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April 23, 1998
Chapter 3 - Other Topics
INTRODUCTION
This chapter discusses five topics not presented in the previous chapter, which was
organized around major revision topics. Topics discussed in this chapter include: fire and
fuel treatment, fossil resources, heritage resources, landownership adjustment, and timber
suitability. Although not revision topics, the topics found in this chapter are important.
Direction addressing each will be developed and presented in the three revised management
plans.
FIRE AND FUEL TREATMENT
Introduction
This section describes the historic and current roles of fire on the Northern Great
Plains. The need to restore some of the historic fire regime to the Northern Great Plains
planning are while balancing the need to safeguard life and property are addressed.
Management guidelines will be presented for fire and fuel treatment in the three revised
forest plans.
Existing Direction and Historic Condition
The Northern Great Plains region includes North Dakota, South Dakota, Nebraska, plus
the eastern portions of Montana and Wyoming, and extends northward into Manitoba,
Saskatchewan and Alberta. The climate of the region is characterized by an increase in
precipitation and humidity and a decrease in periodic droughts during the summer from west
to east. The climate range influences not only the potential native vegetation, but also
the fire regime and its effects. The short grass prairie on the western and southern
portions of the region is the most arid type, followed by the mixed-grass prairie in the
mid-section of the region with its more moderate precipitation. The tall grass prairie on
the eastern edge receives the most precipitation. The variation in precipitation across
the region greatly influences the growth and expansion of woody plants. In the most
western portions of the region, big sagebrush occupies uplands; in the absence of fire,
big sagebrush persists or expands. Woody draws are examples of communities in more arid
portions that are restricted to sites with greater soil moisture. In contrast to more arid
portions of the region, mesic prairies in the northern, eastern and southeastern portions
of the region are characterized by precipitation amounts high enough to support the
expansion of woody plants onto uplands. In addition to climatic factors, herbivores also
influence the region's vegetation and fire regimes.
Data from adjoining ponderosa pine forests indicates that fire frequency historically
varied from 2 to 25 years. On topography more dissected with breaks and rivers, data
supports an estimated historic fire frequency of 20 to 30 years. In the more mesic
portions of the Northern Great Plains, the average historic fire return interval was
shorter. It is estimated that in the tall grass prairie an historic fire frequency of every
1 to 5 years occurred.
A fire strategy most likely to manage diversity on native rangeland of the Northern
Great Plains is based on two premises: 1) processes that mimic, as much as possible, the
variability found in the native ecosystems should be present and functioning, and 2)
management activities should conserve or restore historical disturbance patterns.
Custer National Forest Units
Direction for national grassland units of the Custer National Forest places emphasis
on:
· prevention, detection, suppression,
· interagency coordination, and
· interstate coordination.
Fuels management direction consists of:
· a combination of treatments that most efficiently meet the fuels management
direction for each management area, including the use of prescribed fire as both a planned
and unplanned ignition tool, and
· treatment levels that, after analysis of hazards, adjust management to meet desired
results.
Fire suppression activities on the Custer National Forest national grassland units are
managed by the local grazing associations, which use Conservation Practice Funds (CPR) to
contract with the local volunteer fire departments for initial attack of wildfires. If the
size of the fire is beyond the scope of control for the volunteer fire department, then
the Forest Service is contacted for suppression action.
Medicine Bow-Routt National Forest Unit (TBNG)
On the Thunder Basin National Grassland, current direction emphasizes; 1) the
protection of life, property, and resource values from wildfire in a cost-efficient manner
that maximizes the benefits of shared resources and developing technologies, and 2) using
prescribed fire as a vegetative and fuels management technique where it is the most
cost-efficient and acceptable alternative to achieve management objectives.
The Thunder Basin National Grassland has agreements with local volunteer fire
departments, which take initial attack action and are then reimbursed for their services.
The volunteer fire departments take charge of the fire until the Forest Service shows up,
if necessary. If the fire is beyond the scope of control of the volunteer fire department,
the Forest Service is contacted for support.
