November, 2012

Exact Details of Rain Potential & Timing Becoming Clearer

November 30th, 2012 at 10:41 pm by under Chad's WLFI Weather Blog

New data is helping to piece together the timing of any rainfall potential late Saturday night, Sunday, Monday & Tuesday.

LATE SATURDAY NIGHT-SUNDAY:

Scattered showers with 30% & perhaps a t’shower or two are likely late, late in the night to early Sunday morning.  This will be followed by a dry & clearing Sunday.

MONDAY: 

Isolated showers are possible in the morning, otherwise Monday looks dry.  Coverage will be around 20%.

LATE MONDAY NIGHT-TUESDAY:

Cold front will pass with a main band of rain & perhaps a few t’storms.  Coverage will be around 50%.

Temperatures will not fall much from where they are right now tonight.  Saturday at 59-63 & Sunday at 60-65 will make for a spring-like weekend.


Native Tree of the Week: Blue Ash (Fraxinus quadralangulata)

November 30th, 2012 at 6:02 pm by under Uncategorized

BLUE ASH (Fraxinus quadralangulata)

45

lacks the diamond-shaped fissures typical of green, white & pumpkin ash, but is a bit more shreddy, especially on older trees.

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Unseasonably Warm Weather This Weekend to Early Next Week…….Rainfall Information

November 30th, 2012 at 3:06 pm by under Chad's WLFI Weather Blog

Low stratus coming up from the Gulf & high cirrus/some altostratus moving in from the west will make for more clouds Saturday & especially Sunday.  Regardless of more cloud cover, temperatures will still be unseasonably warm!  The strongest winds look to be Saturday night-early Sunday with gusts to 32 mph.  This will prevent the low temperature from dropping below 54 Saturday night-Sunday morning!

Some scattered showers are possible Sunday, but amounts look light & coverage will run 25-30%.  A couple showers are possible Monday, but the main band of rainfall will be the early half of Tuesday.

Despite that being the most widespread, soaking rainfall in a while, totals do not look impressive with totals of 0.30-0.60″ currently expected.


Nice Temperatures For Several Days

November 29th, 2012 at 10:42 pm by under Chad's WLFI Weather Blog

After 40s to lower 50s & cirrus/sun today, we are already down into the 30s as of 10:50 p.m.  With a light south breeze, temperatures will only slowly fall to 30-33.  Cirrus & sun will make for a nice Friday with south-southwest winds at 10-20 mph & highs in the 50s.

Saturday looks even warmer with partly cloudy skies (becoming mostly cloudy later) with brisk south to south-southwest winds & highs near 59 (as low, broken stratus/stratocumulus overspread area).  With solid stratus/stratocumulus overcast for most of Saturday night, low temperatures will only run near 51!

 


Drought Worsening & Spreading In Our Area Again

November 29th, 2012 at 5:24 pm by under Chad's WLFI Weather Blog

Drought expansion from the south & northwest is underway with drought conditions returning to our north with areas south ofg U.S. 36 seeing a resurgence of drought.

This is largely due to 2012 having one of the driest Novembers on record.  As of November 27, the Wabash River is just 1.9′ at the Brown Street Overlook gauge station, after dropping to 0.8′ this summer.   It is projected to go down to about 1.0′ by early next Tuesday.

2012 deficit at the station is -2.57″ as of November 29.

TOP 3 LOWEST WABASH RIVER LEVELS AT THE BROWN STREET OVERLOOK:

1.  0.24′  August 18, 1901

2.  0.30′  September 26, 1941

3.  0.82′  July 19, 2012

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Interesting Look at Wind Farm Influence of Localized Weather

November 28th, 2012 at 10:56 pm by under Chad's WLFI Weather Blog

Wind farm turbines can mix the air underneath & around them, dissipating fog quicker than the surrounding countryside or keeping from getting as dense as surrounding areas.  This can be seen in recent dense fog satellite images here in late November.  On November 21, this was especially seen.  Check out the visible satellite images.  The holes in the fog occurred where wind farms are located in central Illinois & western Indiana.

Satellite images are courtesy of NWS Chicago.

 

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Cold Start, But Warmer Weather Gradually Moving In

November 28th, 2012 at 4:16 pm by under Chad's WLFI Weather Blog

After a cold, frosty start, it has turned into a pretty nice afternoon with sun & 40s.  Some high cirrus may blur the beautiful full moon some late & may bring a halo, but it will still drop into the middle 20s.  Highs tomorrow will be warmer near 50 with high cirrus with some altostratus/patchy altocumulus dimming that sun at times.  Winds will be southerly at 10-15 mph.  With a light south wind, lows of 32-35 are likely tomorrow night.

You can see the polar jet flattening out & gradually shifting northward, showing the change in the weather as very stormy weather hammers the West Coast.  In fact, over the next 5 days, up to 12″ of rain may fall in central California with flooding & mudslides.  The potential of showers may occur for 6-7 consecutive days in Los Angeles as the “Pineapple Express” floods California with persistent rain.  Powerful storm systems will continue to bring strong winds, too, with feet upon feet of snow in higher elevations.


On These Dates In Local Weather History

November 28th, 2012 at 3:04 pm by under Chad's WLFI Weather Blog

November 14, 1997

Early-season winter weather dumps snow across the area.  By the time it stops, 7” falls at Rochester, 6.3” falls at Wheatfield, 6.2” Tipton, 4.7” Whitestown, 4.5” Perrysville & Winamac, 4.1” Jamestown, 3.6” Kokomo, 3.5” Remington, 3.1” Morocco & Monticello, 3” Logansport & Rensselaer, 2.8” West Lafayette, 2” Fowler & 1.9” Pence.

November 15, 1955

2” hail Montgomery County with 2.25” hail in Boone County as severe weather event produces at least 5 tornadoes in the state.  In Indiana, 18 were injured with $260,500 in damage from the tornadoes.

November 16, 1988

Widespread damaging straight-line t’storm winds passed in our northwest counties with gusts to 70 mph in Newton County.

November 17, 1978

F1 tornado strikes Cass County during the late morning hours as a squall line passes.  $25,000 in damage was done to farms, as the twister was on the ground for 1 mile.  Straight-line wind damage was reported in Fulton County.

November 17, 1832

A strong late fall storm system spawned severe weather in at least parts of the Plains & Midwest.

Most likely, a QLCS squall line of storms blasted central & southern Illinois to Indiana with strong winds with t’storms reported at Lafayette & Logansport.  Very cold air with flurries followed the storm after unseasonably warm air ahead of the storms.

According to diary at Fort Snelling, Minnesota (Minneapolis), it was mild & well into the 50s just prior to November 17, followed by an unseasonably early Arctic with a high of just 15 on November 18 after 8 in the morning. Diary indicates a very, very warm, summer-like fall at Fort Snelling with warm weather (mid 60s) in early November.

Temperatures fell from high of 66 to 28 in eastern Ohio.

