Leader for today’s
Ramble:
Linda
Authors
of today’s Ramble report: Linda
and Don. Comments,
edits, and suggestions for the report can be sent to Linda at Lchafin (at) uga.edu.
Fungi and lichen identifications:
Don
All the photos that appear in this report,
unless otherwise credited, were taken by Don Hunter. Photos may be enlarged by
clicking them with a mouse or tapping on your screen. Not all of Don’s photos from
today’s ramble made it into the ramble report, so be sure to check out his
Facebook album at this link.
Today’s emphasis: Wildflowers, ferns, and shrubs on the Orange Trail
Perfoliate Bellwort |
Today’s reading: Cathy Payne read a poem by M.K.
Creel, “In the Church of a Weeping Cherry”
After a storm, the miracle
of pale pink flowers,
tissue-paper lanterns
glimmering with honey
light. We seek shelter
in this humming
cathedral, held together
by cascading branches
and hundreds of
cellophane wings
glinting. The gloss
of promise overwhelms,
even in Winter’s false
spring – a feast for bees
already heavy
with pollen baskets.
A chipping sparrow
makes a thrilling entrance,
tilts its copper crown;
together, we listen.
Show and Tell:
Richard introduced a new method for controlling Eastern Carpenter Bees around our
houses: a fake hornet’s nest. Basically, it’s a brown paper bag stuffed with
plastic bags and other soft materials and shaped to resemble the large, papery
nest of a Bald-faced Hornet. Apparently, these bags fool Eastern Carpenter Bees
and make them leave the area – it’s not 100% effective but enough to make a dent in
the numbers of carpenter bees without resorting to a tennis racket. Here’s a video.
Bobbie brought a Luna Moth cocoon she found on the ground in her yard beneath a Sweet Gum tree. Luna Moths use Sweet Gum as well as Tulip, Black Walnut, Hickory, and Persimmon trees as larval hosts. |
Roger displaying a bluestone sample |
Roger brought his recent
collection of diabase rocks and their common look-alikes. Here’s his
presentation:
“Back in February we
took a winter hike at Camp Kiwanis north of Danielsville and walked along
Bluestone Creek. Later, I did some research and found that the creek got its
name from a rock called “bluestone.” I am not a geologist or a soil scientist,
but I’m trying to learn enough about rocks and soil to know how they shape the
natural environment around us. If you don’t know Bluestone Creek, you probably
do know about Stonehenge. The pillars of the inner circle at Stonehenge are
bluestone. Each of these pillars weighs over 4 tons; 4,000 years ago, people
hauled these pillars of bluestone 150 miles from their source to Stonehenge.
Geologists call bluestone
“diabase,” a form of lava or magma that is squeezed up into a vertical crack in
the earth’s crust. As the magma cools, it forms a wall in the rock known as a
dike. This dike may be only a few feet wide, but it can extend for several
miles in length. If you could dig it up, it would look like a blue wall across
the landscape. The diabase dikes in the Georgia Piedmont are about 200 million
years old. They were formed when the supercontinent Pangaea was breaking apart.
As the crust of Pangaea pulled apart, vertical cracks appeared. Magma flowed up
through these cracks and cooled to form diabase.
There are diabase dikes
here in Clarke County, one that runs along Timothy Road and another out on Belmont
Road, but they are deeply buried under the Piedmont soil. The only places you
can see diabase is along highway construction sites or railroad beds – or when
a line of bluestone crosses a creek. And this is what makes Bluestone Creek
special. Not only does the diabase dike cross the creek, this band of bluestone
runs down the middle of the streambed for a full quarter mile. I’m sure
the early settlers found this dark, blue-gray rock striking.
While diabase
is fascinating to me, it is also a stepping stone to learning about other
rocks. Here is a sample of granite from near my home in Oglethorpe County.
Granite and diabase are both igneous rocks, but diabase is a mafic rock that
weathers to form soil with a circumneutral or basic pH. Granite is a felsic
rock – the soil that develops from granite is more acidic and less fertile.
Next is a sample of biotite which at a glance looks a lot
like diabase because of its salt-and-pepper appearance, but biotite is a
metamorphic rock. In fact, biotite is a type of mica, and appears black because
of the iron and magnesium in its chemistry. One of the main rocks under the
Botanical Garden is biotite gneiss. The fourth rock is a chunk of amphibolite,
often similar in appearance to diabase. They are both mafic rocks, but
amphibolite is a metamorphic rock, that is, it’s an igneous rock that
was transformed by extreme heat and pressure into a different kind of rock.” (“Mafic”
is a word formed from magnesium and iron (Fe). “Felsic” rock is
rich in minerals that form feldspar and quartz.)
Announcements and other
interesting things to note:
Bob
Ambrose announced that his latest book of poetry “Between Birdsong and Boulder,
Poems on the Life of Gaia” has officially been published and is available for on-line
ordering at several sources. When hard
copies come in, he has arranged for a consignment to be sold at Avid.
