Great NebraskaNaturalists and Scientists
Raymond J. Pool, Notes, 1912, Part 2
In th morning Folsom and I went out for a collecting trip and to show him the country. Lithospermum gmeliniis in it its prime now — while both L. angustifolium and L. canescens are past their flowering period. Are found Penstemon gracilis and P. grandiflorus very common here. In the afternoon I developed 5 X 7’s and Folsom made up fixing media and grades of alcohol.
June 16— Sunday.
Wrote letters. Changed press. In P.M. Folsom & I walked to Halsey and back.
Still cloudy and cool. Folsom began his work on Yucca. Wrote on “part 2.”
See 1911 notes for the general aspects of the vegetation about Halsey. This is in the Bunch Grass Yucca Association in so far as the uplands are concerned.
Members of first layer in woodlands at Halsey are:
- 1. Parietaria pensylvanica
- 2. Galium triflorum
- 3. Fragaria americana
- 4. Alsine longifolia
- 20. Elymus stricta
- 21. Oryzopsis micrantha
Members second layer are:
- 1. Rhus radicans
- 2. Lappula deflexa
- 3. Geum strictum
- 4. Agrimonia striata
- 5. Monarda fistulosa
- 6. Onoclea sensibilis
- 7. Dryopteris thelypteris
- 8. Muhlenbergia racemosa
- 9. Symphoricarpos occidentalis
- 10. Rosa arkansana (margin)
- 11. Asclepias syriaca
- 12. Celastrus scandens
- 13. Phryma leptostachya
- 14. Circaea lutetiana
- 15. Galium aparine
- 16. Tholitnen pupurascens
- 17. Solidago canadensis
- 18. Salomonia cobrensis
- 19. Vagnera stellata
Members of the third layer are:
- 1. Prunus Americana
- 2. Prunus melanocarpa
- 3. Crataegus occidentalis
- 4. Cornus stolonifera
- 5. Amorpha fruticosa
- 6. Salix longifolia
- 8. Vitis cordifolia
Members of fourth layer:
- 1. Salix nigra
- 2. Fraxinus lanceolata
- 3. Celtis occidentalis
- 4. Acer negundo
July 3 — Left Halsey for Seneca. July 4 left Seneca for a tramp across the hills to the Dismal River. The morning was sultry after a rain during previous night. For about two mi. south
of Seneca the hills are very high and sandy. Bunch grass is develeped to a good degree here
and in general the land and vegetation is very much as at Halsey. About five miles south rather conspicuous valleys begin. These valleys are from
300 yds. wide to 1/2 mi. long to 1/2 mi. wide by 2 mi. long. Some farming is being
attempted in these valleys, all of which are dry valleys. The native vegetation of
these valleys is usuallly dominated by Stipa Comata, with a little S. spartes in mixture.
These rather narrow and short valleys give way a little farther south to valleys much
wider and longer with much hay land or farms which contiunue until the high hills
and ranges near the Dismal are reached. The valleys to the south then gradually lose their importance become
much smaller until about 2 mi.
from the Dismal Valleys disappear entirely and the very high hills on the Dismal are much like those on the Middle Loup at Seneca.
This narrow valley strip marks the eastern limit of dry valleys in the southern hills.
East of of a line drawn from Seneca to the Dismal Valleys of ever small size quickly give way to choppy hills. While westward of the same hills
the valleys rapidly broaden out until the broad wet valleys of McPherson and Grant Counties are reached. From this point westward the valleys again become smaller and
less numerous as one passes into Garden and Morrill counties.
The vegetation on the Dismal south of Seneca is practically the same as at Black’s Ranch farther east. In numerous place here Fraxinus lanceolata is seen climbing the steep south slopes from near the water’s edge and appear to
be spreading to a considerable degree. Considerable Lepargyrea argentea and Juniperus scopulorum was seen at this point. The hills on both sides of the river at this point are very
high averageing about 300 ft.
