through the rugged, sandy, Fall Line hills. The Fall Line Hills occur between the Fall Line and the Fort Valley Plateau. 
​
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​​Rich Hill, which lies south of the state highway, is locally distinct because its capped, like an island which has lost its sea, by Eocene age sediments roughly 34 million years old. The surrounding sands and clays underlying the Eocene fossils beds Cretaceous aged, roughly twice as old at 68 million years.
 
There is such an abundance of Cretaceous sand in the Fall Line Hills that multiple sand mines have operated in the area for decades. 
​One of the fossil rich Eocene sediments of Rich Hill is the Tivola Limestone, In 1943 C. Wythe Cooke, described it thusly; “The (Tivola) Limestone represents the deposits of an invading sea that transgressed beyond the shore line of the preceding epoch and laid its sediments uncomformably on whatever older formations lay in its path.” (2)
In the last 60 million years there have been dozens of times when sea levels rose and coastlines transgressed far inland. There were times when such high sea levels lingered for millions of years. So yes, Rich Hill has been an island multiple times in the geologic past.  

To quote a 2009 paper from Biological Reviews; "Over the last 1.8 million years, North America has been subjected to no less than 27 glacial intervals." (12) That means sea levels risen & fallen (glaciers have advanced & retreated) in North America 27 times in the last 1.8 million years.
​​Fossil Beds
Interestingly, Rich Hill’s three fossil bearing formations are very well known and occur intermittently in Houston County, Twiggs County and Wilkinson County. Even the earliest researchers observed this and realized that these formations were continuous at some point, but weathering or erosion erased vast quantities of clay, sand and limestone. This left our current scattered deposits.
​Sadly no list of vertebrate species has ever been assembled for the Rich Hill, but several invertebrate lists have been created which we’ll be review. Invertebrates are useful in dating sediments. A vertebrate list offers a glimpse into the health & diversity of the environment represented by a deposit.
Access
Veatch & Stephenson’s 1911 visit was only the beginning for researchers; for a few decades the hill became a stop for many earth scientists.
 
In 1919 Charles Wythe Cooke & Harold Kurtz Shearer published their USGS report on Eocene sediments in Georgia. (3) The Eocene spans from 33.9 to 55.8 million years ago. Cooke and Shearer were looking specifically at the more recent end of that time span. Rich Hill was their first stop and they used the location as a standard for Eocene deposits, comparing the Crawford County species to similar fossil deposits they encountered further south.
 
Cooke would report on Rich Hill again in his 1943 report on the Geology of the Coastal Plain of Georgia for the United State Geological Survey. (2) 
​E.H. Rainwater included a stop at Rich Hill for the wide-ranging November 1944 field trip of the Southeastern Geological Society into southwest Georgia. (7)
 
Probably sometime during the 1980s some amateur rock clubs and societies gained access and collected at the site. I know of one knowledgeable amateur Jack Jones, a true Southern Gentleman and longtime member of the Mid-GA Gem and Mineral Society, who participated in a club dig at Rich Hill. I spoke to him about this in the mid-1990s, but even then, the Rich Hill dig had been decades earlier and his memory wasn’t clear. Sadly, Jack passed in 2020.
Below:
Rich Hill Descriptions from
1911 * 1919 * 1943 * 1944

​​In 1991 Paul Huddlestun and John Hetrick included Rich Hill as Stop #2 on the Georgia Geological Society’s 26th annual field trip into the Fort Valley plateau and central kaolin district. (6) So at least at that time there was an access road which offered fairly easy access for a group of researchers. ​
​Twenty-five years ago I was talking to a Crawford County native who’d been deer hunting at Rich Hill in the past, he talked about “pushing shark teeth up with the toe of my boot.” That’s not the kind of report you forget.
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​But for decades now, Rich Hill has notoriously difficult to access. The reason for this is simple, the location is private property leased by hunters and hunted nearly year-round.  The best way to avoid tragic accidents is to strictly limit access. For good reasons, neither the hunters, nor the landowners are too keen on uninvited guests trespassing through the hills. 