An account of a tornado northeast of St. Louis, in southwestern Illinois was given in local press:

In the mean time, the sound had engaged the attention of MR. LUTTRELL, living more than a mile to the west. Concluding that it must be fire, he caught his hat and walked quickly to meet it. It was nearly stationary, exhibiting a dense column of smoke and cinder. What confirmed him to the belief that the smoke proceeded from a bed of coal was, its density, and the peculiar motion of the smoke, undulating, yet boiling up, like water in a vast cauldron over an intense fire. He continued very moderately to advance, but had not adventured more than 15 or 18 feet, as he conjectured, within the volume of smoke, when the tornado, as it seemed to him, gathered tremendous strength. He instantly turned to retreat, but had not turned more than half round, before he was raised from his feet entirely in the power of the wind.
As he rose in the air, the smoke and cinder seemed instantly drawn to the centre, so that objects near the circumference of the tornado, were distinctly visible. While riding round, he reached down to catch hold of a sapling, about 18 feet high, but could not reach it. After riding the engire circuit of the tornado, he was thrown out about two rods beyond the point from which he was taken up. Thus far he possessed his reason; but his stroke on the ground instantly deprived him of sense. He lay senseless, according to the best calculation of time passed from leaving his house, about an hour and a half.
After coming to his senses, he lay about half an hour before he could rise. He then looked around; all was calm; no indication of a coal mine or fire; and with difficulty he walked home.
No bone was broken by the fall, and after three days, he was able to be abroad a little, though he had not entirely recovered on the 1st of December.

November 18, 1848

Northern Lights or Aurora Borealis seen throughout the Midwest.

November 19, 1985

Squall line with flooding rainfall & pockets of damaging straight-line winds knocked down trees, limbs & powerlines in 12 of our 17 counties in the viewing area.  The stormy, very wet weather caused delays in the filming of Hoosiers at New Richmond & caused many of the scenes to still have corn standing in fields.  This was a result of the harvest delays associated with the very wet November.

November 20, 1856
Unseasonable warmth is proceeded by an outbreak of severe t’storms with tornadoes on November 21. Numerous trees were reportedly blown down between Logansport & Kokomo.  Between Logansport “& the Michigan Road” many trees were blown down.  A tornado reportedly damaged factories, gables & homes in Logansport.  Railroad was bent & broken by fallen trees.  A swath of timber is devastated & bridge destroyed near Lagro, in Wabash County.
On the line of the Michigan road between this city and many trees wore blown down and damage between here and Kokomo trees wore blown on the track of the rail breaking or bending it. In the country, the of timber is this city though not as much as been anticipated from the force of the Tipton’s brick on Fourth street was so effected that coiling joist the rouf fell and broke through the floor of the upper and the tin Vius The on the sast gable of the stone residence of wore blown down with a portion of the gable Tiie chimneys on tlie of E. Adams were blown down and broke the roof of the injuring it The chimneys on the residence of M. Forrell were blown down and other was ilone to

November 21, 1908

It was a very warm November in 1908, but not quite as warm as the record warm one in 1931.  Nonetheless, today marked the 11th time in November of ’08 that the thermometer equated or exceeded 60 degrees at Rensselaer (which included 72° on the 19th & 67 ° on the 24th).  This was the 8th such occurrence at West Lafayette, which included 70° on the 24th.  Following the 25th, two more days had 60s at West Lafayette & one at Rensselaer.

November 22, 1992

Two damaging tornadoes tore through Montgomery County of F1 (600’ wide) & F3 (half mile wide) strength.  Damage amounted to $275 million with combined path length of 10.5 miles.  Ping-pong & golfball hail accompanied the storm.

November 23, 1874

A very strong storm system with it pressure down to 975 mb near Kankakee, Illinois (Category 2 hurricane equivalent) was exiting the region.  It brought non-t’storm wind gusts to 60 mph early in the morning as it raced from Kankakee to Detroit to Toronto.  The powerhouse storm brought rain & highs in the 50s to us (followed by 30s), but a severe weather outbreak from the Tennessee Valley to the Deep South with tornadoes.  Many limbs were knocked down & some trees uprooted by the strength of the wind on the low’s backside.

November 24, 1881

One the coldest Thanksgivings on record occurred in the viewing area (ranking with the brutally cold Thanksgiving of 1930).  Highs were only in the teens with lows in the single digits.

November 25, 1857

One of the worst November cold outbreaks on record occurred in the area after 4-8” of snowfall.  Widespread readings of -15 to -5 occurred in the Midwest.  An early record-keeper had a low of -17° on this date in Allen County, Indiana.  At Indianapolis, the weather record entry read “weather uncommonly severe” on this date with 0° at sunrise & only 18° at 2 p.m.  7” of snow was on the ground on this date in Lafayette with snow reportedly on the ground for “5 days”.  On the 19th through the 25th, 2 p.m. temperatures did not exceed the teens at Lafayette, or Indianapolis. It was also a very wet month overall with 7.24″ of rainfall recorded at Indianapolis for November 1857.  Lafayette was said to have had a ”very wet, snowy, uncommonly cold month” with “fields totally unfit for work”.

November 26, 1965

More strong tornadoes hit parts of the viewing area in the active severe weather year of 1965.  On this date, late season severe weather outbreak hit Indiana with F2 & F3 tornadoes in Boone County.  The F3 moved into Hamilton County, injuring 5.  Overall, 6 large F3 tornadoes hit Indiana on this date.  Damage in Boone County was as high as $500,000 with total damage in Indiana at $1.5 million (1965 dollars).

November 26, 1859

Severe weather in the region.

Storms “prostrate trees” in Fountain County

According to NWS Lincoln:

A tornado moved northeast across Pontiac during the late afternoon. Homes, stores and barns were destroyed by this tornado. No deaths were reported.

November 27, 1887

After a long, hot, dry summer & fall & even a warm start to November (74 on November 3rd at West Lafayette), welcome 2-5” rains fell across the area to end the month.  3.45” fell at West Lafayette November 24-27.

However, this was a very strong storm system with lots of wind, t’storms, a severe weather outbreak in the southern U.S & an early Arctic Blast.

After a high of 60 early in the morning on November 27, the mercury fell all day at West Lafayette with “a gale”, 0.3 to up to 2” of snow area-wide.  It was 11 by midnight (a drop of 49 degrees!) & crashed to 1 by morning (a drop of 59 degrees in 24 hours!) with clear skies & calming winds with over some snow pack.  However, after 1 that morning, in true Indiana fashion, the thermometer reached 55 by December 4.

November 27, 1909

1909 featured the second consecutive, exceptionally mild November.  On this date, the mercury hit 68° at Rensselaer, part of a 5-day stretch of temperatures in the 60s to even near 70°. In fact, in November 1909, the temperature did not even drop below freezing until the 18th!  Other highs on that day include West Lafayette at 69°, Crawfordsville 68° & Logansport 69°.  The coldest temperature the entire month at West Lafayette was just 26° with only 7 mornings where the mercury was at or below freezing.

November 28, 1854

Drought lingered into fall 1854 after a hot, dry summer.  Temperatures were as high as 107° in the summer of ‘54, which equaled the hot, dry summers of 1838,1838, 1840, 1841, 1860, 1880 & 1881.  1854 was part of a multi-year drought in the region with some form of summer drought in the viewing area in 1851, 1852, 1853, 1854, & 1856.  The dryness had peaks (severe category) in 1851 & 1854, before major rains occurred in summer 1855 & 1857 with major floods in spring 1858.  However, by late summer 1858, very dry weather returned with corn “rolled up” & “suffering” with ground “hard as stone”.

November 29, 1974

November came to an end with a winter storm arriving to the viewing area.  By the time the snow came to an end on the 30th, 8.8” of snow had accumulated at Kokomo, 8.6” at Crawfordsville, 8” Logansport, 7.5” Kentland, 7.3” at Delphi, 6” Peru, 5.5” at Romney, 5.1” West Lafayette & 5” at Whitestown.

