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376 ENTOMOLOGICAL SOCIETY

burst

upon

us in thevalley,

and

rainwithblastsof

wind

obscured the scenery.

I

went

to sleep for awhile,

and when

I

awoke,

behold theearth

had grown

green with grass.

A

refreshing coolness succeeded the hot breath of the desert.

The

mountains

came

closer

and

the valley rose

between

them,

and

cultivated fieldsofalfalfa

began

to appear. Finally, grovesof red-limbed fruittrees, with shining threadsofirrigation waters, linedour way,

and

at sunsetthe

cows came

trooping

home

tothefarm yards

wading

knee deepinclover.

This

was

the end of the desert

and

the

summit

of the divide at

Beaumont. Thence we

whirled

downwards

in the darkness, passing

towns

innumerable, with junctionstoPasadena, Redlands,

Pomona, and many

others, well

remembered

names.

At

last

we saw

the twinklinglights of a great city,

and

the various stations of

Los 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 by

me

in the desert

washes

at

Palm

Springs,thattheCalifornia desert

was

once an

arm

of the Californiagulf,

you

are surely mistaken.

The

shells foundinallthisregion areallfresh-waterremains;

and

themarine shells are found only to the south of the divide

which bounds

theSalton Sea.

The

desert sands bordering thisdepression are white withsmall shells, but they areall of the usual fresh-water forms. I havepreserved a

few

of the smaller

and most abundant

forms. I believe even from

my

short visit to Salton that I

havegot the essentialcharacter of the fauna. It contains abso lutely no marine forms and

none

at all'modified

by

the peculiar environment, except, perhaps, the brine fly

(Ephydra), which

is quitedifferent from the species inhabiting the GreatSalt

Lake

of Utah.

There

is no Brine

Shrimp (Artemla)

in anyof the saline springs,

and

it isveryevidentthatthe origin of the salinedeposit

isquite recent

and

even

now

in process of formation

from

the

numerous

saline springs

which

surround the basin both

on

the north

and

south.

At

the surface these springs contain only

from

i to6 per cent, of solid saline matter, but at a depth of

one

or

two

feetthe brine has a density or 27 per cent.,consisting ofboth chloride of

sodium and

sulphate of soda (Glauber's salt).

At

no very remote period thisbasin

was

filledwith fresh water, but neither thisnor any other part of theColoradodesertnorth of the

San

Jacinto range

was

ever marine.

(2)

OF WASHINGTON. 377 The

SaltonSeaor

Lake

isoneof the greatest natural

wonders

of theworld. Itisashallowdeposit,onlyoneor

two

feet indepth, of solid saline matter

and

is 8 miles

wide and

20 miles long, surrounded

by

saline springs

which

build

up mounds and

cones ofsaline matter and mattedroots of cane grass, back of

which

is

the 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 I

know.

This plant is Allenrolfeaoccidentalis,

and

I mail

you

herewith a few sticks

which

containlarvaeofaPtinid beetle1

and

alsoa Clerid

enemy and

perhaps

some

other things. It yieldsat last to thesolid induratedcrustof salt

and

soda

which becomes

finallyan

unbroken

plain ofpuresalt,the lowestdepression being 280 feet

below

sea level at four miles from the edge of thesalt plain.

Here

thesoda sinks

below and

formsa.layerabouta foot thickand solid as a rock.

Above

this isa layer ofblack

mud and

then a surface layerofpuresaltfrom afoot to 18 inches in thick ness.

The

surface ofthesalt isdry and hard, resembling ice

and

glistening in the tropical sun with the million scintillations of a polarice floe; white, harder and smoother than a sheetof

snow.

I reached Salton late

on

Saturday

(March

28).

Sunday was

a fine

day and

I devoted the

morning

to an examination of thesalt springs

and

the fauna of the basin.

The

line of debris from the great overflowof the waters of the Colorado River in 1891

was

plainlyvisible

upon

the surface of the salt nearthe shores.