​To my knowledge, no organized paleo group, geological society, informed amateur, academic, nor professional paleontologist has visited or published any report on Rich Hill fossils in 30 years, since the 1991. So the written histories is all we really have until the site is visited again and a report is published.  
Modern Nomenclature for the Eocene Beds
There are three deposits reported from the hill which are known for fossils, all are late Eocene. In order, and using modern nomenclature they are:
  • The Twiggs Clay
  • The Tivola Limestone
  • The Clinchfield Formation 

​The Twiggs Clay

Immediately beneath the cap of red sand is about 7 meters (23 feet) of the Twiggs Clay Member of the Dry Branch Formation (6). The Twiggs Clay dates to approximately 34.3 million years old. It is a widespread deposit of clay and silt laid down in a generally quite environment with minimal currents where clay minerals were able to settle out undisturbed. Limestone beds occur rarely in the Twiggs Clay in scattered locations. There is a 2-meter (8 foot) limestone bed in Oaky Woods, dense with fossils, which represents a tempest deposit.  
​It was once believed that the Twiggs Clay was of volcanic origin and was weathered volcanic ash. But during a field survey published in 1970 Sam Pickering showed that this was an error. “The writer finds it most difficult to believe that the sediment was once a volcanic ash embedding consistently abundant benthonic foraminifers or that the ash could have weathered so completely as to destroy any glass and volcanic minerals and leave the delicate hyaline foraminifer tests intact and shiny.” (5)
​Vertebrate fossils occur in the Twiggs at many scattered locations, invertebrate fossils, especially bryozoans, often occur in dense quantities, but all fossils tend to be concentrated in localized outcrops and in most localities the Twiggs is nearly devoid of fossils. 
In 1919 Cooke and Shearer  reported two distinct beds of the Twiggs Clay at Rich Hill with both being fossiliferous. As no mention is made of species, the author assumes they were invertebrate fossils. In 1911 the Twiggs Clay was as yet undescribed, so Veatch and Stephenson didn’t mention it by name but seem to describe 4 beds. The 1911 description was essentially edited and re-used in both the 1943 and 1944 descriptions of the Twiggs Clay at Rich Hill.
In 1991 Huddlestun & Hetrick published their research on the locale for a Georgia Geological Society field trip and this included a new section drawing & description using modern nomenclature. Huddlestun & Hetrick described a single bed of Twiggs Clay measured at 7 meters (23 feet) thick. (See Section 14D of this website for a partial list of Twiggs Clay vertebrates.) ​
Partial list of  Twiggs Clay vertebrate species from various Georgia locations
Twiggs Clay Vertebrates reported in 1970 by Sam Pickering (Bulletin 81)
Genus & Species                    Common name                   Frequency
Lamna apppendiculata       Mackerel Shark                   Common
Carcharias cuspidate          Great White (Warm Sea) Abundant
Galeocerdo latidens             Tiger Shark                          Common
Myliobatis (species?)           Eagle Ray                             Abundant
Basilosaurus (species?)       Early whale                         Very Rare
Eosiren (species?)                  Manatee                               Rare

The American Museum of Natural History in New York
Twiggs Clay.GA Location: Huber Mine Pit #1
Reported by Gerard R. Case
Genus & Species                     Common name                   Finds
Lamna twiggsensis               Mackerel shark                  2 teeth
Ginglymostoma obliquum  Nurse shark                        2 teeth                  
Odontaspis acutissima         Sand shark                          3 teeth        
Propristis schweinfurthi     Sawfish                                3 snout teeth
Myliobatis (species?)           Eagle Ray                            8 teeth
​
​The Tivola Limestone
Historically the Tivola Limestone was once known as the Ocala Limestone, but in 1986 Paul Huddlestun and John Hetrick correctly re-assigned much of the traditional Ocala as the Tivola Limestone member of the Ocala Group. The two are of similar age but distinct. The name Tivola was derived from the extinct village and train station of Tivola in Houston County, about half a mile southeast of the Perdue Farms Plant on the Highway 247 spur in Houston County. The train station apparently once stood where AE Harris Rd crosses the railroad tracks.  
​The Ocala Limestone can still be seen in southwest Georgia.
 