Contrastingly, this was the warmest Thanksgiving on record with highs in the lower 70s area-wide in 1900.  The Thanksgiving of 1896 was also very warm with highs in the upper 60s to 70 area-wide.  West Lafayette reportedly hit 71° in 1900 & 67° in 1896.

November 30, 1991

Shortly after midnight, a long-lived QLCS squall line with an embedded derecho of widespread damaging straight-line winds of 60-80 mph passed through viewing area.  Wind damage was reported in Newton, Jasper, Benton, Tippecanoe, Clinton, Miami & Montgomery counties.

Winds gusted to 100 mph just southeast of the viewing area in Hendricks County.

December 1, 1905

A winter storm with rain, freezing rain, sleet & snow struck the area on this date.  Ice accumulations were as high as 1/4″ with a coating of sleet.  It was nearly/all glaze ice in our southern counties, but central & northern counties received 1-4″ of snow with the glaze ice & sleet.  Crawfordsville picked up 0.95″ of melted freezing rain with a bit of sleet, while West Lafayette had 0.62″of precipitation melted from glaze ice, sleet & 1″ of snow.  The 0.70″ of liquid at Whitestown was largely freezing rain with some rain.  Kokomo measured 0.70″ of liquid with part of that the 1.5″ of snow.

December 2, 1837

An early morning likely derecho brought a “violent gale” with damage to the area.  “Scores of trees were uprooted” by the t’storms.  Temperatures fell rapidly from unseasonable 60s & 70 ° to 30s.  Scenario bears superficial resemblance (although observational data is scant) to the derecho of December 1998.  The storm system brough unusually warm weather to not only our area, but as far north as northern New York, where 64° was recorded at Governeur, New York at 7 a.m. on December 3.

A pelting sleet storm on the night of December 1-2 was reported at Fort Snelling (at present-day Minneapolis, Minnesota).  The sleet melted down to 1.15” liquid.

December 3, 1998

1998 had a very mild late fall & early winter.  Today was the 6th day since November 27 that the temperature was at or above 60°.  3 more days would be above 60° until 70s & a strong cold front would end the streak on December 7.

December 4, 1982

Today was the third consecutive day with a record high temperature in the very warm December of 1982.  In fact, these three days had highs above 70°, before additional records were broken December 25, 26 & 27 with highs in the 60s.  The winter of 1982-83 was unprecedented for its lack of snowfall & appreciable cold caused by one of the strongest El Ninos on record in the Pacific & a persistent, positive NAO & AO.

December 5, 1991

Unusual Arctic outbreak welcomed December with not much snow cover (1-2” snowfall in parts of Newton, Jasper & Pulaski counties with trace to 0.8” elsewhere).  The temperature fell to 1° at West Lafayette, Rensselaer & Attica, Boswell -1°, Kentland 0°, Crawfordsville, Frankfort, Kokomo, Romney, Rochester, Jamestown & Delphi 2°, Wheatfield, Winamac & Logansport 3.  Interestingly, on December 9, temperatures soared in the 60s with 65° at Kentland & Delphi, 64° at Attica & 62° at Frankfort.

December 6, 1998

Between 12:30 & 2:15 a.m., a serial derecho with widespread straight-line winds of 60-70 mph with cores of 90-100 mph gusts blasted through the area.  University Hall on the Purdue campus had major roof damage totaling $100,000.  The wind blew over a 35-car freight train in Carroll County near Rockfield, while the third story of a Total Discount store in Logansport collapsed & fell into a restaurant.  A grain bin was blown over near Walton & a barn was partially unroofed.  At Peru, several buildings & homes were damaged in the city with the roof blown off a warehouse. A mobile home was destroyed near the city & another was overturned while trees fell on automobiles near Logansport.  Widespread tree, powerline & barn/farm damage occurred area-wide.  A wind gust of 82 mph was recorded at Grissom Air Reserve Base & 77 mph at West Lafayette.  The only hail report was 0.75” at Wheatfield.  Record warmth with highs of 68-74° preceded the storms & just prior to storm passage just after midnight, temperatures were still 65-70°.

December 7, 1927

From the 7th to the 8th, the temperature fell from 55° to 3° at West Lafayette as an Arctic cold front blasted through with strong winds.  This occurred after 1-2” of rainfall on the 7th.  At Rensselaer, the temperature fell from 53° to 3°, at Kokomo 55° to 5°, Crawfordsville went from 56° to 6°, Wheatfield crashed from 52° to 0° & Whitestown 54° to 4°.  Southeast of Indianapolis as Rushville, the mercury went from an astonishing 65° to 6° in 24 hours.

The 1.53” of rainfall at Wheatfield to the 1.11” at Crawfordsville to 0.93” at Kokomo & 1.32” at West Lafayette caused ponding in fields that froze solid nearly instantly with passage of the front.

December 8, 1966

Rare December severe weather event produces F2 tornadoes in Jasper & Montgomery counties.  1 person was injured in Jasper County with additional straight-line wind damage in White & parts of Montgomery County.  The wettest December day on record occurred at Logansport with this event when 3.20” rain fell.

December 9, 1930

1930 had the driest December on record for part of the viewing area.  Precipitation totals amounted to just 0.16” at Frankfort, 0.23” Logansport, 0.24” West Lafayette, Crawfordsville 0.43” & Kokomo 0.48” for the month.

December 10, 1971

QLCS squall line with damaging straight-line winds moved through central & southern Indiana.  Straight-line wind damage with gusts to 65 mph occurred in Montgomery & Boone counties.

December 11, 1967

7 tornadoes are confirmed in Indiana along with damaging straight-line winds as strong low pressure moved north-northeastward from Memphis, Tennessee to northwest Michigan.  One person was injured from an F1 in Putnam County & wind gusts to 65 mph occurred in southeast Montgomery & Boone counties.  After such a wet, cool fall, only 60-70% of the soybean & corn crop in Indiana & Illinois was harvested.  Tornadoes & damaging winds damaged & even flattened acres & acres of crops.  Structural damage from the tornadoes alone amounted to $358,000 (1967 dollars).   Many other tornadoes, wind & hail occurred in the southeastern United States with damage in the millions of dollars.  Just 10 days later, another significant severe weather outbreak would occur in the same regions of Indiana with more heavy rainfall, which continued to delay the harvest.

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Cold, Frosty Night……………Gradual Warming Trend Over the Next Few Days

November 27th, 2012 at 9:55 pm by under Chad's WLFI Weather Blog

It is a cold, frosty night with high cirrus & a nice, bright moon!  You see these temperatures & you think they are tanking & headed for teens, but they will tend to level off overnight & then may fall a bit faster just before sun-up as all the high cirrus/some altostratus move eastward.

Temperatures will slowly warm over the next few days with a good amount of sun & reasonably light winds (5-15 mph).


