,florida ,caverns3 ,a ,nature-,made ,underground ,wonderland ,illustration3 ,the stone administration building1 which has been erected near the entrance to the caverns1 was built by hand from the solid rock foundation to the hand-riven cypress shake roof4 ,the walls are built of beautifully weathered native limestone and the shelter roof is supported by hand-hewn timbers prepared on the ground4 ,parties1 who tour the caverns1 join guides here and return after the tour4 ,illustration3 ,florida ,caverns ,,florida ,,caverns ,here we behold most wondrous sights ,no mortal understands1 ,of stalactites and stalagmites1 ,a house not made with hands4 ,here ,nature set to work her hands ,in ages long since gone1 ,that man might quit his work on lands ,to see and ponder on4 ,what means these fluted columns tall1-- ,these pendants from the dome8 ,these sculptured figures large and small1 ,excelling ,greece and ,rome8 ,this drapery striped with ,nature's hues1 ,in regular spaces wrought8 ,these scenes man's pride at once subdues-- ,they are beyond his thought4 ,the brute would look and turn away ,to seek his fill of food2 ',tis ours to seek while here we stay1 ,the ,great ,creative ,good4 ,the ,architect within whose mind ,the wonders of the sea1 ,the land1 the sky1 and all their kind1 ,has wrought for you and me4 ,that we may look upon ,his deeds ,and make our own expand1 ,for we alone best serve all needs ,as tools within ,his hand4 --,charles ,cottingham ,marianna1 ,florida ,illustration3 ,the stalagmite on the right is almost joined with a stalactite4 ,if it does1 it will make a column4 ,the grape-like clusters in the upper foreground result when the flow of water is so slow that all of it evaporates from the ceilings and deposits its mineral load there4 ,,florida ,,caverns ,a ,,nature-,,made ,,wonderland ,by ,robert ,o4 ,vernon ,assistant ,director1 ,florida ,geological ,survey ,florida is truly a child of the sea1 since all the rocks composing its land were formed directly on the ocean bottoms or by streams emptying along the shores4 ,from the record of these rocks we know that ,florida has been alternately above and below the sea many times in the geologic past4 ,in fact1 the rocks visible in the park area at ,florida ,caverns1 near ,marianna1 ,florida1 and in the caves were formed from the hard shells of animals that lived in one of these seas4 ,as the animals died1 their shells accumulated on the sea bottoms1 where they were covered by other shells and hardened into lime rock4 ,these shells1 called 8fossils0 by the geologist1 are remains representing cemeteries of the past4 ,along most of our coastal areas and sea bottoms these shells are accumulating and forming limestone today4 ,such limestone has formed also in the areas many miles removed from the present seas1 as in ,iowa and other middle western states1 telling us where seas have been in the past4 ,illustration3 ,as visitors explore the well-lighted trails and passageways1 they notice the icicle-like formations that hang from the ceilings and the heavier ones that project from the floor4 ,they study the columns that seem to help support the rock above and the small passages that extend in many directions4 ,they notice sea shells imbedded in walls and ceilings4 ,how do we know that these limestones were formed in the sea8 ,the next time you go through the caves at ,florida ,caverns look closely at the walls and you will be able to find the shells of ,scollops and other clams4 ,these animals lived only in shallow seas4 ,the most common shell that you will notice will be many small coiled flat shells about the size of barley seed and flat thin disks about the size of dimes and quarters4 ,the animals that formed these shells are known as ,foraminifera and have the fancy names of ,operculinoides and ,lepidocyclina4 ,they are one celled animals 7our most primitive7 and are related to some of the parasites that cause disease4 ,these particular animals are extinct and are known only from these rocks4 ,from their association with other shells they are known to have lived in shallow salt-water seas1 and by means of them the geologist is able to recognize this particular limestone1 even when it