Here is is again for you with primitive mail service :) For those who already got this then I apologize for wasted bandwidth. BS (That's Blue Spring) REPORT This is not a supported project of any organization but an ongoing effort began by a group of "dry cavers" in 1963. The mapping of Blue Spring Cave (A.K.A. Bluespring Caverns) in southern Indiana (at least the underwater parts) has been taken over by Sam Frushour with the apparent cave diving retirement of Steve Maegerlein. The "dry" portions of the cave now has been mapped to approximately 20.4 miles in length (and there is a bit more dry passage to survey). To produce a more complete map and to beat the mapped total of Binkley's Cave (even though those cavers seem to be creating their footage), an effort is underway to survey the submerged portion of the main stream of the cave. The latest effort began last summer when Patti Cummings and I dragged a canoe and my dive gear into the Colglazier Entrance down steep walkways and down the main stream over 800 feet of loose rocks. We paddled 3/4 mile down the stream and I swam an additional 1100 feet on the water's surface. The swim is through sinuous arched passage where the ceiling is about fifteen inches above the water but occasionally dips nearly to the water surface. Sloping soft mudbanks under water are everywhere and waiting to catch fins and gear. I had chosen to use side mount gear and this proved a sound decision as it was easier to carry individual tanks into the cave rather than carrying doubles over slippery mud and loose dinner plate sized rock. On a previous occasion with Robin Fitch I used back mounted doubles with great difficulty and excessive risk of injury while hauling them. On this attempt I found the sumped passage to be ten feet high and 10 to 15 feet wide with a more solid bottom than in the air-filled sections (which have very soft silt and clay). At the beginning of the sump I pushed a 4 foot section of iron pipe into a mudbank leaving one foot and the T fitting on the end for my tie-off.. The visibility was only about 4 feet even though there had been no rain for about 2 weeks and I knew if one waits for good visibility in Indiana then there will be no diving done. At any rate, the current was barely perceptible and the visibility should have been about 8 feet but it was not. Because the surface swim down the cave stream took longer than anticipated I had time to only lay 560 feet of line before turning around and heading back to Patti who was waiting. I had promised to be gone only one hour. At the place where I turned around the passage showed no sign of changing in size and was heading due west. The notched PVC pipes carried for line attachments definitely were needed as there were no natural tie-offs observed and the fine-grain clay sediments that sloped upward hiding the rock walls were scoured with grooves that reflect the high velocity of the stream during floods. The return swim upstream was in less than one foot visibility as it is impossible not to disturb the clay sediments. The long swim back to the canoe was made easier by not having to concern myself with avoiding disturbance of silt and the paddle back upstream was a pleasant one through scenic cave passage. We carried the gear out and uphill to the vehicle with a lot of muttering about how great it would be to have access to the spring outlet of the cave. Then very soon the rains came and I could not get back to carry on the survey. The difficulty of carrying gear into and out of the cave really brought home the need for a better way of doing things and with resolve I again contacted the owner of the spring where the cave empties into the river. This time I had much better luck.. After our initial communication he came down to visit at our commercial operation (Bluespring Caverns) and after being plied with free passes to visit the cave, he at last agreed to allow me to dive on his property at the spring. This would create a whole new approach to mapping the submerged section of the cave and I became determined to keep moving on the mapping effort. Date: 13 September 1998 I enlisted Sue Sharples to help check out the conditions in the spring and so on a pleasant late summer day we parked her van as close to the spring as we could amid a gaggle of fishing shacks built up amazingly high on concrete blocks. The spring has migrated along the river over the millenniums, and in doing so, has left a large alcove with a flood plain only fifteen feet above normal river stage; so the summer fishing shacks there are vulnerable to inundation (and some of them do get flooded annually). Beyond the last shack we rigged a rope to aid clambering down the steep bank of the spring run and observed that the nearby river had deposited a lot of sand in the spring run during unusually high spring flooding. This made it nearly impossible to walk in the run. The nearby mudbanks (slimy mud) were no better so the footing was treacherous carrying heavy gear. Sue had opted for back mounted 95's and I had my own steel 95's but with side mount rig and we both were using TLS350 drysuits. Sue was given the honor of laying a primary line into the spring and she soon disappeared down the narrow canyon under a rock overhang. After a short search she located the line Steve Maegerlein laid in about 1980 on a steel wagon wheel tire and returned to announce the primary was installed and that Steve's line appeared intact at it's initial tie-off 42 feet down. She sent me up the line to check it out; so I dropped down the canyon and at about a depth of 16 feet it widened abruptly; then I encountered the beginning of Steve's line. It was at the bottom of a rocky slope tied to the wagon wheel tire just as he had described. While I swam along in 3 foot visibility Sue followed a few feet behind. The low visibility was probably due to river water being pushed into the cave. I passed a log 250 feet in that is trapped crossways in the passage by the wall and a rock pillar. Easily rotating it I noticed a deep groove completely girdling the log. This is surely due to rotation against a rock projection in strong current. Farther in there were small shreds of sheet plastic caught on the line (probably washed down from our tour cave operation