In general the Tivola Limestone is rich in invertebrate material but rather poor in vertebrate fossils. Sand dollars, scallops, and especially bryozoans can occur in great numbers. It is an offshore, high energy, current driven deposit typically requiring some water depth, perhaps 100 ft. It was primarily formed by material “falling out” of a strong current. This would have been the mighty Suwannee Current which carved a great trough in South Georgia. (For more info see Section 8 of this website.)
​The 1911 report of abundant fish teeth came from the Tivola Limestone. The entire quote states; “Limestone, generally soft and friable (easily crumbles) but in places hard and compact: in places it is a bryozoan marl so soft that it may be scraped up with the hands. Fossils chiefly Bryozoa, pecten perplanus, and Mortonia sp.; fish teeth also abundant in places.” 
​The fossil rich Tivola the largest limestone deposit occurring in Houston County, Ga. It has long been mined. In 1911 there were already “old” limestone quarries just south of Perry, GA (1) which still exist. ​To date the Tivola has produced two historically and scientifically important early whale fossils; in 1911 Veatch & Stephenson reported an important find in the Tivola of Bonaire and then in 1937 another was recovered which went on to become part of the displays at the Smithsonian Museum of Natural History in Washington DC. (See Section 14C of this website for a more detailed description of the Tivola Limestone and a partial list of vertebrate fossils.)    
Partial list of Tivola Limestone vertebrates from various Georgia locations. 
Georgia Geologic Survey; Sam Pickering 1970 (Bulletin 81)
Genus & Species                    Common name          Frequency
Lamna apppendiculata      Mackerel Shark          Rare
Carcharias cuspidate          Great White                Rare   
Galeocerdo latidens             Tiger Shark                 Rare
Myliobatis (species?)           Eagle Ray                    Common
Basilosaurus cetoides          Early whale                 Very Rare
Siren (species?)                     Manatee (rib frags)   Rare

Dr. Michael Voorhies University of Georgia (1982)
Genus & Species                   Common name           Frequency
Entelodont (Genus?)            Terminator pig           Very Rare
 
Recently reported by Doug Holder, Cemex, Clinchfield, GA
Genus & Species                   Common name           Frequency
Carcharocles auriculatus   Megatooth shark        Rare
​
Smithsonian National Museum of Natural History
Collected & donated by Bill Christy
Genus & Species                   Common name      Specimen - County
Carcharhinus (species?)     Requiem shark           Tooth- Twiggs        
Cretolamna (species?)        Mackerel shark           Tooth- Twiggs        
Galeorhinus (species?)        Hound shark               Tooth- Twiggs        
Hemipristis (species?)         Snaggletooth shark    Tooth-Twiggs
Odontaspis (species?)          Sand Shark                  Tooth-Twiggs         
Sphyraena (species?)           Barracuda                    Tooth- Twiggs        
 
Smithsonian National Museum of Natural History (online catalog)
Barnwell Formation vertebrates (Land Mammal)
Genus & Species                    Common name       Specimen
Leptotragulus medius         Camelid                    Tooth & jaw
Jefferson Co. Reported by McCallie
​
​The Clinchfield Formation
The Clinchfield Formation is naturally exposed on Rich Hill as a yellow/brown sand with invertebrate fossils. The Clinchfield is Georgia’s most productive source of vertebrate fossils, especially sharks teeth. It is exposed very rarely as fossiliferous sand, there are a few other natural outcrops but these are hardened, silicified deposit rich in shelly fossils and gastropods but seemingly lacking vertebrate material. 
​There is one such hilltop on the county line of Bibb’s & Twiggs County, know as Christy Hill by local amateurs it is capped by hard chert, silicified Clinchfield Formation. This site has produced a surprising quantity of small, thumb sized gastropods and several shelly fossils and some dense, pure jasper often seen in seams in the rock, but not a single shark tooth. (13)   
​However, Georgia’s Clinchfield Formation has produced more than 9,700 scientifically reported vertebrate fossils scattered among about 50+ species of sharks, bony fish, reptiles, marine mammals, terrestrial mammals & one bird. These were all reported from mines in either Houston County or Wilkinson County. Such a wealth of material makes the Clinchfield our state’s richest source of vertebrate material. 
​To my knowledge, no vertebrate fossils have ever been reported from Rich Hill. Was the toe of that hunter’s boot in the Clinchfield Sand? This is an issue that begs to be addressed.
​The Clinchfield is a coastal deposit sometimes influenced by rivers, quartz sand is always involved to some degree. But in places the Clinchfield is a shell hash of fossils, it is named for Clinchfield, Georgia which is a tiny town in Houston County 7 miles southeast of Perry. 
​In 1970 Sam Pickering was researching the Clinchfield Formation and reported that he’d observed "reeflike" accumulations of articulated oysters in their growth positions. (5) The species he observed was Crassostrea gigantissima, this oyster genus typically tolerates being exposed at low tide.
“Reef-like accumulations of articulated oysters.” Pickering reported and collected some samples to deliver into the hands of Stephen M. Herrick, a biostratigrapher with the USGS. In 1972 Herrick published a paper reporting the contents of the Crassostrea gigantissima Pickering had given him. He reported the 50+ species of foraminifera fossils found trapped inside the sealed oysters. Identifying these species gave a date of between 35.42 to 36.18 million years old. (See Section 14B of this website for details.)
Partial List of Clinchfield Formation shark teeth from other locations in Georgia.
This list does not include other vertebrates