Native Trees of the Week

November 27th, 2012 at 4:17 pm by under Chad's WLFI Weather Blog

NORTHERN PIN OAK (Quercus ellipsoidalis)

GLACIAL SURFACE GEOLOGY & THE NORTHERN PIN OAK…………

At the end of the Wisconsin Ice episode or end of a series of Ice Ages (Pleistocene) that totally buried the ancient Teays River Valley & leveled the landscape in our area, much water remained from the melting ice.  With the land totally re-worked, the land was considered geologically young…………….& still is.  Water was back-upped by piles of sand & soil left over in the geologically-young land, scraped from Canada & large, large areas of stagnant water, unable to drain sat.  With time, such water drained as the ice totally receded & the sediment laid down became wind-borne as winds were very, very strong in a band south of the great ice sheets.  This wind blew the sand & silt into rolling drifts across Newton, Jasper, Pulaski, Fulton, White & Cass counties.  Such sandy dunes make a lot of land in our northern counties in need of irrigation for crop production in the summer.  These were & still are the haunts of Northern Pin Oak (also known as Hill’s Oak).  Dry, sandy savanna & prairie is its home.

SAVANNA SPECIES…………..

A tree of these wind-blown dry, droughty, sandy dunes, mixed with Black Oak savannas of northern Indiana, Northern Pin Oak is an over-looked native tree.  Though farming has eradicated much Northern Pin Oak, this tree formed thickets, scrub & scattered trees on the prairie dunes & savannas.  In fact, this species, with Black Oak, formed a transition between the large prairies & the oak openings as one moved eastward from Jasper & White to Cass & Pulaski counties.  Very drought tolerant, Northern Pin Oak is so intolerant of shade that its own limbs will die off & shed if its own foliage shades it self.  Very fire tolerant, it is a substantial component of the sand savanna & prairie environment in northern Indiana & it usually found with Black Oak.  In fact many dunes that are labled purely Black Oak savannas contain much Northern Pin Oak, but they all just seemingly blend together.

It is also a component of the original “oak openings” throughout northern Indiana on typical loam & clay loam soils with bur, shingle, scarlet, white & black oak with hickories in that transition zone between largely beech-maple forests & the prairies to the west.  It also has an affinity for the gravelly, rather sandy slops of glacial kames (gravelly hills) & eskers (snake-like ridges of gravel & coarse materials that were deposited by streams of melt water within the ice sheet).  However, it seems to have issues with competition from Bur Oak in these areas, so is most common on the sandy dunes.

NORTHERN PIN OAK’S ATTRIBUTES………….

Vibrant in orange & scarlet fall color, this species has a nice form with broad crown & fairly short stature with a peak height of 50-60′, but may spread out nearly as much.  Its shiny foliage, fall color & decent form, as well as durability to droughty, coarse & hard, clayey, dry soils has made it a bit more popular recently in the nursery trade.  It grows reasonably fast & for the first time, I saw it offered at a nursery in Lafayette this summer.  It doesn’t really need any irrigation in summer drought, even if planted on the driest gravelly soils.  The only issue is its self-pruning, as it sheds a lot of snags & dead branches with age & tends to have quite a few dead branches in the crown as it matures.  However, this attribute made it an important nesting site for savanna-loving eastern bluebirds.  Before European settlement, bluebirds were THE savanna bird, loving grassland with oak openings & scattered trees.  The fire-scarred oaks with decay were perfect for cavity nesting.  Northern Pin Oak provides nice snags & cavities for this colorful native thrush.

Northern Pin Oak likes to hold onto its leaves through winter, as dry, brown, crispy foliage.  Entire young trees will be clothed in foliage all winter, until pushed off in the spring.  Older trees with have a brown, dried foliage skirt on their lower branches.

For germination, this tree must have 95-100% light & rather bare, mineral soil with little competition.  It can contend with some little bluestem & dropseed grass competition, but cannot handle lots of vines, trees & plants crowding it.  It likes a fire regime to accomplish this, as it will even bud as a young tree after fires (as long as they are not overly frequent).

 

 

Fall Leaf Coloring Page


POST OAK (Quercus stellata)

If Bur Oak is the tree of the black loam prairies & savannas in northern Indiana & Black Oak is the tree of the sandy prairies & savannas in northern Indiana, then Post Oak is the tree of the gray prairies & barrens of southwestern Indiana.  It is certainly a more southern oak in the U.S. with large amounts of Post Oak on the Blackland prairies of Texas & Oklahoma.  It is frequent in the southern U.S. pine barrens & in the Karst barrens/prairie region of Kentucky & Tennessee.  It cannot not thrive in a closed, crowded forest situation & survived in either a regime of fire or on really poor, dry sites where other trees cannot crowd it.  Where it is found on the richer soils of southwest Indiana, it was historically maintained by fire.

An isolated native population of Post Oak exists on the sandy/gravel slopes near Wea Creek in Tippecanoe County.  The closest population outside of this is in northern Clay County, Indiana near Route 159 & 246 intersection (a good 85 miles to the south), where I found several individuals growing mixed with White, Shingle & Black oaks, as well as Shagbark & Mockernut hickories.  Open woodland was on an upland slope of thick silty loess overlaying Illinoian glacial till.  Native vegetation of this area was prairie mixed with barrens & ribbons of timber.  It was south of the large prairies running from Prairie Creek & Prairieton, Indiana to Blackhawk, Lewis & Clay City, Indiana.

This Tippecanoe population is an outlier from a much warmer, drier time in Indiana when Post Oak’s range greatly expanded to northern & central Indiana, before being crowded out & dying out by cooler, moister times in the climate pendulum.  Like a tidal pool, southern & western species’ ranges shrunk with the wetter regime & the island of more southern & western species remained along the sandy & gravelly areas around Granville.  This Post oak population may date back to Medieval times, perhaps the Hypsithermal.

There are really three types of Post Oak in Indiana that may be vague subspecies.

POST OAK TYPE #1:  SOUTHWESTERN INDIANA GRAY PRAIRIES/BARRENS………HIGH FLATWOODS OF LAKE PLAINS NEAR/AROUND PRE-SETTLEMENT BARRENS………..DRY UPLAND SLOPES WITH BLACK OAK

One grows on the gray prairies/barrens region of southwest Indiana on the silty loess soils & clay-loam soils of the region (Western Illinoian Till Plain).  In far southern & southwestern Indiana, it grows on clay soils of the Driftless area on acidic flatwoods, often on soils with a fragipan or a hard pan layer restricting downward movement of water.  It also grows in Black oak woods with hickory on dry, upland, south-facing slopes of the Driftless area.  It grows on higher flatwoods on the old lake plains (lacustrine soils), clay soils of southern Indiana, too.  These lake plains are layers & layers of silt & clay from trapped glacial meltwater settling in this part of the state during the Pleistocene.

In pre-settlement barrens areas of Spencer & Warrick County (nature area to view this environment:  Bloomfield Barrens Nature Preserve), the Post Oak grows on those clay flatwoods that are acidic & have a fragipan or pan in the soil that restricts downward movement of water.  They are wet in spring & bone-dry, desert environments in summer & fall.

Often a southern barrens & prairie indicator species, Post Oak is found with red cedar, blackjack, black oak in rocky glades on high, south-facing slopes in south-central Indiana hill country.  I also grows with Chestnut Oak & Virginia Pine in the “knobs” area of far southern Indiana on rocky slopes.  Post Oak is found on the Mitchell Karst Plain in former barrens & prairie areas with Black, White & Blackjack Oak & hickories from Orange through Washington & Harrison County, Indiana.