We passed through some sheep pasture where the range was suffering very greatly from
these animals. The grains and all herbiage was
being cropped and tramped to very dangerous degree. The animals were very “measley”
looking — about 1000 head of ewes & rams & 300 lambs.
I saw some fields that had been broken out about 7 mi. south of Seneca that were
in a deplorable condition. They were in good level valleys with good soil for alfalfa
but had been allowed to go to weeds to a frightful degree. Helianthus petiolaris and H. Annuus controlled practically all such fields some of which contained as much as 60 a. If fields are allowed to stand idle here, i.e. if not used for crops, They should
at least be surface cultivated to keep down weeds and to conserve or “store” water
for succeding crops. All such fields would produce fine crops of alfalfa or timothy.
Left Seneca at 10 am for Orella. All along the way to Alliance there waere many signs of the recent heavy rains. Water was standing in many of the
dimensions and all streams were muddy. Ipomoea leptophylla was just begining to bloom, and Phalaris arundinacea, Asclepias speciosa and A. incarnata were in full bloom in wet meadows and valleys. Batrachium divaneaten was still in blossom in many places. Arrived Ocella at 5 p.m.
From Crawford northward from Pine Ridge one soon comes to the [Buce?] Clay formation with its characteristic erosion figures and Bad Lands. There extends alon g the north face of Pine Ridge for many miles from the Wyoming line in Nebraska. They extend from the base of the Ridge for an average of 6-10 mi. northward. In some places they are very rough, deep and
barer. While in others they are little more than patches of outcropping clay which
here and there some rock in mixture.
In some places the whole region is no more than a mile across from south to north
while in others it is several miles. Here and there great knobs or points of clay
stand out as isolated points over the generally rolling landscape. Some such points
are 100 — 150 ft. in height and absolutely bare of vegetation. there are two quite
distinct clays here: one a light green which is least common, and the other a red
or flesh colored clay which is much the more common type. The green clay is in some
places beneath the red clay. The two contain much rock, quartz and fossils.
Bad Lands Plants 1912
- 1. Sideranthus grindelioides
- 2. Pachylophis caespitosus
- 3. Arenaria hookeri
- 4. Leucelene ericoides
- 5. Artemisia cana
- 6. Allium reticulatum
- 7. Kuhnistera purpurea
- 8. Kuhnsitera candida
- 9. Paronychia jamesii
- 10. Agropyron dasystachum
- 11. Opuntia polyacantha
- 12. Cymopterus montanus
- 13. Sitanion elymoides
- 14. Eriogonum multiceps
- 15. Malvastrum coecineum
- 16. Prosalea floribunda
- 17. Linum rigidum
- 18. Calochortus gunnisonii
- 19. Koeleria cristata
- 20. Artemisia tridentata
- 21. Eriocoma cuspidata
- 22. Bulbilis dactyloides
- 23. Bouteloua oligostachya
- 24. Atheropogon curtipendula
- 25. Carex filiformis
- 26. Helianthus petiolaris
- 27. Stipa viridula
- 28. Stipa Comata
- 29. Oreocarya suffruticosa
- 30. Mentzelia decapetala
- 32. Artemisia frigida
- 33. Chenopodium album
- 34. Sarcobatus vermiculatus
- 35. Agropyron repens
- 36. Lesquerella spatulata
- 37. Yucca glauca
- 38. Artemisia filifolia
- 39. Phacelia leucophylla
- 40. Erigeron pumilus
- 41. Chrysothamnus graveolens
- 42. Gutierrezia sarothrae
- 43. Atriplex hastata
- 45. Dondia depressa
- 46. Opuntia humifusa
- 47. Cactus viviparus
- 48. Homalobus montanus
- 49. Atriplex canescens
- 50. Rhus trilobata
- 51. Lepargyrea argentea
- 52. Polygala alba
- 53. Juniperus scopulorum
- 54. Betula occidentalis
The Bad Lands are cut thru a grass sod composed of Bouteloua oligostachya, Bulbilis, Stipa comata, Stipa viridula, Agropyron repens, A. dasystachyum, and Sitanion elymoides. This has been cut and gullied in every direction leaving many isolated pastures
of the short grass sod. Secondary species in the sod are Opuntia polyacantha, O. humifusa, Eriogonum multiceps, Allium reticulatum, Kuhnsitera candida,K. purpurea, Koeleria cristata, Psoralea floribunda, Calochortus gunnisonii, Linum rigidum. Carex filifolia random in many place the the principal grasses in abundance.