Nebraska National Forest Units
On the Nebraska National Forest units, direction emphasis is placed on:
· providing a level of protection from wildfire that is cost efficient and meets
management objectives for the area. To accomplish this, the following variables are
considered:
· the values of the resources that are threatened,
· the probability of fire occurrence,
· the fuel beds in which fires are likely to occur,
· the weather conditions that will probably influence fires that occur,
· the costs of fire protection programs,
· the social, economic, political, cultural, environmental, life and property
concerns,
· and the management objectives for the area.
· taking suppression action on all escaped fires, after considering the following:
· the values of the resource threatened,
· the management objectives for the threatened area,
· the fuel beds in which the fires burn,
· the current and projected weather conditions,
· the natural barriers and fuel breaks,
· the social, economic, political, cultural, and environmental concerns,
· the public's safety,
· the firefighters' safety,
· and the costs of alternative suppression strategies, and
· maintaining fuel conditions that permit fire suppression forces to meet fire
protection objectives for the area.
In South Dakota, the Buffalo Gap and Fort Pierre National Grasslands have agreements
with local volunteer fire departments for initial-attack fire suppression. This is
coordinated with the State of South Dakota in accordance with the state-wide agreement. In
the Nebraska, the Bessey unit is a member of the Sandhills Mutual Aid and coordinates fire
suppression activities with the local volunteer fire departments. Due to the Samuel R.
McKelvie National Forest's isolation, the Forest Service responds to initial attack, but
then relies on volunteer fire departments for additional response until other Forest
Service units can respond. The Pine Ridge Ranger District has a mutual aid agreement with
the volunteer fire departments of Chadron and Crawford, Nebraska, and takes initial-attack
suppression action on both the Pine Ridge area and the Oglala National Grassland.
Each level in the Forest Service organization is trained and equipped to deal with
fires of certain size, number or severity. Fire strategy calls for maintaining a national
organization capable of coming to the assistance of any one or more Forest Service Regions
as needs develop. The control center for management of the national and international fire
organization is in Boise, Idaho.
A Listing of Fire Occurrences by National Forest
Custer National Forest Units
Little Missouri, Cedar River Grand River 7 fires per year 1,130 acres per year
Sheyenne National Grassland* 2 fires per year 21 acres per year
Sheyenne National Grassland personnel have conducted prescribed burns on approximately
2,000 acres per year for the past five years.
Medicine Bow-Routt National Forest Unit
Thunder Basin National Grassland 9 fires per year 3,500 acres per year
Personnel on the Thunder Basin National Grassland conduct prescribed burning on
approximately 100 acres per year.
Nebraska National Forest Units 21 fires per year 8,471 acres per year
Between 1981 and 1985, personnel on the Pine Ridge Ranger District conducted 400 acres
of prescribed burning. Two-hundred seventy acres were in the Soldier Creek management
unit. Between 1988 and 1990, prescribed burns were conducted on approximately 900 acres in
the Bordeaux Creek area.
Opportunities To Improve Existing Direction
Reinstituting a fire regime based on historical processes, including burning at varying
intervals to reflect climatic patterns and in differing seasons, is the first step in
developing a strategy for using fire to manage for biological diversity on native
rangelands in this region. Focusing on mid-summer burns, rather than concentrating all
prescribed burning in the spring and fall, would better mimic natural, historic
disturbance patterns. The second step involves adjusting fire regimes to best sustain
special habitats, such as wetlands and riparian zones, and sensitive species, especially
threatened and endangered ones. The third step requires that fire prescriptions be planned
so that burning does not enhance the spread of invasive species. By understanding historic
fire processes and ecosystem interactions, Forest Service managers can better realize the
many opportunities for improving current conditions on the units under review.
A "fire protection assessment" is needed. This assessment is an analysis
using fuel flammability, potential value change from fire, and the potential an ignition
will occur. The analysis is followed by an examination of historic fire regime patterns
and current fire patterns. Current fire regime intervals are not the same as historic
intervals.