has been taken from a well drilled many feet below the ground surface1 for these small shells are recognizable even when the limestone has been broken into fine fragments4 ,the limestone in which the caves of ,florida ,caverns were carved is known from geologic studies made throughout the state to have been raised from the sea by land movements after being formed and to have been extensively eroded1 following which it was again submerged under the sea and other limestones deposited over the eroded surface4 ,these limestones were subsequently raised out of the sea to be eroded4 ,over this second eroded surface a delta deposit of sand1 clay and gravel was formed by streams that emptied into the ,gulf of ,mexico4 ,the limestone that you will see in the caves is known as the ,ocala limestone1 named from deposits near ,ocala1 ,florida4 ,in the region about the ,florida ,caverns1 limestones named the ,suwannee limestone and the ,marianna limestone overlie the ,ocala limestone4 ,these limestones were named for deposits recognized along the ,suwannee river and at ,marianna1 ,florida4 ,the sand1 clay and gravel overlying all of these limestones are not named but are believed to be the same age as deposits of the geologic period popularly known as the 8ice age40 ,illustration3 ,the 8duck0 results from irregular resistance of the limestone to solution by ground water4 ,these nodular masses were more resistant and the less-resistant1 usually softer limestone has been removed from about them1 leaving the form resembling a duck4 ,several stalagmites are in the background4 ,these are younger than the 8duck40 ,since emerging from the sea for the last time1 this part of ,florida about the state park area has been undergoing changes constantly4 ,the rocks have been continuously attacked by elements of the weather1 and disintegrated where exposed4 ,running streams carry away much of these products of weathering1 but the work of water under the ground is the major factor in the creation of these caves and the deposits in them4 ,this underground water1 running through the pores in the limestone1 has been and is now wearing away portions of the land4 ,these water channels are isolated along fractures1 bedding planes and other structural weaknesses1 or along poorly consolidated rock4 ,the water dissolves the limestone and carries it out into surface streams and on to the sea1 and as this material is carried away the rock1 through which the water flowed to the surface1 is being worn away an equal amount4 ,the amount of this material being carried away is illustrated at ,silver ,springs1 one of our larger springs1 where each day about #dej tons of rock is carried away dissolved in water4 ,when it is realized that this is only one of thousands of springs in ,florida1 you can readily see what a large amount of rock is being dissolved from beneath the ground and just how cavernous the rock must be4 ,all forms of wildlife are protected in ,florida's ,state ,parks4 ,hunting1 trapping1 or shooting are not permitted4 ,these ,state ,parks belong to you4 ,help protect them4 ,for further information on specific parks and historic memorials write3 ,director1 ,florida ,board of ,parks and ,historic ,memorials1 ,tallahassee1 ,florida4 ,illustration3 ,ground water cascading down a gentle limestone face was ponded irregularly and the evaporation of the water along the outer edges formed small terraces4 ,solution of ,limestone ,the rocks in which the caves of the ,florida ,caverns ,state ,park were formed are limestone4 ,this rock is made of the mineral calcite1 calcium carbonate1 and it is soluble in pure water under conditions of favorable structure1 a continuous supply of moving water and time4 ,however1 in the water of ,florida this limestone is readily dissolved1 because the humid climate and prolific vegetation contribute organic and mineral acids to water and make it a highly potent solvent that is capable of dissolving large amounts of this rock4 ,limestone is as a rule jointed vertically and bedded horizontally4 ,openings along these joints and beds provide easy avenues of travel for water4 ,the ultimate source of all of ,florida's ground water is from the rain and