Such vegetation as this covers the rolling ground everywhere outside the bad lands
proper or in old established grassland within them. A close sod is usually present
over such areas. Agropyron pseudorepens and Stipa comata are the most abundant grasses and there share with Bouteloua and Carex filformis in producing said sod.
It is through such a sod as this underlain by Bank Clay that the Bad Lands have been cut. The Bad Lands are merely excessive gullies eroded from Bank clay. In each area one finds a completely
developed drainage system of small scale. The sides of the ridges or gullies are
usually absolutely barren and is steep as to make very precarious footing. The clay
is very hard and takes into small surface scales about 1-3 cm. across. There being somewhat like shale break off under ones weight and introduced
considerable danger in climbing about over such places. Here and there one sees a
bit of fossil or areas in which there is considerable hard rock. Sometimes this hard
rock is left while the clay is taken away from beneath it thus producing a so—called
“mushroom” effect. In one place south of Ocella about 3 mi. very large rocks have fallen into the gullies and there are now balanced in all sorts
The most of such slopes are devoid of plant life. But sooner or later vegetation begins
to creep up from below and to fall in over the rim so that one frequently finds some
of the characteristic species of the surrounding sod land becoming established with
the Bad Lands area.
The first plants to share in the succession are mat and rosette species such as Arenaria hookeri, Atriplex hastata, Paronychia jamesii, Eriogonum multiceps. One finds there species widely distributed throughout the bad lands on the lower
slopes and narrow bottoms or flats that abound. The vegetation of such places is often
comprised of scattered mats or rosettes of these species alone. One frequently sees
Mentzelia decapetala along the sides of dry gullies associated with Eriocoma cuspidata, Penstemon glaber, Phacelia leucophylla, and Stipa spartes. Agropyron dasystachyum is frequently very abundant over the more alkaline areas within and without the Bad Lands.
As the succesion progressese such plants as Artemisia frigida, A. cana, A. filifolia, Chrysothamnus graveolens, and Atriplex canescens appear. Then Gutierrezia sarothrae, the cactuses and the grasses and sedges until the characteristic short grass sod
is again developed.
July 7 — Sunday
Went to Crawford on way to Oasis
July 7 — evening — arrived Chadron
July 8 — Chadron
Chadron is north of Pine Ridge about 1 mi. in a Stipa — Schedonnardus area. Stipa comata is very abundant here, and of Schedonnardus paniculatus is also very abundant as a secondary layer. These two graves control the situation
scattered thru there are the various legumes and other species characteristic of the
High Plains Region.
Penstemon grandiflorus in great abundance all along here.
Sagebrush — Greasewood Foundation
Agropyron association of alkali feats.
Pepper — grass Cactus assoc.(387)
Mar & rosettes (379)
Stipa formation 387
Agropyron formation 387
As modifying the pepper — “grass—cactus formation”
Beard-grass formation 361
Prarie gras formation
Buch Grass assoc.
Blow out ”
Botanical Survery of Nebraska
Conducted by the Botanical Seminar
South from town one comes to an outlying spur of Pine Ridge which posseses the most of the characteristics of the P.R. vegetation. in the evening
of the 9th we left for Valentine. These same conditions prevail for many miles east from Chadron. There is much timber along White River here — in many places producing a dune forest composed of Populus sargentii, Ulmus americana, Celtis occidentalis, Acer negundo, Salix nigra, Fraxinus lanceolata, and Prunus melanocarpa, and P. americana.