FOSSIL RESOURCES
Introduction
The need to develop management guidelines that address fossil resources has become
apparent, particularly as interest in and the collecting of fossils for scientific,
recreational and commercial purposes has increased. The current management plans provide
little guidance. More guidance will be provided in the three revised management plans.
Existing Direction and Conditions
In the early 1990s, it became apparent that interest in scientific, commercial and
recreational fossil collecting was growing, and management and protection of fossils
within the planning area was needed. The planning area is rich with fossil resources. The
existing management plans contain little or no direction for fossil management. There are
varying public views as to the type of collection that should be allowed and who ought to
be able to collect. There are also varying views as to how the fossil program should be
managed if fossil collection is allowed. Several fossil-bearing formations occur that
outcrop within the planning area. Some of the formations and types of fossils found within
them are listed in the following table (Information from Northern Great Plains Ecosystem
Assessment Broad scale Paleontology):
Table FOS-1: Fossils by Formation
FORMATION
|
FOSSIL TYPES
|
Recommended Class*
|
Skull Creek Shale |
Invertebrates and microfossils. |
3 |
Newcastle Sandstone |
Few marine vertebrates. |
3 |
Mowry Shale |
Fish scales, teeth, bones and
occasional marine vertebrates. |
3 |
Belle Fourche Shale |
Invertebrates, microfossils and
vertebrates - fish and plesiosaurs. |
3 |
Greenhorn Formation |
Invertebrates, microfossils and
vertebrates - fish. |
3 |
Carlile Shale |
Invertebrates such as Inoceramus,
ammonites, and gastropods. Vertebrates such as fish and marine reptiles. |
3 |
Niobrara
Formation |
Invertebrates and microfossils. Marine
vertebrates such as fish, birds, pterosaurs, amphibians, and reptiles-mosasaurs and
plesiosaurs. |
5 |
Pierre Shale |
Invertebrates of ammonites, snails, clams and
crabs. Marine vertebrates such as mosasaurs, plesiosaurs, fish, turtles, pterosaurs and
flightless birds. |
3 |
Fox Hills
Sandstone |
Invertebrates such as ammonites, plant fossils
and relatively rare vertebrates. |
3 |
Hell
Creek/Lance Formation |
Well known for dinosaur faunas-Triceratops,
Anatosaurus, Tyrannosaurus rex, Pachycephalosaurus, Stygimoloch, Ankylosaurus, and
Ornithomimus. Also fish, turtles, champsosaurs, and crocodiles. |
5 |
Fort Union
Formation |
Many excellent fossil plants, invertebrates,
and vertebrates are found in this group. |
3, 5 |
Ludlow
Formation |
Vertebrate fossils may be locally abundant. |
3, 5 |
Cannonball
Formation |
Only Tertiary unit in which sharks, rays and
other marine vertebrates and invertebrate fossils are preserved in situ. |
5 |
Slope
Formation |
Vertebrate fossils may be locally abundant. |
3, 5 |
Bullion Creek
Formation |
Significant leaf and pollen
floras, many invertebrates, and a wide variety of vertebrates such as fish, salamanders,
frogs, turtles, crocodiles, champsosaurs, lizards and dozens of mammals. |
3, 5 |
Sentinel Butte
Formation |
Plants, invertebrates, and
vertebrates including amphibians, reptiles - crocodiles, champsosaurs and turtles, and
mammals. |
3 |
Golden Valley
Formation |
Vertebrates and plant fossils in
some areas. |
3, 5 |
Slim Butte
Formation |
Fauna from this formation is the
only Duchesnean age mammalian fauna from the Northern Great Plains area. |
5 |
White River
Group |
Vertebrates range from fish,
frogs, lizards and turtles, tiny rodents, rabbits, and insectivores, to saber-tooth cats,
dogs, horses, camels, oreodonts, rhinoceroses, birds, and titanotheres. Invertebrates
primarily snails. |
5 |
Chadron
Formation |
Vertebrates range from fish,
frogs, lizards and turtles, tiny rodents rabbits, and insectivores, to saber-tooth cats,
dogs, horses, camels, oreodonts, rhinoceroses, birds, and titanotheres. Invertebrates
primarily snails. |
5 |
Brule
Formation |
Vertebrates range from fish,
frogs, lizards and turtles, tiny rodents rabbits, and insectivores, to saber-tooth cats,
dogs, horses, camels, oreodonts, birds, and rhinoceroses . Invertebrates primarily snails.