But

every stick

and

floatedrailroad tie

was

solidly fastened

down and

onlyafew spiders lurked under the fragment, evidently living

upon

insects

blown

out

upon

the saltplain.

Far back

from the

margin

of the lake the earthisstiffened with saline matter,

and

thefeetbreak throughas in

walking

over cul

tivated fields

on

frosty

mornings

in spring.

Here

there is no vegetation except the Allenrolfea

bush growing upon

small

mounds, and

the grass about the salt springs, but even this last is

encumbered and

encrusted with

snowy

incrustations.

There

islittlechance for insect lifebecause of these thick incrustations,

which

bind

down and

solidify every particle of soil

and wood,

but on the

mounds and

aboutthe rootsof the Allenrolfeabeneath the thin crust isa dry

and

dustysoil, largelyconsisting of pulver ized salinematter, and here are a few

Hemiptera

andspiders;

and

in the larger stems of the Allenrolfea I found the larvae

men

tionedbefore.

Where

the springsbreakforth inlarger

volume and

form smallflowingstreamlets there are patches of grass encrusted with mineral matter,

and

even the

mud

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.

(3)

378 ENTOMOLOGICAL SOCIETY

bordered with ice-like crystals

and

crusts.

Where

these enter the water,

when

turned over they are lined with greenalgae

and upon

thesethere is in vast

numbers

asmall Hydrophilid (Creniphilus n. sp.) with pale elytral tip,

and

in almost equal

number,

in the

mud

beneath, a palePhilhydrus (Ph.diffusus Lee.) of largesize,

and

less

commonly two

species of Ochthebius (O. rectus Lee.,

and

n. sp.}. In the surface of theslimypoolsis

common

asaltfly, evidentlyan

Ephydra,

ofbronze color, its

pupa

to be found in the rust-colored

mud and

algae under the water.

A

few insig nificant looking Staphylinidae

(Homalota

and Trogophloeus} are tobe found in thesalt-grass

around

the edgesofflowingsprings; thereisalso Actobius pcederoidesLee. a smallDyschirius(7). in teger}

and some

semiaquatic

Hemiptera

(Salda) inthe

pupa

stage.

There

is finally a small black

Tachys

(

Tachys

corax) running

commonly

about

on

the salt

mud.

Around some

of thesespringyplaces are large

clumps

of a very

tallcanegrass,

which

form

mounds

severalfeetin height.

These

are toodense

and

matted to enter usually, but sometimes,

where

the

mounds

are abrupt

and

not too wet, there isa hard crust of salinesoil, under

which

is a moist and even pasty

mass

of rotten grassin

which two

species of antshave

formed

extensivecolonies.

One

of these is a small red species (

Cremastogaster

sp.), the other a very large pellucid, honey-yellow

form (Camponotus

fragilis},

and

alwaysin, under, or aboutthese colonies arefound specimens,inconsiderablenumbers,of

two

species of the

Ca

rabid genus Thalpius(Th. dorsails,Lee., hornii Chd.). Idonotsup pose thatthesebeetles are so

much myrmecophilous

as they are attracted by the

honey dew

of a

Homopteron which

occurs in

large colonies

among

the ants.

The

mature insect of this

Ho

mopteron

isgrey,withthinbroad wings,

and

the

young

with

wide

flaringcaudal tufts of

wax.

I have very

few

other insects

from

Salton, but I

saw many

frag ments ofa

summer

fauna preserved in the salt crust,

and among them

there is Cicindela hcemorrhagica,

which

certainly belongs

to the saline fauna.

The

salinefauna of Salton seems tobeverypoor; in fact,there

istoo

much

salt here,

and

I did not find any of the Great Salt

Lake

species. Moreover, the investigation of this fauna is very difficultbecause everything is

cemented

solidly by salt

and

soda sulphate.

Some

discussion ensued

on

the question as to

whether

the Colorado desert

had

been occupied at

any modern

period

by

an

arm

of the sea, Messrs.

Vaughan, Schwarz, and

Gill takingpart.

As

the time for

adjournment

had not quite been reached at

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