At Gordon, about 2 mi. east the new R.R. first enters the Sand Hills. Here Stipa is the controlling grass over the Sand Hills. Such hills are characteristic for the whole way to Valentine and extends for several miles north from the Railroad.
July 10 — Arrived Valentine last night.
In morning at 8 left Valentine for Mrs. Cook’s. For 4 – 5 miles south of Valentine the land is rather level and the soil, relatively. At 4 — 5 mi. out we came to the
first sand hills, which however, are rather old since they are few blowouts here, i.e. few active blowouts. There conditions prevail until the Niobrara is reached with its two types of vegetation — the hardwood and coniferous types.
Crossing the river one comes at once to the abrupt sand hills with many blowouts and Yucca — Andropogon
The hills immediately south of the river are very high and steep. The Pinus ponderosa and less noticeably the hardwoods follow the Gordon Canyon and simliar spring trenches, tributaries to the Niobrara, for many miles into the hills. The Gordon carries pines for at least 8 mil. into the hills from the Niobrara. With this arborescent vegetation then follows many of the species of high plains
and Pine Ridge plants.
Arrived at Mrs. Cooks at 2 p.m. Had dinner then Folsom and I went out on Hackberry Lake for a couple of hours. Potamogeton richardsonii, P. pectinatus, P. zosterifolius, P. natans, and P. lonchites, Ceratophyllum demersum, Batrachium dwanicatum and Myriophyllum spicatum were abundant, as were also Lemna trisulca which was beginning to come to the surface
Went out southeast between Dewey and Clear lakes then came back home via north shore of Clear. On the divide between there two ladies the are high and there are numerous blown
outs in various stages of being reclaimed. There are no active blows here however,
i.e. blowouts into which plants have not yet obtained a start. this area has been
heavily grazed so the Muhlenbergia pungens, and Redfieldia are everywhere common and the sand shows at short intervals. There is no Ceanothus ovatus here at all, and Prunus besseyiis only moderately common. Yucca glauca is very abundant, so that with Muhlenberigia the formation here has a little stronger relation to the Yucca-Muhlenbergia association than to the Yucca-Andropogon association though this relation various on the different hills.
On the north shore of Clear Lake wear the east end there are a number of large “cattle runs” that are very rugged
and bare. There have been blown out from the beach to several hundered feet back in
somes cases. Redfieldia is begining to cover some of the slopes of these incipient sand draws and Psoralea lanceolata is also coming in in many places. Most of the swampy area about Clear Lake is at the east end, tho the lake as a whole is quite freom from Rushes or aquatic
In the afternoon I went out on Hackberry Lake and made a number of hygrometric determinations which are found on another page.
Went to falls on Snake River about 15 mi. N.W. from Mrs. Cooks. All the way over we traveled by way of the hay meadows. the hills are of average
height but are much better covered by vegetation than those in Thomas Co. or in eastern Cherry Co. There were very few blowouts seen on the way — even the older ones were scarce and
were well covered. The valley of the Snake is lined by very high hills especially on the north and west side. These hills are
about 400 ft. about the river level. On the east side there is extensive river flat
vegetation upon a clayey soil with Bouteloua predominating. Considerable
Andropogon scoparius has come down from the hills and has become established on the flats. No Ceanothus was seen on the way.
The gorge of the Snake at and below the falls is very precipitous and rocky. The river has cut through the
hills and the Arikarce formation to a depth of about 400 ft. The sides of the hills
on the upper slopes and the outercropping rocke covered by the typical Pine Ridge vegetation of Pinus ponderosa comprises the bulk of the first layer. Some of these trees are very large and stocky.
Mixed with the pine Juniperus scopulorum is quite frequent also as very well developed trees some of them 40 ft. in height.