Closest associates to Post Oak in this area:  Swamp White Oak (Quercus bicolor); Shingle Oak (Quercus imbricaria); White Oak (Quercus alba); Black Oak (Quercus velutina); Shagbark Hickory (Carya ovata); Mockernut Hickory (Carya tomentosa)

POST OAK TYPE #2:  POPULATION A NORTHERN PROTRUSION CLOSELY-RELATED TO DELTA POST OAK (A SUBSPECIES THAT IS LARGER, MORE VIGOROUS & GROWS WITH OTHER HARDWOODS IN THE HIGH BOTTOMS OF THE MISSISSIPPI RIVER VALLEY) IN FAR, FAR SOUTHWEST INDIANA

There is a different genotype of Post Oak that grows faster, gets larger & is better able to compete with other oaks in Posey & Vanderburgh counties in Indiana.  It competes with the Southern Red Oak, Cherrybark Oak, Pin, Swamp White, White Oaks in flatwoods of this area well & gets to be a very large tree up to 100′.  This genotype is more closely-related to a subspecies of Post Oak called Delta Post Oak.  In fact, this population may be a northernmost protrusion of Delta Post that has naturally hybridized with the typical southwest Indiana Post Oak.

Closest associates to Post Oak in this area:  Winged Elm (Ulmus alata): Southern Red Oak (Quercus falcata); Cherrybark Oak (Quercus pagodafolia) Swamp White Oak (Quercus bicolor); Shingle Oak (Quercus imbricaria); White Oak (Quercus alba); Black Oak (Quercus velutina); Blackjack Oak (Quercus marilandica); Shagbark Hickory (Carya ovata); Mockernut Hickory (Carya tomentosa); Shellbark Hickory (Carya laciniosa)

POST OAK TYPE #3:  MORE RELATED TO SAND POST OAK (GROWS ON DRY EOLIAN SAND HILLS OF LOWER WABASH & WHITE RIVER VALLEYS IN SOUTHWESTERN INDIANA)

There is a type of Post Oak that is restricted to the sand hills of southwestern Indiana.  It tends to be shorter & squatty compared to the gray prairie Post Oak & will not grow in loam or clay soil well at all.  It grows in the very well-drained Eolian sands bordering the east side of the Lower Wabash & White River Valleys.  I have tried to plant the sand Post Oak on gray prairie or loess soil & the tree never survives.  The sand barrens Post Oak genotype is different than the Post Oak of the gray prairies.  It is more related to the subspecies of Post Oak called Sand Post Oak, which is not found in Indiana.

Closest associates to Post Oak in this area:  Blackjack Oak (Quercus marilandica); Black Oak (Quercus velutina); White Oak (Quercus alba); Chinkapin Oak (Quercus muhlenbergii); Sand Hickory (Carya pallida); Arkansas Black Hickory (Carya texana var. arkansana);

Post Oak is generally a slow grower.  In acorns I germinated from a Post Oak woods on an old prairie 40 miles northeast of Vincennes, Indiana (Odon, Indiana), the trees are just above my waste (I am 6’3″)& I germinated them in 2001.  The same redbud trees I germinated are over my head now.  A tuliptree I planted at the same time & was 1′ tall, is 20′ tall at the same site!  I just keep thinking I really won’t see this Post Oaks do much until I am 60 or 70 years old!  Truly, it takes a lifetime from seedling to even start to see Post Oak tree really develop.

It is like Shingle Oak in that it cannot tolerate shade & needs warm, open areas to germinate.  It cannot compete with most other species well.  The genotype more closely related to Delta Post Oak is much better at competition & some shade than the other genotypes.  When Post Oak reaches 150-200 years old, though, it is a magnificent tree & still ranks as one of my favorites.  I have seen 200-300 year-old Post Oaks in the open that resemble the idyllic very old English Oaks of the British countryside.

Its bark resembles White Oak to sometimes Swamp White Oak, its old limbs are often contorted, twisted & picturesque.  It hold its dry, rusty foliage into the winter, especially on younger trees & lower limbs.

Tolerating fire as good as Bur Oak, it sprouts well after a burn & was a main species with Black Oak in the “oak stool” environment of the Karst prairie & barrens in far south-central Indiana at European settlement.  Each fire burning over the Post Oak would initiate healing of burned, thick bark, causing large chunks of tissue to form above & just below ground.  These reportedly made plowing the virgin reddish Karst soil difficult as these oak stool would break steel plows.  This would form thickets & shrubbery of Post Oak.

Being a slow-grower, Post Oak puts a lot of energy into growing deep roots (specifically tap root when young) & put dense, dense rings into the wood.  The wood is very heavy & resistant to rot.

Post Oak barrens/savannas:

Leaves, acorns, bark, shape & early fall color of Post Oak:

Fall Leaf Coloring Page

AMERICAN BEECH (Fagus grandifolia)

AMERICAN BEECH IS A RATHER SENSITIVE SPECIES THAT REQUIRES THE FOREST ENVIRONMENT………….

If you have large beech trees on your land, more than likely, the land was forest at the time of settlement.  American Beech is strictly a forest tree.  It doesn’t like direct exposure to the elements, doesn’t like open, exposed countryside, prefers shade & has bark so thin that it blisters very, very easy in the elements.  The tree does not tolerate drought well at all & needs sustained, persistently moist soil through the year.  The species also is intolerable of fire.  Even a low fire will severely blister beech bark, especially on younger & pole sized specimens.  It will greatly weaken older trees.  Heat & drought will wither foliage & cause scorch much like Ohio Buckeye, especially in soils that are exposed.  The tree is also very susceptible to construction projects, as it does not like it roots disturbed or elevation changed in any way.  Many times, when homes are being built or subdivision constructed, it is hard to save the beeches if you want a more wooded subdivision if any soil is moved around the tree.  Some may make it for a while, but boy do they struggle.

AMERICAN BEECH’S NATURAL ABSENCE IN CHUNK OF THE VIEWING AREA………….

In our viewing area, it is highly-likely that there were no beech trees in Newton, Jasper, Benton, White & Pulaski counties at settlement with beech confined to the deeply-eroded ravines of creeks & streams in Tippecanoe, Warren, Fountain, Montgomery & Carroll counties.  Its occurrence tended to be higher in Tipton, Howard, Miami & parts of Fulton counties.  In parts of the viewing area there is a real dicotomy in natural areas & native vegetation, largely due to geology & geomorphology.  An area I like to call the Sugar Creek Entrenched area is a natural division where glacial meltwater & floods have carved out picturesque canyons & ravines in areas of thinner glacial till.  This environment is common in Turkey Run & Shades State Parks, as well as areas in Warren, Fountain, Montgomery, through Tippecanoe to Carroll, Cass, Miami & as far northeast as Huntington.  These deeply-eroded ravines are cool, moist, forest environments with lots of beech, sugar maple & tuliptree.  They are refugia for forest species in an increasingly prairie biome.  This habitat has acted as a refugia for odd, disjunct populations of Eastern Hemock, Canada Yew & native Eastern White Pine in Turkey Run, Pine Hills & Shades State Parks (pocket populations left over from the cold, wet climate at the end of the last Ice Age).