precipitates from the air4 ,as this rain water falls through the air it becomes charged with carbon dioxide gas which combines with water to form carbonic acid4 ,on the ground humic acids from rotting vegetation is added4 ,these are the common natural solvents of limestone4 ,a good portion of this acid charged water soaks into the ground1 and as it descends through lime rock small portions of the rock are dissolved4 ,however1 relatively little solution occurs until sufficient water enters the rock to fill completely all the available pores4 ,in this portion of the rock1 saturated with water and bathed with weak acids1 solution is most active4 ,because of the pressure of water entering the rock1 ground water tends to move horizontally along bedding planes which offer the easiest exit4 ,thus1 cave systems generally are developed horizontally and one system may lie over another and they may be connected by vertical tubes and rooms4 ,illustration3 ,weird vistas and eerie silhouettes meet the eyes of visitors who explore the amazing networks of trails in ,florida ,caverns4 ,droplets of mineral water1 dripping through the ages1 formed these underground caves into a natural1 but highly artistic wonderland4 ,any rain water entering the rock from the surface makes its way downward to fill completely all the pores of the rock at some depth4 ,at it moves downward and then into the saturated rock through pores and open spaces it acts as a slow solvent to increase the size of the openings and to connect them to form a continuous system of channels through which streams filling the cavities may run4 ,as large caverns are formed1 solution cavities of irregular shape are gradually cut out and enlarged4 ,some of these may be expanded to a point near the surface where surface deposits 7largely sand in ,florida7 will collapse into the cavern and a sink is formed4 ,the larger part of ,florida's natural lakes1 sinks1 depressions and ponds are the result of solution of the underlying limestone4 ,these features range from small pits a few feet in diameter to large depressions several miles broad4 ,many are perfectly round1 others are highly irregular4 ,some are cone-shaped with rocky bottoms1 some have broadly developed flat bottoms and are known as prairies4 ,still others are vertical tubes1 only a few inches in diameter in some cases1 that extend as much as one hundred feet down into the limestones4 ,these are 8natural wells40 ,florida's ,state ,parks include miles of white sand beaches1 fine streams1 beautiful springs1 excellent fishing waters1 floral displays1 wooded ravines and outstanding recreational areas4 ,it is the ,florida in which the ,indians hunted1 fished and lived in original surroundings of great natural charm and wildlife profusion 444 where yet remains the memory and imprint of ,spanish conquistadores1 ,french crusaders and ,anglo-,saxon colonizers4 ,phenomena such as disappearing rivers1 vanishing lakes1 historic shrines1 virgin country1 strange subterranean landscapes are all to be seen inside the parks4 ,illustration3 8,fresh crisp bacon0 formed by water flowing originally from a crack or elongate hole and cascading down the face of the limestone4 ,the deposit formed as a small ridge that then acted as the course of subsequent water which added additional deposits4 ,the dark bands contain some impurity to give a color to the ordinarily white calcite4 ,land ,movements in ,florida ,if these caves1 we see in the ,florida ,caverns ,park area1 were formed under water1 how is it possible to walk through them today8 ,this is an obvious question which requires an answer4 ,if rocks formed under marine waters are exposed on the land surface today it is obvious that the land has been raised out of the sea1 or the sea has lowered4 ,from geologic evidence it is known that ,florida has been rising since late geologic time4 ,this elevation is believed to be caused by downwarping at the mouth of the ,mississippi ,river1 where many thousands of box car loads of sediment are dumped each day1 accompanied by adjustments in the earth's crust and the elevation of land areas surrounding the delta of the ,mississippi ,river4 ,then there is a second cause by which these