|
5 |
Sharps
Formation |
Many kinds of vertebrates
including diminutive saber-tooth cat, hedgehogs, true moles, and mountain beavers. |
5 |
Arikaree Group |
|
|
Gering
Formation |
Fauna includes rodents, dogs, and
other carnivores, oreodonts, a hedgehog, and a mole. |
5 |
Monroe Creek
Formation |
Vertebrate fossils only locally
abundant, including fish, frogs, lizards, snakes, birds, a marsupial, hedgehogs, shrews,
moles, rabbits, rodents, carnivores, horses, camels, and oreodonts. |
5 |
Harrison
Formation |
Much of same as Monroe, plus large
and small carnivores, chalicotheres, other articodactyls join a group of horses, rhinos,
giant pigs, and camels. Invertebrates such as snails, and some aquatic plants. |
5 |
Oglala
Group |
Fossils include true cats, otters,
abundant horses, camels, oreodonts, Moropus, pikas, musteline and procyonine mustelids,
extinct horned artiodactyl groups, rhinos, rodents dogs, pronghorns, saber-tooth cats,
sloths, bears, tapirs, and mastodonts, birds, fish amphibians, and reptiles are also
represented. |
5 |
*A draft classification system has been developed wherein geological
units, usually at the formation or member level are classified according to the
probability of yielding paleontological resources that are of concern to land managers.
The classification is based largely on how likely a geologic unit is to produce vertebrate
fossils of terrestrial (i.e. non-marine) origin. The five classes in the system are
described below. (Probable Fossil Yield Classification, 1-4)
Class 1 - Igneous and metamorphic geologic units that are not likely to
contain recognizable fossil remains.
Class 2 - Sedimentary geologic units that are not likely to contain
vertebrate fossils nor scientifically significant non-vertebrate fossils.
Class 3 - Fossilferous sedimentary geologic units whose fossil content
varies in significance, abundance, and predictable occurrence. Also sedimentary units of
unknown fossil potential.
Class 4 - Class 4 geologic units are Class 5 units (see below) that have
lowered risks of human-caused adverse impacts and/or lowered risk of natural degradation.
Class 5 - Highly fossilferous geologic units that regularly and
predictably produce vertebrate fossils and/or scientifically significant non-vertebrate
fossils, and that are at risk of natural degradation and/or human-caused adverse impacts.
Custer National Forest
Moderately to highly dissected badlands terrain occurs in the Little Missouri National
Grassland study area of western North Dakota. Paleocene-age Fort Union Group formations
are the primary rock units exposed in the sparsely vegetated buttes and along waterways.
The Cretaceous-age Hell Creek Formation crops out beneath the Paleocene units in the
southern part of the Little Missouri National Grassland.
Field surveys of the Little Missouri National Grassland found fossils at 104 sites. The
following is a listing of the number of fossil sites containing specific kinds of fossils
(Hoganson 4-6):
Number of fossil sites discovered in each county :
Billings County .......................................70 sites
McKenzie County...................................17 sites
Golden Valley County.............................6 sites
Slope County...........................................11 sites
Number of fossil sites per rock formation
Quaternary alluvium.................................1 site
Sentinel Butte Formation....................92 sites
Bullion Creek Formation.....................11 sites
Number of fossil sites containing fossil
Petrified wood.......................................... 2 sites
Petrified tree stumps..............................11 sites
Leaf impressions and seeds...................11 sites
Invertebrates...........................................45 sites
Vertebrates..............................................62 sites
Mammals (Quaternary)............1 site
Mammals (Paleocene).............. 1 site
In addition to the Little Missouri National Grassland, a very precursory survey was
conducted on the Grand River National Grassland. The Hell Creek Formation is the formation
mostly exposed. Types of fossils located have included dinosaurs, plant material--such as
pine cones and stumps--as well as crocodiles, turtles and champsosaurs. Approximately 30
to 40 sites were documented during the inventory.