Cathy Payne reminded us that she will
bring name tags and markers for us to make name tags. If you already have
one, please wear it. Lots of new ramblers this year means lots of new names!
Gary announced that the next Audubon meeting will be held at the Hargrett Rare
Book Library on Thursday, April 4, 7:00 p.m. at 300 S. Hull Street on north
campus. Jim Porter will lead a tour of his exhibit “Sunken Treasure: The Art
& Science of Coral Reefs.”
Today’s Route: We left the
Children’s Garden, crossed the entrance road, and headed up the steps through
the Upper Shade Garden. After crossing the parking lot, we walked along the
Orange Trail, following the creek, then crossing over the stream at the new Hi-Water
Bridge. We returned on the Purple Trail, which we followed back up to the
International Garden.
Spring Snowflake, a European native, is planted near the Children’s Garden arbor. |
Yoshino Cherry, one of several ornamental |
Don’s photographer eye was caught
by these slug grazing tracks on a lichen growing on the bark of a Beech tree
along the walkway through the Upper Shade Garden (on the slope between the parking lot
and the Visitor Center).
Slugs have a tongue-like structure called a radula in their mouths that are covered with very many, very sharp, microscopic teeth. Here are some photos. |
Woodland Phlox and Golden Ragwort planted along |
Juneberry, planted in the Upper Shade Garden and widespread in the woods at the Garden, is the earliest of our native blueberries |
The winter woods at the Garden are characterized by the visually dominant layer of pale, papery leaves that persist on the branches of Beech trees. |
In a process called marcescence, Beech, Hop
Hornbeam, and some oak species hold onto their leaves through the winter,
finally dropping them in the spring. We know how the first part of this process
works – a layer of weak cells (called the abscission layer) that forms at the
base of the leaf stalk on most other deciduous trees in the fall does not develop in these
species. But what about the last stage of this process? What triggers the trees
to finally let go of their leaves in the spring? Are the leaves torn off by wind
and rain? Or is it an active process triggered by the same cues that lead trees
to break dormancy and activate their buds in the spring?
Beech leaves are suddenly accumulating everywhere on the ground at the Garden. |
Once on the Orange Trail, we began to see wildflowers
in their native habitats.
Wild Geranium |
Three-parted Yellow Violet |
Pennsylvania Bittercress |
Kidney-leaf Buttercup |
Wood Rush is an inconspicuous grasslike plant, but a close look (below) reveals that its small heads are full of delicately shaped and colored parts. |
Rue-anemone |
The Orange Trail is famous (at
least among ramblers) for its fern diversity.
Christmas Fern “fiddlehead” This type of uncoiling by ferns is called “circinate vernation” and is the most common type of fern frond formation. |
Broad Beech Fern unfurling its fronds |
Rattlesnake Fern is unfurling its two types of fronds: a larger sterile frond (above) that does the heavy photosynthesis lifting for the plant, and small frond (below) that produces spores. |
Southern Grape Fern |
Rust-colored hairs cover the lower leaf surfaces, leaf stalks, buds, and new twig growth of Rusty Blackhaw. |
Here’s a photo of Rusty Blackhaw in flower, taken by Gary this week in Oconee County |
SUMMARY OF OBSERVED SPECIES:
Spring Snowflake Leucojum vernum
Woolly Ragwort Packera dubia, synonyms: Packera
tomentosa, Senecio tomentosa
Algal leaf spot on Southern Magnolia leaves Cephaleuros
virescens
Yoshino Cherry Prunus X yedoensis
Juneberry, Elliott’s Blueberry Vaccinium
elliottii
Daffodil (white) Narcissus
papyraceus (tentative; scientific name for a/the white daffodil)
American Beech Fagus
grandifolia
Golden Ragwort Packera aurea
Woodland Phlox, Blue Phlox Phlox
divaricata
Tufted Titmouse Baeolophus bicolor
Common Blue Violet Viola sororia
Rue Anemone Thalictrum
thalictroides
May-apple Podophyllum peltatum
Wild Geranium Geranium maculatum
Wood Rush Luzula echinata
Kidney-leaf Buttercup Ranunculus
abortivus
Pennsylvania Bittercress Cardamine
pensylvanica
Three-parted Yellow Violet Viola
tripartita
Perfoliate Bellwort Uvularia
perfoliata
Wild Chervil Chaerophyllum
tainturieri
Tall Rattlesnake-Root
Nabalus altissimus, synonym:
Prenanthes altissima
Southern Grape Fern Sceptridium
biternatum, synonym: Botrychium biternatum
Rattlesnake Fern Botrypus
virginianum, synonym: Botrychium virginianum
Christmas Fern Polystichum
acrostichoides
Broad Beech Fern Phegopteris
hexagonoptera
Painted Buckeye Aesculus sylvatica
Rusty Blackhaw Viburnum rufidulum