3 TYPES OF AMERICAN BEECH IN INDIANA………..

TYPE #1:  Southern Flatwoods Beech

There are 3 types, subspecies or genotypes of American beech in Indiana.  The first type has a much greater tolerance of wetter, tighter, clayey soils compared to the other two.  With genetic origins in the southern U.S., this beech is a significant part of the dense flatwoods forests of southeastern Indiana.  Here a strictly pin oak-sweetgum-beech-red maple forest formed pure stands.  Here, it not only grows densely in the understory of the flatwoods, but also in the overstory with large specimens in nearly pure stands in older forests.  There are some areas in the Driftless area of southwestern Indiana & in the southern bottomlands region of southwestern Indiana where you can find this type of beech.  I have actually seen this beech frequently with Cherrybark Oak (Quercus pagodaefolia) near the Ohio River in Spencer & Perry counties in Indiana & frequently with Sweet gum in Pike County & Dubois counties in southern Indiana.  In these areas, it tolerates standing water well, but cannot tolerate deeper river flooding.

TYPE #2:  Appalachian Beech

Trees in the hill country of south-central Indiana have more of an Appalachian origin. It is usually accompanied by more mesophytic species like tuliptree, various oaks & hickories, white ash, maples, basswood.  These beeches grow on lower slopes, usually with a north-facing tendency & in coves where it likes the company of tuliptree & maples.

TYPE #3:  Central & Northern Till Plain (& Moraine) Beech

Finally, in central & northern Indiana, beech is apart of the maple-beech belt from the till plains of Ohio & Ontario, where it is usually accompanied by American basswood, White Ash, Sugar & Black Maples & Chinkapin & Northern Red Oak.  In this often calcareous glacial till, the species formerly formed pure stands & is considered a climax species with maple in these areas.

In the eastern part of the Tipton Till Plain & Northern Lakes & Moraine Region of Indiana, however, it is a relatively new tree to the landscape.  Pretty Lake corings in Noble County (Williams, 1974)  indicate that Beech largely arrived at that location just prior to the Hypsithermal (main prairie period of hot, dry weather with climate here more like Oklahoma or Nebraska) with greater frequency than currently, then radically dropped in numbers for about 2000 years (prairie & oak pollen skyrocketed at this time & remained very high until an all-time peak [at least in the 14,000-year coring], roughly 2500 years ago) until its greatest extent in the 14,000 years of the coring at 1500 years ago.  Since that time, it has declined, but has seen resurgence in recent years in the understory of nearby woods.  There is a bit of beech pollen for a few hundred years centered around 9000 years ago, when pine pollen had radically diminished.

There is also a tiny pulse of beech pollen around 13,000 years ago that was found for about 300 years with a little spike in hornbeam, elm & pine pollen in the set (with LOTS of spruce pollen & a bit of fir [fir pollen peaked around 10,500 years ago in the data set]).

It is interesting that other than that 9000 year old small stretch of minute amounts of beech pollen, that no beech was found on the site or nearby for another 2500 years after glacial ice recedence, but ash, elm, hornbeam & at least some oak pollen had been on site since the very tail end of the glacial ice.

Beech nuts are very oily, fatty & high in calories, making it an important food source for wildlife.  An interesting, triangular nut, beech oil can be extracted from it & can be used in a lantern to burn.  The triangular nuts are enclosed in a spiny, bur-like husk on the trees.

Beech is easy to spot in the forest in winter.  Young floor & understory beeches retain their leaves through the winter.  Highly sensitive to wind & ripping, the papery, thin leaves are tan/peach colored to rust color when retained on the trees.

As beech gets very old, it tends to hollow-out in the middle & eventually, topples from this at 300-400 years of age.  Large, hollow beeches provided important nesting habitat for chimney swifts in forest openings prior to chimneys.  My dad told me a story of how when we was a kid in the 1950s & 1960s there was a gigantic beech near Raglesville, Indiana (45 miles south-southwest of Bloomington) near my relatives’ that all of the kids would play in.  In typical old, old beech fashion, the tree was hollow & provided a natural cave for all the country kids to play in.  Dad still remembers how gigantic this old tall stump was.

Fall Leaf Coloring Page

SHINGLE OAK (Quercus imbricaria)

This member of the Black Oak group is the oak with its conspicuously oblong, shiny, rather leathery leaves that tend to brown, dry & tend cling to its twigs in winter.  We called it “Peach Oak” growing up in southwest Indiana (due to the leaves that look a bit like those of a peach)& also (I hope no one is offended by this, but farmers where I grew up called it this) P-ss Oak, as the wood emitted a uriney odor.  In the History of Clarksburg & Early Odon, it was called “Shingle Tree”, as the wood splits very well for shingles & was used for such exhaustively in pioneer times.

Shingle oak is THE tree of the gray prairies & barrens in southwestern & western Indiana.  No where in the state does it reach greater occurrence than there.  As a kid, remember seemingly every old farm fencerow having Shingle oak, mixed with the sassafras & black cherry, of course in traditional gray prairie & barrens areas.  Many times, I would go into the fencerows & dig out Shingle Oak seedlings in fall & winter to transplant (they are pretty sensitive too it, though…………you can only do it in late fall or spring, as it has a heck of a tap root.  You have to get lots of lateral roots when you dig it).  It is a barrens species on the loamy, clayey loess & Illinoian till soils that tend to be on the acidic side.  “Gray” is a term to describe the soils of that region, as they lack the deep chernozem soils of Benton & White counties of those prairies that were there for a long, long time.  The ashen-gray to dark-gray soils tended to have prairie & barrens on them in a state of flux.  It wasn’t solid prairie for thousands & thousands of years, but a pendulum of back & forth, thus the coal-black soils were not as common as areas in north-central Indiana.

Shingle oak is a slow grower can’t compete with most other species, other than other slow-growing oaks & hickories.  For it to develop, it cannot be disrupted by more aggressive species growing underneath it & them around & over it.  So intolerant to shade with age, the branches shaded by its own foliage frequently die & fall off the tree.  There is a very narrow window for this tree to handle shade & that is in its first 2-5 years, generally & it usually only germinates in response to a sunny opening.  In presettlement times, it was fires that did the job of prevent other more aggressive trees from competing with it.  It can’t have such a fire regime to keep prairie prairie & it did best in presettlement barrens/savanna in a cyclical, semi-frequent or more occasional fire regime with prairies around it/nearby.

It seems to handle fire pretty well, especially low-growing fires.  It will frequently re-sprout after fires as a small tree, but fires kill young seedlings.  I have found that it is not as fire-hardy as Bur, Black or Post, or Blackjack Oak, but does as good, if not a hair better than White Oak.

Since it does not quite live as long as alot of our Indiana oaks, it must have thrived in a presettlement landscape environment of flux on the pretty rich, not too wet soils that it loves.  What I mean, it that if the Shingle oaks in a savanna are dying because they are 170 years old & fall, but the huge White oaks live to 400, they will take over more than the Shingle Oak.  That said, open environments with no closed canopy & borders allowed this species to go.  In the world of vegetation dynamics in presettlement there are so many things going to determine where populations of species set up, for sure!

In that Illinoian Till Plain area of west-central & southwest Indiana, it reached & still reaches its greatest occurrence on those loamy/clayey soils of till plains & the rolling landscapes & bevels of the region.  It also likes the wind-blown sandy soils of that region of Indiana.  In the oak-hickory woods of the Driftless region of southwest Indiana, it likes the upland black oak woods & then also grows on the higher flatwoods of Post Oak in far southwest Indiana.

Shingle oak can also be found in our viewing area, especially in areas ringing the historic Grand Prairie region.  It was most likely found in savanna/barrens bordering solid prairies.  It probably reaches its second greatest occurrence in our viewing area & third greatest occurrence in the sandy soils & clayey soils of historically Black Oak & Black Oak/Northern Pin Oak barrens from Fulton to Kosciusko, Marshall, Elkhart to Allen counties.