Medicine Bow-Routt National Forest Unit
The investigation of paleontology on the Thunder Basin National Grassland is relatively
recent; however, the Lance Formation, which occurs on the unit, has been heavily
investigated on nearby lands since at least 1888. The Cretaceous Lance Formation includes
a wide range of fossils from virtually all vertebrate classes, including early
insectivorous mammals (Ritchie 3). Thus, the deposits include not only the massive fossils
of large dinosaurs (like ankylosaurs and hadrosaurs), but also important deposits of
microvertebrate fossils. A survey completed in 1997 within the Lance Formation found 116
fossil localities (Martin and Finlayson 7). Another survey completed in 1996 located 15
fossil sites. This survey identified sites in the following formations: Mowry Shale,
Greenhorn, Carlile, Lance, Niobrara, Newcastle, and Pierre Shale (Finlayson and Cicimurri
2-3).
Nebraska National Forest Units
According to Beasley:
The paleontological resource within the Nebraska National Forest administrative units
spans a wide realm of depositional environments ranging from deep marine deposits to
terrestrial volcanic deposits containing paleosols. However, within the units administered
by the Nebraska National Forest the geologic and paleontologic records span a relatively
short time with the oldest exposed unit, the Late Cretaceous Mowry Formation, located on
the Fall River District of the Buffalo Gap National Grassland to the youngest unit,
Pleistocene deposits which have produced the well-known Hudson-Meng Bison Bonebed, located
on the Oglala National Grassland (4).
The most highly fossiliferous rocks exposed within the Oglala National Grassland are
the clay stone, siltstone, and sandstone of the White River Group. Field inventories have
identified 162 sensitive paleontological sites. These sites are primarily vertebrate
localities within the Late Eocene, Oligocene, and Miocene Epoch of the Tertiary System
(approximately 45-20 million years ago) (13). Within the Oglala National Grassland, the
Toadstool Park Badlands contain very significant fossil resources. These resources include
vertebrate track ways representing at least 11 contemporary vertebrate species, as well as
fossils of the White River Group (15-26).
The majority of Arikaree rocks exposed on the Pine Ridge Ranger District of the
Nebraska National Forest belong to the Gering, Monroe Creek, and Harrison Formations. A
fossil inventory identified 15 fossil sites producing partial skeletons of oreodonts, a
horse, entelodont, bird and several unidentified specimens (29-30).
The dominate geologic feature in central Nebraska, which includes the Bessey Ranger
District of the Nebraska and the Samuel R. McKelvie National Forests, is the Nebraska
Sandhills. Underlying the Sandhills, a large paleo-valley was eroded into the Miocene
Oglala Formation, and subsequently filled by younger deposits, ending with the sand
dunes of the Sandhills. Although these formations are known to contain fossils, an
inventory conducted on the units did not locate any fossil sites (30, 35).
The fossil faunas located within the geologic units of the Buffalo Gap and Fort Pierre
National Grasslands are very diverse, because these units contain marine vertebrates and
invertebrates that once lived in the Interior Sea. Most of the rocks exposed within the
Buffalo Gap and Fort Pierre National Grasslands are the remnants of ancient marine
animals, such as plesiosaurs, mosasaurs, toothed diving birds, large sea turtles, sharks,
sting rays, a wide variety of fish, and a myriad of invertebrates such as clams, oysters,
ammonites, coral, and barnacles. Each marine formation, preserves the fossils differently
and, therefore, the state of preservation varies from one formation to the other, as well
as within the formation. Inventories concentrating on the Late Cretaceous marine
sediments, primarily exposed on the western portion of the Buffalo Gap National Grassland,
located 63 paleontological localities that are primarily Late Cretaceous marine
vertebrates. Another inventory concentrating on the Tertiary units on the Buffalo Gap and
Fort Pierre National Grasslands located 67 fossil localities, with 25 on the Fall River
District, 37 on the Wall Ranger District and 5 on the Fort Pierre National Grassland (12).
