Saturday, August 28, 2010

An Old Man, a Gorge, and a Cave...



Old Man @ Chesterfield Gorge

Old Man of the Gorge (aka: Old Man in the Rocks). Postcard postmarked 1935



It does happen every so often that I 'connect' with a group of other like minded individuals. On one beautiful late summer day I met local naturalist Aimee Gelinas and others at the Chesterfield Gorge for an examination of its natural history. This is also the location of a marginal profile in the rocks sometimes know as the Old Man of the Gorge. Towards the end of Aimee's program we were treated to a flock of four merganser ducks floating their way down through the gorge on the Westfield River.

Afterwards, going solo, I dove into some remote wilderness to relocate a cave used a couple decades back by a modern day hermit. On my initial visit a few years ago visible signs of his presence remained. On this day it was seen to have been 'refurbished' by more modern day visitors.

Saturday, August 7, 2010

Soapstone


Recently a friend from Gloucester expressed an interest in stone carving mentioning soapstone. I had visited several sites over the years that also included a couple (there are four in Massachusetts) used by Native Americans for pottery. All this rekindled an interest in my second favorite rock soapstone (conglomerate being the first) or its more 'scientific' name: steatite.

Modern day geologic bedrock maps show the existence of bodies of ultramafic rocks mentioning some as talc sites. Historically, they have been labeled as soapstone. These bodies extend roughly along the area of the Berkshire County border with Hampden, Hampshire, and Franklin Counties, and indeed one big old mine has become a habitat for bats.

But on this particular day, I revisited a massive open cut quarry in the southwest portions of Hampshire County. A damp, bug infested old hole it remains much as I remerged it some years ago. Obvious signs of people carving and hammering on the rock exist. But most of what exists as the 'greasy-feeling' rock soapstone is know for, is a crumbly schisty rock.

In the immediate area I investigated a similar mass marked on the geologic map but it looked to be a very small quarrying operation. Any signs of those operations seem obliterated but some minor ledge is exposed in the area.

The trip home brought me by way of the Middle Branch Westfield River where once again the geologic map indicated the presence of ultramafic rock. Although I somewhat confirmed the rocks exist, almost none of it really qualified as talc - or soapstone.

Wednesday, August 4, 2010

On the road ... again!



Indian Cave

Indian Cave entrances

Day One: brought me into Norfolk County by way of the Mass Pike and Rt 495. First destination was an old canal site along the Charles River and an Indian Cave in the immediate vicinity. The origin of this cave seems quite interesting as a softer, almost chalky, lens of rock (sample now being analyzed) in the surrounding bedrock was susceptible to weathering.

Rocky Woods is a name that pops up in local geographical databases every now and then. I dropped farther south to take a look at one such area. I had started working this area a few years back when a written work on the area mentioned a cave in these woods, a House Rock, and a Great Rock. It is primarily within the region of Dighton Conglomerates and many of these 'puddingstone' boulders and outcrops were indeed to be seen in Rocky Woods. Somewhere in the local area is the site of an old postcard called the Playmate, paying homage to a rock that was played upon by someone's Father during his childhood.

But Rocky Woods are an immense piece of territory and any cave would have to be guided to. I saw no such thing. I did see House Rock once again at the farthest reaches of my hike, another large accumulation of conglomerate boulders forming a sort of small Garden of the Gods/Rock City effect. A gargantuan boulder of conglomerate also exists here with a circumference of 103.5 feet!

While in the general area, I decided to drop in on some of my other favorite conglomerate features laying a couple towns away. Abram's Rock, Wildcat Rock, and Lion (or Lion's Head) Rock are some of these. One having petroglyphs upon it's surface.

Day Two: At dawn I made the trip down into Rhode Island to give my kayak its maiden voyage upon the ocean and finally bring it into use as a bona fide piece of research equipment. My original destination was quite busy even at early morning light so I retreat a bit north where an old ferry route provided ocean access to an area where an old report on bird count mentions Swallow Cave. Sailing the coastline where the ocean is in non stop motion proved both interesting and challenging. The conglomerate ledges of the coast offered many fractures, some even where the sea could get behind, but nothing in the way of a true cave. Perhaps the birds nested with the multitude of fissures to be found along the coast.

The rest of the morning was spent visiting old haunts with the hope of once again putting in the kayak. But - not unexpected - this time of year is not good to visit a tourist favorite such as the Newport area. My springtime trips to the region have always offered the better opportunities at getting into the variety of geologic sites along the coast.

Returning to Massachusetts, I decided to hike in to another Rocky Woods, which was a primary destination and research topic for this trip. It is reported to have an abundance of geologic features, the best being one of the many rocky features know as King Philip's Cave. Other notable sites include Devil's Hoofprints, King Philip's Soup Bowl, and the Devil's Bowling Alley. After departing King Philip's, I headed on over to Profile Rock before finishing up the afternoon at one of the two local libraries in Town.