upstream). The line mostly followed the left wall and came up shallow to 5 foot depth at one point about 400 feet in. We found the passage configuration to be a tall canyon about 45 feet high and 8 to 10 feet wide; but even wider at it's bottom near the spring. Every ledge was covered by the lightest silt that billowed from my passing even several feet away and when I turned to retreat at about 700 feet in Sue and I collided as we could not see each other in the disturbed silt until a second before we met. The exit was uneventful and I could sometimes see the dim glow of Sue's 50 watt light ahead. We were happy to find the line intact and made plans to replace it with new knotted line and begin the survey. Date: 4 October 1998 Patti Cummings and I showed up at the spring on a warm day to replace the line left by Steve Maegerlein many years ago and to survey the new line out to the spring. Patti was going to keep an eye on things outside since on the last visit some local juvenile delinquents had stolen and destroyed my prescription sunglasses (we have dumb rednecks in Indiana too). I again rigged a hand line to get down the steep bank of the spring run and fastened a reel for my primary line to rocks near the rock overhang. We carried gear down to the spring and I got into my wet suit; as my TLS350 dry suit needed the neck seal replaced. On this occasion I opted to do the dive in back mounted aluminum double tanks (thus reducing the magnetic affect tanks would have on the compass) and later found the doubles do just fine fitting into the narrow canyon just inside the spring. The wetsuit became a problem; as will be explained later. Just under the water surface I found a suitable rock pinnacle for my secondary line tie-off and headed near vertically down the canyon to Steve's line. The visibility was improved over my previous visit here with rock walls six feet away visible. I fastened the new line beside Steve's and headed south passing the log and feeling some excitement that at last I was going to get some real survey going here. The floor began rising about 600 feet in and the passage gradually turned left. I was forced to follow the floor up steeply along the left wall and found the final tie-off of Steve's line at only 14 feet deep on a large rock projection. The passage ahead was 12 feet high and about as wide and with plenty of line remaining I was ready to strike out into the unknown. The ceiling was at about zero depth; so air would last well.. As I progressed there were numerous sticks and limbs laying about and two small pieces of plywood that surely washed down from the commercial operation upstream. About 400 feet along I was getting colder than I should have and decided to find a tie-off but was unsuccessful and did not have any PVC pipes with me (I surely will not forget them again).. The cold was getting to me enough (damned chilled) that I did not feel it appropriate to survey out; so I reeled up enough line that a tie-off was found on the wall among some small limbs only 50 feet south of the end of Steve's line. So that the swim out would gain some information, I watched the walls closely for side passages but found none, although there were several places where I could not see the wall.. Removal of Steve's line would also have to wait for another day and concluded that he had placed it very well when he was in the cave many years ago. Once outside I found a seam behind my left shoulder had separated allowing cold water into my "semi-dry" wetsuit (bummer). Date: 25 October 1998 It was drizzling rain when Patti and I arrived at the spring. The weather forecast was for several days of intermittent heavy rain; so I figured this would be the last time the cave would be divable until we got a lengthy freeze (unlikely) or the climate dried out next summer. This time I was going back to using a TLS350 dry suit with argon and expected to be toasty warm. Grim memories of the split seam in my wetsuit on the previous visit were still sharp in my head. I was also going to carry plenty of air with back mounted tanks and a stage bottle for an extensive push and mapping. I also had a supply of five notched PVC pipes since the likelihood of finding natural tie-off points was slim. The water level was still low enough to expose the entire rock face and a few feet of cave at the spring. Patti and I carried my gear down the steep bank after rigging a hand line and a conversation with one of the residents of the fishing shacks in which we were told that once a tractor tire was flushed out of the spring during a severe flood. I donned all gear but mask and stage bottle and was hunkered down on my knees in the soft bed of the spring run contemplating the next step in the process of getting underwater when I stretched the mask strap just a bit to test it and it broke behind a buckle. A few unkind words from my lips followed and Patti volunteered to get a spare from her vehicle. The strap was replaced in good time. While descending the narrow canyon at the entrance I went ahead a bit too far and found that I could not fit down the canyon; so I backed up about 10 feet and easily dropped down to the beginning of the line. As I began my survey it immediately became obvious that the stream was already affected by rain and the rising river and visibility was down to three feet or less. I mapped the line installed on the previous visit with no problems and could sketch the walls in some places in the bad visibility. At 793 feet in I was at the end of my line and decided to start a new reel. After only about 60 feet of swimming the visibility went even worse (couldn't see diddly squat); so I reeled back in and headed out. It looked as though the cave would have to wait for a dry spell to make mapping reasonable. Remaining for future investigations are answers to the questions, how far is it to a connection with already mapped portions of the cave and are there any side passages underwater that lead into the sinkhole plain to the south where no cave is now known. With the likelihood of no visibility for awhile it looks like other places will be visited over the winter: Hmmmm...Missouri sounds pretty good and it is only a few hours away. Sam Frushour
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