Opportunities to Improve Existing Direction
There is little to no direction within current land and resource management plans to
provide for the management of fossil resources. Decisions to be made are listed below:
· How fossil inventories should be conducted (timing and type);
· How fossils should be protected;
· What types of collection techniques are allowable and how collection is to be
permitted;
· What types of research opportunities are to be provided;
· What curatorial arrangements are to be required;
· What strategies for fossil interpretation are needed.
HERITAGE RESOURCES
Introduction
Forest System lands on the Northern Great Plains contain a great wealth of heritage
resources in light of the legacy left this generation through American Indian presence,
the settlement history of Euro-Americans--including cattle ranchers and homesteaders--the
Dust Bowl era, and subsequent changes in land use and occupation. Management direction
will be provided for heritage resources in the three revised management plans.
Laws and Executive Orders Providing Direction
Several laws apply to the management of heritage resources on federal lands. These laws
include:
· the Antiquities Act of 1906,
· the Historic Sites Act of 1935,
· the National Historic Preservation Act of 1966,
· the National Environmental Policy Act of 1969,
· the American Religious Freedom Act of 1978,
· the Archeological Resources Protection Act of 1979, and
· the Native American Grave Protection and Repatriation Act of 1990.
Existing Direction and Conditions
Evidence for human occupation and use of the Northern Great Plains planning area is
culturally diverse and spans over 12 millennia. Although archaeological site densities are
as high on the Northern Plains as they are in most other landscapes in North America, our
understanding of the human history of the region is still in its earliest stages. Early
researchers were attracted to the study of past cultures that built impressive villages
and monumental earthworks. Such preferences meant that the Northern Plains, where even the
most ephemeral of architectural features are rare, were passed up for the prodigious
structures of the Southwest or the artifact-laden ceremonial mounds of the Mississippi and
Ohio River Valleys. It was not until the 1930s that archaeologists began paying serious
attention to the Northern Plains, and research did not commence within the assessment area
before 1961. Since then, most archaeological sites have been recorded in response to
federal mandates for historic preservation.
Approximately 20 percent of National Forest System (NFS) lands within the Northern
Great Plains planning area has been inventoried for cultural resources. Most evaluations
have been performed since 1977 and, as a result, 3,437 sites have been recorded. Because
most cultural resource inventories on federal lands are conducted to evaluate the impacts
of proposed actions, a bias is created that skews our understanding of the past, and a
comparison of the planning areas within this assessment helps demonstrate this problem.
Oil, gas and mining exploration and extraction require archaeological inventories of large
areas of land. Within the assessment area, the Thunder Basin planning area has received
the most interest by energy companies for exploration, and the Nebraska planning area the
least. As a result, 40 percent of National Forest System lands within Thunder Basin
National Grassland has been evaluated. This compares to 15 percent for the Custer and only
3 percent for the Nebraska planning areas.
A Brief Overview of Each Planning Area
Custer National Forest Units
Within the Cedar River, Grand River, Little Missouri, and Sheyenne National Grasslands,
approximately 15 percent of the land has been evaluated for cultural resources. As a
result, 1,517 sites have been recorded, which represent a site density of four sites per
square mile. As with the Thunder Basin National Grassland, the sites on the Custer
National Forest planning area represent almost the full range of human history on the
plains.
