376 ENTOMOLOGICAL SOCIETY
burst
upon
us in thevalley,and
rainwithblastsofwind
obscured the scenery.I
went
to sleep for awhile,and when
Iawoke,
behold theearthhad grown
green with grass.A
refreshing coolness succeeded the hot breath of the desert.The
mountainscame
closerand
the valley rosebetween
them,and
cultivated fieldsofalfalfabegan
to appear. Finally, grovesof red-limbed fruittrees, with shining threadsofirrigation waters, linedour way,and
at sunsetthecows came
troopinghome
tothefarm yardswading
knee deepinclover.This
was
the end of the desertand
thesummit
of the divide atBeaumont. Thence we
whirleddownwards
in the darkness, passingtowns
innumerable, with junctionstoPasadena, Redlands,Pomona, and many
others, wellremembered
names.At
lastwe saw
the twinklinglights of a great city,and
the various stations ofLos Angeles were
called.LETTERS FROM THE SOUTHWEST.
SaltonLakeinthe Colorado Desert andItsInsectFauna.
BY H.
G.HUBBARD.
YUMA,
ARIZ.,March
30, 1897.In regard to
what you
say of the insects collected byme
in the desertwashes
atPalm
Springs,thattheCalifornia desertwas
once anarm
of the Californiagulf,you
are surely mistaken.The
shells foundinallthisregion areallfresh-waterremains;and
themarine shells are found only to the south of the dividewhich bounds
theSalton Sea.The
desert sands bordering thisdepression are white withsmall shells, but they areall of the usual fresh-water forms. I havepreserved afew
of the smallerand most abundant
forms. I believe even frommy
short visit to Salton that Ihavegot the essentialcharacter of the fauna. It contains abso lutely no marine forms and
none
at all'modifiedby
the peculiar environment, except, perhaps, the brine fly(Ephydra), which
is quitedifferent from the species inhabiting the GreatSaltLake
of Utah.There
is no BrineShrimp (Artemla)
in anyof the saline springs,and
it isveryevidentthatthe origin of the salinedepositisquite recent
and
evennow
in process of formationfrom
thenumerous
saline springswhich
surround the basin bothon
the northand
south.At
the surface these springs contain onlyfrom
i to6 per cent, of solid saline matter, but at a depth of
one
ortwo
feetthe brine has a density or 27 per cent.,consisting ofboth chloride ofsodium and
sulphate of soda (Glauber's salt).At
no very remote period thisbasinwas
filledwith fresh water, but neither thisnor any other part of theColoradodesertnorth of theSan
Jacinto rangewas
ever marine.OF WASHINGTON. 377 The
SaltonSeaorLake
isoneof the greatest naturalwonders
of theworld. Itisashallowdeposit,onlyoneortwo
feet indepth, of solid saline matterand
is 8 mileswide and
20 miles long, surroundedby
saline springswhich
buildup mounds and
cones ofsaline matter and mattedroots of cane grass, back ofwhich
isthe ordinary desert vegetation,gradually disappearing as it de scends from the level of260feet toabout 265 feet, at
which
point only oneplantflourishes, andthis plant isthe onlypeculiar saline plant, outside of thegrasses, to be found in thebasin as far as Iknow.
This plant is Allenrolfeaoccidentalis,and
I mailyou
herewith a few stickswhich
containlarvaeofaPtinid beetle1and
alsoa Clerid
enemy and
perhapssome
other things. It yieldsat last to thesolid induratedcrustof saltand
sodawhich becomes
finallyan
unbroken
plain ofpuresalt,the lowestdepression being 280 feetbelow
sea level at four miles from the edge of thesalt plain.Here
thesoda sinksbelow and
formsa.layerabouta foot thickand solid as a rock.Above
this isa layer ofblackmud and
then a surface layerofpuresaltfrom afoot to 18 inches in thick ness.The
surface ofthesalt isdry and hard, resembling iceand
glistening in the tropical sun with the million scintillations of a polarice floe; white, harder and smoother than a sheetofsnow.