The upper stretches of the canyon show such shrubs as Rhus trilobata, Ribes aureum, R. floridum in abundance. As one descends into the gorge the deciduous trees become commoner
until in the bottom this belt is very well developed. The tree that are common are
Populus sargentii, Ulmus americana, U. racemosa, Celtis occidentalis, and the two prunis P. americana and P. melanocarpa. The first three species occur as very large individuals while the last ones form
thicket type of vegetation. Parthenocissus quinquefolia, and Vitis cordifolia, Clematis ligusticifolia, and Celastrus scandens are common liamas that cover the low trees and shrubbery with a dense cover of tangled
wire — like stems. Rhus trilobata occupies rocky areas by the characteristic colonies of 4 — 10 ft. in diameter. Rhus glabra is abundant on the upper slopes where it exists in the usual thicket association
with grasses beneath. Campanula petiolata, Amelanchier alnifolia, Arenaria hookeri, Paronychia jamesii and Orophaca cespitosa one other common Pine Ridge species that were common.
Toward the valley of the Sanake and on the lower slopes of the hills on each side of the canyon the Stipa comata association is very conspicuous. This grass covers wide stretches of blow out, less
hills back from both sides of the river and sharing the uplands with Andropogon scoparius. There is little Yucca glauca here and not Muhlenbergia purpens was seen anywhere on the uplands. The hills here then are relatively old as compared
with those farther east and south.
July 16 — Wet Meadow Studies
The earlist stage of the wet meadow that may be considered as terminating the Marsh
Formation or imitating the Wet Meadow Foundation in the Rush Assocication or Meadow.
As a rule this association is found upon soil that is still way wet, was in mid summer
water may be squeezed by the hand from the soil and the ground is more or less springy
if the soil is humic, if sandy, the springy nature is not present. As a rule however
there is a great amount of humus present and the general nature of the soil in many
places is decidedly “mucky.”
The facies of this association as usually Juncus balticus, J. tenuis, J. longistylis, Eleocharis palustris, E. acicularis, and E. acuminata.
Cat Tail & big Sedge in middle, with Calamagrostis, as upper layer — Campanula, Dryopteris, Mentha, Nanubergia, Scutellaria as 24 layer.
E. acuminata persist for long time within shade & moisture of Typha and big Carex where ground covered with carpet of moss and few straggling G. trifidum — wet in Spring. In some places Typha occurs first in with Scirpus. Little farther toward W. in the
fern Campanula belt begin.
Wet Meadow Species
- 1. Juncus balticus
- 2. ” tenuis
- 3. ” longistylis
- 4. Scirpus pallidus
- 5. Eleocharis palustris
- 6. ” acuminata
- 7. ” acicularis
- 8. ” glaucescens
- 9. Dryopteris Thelypteris
- 10. Ovoclea sensibilis
- 11. Phalaris arundinacea
- 12. Calamagrostis canadensis & neglecta
- 13. Typha angustifolia — relict
- 14. Scirpus americanus relict
- 15. ” validus — relict
- 16. Asclepias incarnata
- 17. Mentha canadensis
- 18. Stachys palustris
- 19. Teucrium occidentale
- 20. Scutellaria galericulata
- 21. Campanula aparinoides
- 22. Naumburgia thyrsiflora
- 23. Polygonum emaciatum (relicts)
- 25. ” amphibium (relicts)
- 26. ” hartwrightii (relicts)
- 27. Salix fluviatilis — belt about Typha etc.
- 28. Cicuta maculata
- 29. Carex — big — stem
- 30. Ranunculus cymbalaria
- 31. Strophostyles pauciflora
- 31. Sagittaria arifolia —relict
- 32. Rumex britannica (relict)
- 33. Rumex hydropiperoides
- 34. ? datum (in ferns)
- 35. Helianthus tuberosus (on margins)
- 36. Steironema ciliatum
- 37. Galium trifidum
The Wet Meadow Formation
Wet meadows are always members of a succession of which the Lake and stream formation
and the Marsh Formation are preceeding types. The earliest stage of association in
Wet Meadow Formation may either be considered as terminating the Marsh Formation.