National Register eligibility status for the sites within the Custer National Forest
planning area includes 210 sites that are considered eligible, 175 sites that are not
eligible, and 841 sites that have not been evaluated for eligibility. The most common site
type is prehistoric scatters of stone tools and tool manufacturing debris. There are no
sites listed on the National Register.
Medicine Bow-Routt National Forest Unit (TBNG)
Approximately 40 percent (215,000 acres) of the Thunder Basin National Grassland (TBNG)
has undergone some degree of archeological surface examination since the mid 1970s.
Practically all of the inventory was the result of activities related to oil and gas
exploration and coal mining activities. Just more than 1,200 sites have been located and
recorded on the grassland. The variety of individual resources (sites) range from
aboriginal encampments, to historic trails and wagon roads, to more recent homesteads and
pastoral camps. Although the average site size is under one-half acre, some linear
features, such as the Bozeman and Texas Trails, extend for many miles across the TBNG.
Approximately 160 of the historic and prehistoric sites recorded on the national
grassland have been determined eligible to the National Register of Historic Places, but
none are currently listed on the National Register. Site densities are high, with an
average of four sites per square mile. The most common sites encountered consist of small,
temporary, prehistoric hunting camps and historic pastoral camps.
Nebraska National Forest Units
The surveyed lands administered by the Nebraska National Forest contain 740 recorded
cultural sites, which represent a density of four sites per square mile. Of these sites,
54 are considered eligible for listing on the National Register, 620 are not considered
eligible, and 45 have not been evaluated. As with the other two planning areas, most of
the sites within the Nebraska administered units are prehistoric scatters of stone
artifacts.
The Bessey administrative complex and the Hudson-Meng Bison Bonebed have been listed on
the National Register of Historic Places. Both of these sites have strong public
interpretation components to their management. In addition, the Warbonnet Battlefield and
the Fiddle Creek Cultural Complex will likely be proposed for listing on the National
Register in the future.
Opportunities to Improve Existing Direction
During planning, the Forest Service is required, as found in 36 CFR 219.24, to:
· Provide an overview of known data relevant to history, ethnography and prehistory of
the area under consideration;
· Identify areas needing more intensive inventory;
· Provide for evaluation and identification of appropriate sites for the National
Register of Historic Places;
· Provide for establishing measures for the protection of significant cultural
resources from vandalism and other human depredation and natural destruction;
· Identify need for maintenance of historic sites on, or eligible for inclusion in,
the National Register of Historic Places; and
· Identify opportunities for interpretation of cultural resources for the education
and enjoyment of the American public.
LANDOWNERSHIP ADJUSTMENT
Introduction
This section discusses landownership patterns and the opportunities to divest, obtain
or consolidate national grasslands and national forest on the Northern Great Plains.
Management direction concerning this topic will be provided in the three revised forest
plans.
Existing Direction and Conditions
During the planning process, Forest Service policy requires identification of desired
landownership pattern and development of guidelines for landownership adjustments.
Typically, grassland units have a significant amount of intermingled land. This
intermingled pattern makes it difficult for both the Forest Service and private landowners
to meet their management objectives. It also limits public access and use of National
Forest System lands. Lastly, the cost of managing the scattered and intermingled lands is
higher than managing the same amount of consolidated lands. Existing management plans do
not provide guidance concerning where the Forest Service should adjust the landownership
on a large-scale conceptual basis.
There have been 20 land exchanges on Custer National Forest grasslands from 1987
through 1995, totaling 7,365 acres. This represents about an 85-percent accomplishment of
the five-year plan. Two Small Tract Act sales resolved two permanent structure
encroachments. Encroachments are found at an average rate of two per mile of Forest
boundary. Sixty-seven grassland rights-of-way/easements have been acquired with 26 of
these being road or trail rights-of-way. The rights-of-way acquisition program has
averaged 90 percent or more of the five-year plan (Fiscal Year 1995 Monitoring Report 27).
On the Thunder Basin National Grassland, land exchanges and rights-of-way acquisitions
have far exceeded management plan objectives (Monitoring and Evaluation Report 9).