King Philip's Cave

King Philip's Cave

Day Three: Driving through the dark, dawn found me once again returning to the Narragansett Bay in pursuit of another cave lead. Parts of this shoreline had been looked over several times in the past with varying results. Small cave, "quasi-cave" features can be found but I was hopeful of finding a real genuine outstanding sea cave! The kayak was brought in through a narrow access strip to the ocean. Putting in, I began a tour of the coast which eventually landed me in an area of features I had looked at in the past. Some inaccessible from the bluffs above. One I got into several years past by means of a rope. One small cave and one quasi-cave formation existed with a small cove. Turning the boat back around I rounded a corner to be faced with a gaping cave entrance within the cliffs. While circling about the outside, the ocean decided to push me closer then on in. Once beached underground I found the cave to be more substantial than it first appeared from the outside. Total length here, probably 50 to 60 feet.

Retreating to a local wifi site I relaxed over coffee catching up on more mundane matters. Eventually hitting the road, I returned to Massachusetts and the library I had waited to open since arriving in Bristol County. Gleaning all that I could from sources there I mad a quick spin out to Joe's Rock, another historical site of human habitation often mentioned as a cave but just some heavily fractured and split rock outcropping. Then returning past the library I scouted the outside perimeter of Rocky Woods for a couple features I learned of during my recent library visit. Finishing off an early day I connected again with Bob, a local antique dealer who has been a valuable source of information over the years on the immediate area.



Sea cave along the Narragansett Bay, RI

Sea cave along the Narragansett Bay


Day Four: was left during the planning stage as an optional day. Sleeping in to 5 am made it too late to avoid the early morning crowds down at the Rhode Island beaches. Besides: the oppressive summer heat was already making its return. So I decided to take one more early morning walk through Rocky Woods to familiarize myself a bit more with its path system. Then with it already 75 degrees by 7 am, I turned the car homeward.

Sunday, June 27, 2010

Pulpit Rock, Onota Lake, Pittsfield


Pulpit Rock @ Onota Lake

Pulpit Rock - early 1900's


This rock has been worked on several past occasions but with the securing of a 'new' postcard, I gave it a go once again on one sticky, gray, summer afternoon.

By comparing the newer image to other images of the Lake, it seems confirmed that the site was on the south side of Onota. Much of this is now in private hands and been well developed including boat docks.

Although Pulpit Rock still did not present itself on this adventure, I'll be bringing the kayak out on the lake for a final determination. Presently: I suspect it to be gone!

Wednesday, June 2, 2010

Vacation has once again arrived. Unfortunately of the hot, humid type during which I generally limit my outdoor activities. But with that said onward I trekked into the great wide open...

Previous to embarking on what was to be primarily a south Worcester County adventure, a local history on one of the Quabbin Reservoir towns came to light, and it furnished enough information - and incentive - to begin my wanderings there.


The old stone trough

The old stone water trough


Day One: Entering the region just to the east of Quabbin, from the north, I began my search by looking for an old historic spring in Peter Gore's Spring. An issuance of water from the forest floor seemed to be the likely location for this geographic feature.

An underground spring was up next and it proved to be a site I once visited in the past. Some have this on an inventory as a stone chamber and indeed its construction is along those lines.

Bell Rock was revisited after a number of years as it was in the vicinity of some reported caves. Not much was seen for caves other than a small, insignificant overhang on ledge. However, it may be worthwhile to pursue a more expanded search of the area.

Near the center of town, history reported a "huge boulder" marking the "exact geographical center of town". One boulder seems to fit the location.

On an abandoned section of roadway running through the woods, a stone watering trough was located.

Farther into the wilds lay the Lion's Den, a geologic feature comprised of a ledge and natural arch of rock separated from the main face by several feet. One can enter this space between rocks through an opening in the base of the arch.

An extensive search for the Indian's Cave followed but nothing definitive was brought to light. It apparently was a boulder that lay against a ledge. Many ledges were seen in the area where history recorded its location but none had the boulder described. Could it be the boulder has rolled away downhill?

A rocking stone or "Teeter Rock" was also said to exist in this same section of town, but again, this did not show itself.

Before heading southeastward to camp, a quick jump into the woods was made to search for another Devil's Den. Amongst the relentless onslaught of mosquitoes and deer flies, a fast walk-through the forest turned up a nice set of ledges honeycombed with small caves. A more extensive investigation was left for better days.




Ledge quarried for slate. Circa: 1870s


Day Two: After a night of heavy thunderstorms, the air was thicker with humidity than the previous day. But on up into the land of Brookfields was my destination. I had been here the previous year in an unsuccessful search for an Indian shelter cave that was home to the last of the Quaboag Indians. On this quest - I was more triumphal locating the rocky ledge and nearby features of a well and chimney leftover from the days of a previous landowner.