Scattered pockets of the species exists as far east at Tipton to Huntington counties, but the trees is pretty rare or uncommon in the rest of the state.

Every species has its place in the sun, but Shingle oak is one of my favorite native species.  It has nice form, those unique, leathery leaves, I like the dry winter foliage that hisses in the cold winter winds & fall color can be maroon, purple to red & burn orange.  Its form is a lot like a Pin Oak, just not quite as triangular/pyramidal.  There is a long-standing saying that it is time to plant corn & green beans once all of the Shingle Oak leaves (& beech leaves) have totally fallen off in spring.  My grandfather Evans always told me that & it was pretty accurate!  Young trees are usually clothed in dry, brown foliage in the winter, but the larger the trees, the less leaves it tends to hold.  Frequently large, old trees may just have a small skirt of leaves on the lowest branches.

Squirrels & birds really like the acorns.  They are sweeter than a lot of the Black Oak group members, which have a tendency of being bitter.  Animals bury the acorns everywhere & since they greatly dislike competition & need total sun, sprouting next to a southside part of a home or next to a drain or stump is ideal for it to thrive.

Shingle oak doesn’t live as many other oaks & tends to hollow-out with age & eventually topple.  A Shingle oak that split back home in an uncut barrens grove in our city park fell in 2001.  The tree was not yet hollow & the rings showed the tree was a small seedling in 1870, but some of the Post Oaks & a White Oak in the park date back to 1825 as shrubby small trees in a barrens/prairie (now they are huge trees with fat trunks!).

Shingle oak is gaining popularity as a landscape & street tree & rightfully so.  Several are planted along Cumberland Avenue by Applebee’s & Wal-Mart in West Lafayette.  It is a slow grower, but worth it, if you can tolerate its self-pruning of its dead branches as it gets older.

Images of native oak barrens/savannas:

Fall Leaf Coloring Page

OVERCUP OAK (Quercus lyrata)

Also known as Swamp Post Oak, Overcup Oak is a swamp-loving species native to mainly southwestern Indiana with a few trees natively growing up the Muscatauck River swamps as far north as Washington & Jackson counties in Indiana.  It likes consistently wet to submerged feet & is the tree of low, moving, widing, sluggish, silt-laiden southern river systems.  This tree is a substantial component of the baldcypress & water tupelo (often festooned with Spanish Moss) swamps of the southern U.S.  It likes tight, clayey soils of floodplains, oxbows and ponded flats that are very poorly-drained.  It often had a buttressed base to hold the large tree up in soupy, mud environments, like a bowling pin.

Overcup Oak is highly-tolerant of flooding.  I have seen it growing in environments flooded for months at a time, but like Baldcypress, bare soil or at least soil with only 1-2″ of water is required for seedling emergence.  This rapidly occurs in fall after the acorns fall during Indian summer when swamps & wet areas are usually the driest for any time of year, on average.  This is also an adaptive trait to germinate as rapidly as possible, as the acorns are consumed by animals.  The small seedlings go dormant by November, then resume growth in spring.  If seeds to not germinate in fall, they are very resilient in swamp conditions & may still be viable come spring after mid-winter high water transports the acorns to other sites.

A problem for seedlings is floods in the first few years.  They really need 2-3 years without deep flooding to survive, so like Baldcypress, often times nice Overcup Oak reproduction & seedling/sapling establishment occurs during significant droughts.  I have seen this first hand at Twin Swamps Nature Preserve in Posey County, Indiana, very close to where the Wabash & Ohio Rivers meet in far southwest Indiana.  In an Overcup Oak swamp in the preserve, I observed mats of thousands of Overcup seedlings germinating during a droughty fall several years back.  There were no other Overcup seedlings or saplings amidst large Overcup Oak trees, indicating that conditions had not been sufficient for Overcup germination & establishment in the previous years.  These thousands of seedlings occurred in large openings of the forest, which brings up another good point.  Overcup Oak really needs openings in the forest to regenerate, as the seedlings may sprout in shade, but must have a good amount of sun or they will not make it.

The species’ name refers to the corky, light cap around the acorn, which makes identification easly.  This thin, corky layer serves as an important seed dispersing mechanism, as it acts as natural “floaties” so the acorn will float & “swim” in flood water.  Acorns transported in this manner will germinate on a suitable site.  A nice tap root may first be established by the tree, but it quickly roots laterally into a maze of shallow, fibrous roots. In its swampy habitat, this rooting habit is typical of the tight, poorly-drained soils of its habitat.  This does make it seem more vulnerable to topple from storms, but the afformentioned buttressed base usually makes up for this issue.

On better sites than the swamps, the tree is easily crowded out by more aggressive Sweetgum, Cherrybark Oak, Swamp White Oak, etc.  A slow-grower, this tree may take decades to produce acorns.  Similarly-shaped to White & Post Oak, it has a nice, open, broad branching habit that makes it a nice specimen when older & in an open situation.  Its bark is like Post Oak & its foliage superficially resembles Post Oak/White Oak combination.

In Indiana, it grows in groups, not large areas, along rivers & creeks of the southern bottomland region of southwestern Indiana.  Several populations in Jackson, Washington, Scott & Clark County are northern appendages up the Muscatatuck bottoms from a population along the Ohio River at Louisville.  At Twin Swamp Nature Preserve in Posey County, west of Evansville, the species was associated with Swamp Cottonwood & nearby Baldcypress.  At the Patoka National Wildlife Refuge, in eastern Gibson County, Overcup Oak was growing with Sweetgum, Swamp Cottonwood, Pumpkin Ash & Swamp Chestnut Oak.  North of Montgomery in Daviess County, Overcup Oak made up a significant percentage (~60%) of a woods near Prairie Creek with the other 40% largely Swamp Chestnut Oak.  In western Daviess County, near Swan Pond, in the East Fork White River bottoms, the species was found growing with Silver Maple, Sweetgum, Black Willow & Swamp Cottonwood.  The Vanderburgh County bayou woods off U.S. 41 & I-164 yielded Overcup Oak, Silver Maple, Cherrybark Oak, Baldcypress, Pecan & American Elm.  The northernmost trees are said to exist in western Sullivan County, Indiana, but I have not searched, nor had permission to search for the species there.

Jackson-Washington State Forest yields excellent bottomland/swamp oak forest with stands of Pin, Swamp White, Swamp Chestnut & Overcup Oak in Jackson & Washington counties.  Thomastown Bottoms Nature Preserve in Scott County also yields some Overcup Oak.  Like all other Overcup Oak in the state, though, it is not widespread & trees tend to occur in colonies.

Migration of Overcup Oak has occurred in the past up the waterways & their bottoms of southern Indiana, which provide a great avenue for the tree to move north.  The large swamps in southern Indiana as a result of water backing up trying to get into the Ohio & Wabash to Mississippi River at glacial melt, have provided appreciable habitat.  The lake plains, low areas, slow-moving, not-easily-draining, widing rivers that just cannot expel water quickly with the laminated, tight, silty-clayey lake soils of the area helped Overcup oak become a native Indiana tree.