​
Genus &/or Species       Common name                Frequency          Reporting
Abdounia enniskilleni         Extinct Gray Shark               492 teeth                 Westgate
Abdounia enniskilleni         Extinct Gray Shark               589 Teeth                Parmley
Carcharias acutissima        Sand Tiger Shark                  446 Teeth                Parmley
Carcharias cuspidate          Great White Shark                Abundant                Pickering*
Carcharias hopei                  Sand Tiger Shark                  296 Teeth                Parmley
Carcharias hopei                  Sand Tiger shark                  922 teeth                  Westgate 
Carcharias koerti                 Sand Tiger Shark                  123 teeth                  Parmley
Carcharocles angustidens  Megatooth Shark                  2 Teeth                     Parmley
Carcharodon auriculatus   Giant toothed shark             2 teeth                      Westgate
Dasyatis (sp)                          Stingray                                 53 teeth                     Westgate
Edaphodon (sp)                     1st SE Chimaera                  Extremely Rare        Parmley
Galeo latidens                        Tiger shark                            219 teeth                   Westgate
Galeocerdo alabamensis     Requiem Shark                    351 Teeth                   Parmley
Galecerdo latidens                Tiger Shark                           Abundant                  Pickering*
Ginglymostoma serra          Nurse shark                          13 teeth                      Westgate
Hemipristis curvatus           Snaggletooth shark             170 teeth                    Westgate
Hemipristis curvatus           Snaggletooth Shark             635 Teeth                  Parmley
Heterodontus (sp)                 Angel Shark                          1 Tooth                       Parmley
Isurus (sp)                              Mako shark                           4 teeth                        Westgate
Isurus praecursor                 Mako Shark                          27 Teeth                     Parmley
Lamna (sp)                             Porbeagle shark                   124 teeth                    Westgate
Lamna Appendiculate          Mackerel shark                    Common                    Pickering*
Mustelus vanderhoefti         Smoothhound Shark           3 Teeth                       Parmley
Myliobatis (sp)                      Eagle Ray                               Abundant                  Pickering*
Myliobatis (sp)                      Eagle ray        8 dental batteries/284 teeth         Westgate
Nebrius thielensis                 Nurse Shark                          79 Teeth                     Parmley
Negaprion eurybathrodon Lemon Shark                        2127 Teeth                 Parmley
Negaprion gibbesi                Lemon shark                        1538 teeth                  Westgate
Palaeorhincodon                   Whale Shark                        1 tooth                         Parmley
Physogaleus (sp)                   Carchrhinid                          19 teeth                       Westgate
Physogaleus secundus         Sharpnosed Shark               70 Teeth                     Parmley
Pristis (sp)                              Sawfish                                  Very rare                    Pickering*
Propristis schweinfurthi     Sawfish                                  238 rostral teeth      Westgate
Raja (sp)                                 Skate                                      4 skutes                      Westgate
Rhinoptera (sp)                    Cownose ray                          67 teeth                      Westgate
Scyliorhinus gilberti            Catshark                                53 Teeth                      Parmley
Sphyrna (sp)                         Hammerhead                        Rare                            Pickering
Squatina (sp)                        Angel shark                            1 tooth                        Westgate
Squatina prima                    Angel Shark                           6 Teeth                       Parmley
Striatolamia macrota         Sand Shark                            1 Tooth                        Parmley