From 1993 to 1997, approximately 60,700 acres of national grassland were exchanged for
39,350 acres of private land. Through the exchanges, the need for 142 rights-of-way were
eliminated, 61 isolated parcels were traded, 869 boundary corners that would have needed
to be located and marked were eliminated, and 371 miles of land line will no longer need
to be surveyed and fenced (Prochazka 1).
The Nebraska National Forest Management Plan directed that an active land
adjustment program be developed. Between 1985 and 1995, about 70,000 acres of National
Forest System lands have been exchanged for about 68,000 acres of private land. The
exchanges block up the federal land for more efficient management, providing better public
access, and enhance private ranch management. Through the exchange program, 29
rights-of-way were acquired, 41 isolated parcels were traded, 1,806 boundary corners that
would have needed to be located and marked were eliminated, and 737.75 miles of land line
will no longer need to be surveyed and fenced (1995 Monitoring and Evaluation Report
8).
Access to at least two national grasslands, the Little Missouri and Thunder Basin, is
hampered by the lack of legal rights-of-way. In many cases, rights-of-way are used by the
public, but no formal easement has been obtained in the name of the United States (Monitoring
and Evaluation Report, Custer National Forest 11). The most successful method of
acquiring needed rights-of-way has been through the land exchange process. The three
national forests have had varying degrees of success in acquiring rights-of-way outside of
land exchanges.
Opportunities to Improve Existing Condition
Decisions to be made for lands include:
· What opportunities exist for rights-of-way acquisitions through private land to
access public land?
· How should isolated tracts be administered?
· What is the desired landownership pattern and what guidelines should be developed to
direct landownership adjustment?
· What areas should be designated as utility corridors?
TIMBER RESOURCES
Introduction
Although timber resources derived from the planning area are relatively small, the need
to establish suitable lands for timber harvest is apparent. Management guidance will be
provided for timber suitability and production in the three revised forest plans.
The following table shows tentatively suitable forest lands for the Northern Great
Plains planning units. This table was completed using criteria in FSH 2409.13, Chapter 20
and the
Federal Register, Vol. 47 No. 190, 36 CFR Part 219.3 and 219.14:
Table TR-1: Tentatively Suitable Forest Land
Criteria
|
Cedar
River/Cedar River National Grasslands
|
Little
Missouri National Grassland
|
Sheyenne
National Grassland
|
Pine Ridge
District/Oglala National Grassland
|
Thunder
Basin National Grassland
|
| Total acres |
161530 |
1027521 |
70264 |
144660 |
528000 |
| Total acres forested |
496 |
117810 |
5111 |
0 |
30900 |
| Acres Non-forested |
161034 |
909711 |
65153 |
0 |
497100 |
| Forest land withdrawn from
timber production |
0 |
0 |
0 |
7814 |
0 |
| Acres not capable of producing
crops of industrial wood |
0 |
49500 |
0 |
96970 |
4385 |
| Acres where irreversible damage
is likely to occur due to soils |
0 |
0 |
0 |
0 |
6515 |
| Acres that cannot be restocked
within 5 years |
0 |
0 |
0 |
0 |
5500 |
| Acres where inadequate response
information is available |
496 |
67363 |
0 |
0 |
14500 |
| Tentatively suitable
forest land |
0 |
940 |
5111 |
39868 |
0 |
The Pine Ridge Ranger District evaluated tentatively suitable forestland by utilizing
polygons based on soils capable of producing timber as determined by the Natural Resources
Conservation Service. Based on this, the evaluation shows more lands capable of producing
timber than what is actually forested. This is due to fire events that have occurred on
this unit and the loss of forest cover. It is expected that these areas will become
forested and capable of producing timber and, therefore, should be considered in the
evaluation.
The approximately 26,000 acres of forested type on the Samuel R. McKelvie National
Forest and Bessey unit were not considered tentatively suitable based on irreversibility
due to soils, questions on restocking within five years, and the inadequate response
information available.
|