This is the Rush Association or meadow.
As a rule this assoication is found upon a soil that is still very wet and soggy.
There is much humus and one may always bring water to the surface by a little tramping
with the feet. Sometimes the association occurs where there is less humus and more
sand and is such cases the sand may be made to yield water by squeezing in the hand.
Since in may places this association occupies soil that was originally lake bed the
surface is liable to be exceedingly mucky and to reveal the remains of snails and
other aquatic animal forms.
Frequently in those valleys with lakes or ponds present this association is seen
developed in a more or less well defined belt about the body of water back from the
In alkali situations it is common to find Triglochin maritima and Plantago eriopoda. The former often froms a very tenacious sod in soils that are so alkaline as to
have salts separated out on the surface. Distichlis spicata is also often found in such situations covering wide areas with a characteristic
close sod to the exclusion of all other plants. Distichlis spicata is also very commonly present in a dune — soddy layer.
Menyanthes trifoliata is common in low Rush meadows where it forms characteristic low patches of closely
Gerardia besseyana is frequently very abundant in small areas where the rushes and sedges are more open
The dark purplish areas are quite clearly set out by color form the surrounding vegetation.
In meadows from which surface water has disappeared the assoiciation is more diffuse
or irregular and often alternates in the wetter portions with the other associations
of the formation.
The species that give character to this association are Juncus balticus, J. tennis, J. longistylis, J. nodosus, Eleocharis palustris, E. acicularis, E. acuminata, and Scirpus atrovirens, and S. americanus as relicts from the Marsh Formation. Scirpus validus also often persists for a number of years as a relict. So also Typha latifolia remains as a few widely scattered slumps or individual plants until the soil has
become quite dry. From the fact that the association becomes very wet and seems very
much during the spring months one readily sees why these common relicts are able
to persist. The surface of such places is very often cover by water that does not
disappear in some cases until mid-summer.
The presence of te Junci and Eleochari in close aggregation is to be considered as the typical expression of this association.
In such habitats as outlined above there together or in pure stands frequently cover
The dense thickets of Willow — probably S. fluviatilis, belong either in th Rush or Fern meadow associations. Extensions areas composed
of round topped topped bushes about 8 ft. in height are very common in the wet meadow
region. There are to be seen in best development just southside the March Foundation
and occupying ground very similar to that of the Rush or Fern associations. In fact
the willow very often have the appearance of islands or tongues scatterd over both
of there associations. The willows produced a deep shade within which the Ferns are
most abundant of the meadows species although, Campanula aparinoides, Galium triflorum, and a few other species are formed there in greatly modified forms. Amorpha fruticosa is present in small quatities in there willow patches. There shrubby mosses often
exist as a perfect belt about the Rush — Typha — Phragmites combination.
Caltha palustris abundant in many wet meadows.
The ground with a close sod. Eleocharis palustris is often seen in such close stands as to completely dominate wide stretches and to
keep out practically every other plant. Occasionally one finds a cleanup of Pamenlaris ameica or Catabrosa aquatica in such places, or the stems of some of the above named relicts. But where the association
is more open the flora is more varied. A common type of distribution is to have a
rather thru cover E. palustris with an almost equal mixture of the Junci, and from this the relation varies in both directions. Sometimes on the sandy shores
of lakes and ponds throughout the region a perfect carpet of E. acuminata or E. acicularis is developed just outside the water live in which may occur scattered colums of Scripi and Junci. There carpets are especially noticebly about the Cherry Co. lakes. It is here also that the carpets of Halerpestes cymbalaria cover the wet sand for many square meters. These patches are especially striking
when the plants are in bloom.