One town to the east, investigation was made of an old postcard known simply as "ledges". My suspicions were these ledges may have been part of an old slate quarrying operation and that proved to be true. I quickly looked for a stone chamber in town but since entry lay through the parking lot of a (opened) business, I deferred on this one to a later date. Next I killed a couple of productive hours (out of the heat) in the local library where sifting through their records obtained information on the slate quarry, another stone chamber, and a balancing rock.

Retreating to the south, I ended not far from the Connecticut border, trying to outrace the coming rain. I located my site in Dennison Rock just as the heavens opened up and a friendly neighbor invited me in to stay dry. A while later, the rain abated enough for me to venture out for photographs. Just enough - as a night of constant rain began on the drive back to camp.

Day Three: Juggling the possibilities of what to do before returning home, I faced another day of intense heat and humidity. So I opted for the casual, somewhat leisurely option, of working my way back through the Quabbin Reservoir region.

Pulling in to the Rock House Reservation, I remembered an old record of glacial scratches on a rock across from it's entrance. This happened to be a large, heavily fractured, glacial boulder that caught my attention on each previous pass through the area. There are some indications of glacial movement across this rock but I would not say they are significant. Of greater interest, I found a nice talus cave in the broken rock alongside the rock outcrop.

Closer to Quabbin, I stopped only briefly to look for two sites from old postcards: a stone drinking fountain and "Reflection Rocks", a pastoral scene of rocks within a river. Neither were located.

Next stop was to look at the progress of East Quabbin Land Trust's project at Indian Rock before once again taking on heat and bugs in an unsuccessful attempt to located the site of an historical reference to a natural bridge within the Quabbin woodlands.

Finishing up, I passed by the 'center of town boulder' seen two days previous for a couple of quick photos. Then it was all but to head back over the northern end of Quabbin to pick up the Mohawk Trail on my way back to the Berkshires.


Rock House; early 1900's postcard

Early 1900s postcard: The Rock House

Monday, May 24, 2010

The Mighty Connecticut


After paddling around local lakes for the past several weeks it was time kick up the learning curve and take on a river - the mighty Connecticut. My main objective was to scout the mid portion of the River in Massachusetts for access points, but I also hoped to work some of my more normal geologic investigations into the mix.

Internet sources mentioned a state owned 'beach' area on the Connecticut's east side so I took that up first. Most of morning was spent trying to locate the site in vain. I talked with two local people, drove to the top of Mount Holyoke looking for DCR (state) employees all without success. The feeling here is it my be an isolated parcel of land and only accessible by water but I will be looking into that further.

Meanwhile back over on the other - west - side of the river the journey took me as far south as the Dinosaur Footprint Park in Holyok. The dino park does offer an expansive view of the river with several rocky ledge outcrops on the river's opposite bank. Somewhere a bit north lies a future watery destination in Titan's Pier, an outcrop lying along side the water.

After briefly looking over an access point at the Oxbow, it was decided to head north for a quieter portion of the river at Sunderland. First order of business was to check some 'non formal' areas of river access and try to verify the exact location of reported riverside rock ledge. After locating the ledge (indeed walking over the top of it) I decided to head downstream to the formal, legitimate access point in town to put in my kayak.

Paddling north - and upstream - presented no real difficulties initially. I landed at the first of the two islands that would be passed, then continued upstream to located the ledge lying along the river opposite island #2. The area between island and shore proved to be a major challange with heavy currents, eddies, and even the occasional whirlpool. But upon making the ledge, a couple quick photos were shot before turning around to ride the current back south. From there it was all but to pack up and head on back over to the Berkshires.

Sunday, May 9, 2010

Since my return from Rhode Island less than three weeks ago several things have been happening. I finally received my long awaited kayak and have been familiarizing myself with its use. One adventure took me down pass the backside of old quarry buildings used in the refining of limestone located on Cheshire Reservoir. Another - out to several islands.

You might ask, what that has to do with geology - or even history. However, I have become increasing aware that certain sites are best - or only accessible from water. Certainly this all plays in to my searching out sea formed caves. And I am reminded of a certain cave report in western Massachusetts that was located on a island. In this instance, a buddy and his canoe were able to paddle me out to my destination although the 'cave' was more of just a rocky formation. So a new activity to keep me going during those hot humid days I don't wish to be in the woods.

Old Berkshire Park, once located just to the east of the southern end of the Ashuwillticook Rail Trail, often appears on old postcards. After a long absence from this picturesque trail I returned one cold, brisk Mother's Day morning to investigate one site visible on one of those old postcards. I also reexamined part of a long ago abandoned road that ran out across the rail trail and entered southern Berkshire Village. This in the days before a Route 8 (approximating the old trolley route) existed from near the present day Berkshire Mall north to the Berkshire Village area.


Island 'cave'- late 1990's