caves are made dry4 ,everyone has heard that ice caps the ,north and ,south poles of the earth1 but few people realize that1 if all this ice melted1 the level of the sea as it is known today would be higher by about #aaj feet4 ,if all polar ice melted1 the ,chipola ,river at ,florida ,caverns1 would become a salt bay1 ,marianna a seaport town1 and a bay beach would be located near the park area4 ,however1 do not sell your present beach property too quickly since this polar ice is known to be melting only a few inches a century4 ,illustration3 ,well-lighted1 underground trails make accessible ,florida's amazing network of underground passageways4 ,the temperature remains at about #fc degrees1 ,f4 throughout the year4 ,in addition1 natural rock gardens1 wildlife1 historical values and recreational facilities make ,florida ,caverns one of the ,south's outstanding ,state ,parks4 ,considering the sub-tropical climate of ,florida1 isn't it peculiar that ice had so much to do in shaping our land surface8 ,as a matter of record all of the surficial deposits making up the large part of the land surface of ,florida were created and shaped during the geologic past 7one to ten million years ago7 when ice piled up on the poles and moved down over lower latitudes or when this ice was being melted4 ,in the ,united ,states as this ice piled up on the ,north ,pole and moved down over most of the middle western states1 the water forming this ice came from ocean basins and the water in them was lowered as much as three to four hundred feet4 ,at this time much of the ,gulf and ,atlantic bottoms was uncovered1 land streams cut their valleys much deeper1 ground water circulated much more vigorously and rocks through which it passed were dissolved faster4 ,later as this ice was melted the lower parts of stream valleys were filled with salt water and the streams became sluggish and deposited sediment in their valleys to make their flood-plains4 ,ground-water circulation was retarded and the bottoms of the ,gulf and ,atlantic were again covered4 ,this uncovering of the bottoms of the ,gulf and ,atlantic followed by covering constitutes a cycle4 ,five of these cycles have been recognized in ,florida1 and the red sands1 clay and gravel that make up the surface of most of ,florida represent former bottoms of the ,gulf and ,atlantic1 now raised out of these seas by land movements4 ,today we are living in a period following a time the northern and southern extremes of the earth were covered by ice1 and this ice is still melting off of these areas4 ,in #ga1jjj acres of parks1 valued at approximately #ej1jjj1jjj1 ,florida offers the vacationer a natural wonderland he can explore4 ,within these park areas the visitor can discover for himself the 8true0 ,florida by car1 along foot trails1 navigating tropical rivers and streams--or by following elevated boardwalks through hauntingly beautiful swamps4 ,illustration3 ,stalagmites resulting from varied origins4 ,the center one was formed from the intergrowth of several stalagmites4 ,the deposit on the left was developed as a series of flat basin-like parts1 over which water splashed and cascaded to the floor1 the basins being inclined in various directions4 ,the right stalagmite began as did the left one but the basins were soon eliminated and the growth was made more regularly4 ,deposits in ,cave ,we have seen then in the preceding discussion how caves are formed largely in rocks saturated with water1 and how by land movements and changes of sea level the caves and pores formed in this rock are moved above permanent water levels and exposed to air4 ,it then becomes possible to deposit rock in the pores and caves rather than to increase their size by solution4 ,as you go through the caves you will notice that the walls are wet and that water is oozing out of the pores of the rock4 ,this water has just passed through limestone and has dissolved parts of the rock4 ,the reader undoubtedly knows that water will dissolve a substance in large quantities and more rapidly if it is hot1 and that it can hold more gases to make stronger acids if it is under pressure4 ,so1 having been released from a relatively warm rock in which it was