Clearly, Twiggs Clay, Tivola Limestone and Clinchfield Formation represent three distinct environments requiring high sea levels. 
​         
​
​Beneath the Clinchfield Sand at Rich Hill? Huddlestun reports the Gaillard Formation’s kaolin which is at least 68 million years old. 
​So What About the Sharks, the Fish Teeth?
Excellent question.
Shark teeth are notoriously difficult to identify.
​Human adults have 32 teeth which break down into 4 types; incisors, canines, premolars & molars. Each tooth is distinct and has evolved into a certain position in your mouth. We grow one set as children and a second set as adults.  
​Sharks have 50+ teeth depending on the species, and they are constantly losing old teeth and growing new ones. However, each tooth still occupies a certain position in the mouth and is slightly different than the teeth around it. This makes ID difficult even today. 
​The fact that Veatch & Stephenson did not report occurring fish species in Eocene sediments strongly suggests that they simply lacked such information. Reading the 1911 report you notice that at every list of species they report credits whoever identified the specimens.  
​Elsewhere in the 1911 reports Veatch and Stephenson record Cretaceous deposits from West Georgia and the published lists of identified shark species. This shows that they were often relying on the work of local researchers. Different researchers have different specialties, interests, and on-hand research materials. So clearly, Veatch & Stephenson lacked identification information on the fish teeth they reported at Rich Hill.  
 
Today such reference material is available, it’s time a fossil record was created for Rich Hill.  
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​1991 Section Drawing
In 1991 Paul Huddlestun and John Hetrick led a Georgia Geological Society field trip into the Fort Valley plateau and Fall Line Hills area. The researchers explained that their objective was to define and introduce these largely unnamed Middle Eocene, Paleocene & Cretaceous deposits of kaolinitic sands to the geologic public.

Notice that the younger, long named, fossil bearing sediments which had drawn so much interests were of Eocene age, significantly younger than the sediments Huddlestun & Hetrick were focusing on in this study. However, they still produced the best info available on those deposits. 
​They divided the older, newly named deposits into two groups. (6)
  • The Oconee Group is of fluvial (river-related) deposits.
    • The Oconee Group:
      • The Pio Nono Formation (Late Cretaceous)
      • The Gaillard Formation (Late Cretaceous)
      • Huber Formation (Early Paleocene, late Middle Eocene)
    • Fort Valley Group is coastal marine; sea shore.
      • Nakomis Formation (Late Cretaceous)
      • Marshallville Formation (Early Paleocene)
      • Mossy Creek Sand (Middle Eocene, late Claibornian age)
      • Perry Sand (Middle Eocene, late Claibornian age)
Other deposits recognized by Huddlestun and Hetrick included channel deposits in the Fall Line Hills area near the Flint River, Upper Eocene channel deposits east of the Ocmulgee River and “high terrace” fluvial deposits of both the Flint and Ocmulgee Rivers.
They also recognized that they weren't presenting a complete stratigraphic review.  “Rather, our purpose is to lay a lithostratigraphic foundation based on the various codes of stratigraphic nomenclature, upon which further geologic studies and stratigraphic refinements may be made.”      
Drawing & Description of the Section Exposed at Rich Hill,
Stop 2of the 
26th Annual Fieldtrip of the Georgia Geologic Society, Oct 1991
by Huddlestun and Hetrick (6)
Section height; 37.5 meters (123 feet)
​
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Description of the Section Exposed at Rich Hill (6)
 
Barwell Group, Dry Branch Formation, Irwinton Sand Member
Bed 11; (3 meters/10 feet)
  • Sand, residuum; argillaceous (clay bearing), fine to medium grained, well sorted, massive, structureless, moderate reddish brown; gradationally overlies…
Bed 10: (2 meters/7 feet)
  • Sand and clay; Thinly interbedded, fine-grained, well sorted sand with thin interlayers or laminae of Twiggs-like clay, beds essentially horizontal to subhorizontal; deeply weathered.
 