In the outer or or drier potrtions of the association such plants as Lycopus lucidus, L. americanus, Mentha canadensis, Lythrum alatrum, Steironema
Spirodela polyrrhiza in colonies on wet sand midst rushes.
Sometimes the associations of this formation are so telescoped that the identity of
the various assoication is all or very nearly lost.
ciliatum, Potentilla paradoxa, P. monspeliensis, Scutellaria glabriuscula, Lotus americanus, Naumburgia thyrsiflora, and RumexHydropiperoides, are more or less frequent and abundant. Some of these often form extensive patches
through this and the following association.
The Fern Meadow Association
In the regular succession backward from the shore the one association that is most
widespread and typical is the fern meadow. This
is usually occupies rich soil which has been badly broken up by cattle and horses coming
down to water until there arem innumerable depressions in elevation with a differences
in elevation of about 2 ft. ofcourse in many places not open to the stak the ground
is much more smooth. The soil is always higher and dries than in the last association
and is better drained.
Color is given to there areas by the presence of two ferns, Dryopteris Thelypteris and Onoclea sensibilis. The former is much the more frequent and abundant throughout the wet
meadow lands of the region. Often there ferns, especially the former, are developed
to the degree that alomst everything else is excluded from the area of ferns — sometimes
a few plants of Calamagrostis canadensis or others. Dryopteris is rarely seen within th eshade of deeper associations but Onoclea is a frequent members of shaded habitats. In thy extensive wet meadow of Cherry Co. These areas dominated by the ferns are often more or leass notted by the presence
of patches of accessory species that dominat their own particular patches: Campanula aparinoides frequently occurs as a layer from this association well into the hay meadow and covers
hundreds of square meters with its tangel of sprawling stems; the source is true in
less degree for Galium trifidum, Naumburgia thyrsiflora, Crepis runcinata, and Asclepias incarnata, and many species that are probably members of the following association.
The Hay Meadow Association
In the most of the many extensive and broad valleys of the northern portion of the
Sand Hill Region, even with those that still show ponds or lakes, there is usually a wide expanse
of drier land coverd by grasses and associated plants that are cut for hay the owners.
In the broader valleys this type of vegetation covers by far the most of the land.
* The soil as a rule is hard and smooth and provided with a good water supply river
it is only a few feet above the water table. I have chose to call this the Hay Meadow Association from its very obvious economic importance. This association is included in the Wet
Meadow Formation of Pound and Clements but is not treated to any degree by these authors. The association gives way in the
drier situations in wet valleys and in the dry valleys outside the wet valley region
to the dry valley or pocket association which very soon then becomse the Bunch Grass
The species that give color to this association are in the main grasses. These are
many hundreds of acres of
Agropyron smithii common
Panicum implicatum forms low hairy carpets in more open areas.
Spartina cynosuroides as scattered tall stems in low places. Eatonia obtusata is very common and of valuabel grasses of the drier situations.
Bromus ciliatus common on the highest land in there valley there is considerable Stipa comata, but here the grass is much thinner and the vegetation is more of the dry valley
or high plains type.
this sort of vegetation within the wet valley region. The soil sandy loam is firm and soddy and is provided with a considerable supply of humus. The species
that are of widest distribution in such areas are: Agrostis alba, A. hyemalis, Agropyron repens, A. tenerum, Calamagrostis canadensis, C. neglecta, Panicum virgatum, Elymus canadensis, Beckmannia eruciformis, Equisetum variegatum, Koeleria cristata, Andropogon provincialis, and Muhlenbergia racemosa. In some places certain of there are more abundant than others, for instance the
Agropyrons are liable to be found in greater abundance on the higher and dryer areas while Elyrum is to be found usually in the lower areas. But typically the grasses are so mixed
that no alteration of species can be discovered at all.