Fall Leaf Coloring Page

CHERRYBARK OAK (Quercus pagodaefolia)

No other area of the state does the rich bottomland oak & oak swamp forest reach a creshendo like those lake plains & river/stream bottoms of southwest Indiana.  Dominated by swamps more reminiscent of the southern U.S. & wet oak forests like those of the Lower Mississippi region, southern earmarks in the flora appear in these areas.  Here you see native Baldcypress, mistletoe, Winged Elm, Overcup Oak, Swamp Chestnut Oak & others that are strictly southern U.S. flora.  The streams in this part of Indiana are typically slow-flowing, prone to long, murky, silty floods & water backing up, where low, wet woodland is common.  This is the domain of Cherrybark Oak.  A large, massive, long-lived species, with greatest development in the state in Posey & Vanderburgh counties, this tree usually grows in the company of other bottomland oaks (specifically more southern oak species), like Swamp Chestnut, Shumard, Post (Delta Post Oak variety & genotypes) as well as our more frequent Swamp White & Pin Oak (the larger type closely associated with var. mississippiens).  It likes the low, wet woodland which has ponding occasionally, where it grows it has a close association with sweetgum.  It also likes the bottoms near rivers in general that do not flood really deeply, but for shorter periods, in a more shallow manner & likes wetter locations than its close relative the Southern Red Oak (Quercus falcata).

Interestingly, I have found some Cherrybark in the rich coves of hills of deep yellow-brown silty loess with tuliptree, sweetgum & black walnut in its Indiana range.  I especially found this across the Ohio at Audobon State Park in Henderson, Kentucky, where Cherrybark, tuliptree, sweetgum & American beech were found mixed together.  The higher ridges of the park had Southern Red, Black, White oaks, Shagbark & Mockernut hickories with tuliptree & white ash.  It appears the species may creep up coves off river bottoms to these pockets.

Cherrybark Oak is named for its bark, which resembles Black Cherry & its Latin species name pagodaefolia refers to the leaves, which resemble Chinese pagodas when turned upside down.  Also called Swamp Spanish Oak, named after Spanish Oak, another name for Southern Red Oak.  This tree is a beautiful one in shape, foliage & fall color.  That said, it is becoming increasingly available in the nursery trade each year.  I just noticed a garden center in West Lafayette just received a shipment of Cherrybark Oaks.  It seems to have decent tolerance for colder climates north of its native range & with rapid growth, I think you will see more & more of Cherrybark Oak planted in Indiana.  It is a good alternative to Northern Red Oak & Pin Oak.  Like Willow Oak, it is becoming more of a star in the garden trade outside of the southern U.S.

Wind blowing through Cherrybark Oak foliage is beautiful.  The undersides of the leaves are covered in white downy fur & the upper leaf sides are shiny dark forest green.  The wind makes a shimmering appearance with the foliage with the contrasting colors & the finer foliage (compared to Northern Red Oak) looks better.  Leaves often turn maroon, scarlet & red in autumn, while younger trees & the lower limbs of larger trees retain dry, brown winter foliage.  Despite it bottomland & flatwoods habitat, it is adaptable to urban environments & subdivision planting.

Needing openings to re-generate, this tree can only tolerate partial shade for the first few years as a seedling & sapling, then must have lots of sun to survive.  The species is very vulnerable to withthrow, having a shallow rooting habit, which ironically opens up the forest to new Cherrybarks.  Cherrybark Oak has a very competitive relationship with its closest associate, the Sweetgum.  It has to compete with the more aggressive Sweetgum.  According the the U.S. Forest Service, an acid is leached from the leaves with rainfall that suppresses Sweetgum growth.

Found usually as scattered individuals or in groups in its native habitat, it is occasionally very common in a stand (usually with Sweetgum).  I found this in Posey & Vanderburgh County near the Ohio River in bottomland forests.  Growing on those rich, low bottomland soils, Cherrybark Oak has been a real victim of land clearance for agriculture.  In Vanderburgh County, in a sea of farmland of the Ohio River bottom, I found scattered large trees in the middle of the vast farmland, remnants of the bottomland forest.  Considered one of the best of the red oaks, this tree is an extremely important timber trees in the Lower Mississippi area & Mississippi Delta region, where Northern Red Oak does not exist.  Forest trees have long, clear boles with trees reaching 150′ in height.  The trunk may be clear of branches for the first 90′.

Quercus pagodaQuercus pagoda

 Quercus falcata, I_TQBH1590

 

Fall Leaf Coloring Page

COMMON HOPTREE (Ptelea trifoliata)

Most are not familiar with this species of this small understory floodplain & low woods, often near streams, rivers & lakes.  A native Hoosier member of the Citrus family, it is sort of an odd ball species with leaves that look like poison-ivy & interesting, papery & circular seeds, like Rock & Slipper Elm, but larger.  With nicknames of Wafer Ash, Skunkbush (its flowers, wood & bark have an unpleasant odor) & Prairie grub, it doesn’t get too large at 30′ with a diameter of 1′ underneath much bigger trees.  Liking the same habitat as Ashleaf Maple (Boxelder), Black Maple, Ohio Buckeye, American Sycamore & Black Willow, it may prefer the understory of low woods, but can be found in full sun, too on swamp borders & near lake sides.  An example are the hoptrees growing at Celery Bog near the trail by the apartments at the end of Cumberland Avenue.  Here, it grows with Black Willow, Green Ash & Rose Mallow, as well as Swamp Milkweed.  In the understory it may be crooked with one trunk, but trees more in the sun often have multiple trunks.

The most common associates of Common Hoptree are Black Willow, American Sycamore, Silver Maple, Green Ash, Ashleaf Maple, Eastern Cottonwood, Buttonbush, Black Walnut & American Elm.  In far southern Indiana, you can find it with Cherrybark Oak & Sweetgum, as well as Swamp Privet.  So, it can tolerate periodic, but not long, long duration flooding & germinates on fresh floodplain loam of the understory woods in shade or sun.  It has impressive flood depth tolerance, similar to Ashleaf Maple, Silver Maple & American Sycamore.  Like Silver Maple, it doesn’t mind a deep flood, it just can’t have constant, consistent standing water.  That is an oddity about Silver Maple, it tolerates floods well, but if it will struggle big time if it is growing in a long-duration submergence event as a young tree & even older one.  I have seen Silver Maples all wilted, half dead & with red & orange foliage in summer when stuck in tight clay soil with standing water.  Ohio Buckeye likes brief floods in loamy/sandy loam floodplain soil & low, wet woodland, but doesn’t like persistent inundation & saturation.  Common Hoptree is no different.

Leaves of the hoptree turn often yellow in the fall & occasionally red & orange.

A slow-grower, this tree blooms in late spring-early summer & sheds its seeds through late fall & into winter.  Frequently, the papery seeds will cling to the tree well after the foliage has been shed in fall.  The seeds are carried by wind on its papery “wings”.

There are several subspecies of Common Hoptree in the United States.  Ours, which is found viewing area-wide is found strictly in the historic prairie/barrens band from Missouri to Illinois, Indiana & Ohio to southeastern Ontario.  This subspecies does have an affinity for the low, wet woodland near/around prairies, savannas & barrens.

About 5 other subspecies are found in the U.S.  One from Arizona to Mexico to Texas, another Texas to Kansas, another in the southeastern, even another in Florida.

Ptelea trifoliata - Common Hoptree

[Ptelea trifoliata Common Hoptree at Minnesota Landscape Arboretum]
photo1456638.  Leaf buds of a common hoptree, Ptelea trifoliata, sprouting in spring.

Common Hoptree (Ptelea Trifoliata)

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