Covered Interval
 
Twiggs Clay Member
Bed 9; (7 meters/23 feet)
  • Clay: calcareous toward base, with thin beds or lenses of fine grained limestone scattered throughout, some calcareous concretions in the lower part; clay is sticky and plastic when wet, well bedded to laminated, with blocky to conchoidal fracture; yellowish gray; grades downward through a thin interval (about 1 foot) of thinly bedded, argillaceous limestone into…
 
Ocala Group; Tivola Limestone
Bed 8; (6.4 meters/21 feet)
  • Limestone; abundantly fossiliferous; medium to coarse textured, uneven-grained due to the abundance of clastic (fragmentary) bryozoan debris; very tough and brittle with irregular, bioclastic fracture; some minor quartz sand in the basal (lowest) 1 foot; rudely bedded with scattered thin beds or ledges of more indurated (hardened) limestone, otherwise massive and structureless in appearance. Aequipecten spillmani (scallop) common, rare Periarchus pileussinensis (sand dollar) and molds of mollusks; very pale orange to pale yellowish-orange; grades abruptly downdip into…  
 
Barnwell Group; Clinchfield Formation
Bed 7; (1.5 meters/5 feet)
  • Sand: very calcareous, some calcitic shell debris with scattered fragments of Periarchus (sand dollars), less calcareous near base of bed; sand fine to medium grained and well sorted: massive and devoid of sedimentary or biogenic structures except at the top of the bed, the upper 1 foot of Bed 7 consists of a ledge of shaley, granular calcarenite or calcarenitic sand suggesting a discontinuity in deposition; separated from underlying bed by a thin (6 inch) calcareous sandstone ledge:
Bed 6; (1.2-1.5 meter/4-5 feet)
  • Sand: calcareous with a discontinuous ledge or series of calcareous concretions in the middle and basal (base) part of the bed, some calcitic shell fragments, especially in the upper part of the bed; sand fine to medium grained and well sorted; separated from the underlying bed by a calcareous sandstone ledge.
Bed 5; (.6 meter/2 feet)
  • Sand; noncalcareous, slightly argillaceous; unconsolidated; medium-grained and moderately well sorted; massive and devoid of sedimentary structure.
  • On the east side of the ravine, the sand that occurs in this stratigraphic position is that of typical weathered, poorly sorted sand of the Riggins Mill Member.
 
Covered interval on west side of ravine; on the east side of the ravine the Clinchfield Sand disconformably overlies…
 
Oconee Group
Gaillard Formation
Bed 4; (6.4 meters/21 feet)
  • Kaolin: silty to finely sandy, micaceous, some dark minerals, massive and structureless, blocky fracture, grades downward into…
Bed 3; (.6 meter/2 feet)
  • Sand; slightly kaolinitic and micaceous; rudely and horizontally stratified; poorly sorted; abruptly overlies…
Bed 2; (1.2 meter/4 feet)
  • Sand; kaolinitic, pebbly; very poorly sorted, generally trough cross bedded; abruptly overlies…
Bed 1; (2.4+ meters/8+ feet)
  • Sand; kaolinitic, somewhat micaceous, some scattered, thin kaolin lenses; sand medium to medium/coarse grained; moderately to moderately poorly sorted; horizontal to lenticular to planar cross bedded on small scale. 
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Does a Rich Hill quarry exist?
In 1947 Harry E. LeGrand, a hydrogeologist with the Georgia Geologic Survey, published excellent research on the ground water resources of the Macon area and reported that the Tivola Limestone of Rich Hill had been quarried. (11) In 1990 John Hetrick also mentions “an abandoned quarry at Rich Hill…” (13) But in a 23/April/2021 phone conversation Paul Huddlestun said no such quarry existed to his knowledge and all the outcrops were natural. 
​Preservation.
So, would it be worthwhile to preserve Rich Hill for its scientific and educational value? Yes, but only if it is properly protected yet available to researchers with permission fr0m landowners. 

It offers valuable lessons in our ever changing Earth and clearly shows our restless coast lines. There are 34+ million year old sand dollar and sea urchin fossils 177 miles inland and 700+feet above modern sea levels. 