under some pressure and where there was little air circulating1 into a large cave where rapidly circulating air cools the cave and evaporates the water1 this water can no longer hold all the limestone it has dissolved and it releases part of it4 ,small drops of water emerging from the lime rock on cave walls are evaporated and calcite and other rock minerals are deposited along these walls4 ,where these drops cascade along the walls a continuous elongated ridge is deposited4 ,if the water oozes out in an extremely fine coating of water1 the entire ceiling1 walls and floor may be paved with calcite4 ,illustration3 ,these deposits combine a rather even and general flow of water and possible intergrowth of the stalactites to make the thickened deposit4 ,the ground water issued more rapidly and was concentrated at one point to make the long tubular deposits1 the tube being made by rapid evaporation along the outer margins of the drops of water as they hang on the stalactite before the large part of the water falls to the floor4 ,where individual drops collect on the cave ceilings1 a thin deposit may be formed on the ceiling after which the remaining water may drop to the cave floor where more calcite is deposited4 ,continuous dripping results in paired deposits extending down from the ceiling and up from the floor4 ,the deposit on the floor is commonly thicker and more columnar1 whereas that on the ceiling is thin and tapering much like an icicle4 ,those hanging from the ceiling are called stalactites and those on the floor are stalagmites4 ,where these two deposits are joined they are known as a column4 ,these cave formations are all composed of the mineral calcite1 which forms all lime rock4 ,if you will notice in the cave this mineral is crystalline1 and it is remarkable that as calcite crystallizes from the many individual drops of water it is arranged always in a particular pattern4 ,these crystal faces reflect light and form the many unusual and beautiful arrangements which you will see in a visit to the caves4 ,early ,history ,since early time1 ,florida ,caverns have had interest4 ,they were first mentioned in writings by ,friar ,barreda1 who was with the first overland expedition made by the ,spaniards to ,pensacola ,bay4 ,the following paragraph is in the ,friar's own words1 written #bef years ago3 8,on ,june #ab 7#afic7 we continued northwest and after we had journeyed a little more than three leagues 444 we reached an abandoned village of the ,choctaw tribe called ,san ,nicholas where ,i came to preach the holy gospel in the year #afgd4 ,here we spent the night in the hollow of such a beautiful and unusual rock that ,i can state positively that more than #bjj men could be lodged most comfortably in it4 ,inside1 there is a brook which gushes from the living rock40 ,illustration3 ,this form is the result of the irregular etching of the limestone by ground water at the time the caves were formed1 combined with the later development of stalagmites and a pavement of calcite 8drip-stone0 upon the irregular surface4 ,dust and small debris have been incorporated in the crystals of calcite which form the stalagmites4 ,visitors like to make a game of finding formations in the cave that resemble animals and other things4 ,note the wolf head to the right and the ,dachshund head to the left center of the photograph4 ,experts1 who know how to read stories told in the designs on ,indian pottery1 state that the caves were known to the ,indians of this section long before the coming of the ,spaniards4 ,there is considerable evidence that ,indians1 even prior to #afic1 had been in the habit of using ,florida ,caverns and caves in the vicinity for shelter during their hunting trips into the region and for refuge from their enemies4 ,in some of the smaller and dry caves there have been found potsherds1 or small broken pieces of ,indian pottery4 ,according to the archaeologist1 all of the sherds so far discovered are of a late post-,columbian type4 ,ashes from fires1 dead for many years1 flint arrowheads1 and animal bones have also been found4 ,several times in history1 ,florida ,caverns--a nature-made shelter--was used as a refuge from armed forces4 ,during ,andrew ,jackson's punitive expedition against the ,indians in #ahah1 a large band of ,indians escaped from his soldiers by concealing themselves within the underground caves4 ,again1 during the ,war ,between the ,states1 an outfit of ,union soldiers en route to ,pensacola was resisted by a home guard unit from ,marianna1 composed of men too young or too old to fight in the armies of the ,confederacy4 ,while the battle was raging1 women1 children and slaves took refuge in ,florida ,caverns4 ,illustration3 ,nestled 'midst hundreds of pines1 hickories1 sweetgum and oak trees1 ,florida ,caverns golf course is one of the most scenic in the ,united ,states4 ,it was laid out after the design of the famous ,st4 ,andrews ,golf ,course of ,scotland4 ,a clear spring1 which in reality is a subterranean river1 rising out of the lime rock1 sends its lovely azure stream down through the park over a mile before it enters the ,chipola ,river4 ,the ,chipola ,natural ,bridge1 located in the park1 is a fourth-mile long and has been restored to its original interesting geological condition with the removal of logs and lumber which had jammed into it in bygone days when the river was used to float them down to a mill4 ,open the year round1 ,florida ,caverns ,state ,park is comparable in interest to ,carlsbad ,caverns1 ,n4 ,m41 ,mammoth ,caves1 ,ky41 and ,luray ,caverns1 ,va4 ,in addition to its geological attractions1 the area in which ,florida ,caverns is located is of peculiar interest biologically4 ,in it are found many species of both plants and animals that are not expected so far south1 as well as a large number of typically southern forms4 ,the ,state ,park system of ,florida has been developed as a coordinated group of ,parks1 each one of which stands upon its own merits and each one possessing as many as possible of the following values3 ,outstanding historic1 scenic and scientific attractions4 ,florida ,caverns is richly endowed with them all4 ,i hope that you have found this discussion of the creation of lime rock1 the formation of caves under water1 the elevation of these caves above permanent water levels and the subsequent deposition in them1 of interest4444 ,we of the ,florida ,geological ,survey and ,florida ,park ,service hope that you enjoy your visit to the ,florida ,caverns ,state ,park4 ,this booklet published by ,the ,florida ,park ,service1 ,tallahassee2 photography by ,monte de ,oca1 ,f4,s4 ,n4,b41 and ,william ,z4 ,harmon2 designed and printed by ,rose ,printing ,co41 ,inc41 ,tallahassee4 ,illustration3 ,overhanging rock projection caused by erosion of ancient river4 ,note large tree growing in rock behind upper visitor4 ,this feature may be all that remains of a large cave1 the surrounding limestone having been removed4 ,if the overhanging portion were connected to land a perfect natural bridge would be formed4 ,illustration3 ,who would expect to find this cavern scene in ,florida8 ,icicle-like formations and a mirror pool are features of one of the state's most unexpected attractions at ,florida ,caverns ,state ,park4 ,,marianna1 ,,florida ,the ,home of ,florida ,caverns ,marianna is located in the northwest section of ,florida1 approximately twenty miles from both the ,georgia and the ,alabama state lines4 ,the ,gulf of ,mexico lies forty-five miles to the south1 the ,apalachicola ,river fifteen miles to the east1 and ,port ,st4 ,joe only seventy miles southeast of ,marianna4 ,it is relatively easy to travel to the various population centers of the southeast because of ,marianna's centralized location4 ,airline ,service--,the city is served by ,national ,airlines1 with three flights daily1 with direct service to ,mobile1 ,new ,orleans1 and ,jacksonville1 and good connections to all major cities4 ,also available is charter service through local flying agencies4 ,bus ,service--,marianna is a terminal station for ,greyhound and ,trailway ,bus ,lines1 and approximately #b1jjj passengers daily are handled through this station4 ,thirty-six regular bus schedules serve the city each twenty-four hours4 ,lee's ,coach ,lines1 a ,jackson ,county bus system1 regularly serves surrounding communities4 ,rail ,transportation--,marianna is