Hordeum jubatum another very frequent and abundant species. This species is often seen as a belt
about ponds or wet depressions. Agrostis hyemalis is also often seen in a finely developed belt of 10-60 ft broad about lakes and ponds
just back of the Rush association. Sometimes this association joins directly upon
the various aspects of the Marsh Foundation
Rudbeckia is usually on lower ground than Ratibida — they were frequently show this kind of zonation about low places
where the Rush assoiciation or the Fern association are lacking. Where the soil transistion
is sudden one often finds the hay meadow joining directly the hay meadow joining directly
the Sagittaria, Phragmites or Scirpus combination. More usual however there tow types are separated by a belt of Polygonnum hartswrightii, or as typical the Rush Association tho this may be but a narrow belt.
There are many secondary species to be found in the these meadows. Besides a few relicts
such as Scirpus americanus and S. validus, Typha latifolia etc. from former associatioin the following species of the hay meadows. Those that
from conspicuous patches, that might perhaps be given the name society, are Cicuta occidentalis which is frequently of controlling abundance over the wide stretches in the lower
situation of the association during the month of July. Then also Naumburgia thyrsiflora, Mentha canadensis, and Stachys palustris are very frequent and often abundant in swales so as to be locally very conspicuous.
On the higher ground Psoralea argophylla forms perhaps the most striking groups of any secondnary species. This plant occurs
all the way from scattered individuals to compact patches several
When such a meadow is pastured to a certain degree many of the valuable species are killed out and the secondary species become
thirsty emphasized as the soil becomes drier and more open. Such things as Solidago rigida, Euthamia graminifolia, Solidago missouriensis, and were in more seriously trampled areas, Helianthus petiolaris, and Cleome serrulata come in in dense patches. These meadows should be pastured with great care with reference
to maintaining a good cover of the valuable species and a proper fencing and notation
to keep the stock from the wetter situations at certain seasons in order to prevent
the formation of “bogs” with all disagreeable consequences.
acres in extent that are noticeable from considerable distances. Ratibida columnaris, and Rudbeckia hirta are two composites that show a decided tendency for aggregation and to cover wide
stretches of meadow land with their yellow colors during July. So called Erigeron
ramosusbellidiastrum often occurs in rather close stand over wide stretches in the lower portions of the
meadows Lotus americanus is found in almost all situations in the meadow but is usually more abundant upon
the harder drier soils. In such places the species in sometimes alomst exclusive.
In the moister situations, as in swales. The red lily, Lilium umbellatum, becomes gregarious and producer during July one of the most striking patches to
be found in any sand hill habitat. Lycopus lucidus and L. americanus often form patches of about the height of the associated grasses. Lobelia spicata is a very frequent inhabitant of other meadows, but the individuals are usually widely
scattered. Clusters of Meibomia canadensis are common on lower areas in hay meadows as well as within the Rush and Fern meadow
combinations. Habenaria leucophaea is a conspicuous “solitaire” during the month of July. Linum sulcatum
Additional sedges here from 1912:
- Scirpus fluviatilis
- ” pallidus
- Carex stricta
- Eleocharis glaucescens
- ” scoparia
- Carex comosa
- ” hystericina
- ” nebrascensis
- ” marcida
- ” gravida
- ” longisortius
- ” stipata
is very frequent, and occassionally becomes sufficiently abundant and aggregated to
be conspicuous. Amorpha canescens has wandered in from the hills and is to be found on the elevations then the meadows.
The Stream Side Association
This association differs only slightly frm the Rush and the Fern Meadow associations.
The streams of the Sand Hills usually occupy a narrow valley with little or no flood plain. In many places this
valley becomes so reduced that only a very narrow canyon persists. The most “canyony”
streams of the whole region are Dismal River which rises in a marshy region of Hooker and McPherson Co. and flows eastward to the Loup at Dunning, and the Snake which rises in Sheridan Co. and follows a northeasterly course to Niobrara in norhtern Cherry Co. The Loup rivers, the three of which all arise within the Sand Hill Region should be included in the same series.
This association is to be found in the shady or sandy situations