I reached Salton late
on
Saturday(March
28).Sunday was
a fineday and
I devoted themorning
to an examination of thesalt springsand
the fauna of the basin.The
line of debris from the great overflowof the waters of the Colorado River in 1891was
plainlyvisible
upon
the surface of the salt nearthe shores.But
every stickand
floatedrailroad tiewas
solidly fasteneddown and
onlyafew spiders lurked under the fragment, evidently livingupon
insectsblown
outupon
the saltplain.Far back
from themargin
of the lake the earthisstiffened with saline matter,and
thefeetbreak throughas inwalking
over cultivated fields
on
frostymornings
in spring.Here
there is no vegetation except the Allenrolfeabush growing upon
smallmounds, and
the grass about the salt springs, but even this last isencumbered and
encrusted withsnowy
incrustations.There
islittlechance for insect lifebecause of these thick incrustations,
which
binddown and
solidify every particle of soiland wood,
but on themounds and
aboutthe rootsof the Allenrolfeabeneath the thin crust isa dryand
dustysoil, largelyconsisting of pulver ized salinematter, and here are a fewHemiptera
andspiders;and
in the larger stems of the Allenrolfea I found the larvaemen
tionedbefore.
Where
the springsbreakforth inlargervolume and
form smallflowingstreamlets there are patches of grass encrusted with mineral matter,and
even themud
alongthese rivulets is'ThePtinidbeetlewas successful}'bred atWashington and proves to be Ctenobium cinereum Horn, originally described from southwestern Texas.
The
Clerid larvahasnotbeenbred. E. A. S.378 ENTOMOLOGICAL SOCIETY
bordered with ice-like crystals
and
crusts.Where
these enter the water,when
turned over they are lined with greenalgaeand upon
thesethere is in vastnumbers
asmall Hydrophilid (Creniphilus n. sp.) with pale elytral tip,and
in almost equalnumber,
in themud
beneath, a palePhilhydrus (Ph.diffusus Lee.) of largesize,and
lesscommonly two
species of Ochthebius (O. rectus Lee.,and
n. sp.}. In the surface of theslimypoolsiscommon
asaltfly, evidentlyanEphydra,
ofbronze color, itspupa
to be found in the rust-coloredmud and
algae under the water.A
few insig nificant looking Staphylinidae(Homalota
and Trogophloeus} are tobe found in thesalt-grassaround
the edgesofflowingsprings; thereisalso Actobius pcederoidesLee. a smallDyschirius(7). in teger}and some
semiaquaticHemiptera
(Salda) inthepupa
stage.There
is finally a small blackTachys
(Tachys
corax) runningcommonly
abouton
the saltmud.
Around some
of thesespringyplaces are largeclumps
of a verytallcanegrass,
which
formmounds
severalfeetin height.These
are toodenseand
matted to enter usually, but sometimes,where
themounds
are abruptand
not too wet, there isa hard crust of salinesoil, underwhich
is a moist and even pastymass
of rotten grassinwhich two
species of antshaveformed
extensivecolonies.One
of these is a small red species (Cremastogaster
sp.), the other a very large pellucid, honey-yellowform (Camponotus
fragilis},and
alwaysin, under, or aboutthese colonies arefound specimens,inconsiderablenumbers,oftwo
species of theCa
rabid genus Thalpius(Th. dorsails,Lee., hornii Chd.). Idonotsup pose thatthesebeetles are somuch myrmecophilous
as they are attracted by thehoney dew
of aHomopteron which
occurs inlarge colonies
among
the ants.The
mature insect of thisHo
mopteron
isgrey,withthinbroad wings,and
theyoung
withwide
flaringcaudal tufts of
wax.
I have very
few
other insectsfrom
Salton, but Isaw many
frag ments ofasummer
fauna preserved in the salt crust,and among them
there is Cicindela hcemorrhagica,which
certainly belongsto the saline fauna.
The
salinefauna of Salton seems tobeverypoor; in fact,thereistoo