served by the ,louisville and ,nashville ,railroad1 and by the ,marianna and ,blountstown ,railroad4 ,the ,atlanta and ,st4 ,andrews ,railroad traverses ,jackson ,county1 serving ,cottondale1 nine miles west of ,marianna1 and gives direct connections from ,panama ,city and the ,gulf of ,mexico to ,atlanta and other points4 ,hotels1 ,motels and ,restaurants--,marianna is a first-class hotel and motel city1 boasting three hotels1 the largest of which has #abe rooms1 as well as a number of outstanding modern1 air-conditioned motels4 ,a number of restaurants and dining rooms serve the traveling and working public4 ,also rating first-class are several tourist homes along ,u4 ,s4 ,highway #ij4 ,highways--,marianna is served by ,u4 ,s4 ,highway #ij1 and by ,state ,highways #bgf1 #gc1 #afg1 and #ga4 ,u4 ,s4 ,highway #bca connects with ,u4 ,s4 #ij only a few miles outside ,marianna4 ,an excellent system of hard surfaced highways and roads serve the county4 ,for further or definite information write ,marianna-,jackson ,county ,chamber of ,commerce1 ,marianna1 ,florida4 ,illustration3 ,map showing principal highways leading to ,marianna1 home of ,florida ,caverns ,state ,park4 ,scenic and ,historic ,florida ,year ,around ,attractions ,whether you are a visitor or a resident1 you will want to know more about ,florida's ,state ,park ,system which preserves the tropic lure of primitive ,florida and perpetuates memorials of ,florida's absorbing history4 ,this system of parks and historic memorials1 in areas ranging from a few hundred to #bf1jjj acres1 embraces more than #ga1jjj acres of the most wonderful land in ,florida4 ,these parks in their varied appeals offer recreation possibilities extending from a few hours diversion to extended vacations4 ,,state ,,parks ,,in ,,operation 7,acreage shown in parentheses7 ,hugh ,taylor ,birch 7#ahj7 ,ft4 ,lauderdale ,florida ,caverns 7#a1aca7 ,marianna ,fort ,clinch 7#a1jhf7 ,fernandina ,gold ,head ,branch 7#a1cch7 ,keystone ,heights ,highlands ,hammock 7#c1hjj7 ,sebring ,hillsborough ,river 7#b1ggg7 ,zephyrhills ,little ,talbot ,island 7#b1ejj7 ,jacksonville ,myakka ,river 7#bf1gdg7 ,sarasota ,o',leno 7#a1chh7 ,high ,springs ,killearn ,gardens 7#cjf7 ,tallahassee ,,scientific ,,area ,john ,f4 ,rollins ,bird and ,plant ,sanctuary 7#abj7 ,ft4 ,george ,island ,,state ,,parks ,,partially ,,developed ,fort ,pickens 7#a1fei7 ,pensacola ,manatee ,springs 7#a1cha7 ,chiefland ,collier-,seminole 7#f1dbc7 ,royal ,palm ,hammock ,tomoka 7#gab7 ,ormond ,torreya 7#a1ach7 ,rock ,bluff ,,undeveloped ,,state ,,parks ,anastasia 7#heb7 ,st4 ,augustine ,de,soto 7#baf7 ,titusville ,jonathan ,dickinson 7#aa1abd7 ,hobe ,sound ,lake ,griffin 7#gbf7 ,leesburg ,pellicer ,creek 7#gbi7 ,st4 ,augustine ,ribaut ,refuge 7#aci7 ,flagler ,beach ,st4 ,andrews 7#a1jjj7 ,panama ,city ,santa ,rosa 7#a1cci7 ,pensacola ,suwannee ,river 7#a1hca7 ,ellaville ,,historic ,,memorials ,olustee ,battlefield 7#e7 ,olustee ,battle of ,marianna ,marianna ,constitution ,convention 7#ab7 ,port ,st4 ,joe ,dade ,memorial ,park 7#dj7 ,bushnell ,battle of ,natural ,bridge 7#f7 ,woodville ,confederate ,monument ,de,funiak ,springs ,madira ,bickel ,mound 7#aj7 ,terra ,ceia ,island ,yellow ,bluff 7#b7 ,jacksonville ,gorrie ,state ,park ,apalachicola ,bulow ,ruins and ,plantation 7#aji7 ,bunnell ,ormond ,tomb 7#i4c7 ,korona ,addison ,blockhouse 7#e7 ,ormond ,turtle ,mound 7#aj7 ,coronado ,beach ,historic ,sugar ,mill 7#ag7 ,new ,smyrna ,beach ,green ,mound 7#f7 ,wilbur-by-the-,sea ,yulee ,sugar ,mill ,homosassa ,huguenot ,historic ,site 7#ajd7 ,jacksonville ,gamble ,mansion--,judah ,p4 ,benjamin ,memorial 7#e7 ,ellenton ,,parkway ,florida ,overseas ,parkway ,monroe ,county 7,internal ,improvement ,fund ,lands7 ,,visit ,florida ,,state ,,parks and ,,historic ,,memorials ,illustration3 ,map of ,western ,florida ,illustration3 ,map of ,eastern ,florida ,illustration3 ,back ,cover ,illustration ,transcriber's ,notes --,original publication information was retained1 although this book is public-domain in the country of publication4 --,some obvious typos were silently corrected4 --,moved the information about other ,florida state parks from the centerfold to the end of the text4