Yes, it certainly has scientific, historic, and educational value. Specifically in primary, secondary and advanced educational value, few places in Georgia have a more curious record of climate change. Should field research reveal vertebrate species or tektites this value would increase and nearly demand protection. The site has little commercial value for mining as the deposits are too modest. However, it dramatically shows repeated sea level change and offers a unique glimpse into Georgia’s natural history.

But Rich Hill isn't the only such place in Georgia.

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There was once a town in west Georgia, along the Chattahoochee River, known as Blufftown. It stood atop a high, riverside bluff. Even today the lower 25 feet of that bluff is a massive bed of the 77 million year old, spiral, Exogyra ponderosa oysters.  (See Section 7I of this website for details.)

There's Shell Bluff, rising 150 feet above the Savannah River in East Georgia. It's formed primarily by another bed of uncounted 34 million year old oysters, Crassostrea gigantissama, a giant oyster which reportedly reached 22" in length, and 18" individuals are common. This is the same species Sam Pickering reported from the Clinchfield Formation. The history of ShellBluff goes back to Hernando de Soto's visiting the site in 1540. Then William Bartram, the father of American botany, visited in 1765 and first described the large fossil oysters found there.
(See Section 14K of this website for more details.)   
 
This rich natural history of Georgia is only useful for education if it is accessible to teachers, parents, & students. Currently, such valuable histories are rarely taught in our schools. Many parents object to schools teaching the science that shows a truly ancient Georgia, a truly ancient Earth.

There are 513 million year old fossils in northwest Georgia. (See Section 1 of this website.)

So should state or federal money be spent preserving Georgia's most famous fossil localities? Yes, it should. Eventually Georgia parents will demand that schools teach the science which shows an ever changing, ancient Earth. How can we prepare our children for a warming global climate if we don't show them that this has happened before? ​

​References
  1.  Veatch, Otto; Stephenson, Lloyd, William; Geology of the Coastal Plain of Georgia; Georgia Geologic Survey, Bulletin 26, 1911
  2. Cooke, C. Wythe; Geology of the Coastal Plain of Georgia; United States Department of Interior (Now the USGS), Bulletin 941, 1943
  3. Cooke; Wythe Charles, Shearer; Harold Kurtz; Deposits of Clairborne and Jackson Age, USGS Professional Paper 120-C, 1919
  4. Thurman,Thomas; 14B; Fossils, Impacts & Tektites Dating the Clinchfield Formation - Exploring Georgia's Fossil Record & Our History of Paleontology; GeorgiasFossils.com
  5. Pickering, Sam M. Jr.; Stratigraphy, Paleontology, and Economic Geology of Portions of Perry and Cochran Quadrangle, Georgia; Bulletin 81, Georgia Geologic Survey, 1970
  6. Huddlestun, Paul F & Hetrick, John H.; Stratigraphic Framework of the Fort Valley Plateau and Central Kaolin District, 26th Annual Fieldtrip of the Georgia Geologic Society, Georgia Geological Society Guidebooks, Volume 11, No.1, October 1991
  7. Rainwater E.H.; LaMoreaux, Philip E.; Herrick, S.M. PhD., MacNeil; F. Stearns; Furcron, A. S. PhD.; Southeastern Geological Society, Second Field Trip; November 1944.
  8. Thurman,Thomas; Section 12C; Cynthiacetus; GeorgisFossils.com
  9. Huddlestun, Paul F.; Hetrick, John H.; Upper Eocene Stratigraphy of Central & Eastern Georgia; Georgia Geologic Survey, Bulletin 95, 1986.
  10. Paleo-Data; PDI Paleogene Biostratigraphic Chart – Gulf Basin, USA. Updated March 2o17;  https://www.paleodata.com/chart/
  11. LeGrand, H.E.; Geology and Ground-Water Resources of the Macon Area, Georgia; Prepared by the United States Geological Survey in Cooperation with the Georgia Geological Survey, 1962
  12.  Russell, Dale A.; Rich, Frederick J.; Schneider, Vincent; Lynch-Stieglits, Jean; A Warm Thermal Enclave in the Late Pleistocene of the South-eastern United States. Biological Review, Vol.84, Pgs. 173-202, 2009.